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This library of images provides pictures of the Apollo samples taken in the Lunar Sample Laboratory,
full-color views of the samples in microscopic thin-sections,
cutting views and diagrams that illustrate how the samples were subdivided for scientific analyses,
and in situ views of the samples on the lunar surface.
The atlas contains information about the type of sample (e.g., rock, soil),
the lithology (e.g., basalt, norite), and a description of the sample.
Links to additional information about each sample are provided for those that have
been previously described in The Lunar Sample Compendium and Lunar Sample Catalogs. Version 1 of the atlas was released in August 2009 and version 2 was released in July 2010. The process of scanning lunar sample images continues and the atlas will grow in the future.
A subset of this collection, the Apollo Thin Sections catalog,
includes all samples for which thin-section views are available.
Another subset, the Virtual Microscope catalog, provides interactive views of selected thin sections as they would be seen through a microscope.
Another rich source of thin-section views by William Phinney (formerly with the NASA Johnson Space Center)
and Howard Wilshire (formerly with the U.S. Geological Survey) is the
Digital Petrographic Slide Collection,
which is hosted by our colleagues at Arizona State University.
|
| Apollo 11 |
| Sample Number |
Sample Type |
Lithology |
Description |
| 10000 |
|
|
|
| 10002 |
|
|
|
| 10003 |
rock |
basalt |
Medium-grained subophitic basalt composed of clinopyroxene, two generations of plagioclase, ilmenite with subordinate cristobalite and mesostasis. |
| 10004 |
|
|
|
| 10005 |
core |
|
|
| 10009 |
rock |
breccia |
Highly devitrified breccia with high glass clast content |
| 10010 |
|
|
|
| 10015 |
|
|
|
| 10017 |
rock |
basalt |
Fine-grained, poikilitic, vesicular basalt composed of clinopyroxene, plagioclase, two generations of ilmenite and subordinate opaques and mesostasis |
| 10018 |
rock |
breccia |
Dark grey fine breccia |
| 10019 |
rock |
breccia |
Partly devitrified breccia with low lithic clast content |
| 10020 |
|
basalt |
|
| 10021 |
rock |
breccia |
Partly devitrified typical breccia with a relatively low amount of glass fragments |
| 10022 |
|
basalt |
|
| 10023 |
rock |
breccia |
Sub-rounded, medium dark gray, fine breccia |
| 10024 |
|
basalt |
|
| 10025 |
|
|
|
| 10026 |
|
|
|
| 10027 |
|
|
|
| 10028 |
|
|
|
| 10029 |
|
basalt |
|
| 10030 |
|
|
|
| 10031 |
|
basalt |
|
| 10032 |
|
basalt |
|
| 10044 |
|
basalt |
|
| 10045 |
|
basalt |
|
| 10046 |
|
breccia |
|
| 10047 |
rock |
basalt |
Medium-grained subophitic basalt composed of clinopyroxene, two generations of plagioclase, ilmenite with subordinate cristobalite pyroxferroite and mesostasis. |
| 10048 |
rock |
breccia |
Rounded to subrounded, medium light grey, fine breccia |
| 10049 |
rock |
basalt |
Fine-grained vesicular intersertal basalt with a pyroxene-ilmenite network hosting smaller plagioclase crystals and abundant mesostasis. |
| 10050 |
|
basalt |
|
| 10056 |
rock |
breccia |
Angular to sub-angular, medium dark grey microbreccia |
| 10057 |
|
basalt |
|
| 10058 |
|
basalt |
|
| 10059 |
rock |
breccia |
Slightly devitrified typical breccia with relatively low lithic clast content |
| 10060 |
|
breccia |
|
| 10061 |
rock |
breccia |
Partly devitrified, medium grey fine breccia with marked matrix differences between zones |
| 10062 |
|
basalt |
|
| 10063 |
rock |
breccia |
Sub-angular, dark grey, partly devitrified typical breccia with relatively high glass clast content |
| 10064 |
rock |
breccia |
Angular, dark to light grey, highly devitrified fine breccia with high glass clast content |
| 10065 |
|
breccia |
|
| 10066 |
rock |
breccia |
Rounded, dark grey, fine breccia |
| 10067 |
rock |
breccia |
Sub-angular, dark grey, partly devitrified microbreccia with low glass content |
| 10068 |
|
breccia |
|
| 10069 |
|
basalt |
|
| 10070 |
rock |
breccia |
Subangular, dark grey, partly devitrified fine breccia with many small lithic clasts and few large clasts |
| 10071 |
|
basalt |
|
| 10072 |
|
basalt |
|
| 10072A |
|
|
|
| 10072D |
|
|
|
| 10073 |
rock |
breccia |
Rounded, medium dark grey, partly devitrified microbreccia with low lithic clast content |
| 10074 |
rock |
breccia |
Angular, medium dark grey, partly devitrified microbreccia with low lithic clast content |
| 10075 |
rock |
breccia |
Subangular, medium grey, partly devitrified fine breccia |
| 10082 |
rock |
breccia |
Rounded to subrounded, dark grey to black, partly devitrified microbreccia with no large lithic clasts |
| 10084 |
soil-general |
|
The contingency sample was taken in front of quad IV of the LM. The documented sample was collected 5 meters north of the LM, the bulk sample was collected in front of quad IV by pouring scoops of loose soil to fill the voids left between rock samples in the bulk sample container. 10084 is the bulk soil sample. Soil is fine grained and hard in this sample area. There are few fragments and it is difficult to scoop deeper than 5 cm below the surface. |
| 10085 |
|
|
|
| 10092 |
|
basalt |
|
| 10093 |
rock |
breccia |
Subangular, medium dark grey, fine breccia |
| 10094 |
rock |
breccia |
Subangular to subrounded, medium dark grey breccia |
| 10119 |
|
|
|
Jump to Apollo:
11
14
15
16
17
|
| Apollo 12 |
| Sample Number |
Sample Type |
Lithology |
Description |
| 12001 |
soil-general |
|
12001 is <1 cm fraction of bulk regolith collected about 30 meters northwest of the LM on the first EVA traverse. Astronaut Conrad saw several beads of pure glass while collecting this sample. Fryxell reports that the fines are weakly coherent; they adhere to rocks and do not slump when the sample holder is tipped 45 degrees. |
| 12002 |
rock |
basalt |
|
| 12003 |
soil >1 cm |
|
12003 is coarse (>1cm) split from 12001, along with friable material from the bottom of the sample box. This was collected about 30 meters northwest of LM on EVA-1. These broken up fines from larger rocks do not make a statistical sample. |
| 12004 |
rock |
basalt |
olivine basalt |
| 12005 |
rock |
basalt |
holocrystalline, olivine basalt |
| 12006 |
rock |
basalt |
Oliving Basalt, holocrystalline |
| 12007 |
rock |
basalt |
holocrystalline |
| 12008 |
rock |
basalt |
cumulate (ilmenite) ? |
| 12009 |
rock |
basalt |
|
| 12010 |
|
|
|
| 12011 |
rock |
basalt |
holocrystalline |
| 12012 |
rock |
basalt |
Olivine Pyroxenite; holocrystalline |
| 12014 |
rock |
basalt |
porphyritic olivine microgabbro |
| 12015 |
|
basalt |
|
| 12016 |
|
basalt |
|
| 12017 |
|
basalt |
|
| 12018 |
rock |
basalt |
(terrestrial analogue) medium grained gabbro |
| 12019 |
|
basalt |
|
| 12020 |
|
basalt |
|
| 12021 |
|
basalt |
|
| 12022 |
|
basalt |
|
| 12023 |
|
soil |
Trench sample 12023 (collected at a depth of 20 cm) was collected from the east rim of the 20 meter Sharp crater. The rim material is softer and lighter in ccolor than the surrounding material. |
| 12024 |
|
|
|
| 12025 |
|
|
|
| 12027 |
core |
|
|
| 12028 |
|
|
|
| 12030 |
|
|
|
| 12031 |
|
basalt |
|
| 12032 |
soil-general |
|
Surface soil 12032, along with several rocks were collected from the north rim of Bench crater. It includes some light gray material from just below the surace. Soil collected with "potato" rock 12053. |
| 12033 |
soil-general |
|
Trench sample 12033 was collected 15 cm below the surface, 15 meters from the northwest rim of Head Crater near 12031. The trench bottom is lighter in color than the surace materials. Astronauts otice more large blocks on the west side of benchcrater than on the east. |
| 12034 |
|
|
|
| 12035 |
|
basalt |
|
| 12036 |
|
basalt |
|
| 12037 |
|
basalt |
Soil sample in same sample bag as 12036, a friable basalt. Both were collected near the site of 12035 on the NW rim of Bench crater. Because it includes much broken material from the friable basalt, it is not statistically a soil sample. |
| 12038 |
rock |
basalt |
holocrystalline; diabase (terrestrial analogue); |
| 12039 |
|
basalt |
|
| 12040 |
|
basalt |
|
| 12041 |
soil-general |
|
Soil sample collected about 50 m east of the rim of Bench crater. Sample consists mostly of ine particles but includes a 6.4 mm glass sphere. |
| 12042 |
|
|
12042 is a surface soil taken on the outer flank of Surveyor crater rim, 50 m NW of Halo crater. The sample area is strewn with cohesive clods or aggregates showing a "wrinkled texture". Perhaps this indicates an area of secondary ejecta. |
| 12043 |
|
basalt |
|
| 12044 |
soil-general |
|
Soil 12044 and rock 12043 were collected from the south rim of Surveyor crater. Astronauts observed a prominent double glass bead on the surface. |
| 12045 |
|
basalt |
|
| 12046 |
|
basalt |
|
| 12047 |
|
basalt |
|
| 12051 |
|
basalt |
|
| 12052 |
|
basalt |
|
| 12053 |
|
basalt |
|
| 12054 |
|
basalt |
|
| 12055 |
|
basalt |
|
| 12056 |
|
basalt |
|
| 12062 |
|
basalt |
|
| 12063 |
rock |
basalt |
diabase (terrestrial analogue); ilmenite microgabbro similar to Apollo 11 (Chao) |
| 12064 |
|
basalt |
|
| 12065 |
rock |
basalt |
diabase (terrestrial analogue); holocrystalline |
| 12070 |
|
|
|
| 12072 |
|
basalt |
|
| 12073 |
|
|
|
| 12075 |
|
basalt |
|
| 12076 |
|
basalt |
|
| 12077 |
|
basalt |
|
Jump to Apollo:
11
12
15
16
17
|
| Apollo 14 |
| Sample Number |
Sample Type |
Lithology |
Description |
| 14006 |
rock |
|
Sample 14006 was collected as part of the contingency sample during the first EVA in the vicinity of the lunar module. It was returned in weigh bag 1039 along with the rest of the contingency sample; |
| 14008 |
rock |
|
Sample 14008 was collected from the LM vicinity during the first EVA as part of the contingency sample. It was returned in weigh bag 1039 along with the rest of the contingency samples (14001-14012); sample is fine graned fragmental rock with avg grain size less than 0.1 mm; texturally and mineralogically homogeneous. |
| 14035 |
|
|
|
| 14041 |
|
|
Samples 14041-14046 are fragments from a fractured clod tht broke apart when it was collected by Astronaut Mitchell, collected from Station A, 150 m NW of LM and 90 m N of North Triplet Crater; samples 14041, 14042, 14043, and 14045 are large enough to be considered rocks; sample 14044 is residue and sample 14046 is composed of chips and fines; placed in documented bag 3N and returned in ALSRC 1006. |
| 14042 |
rock |
|
Samples 14041-14046 are fragments from a fractured clod tht broke apart when it was collected by Astronaut Mitchell, collected from Station A, 150 m NW of LM and 90 m N of North Triplet Crater; samples 14041, 14042, 14043, and 14045 are large enough to be considered rocks; sample 14044 is residue and sample 14046 is composed of chips and fines; placed in documented bag 3N and returned in ALSRC 1006. |
| 14045 |
|
|
Samples 14041-14046 are fragments from a fractured clod tht broke apart when it was collected by Astronaut Mitchell, collected from Station A, 150 m NW of LM and 90 m N of North Triplet Crater; samples 14041, 14042, 14043, and 14045 are large enough to be considered rocks; sample 14044 is residue and sample 14046 is composed of chips and fines; placed in documented bag 3N and returned in ALSRC 1006. |
| 14046 |
|
|
|
| 14047 |
rock |
|
Sample 14047 was collected at Station B, 330 m NE of LM and 65 m NNW of the rim of Weird Crater. It was placed in documented bag 5N and returned in ALSRC 1006. |
| 14048 |
|
|
|
| 14049 |
rock |
|
Sample 14049 was collected during the second EVA from Station Bg; placed in bag 6N by the astronauts who said they collected it from a crater rim. The lunar location and orientation are not documented by lunar surface photographs. It is a fragmental rock and is extremely friable and soft. |
| 14051 |
rock |
|
Sample 14051 was collected at station C' which was located 1.29 km ENE of LM and approximately 95 m SE of the rim of Cone Crater. The sample was collected on a gentle southward slope and was partly buried. The area was characterized by abundant fragments ranging from the limit of resolution up to 1.5 m blocks. The sample was returned in documented bag 7N in ALSRC 1006. |
| 14052 |
|
|
|
| 14053 |
rock |
basalt |
holocrystalline, fine-grained, equigranular mare basalt (Carlson and Walton 1978); basalt (Wilshire and Jackson 1972) and (Quaide and Wrigley 1972); and mare basalt (Simonds et al 1977) |
| 14054 |
|
|
|
| 14055 |
rock |
regolith breccia |
F1 Breccia, friable with light clasts (Wilshire and Jackson 1972); porous unshocked regolith microbreccia (Chao et al. 1972); glass rich regolith with breccia (von Engelhardt et al. 1972); and vitric matrix breccia (VMB) (Simonds et al. 1977) |
| 14056 |
soil-general |
|
Sample 14056 was collected from station E during the second EVA. It was returned in bag 15N along with samples 14055-14062; sample is extremely friable and appears to be coherent soil clod, medium brownish in color. |
| 14057 |
|
soil |
Sample 14057 was collected from Station E during the second EVA. It was returned in bag 15N in ALSRC 1006 along with samples 14055-14062. Sample is very friable and is brownish gray in color. |
| 14058 |
rock |
|
Sample 14058 was collected from station E during the second EVA. It was placed in bag 15N and returned in ALSRC 1006 along with 14055-14062. Sample is subangular, elongate rock tapered at one end. It is olive gray in color and is fine-grained with fragments larger than 1 mm comprising 15% of the rock. |
| 14059 |
|
|
Sample 14059 was collected during the second EVA from station E. It was placed in bag 15N by the astronauts, and returned in ALSRC 1006 along with samples 14055-14062. Sample consists of two pieces, larger being irregular in shap and smaller being subrounded. |
| 14060 |
rock |
|
Sample 14060 was collected from station E during the second EVA. It was placed in bag 15N by the astronauts and returned in ALSRC 1006 along with 14055-14062. Sample is well rounded (almost spherical), friable, fragmental rock and is medium gray in color. |
| 14061 |
|
|
Sample 14061 was collected druing the second EVA from station E. It was placed in bag 15N by the astronauts and returned in ALSRC 1006 along with 14055-14062. (Sample 14062 is residue). Sample is friable and appears grayish brown in color. It is an equidimensional, subrounded block. |
| 14063 |
rock |
|
So-Called "White Rocks"; friable with dark clasts (Wilshire and Jackson 1972); annealed or slightly annealed, feldspathic Fra Mauro breccia (Chao et al 1972); "white rock breccia" (Quaide and Wrigley 1972); |
| 14064 |
rock |
|
Sample 14064 was collected in the White Rocks area at Station C1 and was returned in bag 16 along with 14063 and 14065 (residue) in ALSRC 1006. There was a strong feeling at the LRL that 14064 and 14063 are parts of the same rock because not only do they look very much alike, but 14064 has a protruding 1 cm clast, while 14063 has a 1 cm clast mold. Shepard stated that he had put "a couple" of hand specimens into bag 16, which is what was found. Sample 14064 is one of those studied by the Imbrium Consortium. Sample is pale gray with leucocratic matrix and contains approximately 40% clasts and 60% matrix. The sample is friable "white rock". |
| 14066 |
rock |
|
Sample 14066 was collected at Station F on the second EVA. The sample was found in the vicinity of Weird Crater. Sample was returned in documented bay 17N in ALSRC 1006. It is essentally a grab sample and is moderately friable with a blocky subround to subangular surface. It is very light gray in color with some large, darker gray clasts. |
| 14067 |
|
|
|
| 14068 |
rock |
|
Sample 14068 was collected during the second EVA from station C1 and placed in bag number 10. It is one of the surface rocks collected while a gray layer, just under the surface, was samples 14140-14143; blocky, gray, coherent, holocrystalline, melt rock with less than 5% clasts. |
| 14069 |
rock |
breccia |
Sample 14069 was collected at Station C1, 1.28 km ENE of the LM and 100 m SE of the rim of Cone Crater during the second EVA. The material at C1 appears to be material originally ejected from Cone Crater and re-ejected from a 30 m crater just south of Station C1 (Swann et al., 1977). Sample is block, gray, finely crystalline breccia with a sugary texture. |
| 14070 |
rock |
breccia |
Sample 14070 was collected from Station C1, 1.28 km ENE of the LM, and 100 m SE of the rim of Cone Crater during the second EVA. It appears to have been ejected from Cone Crater that was later re-ejected from a 30 m crater in the vicinity (Swann et. al., 1977). This is a blocky, subangular, coherent, light gray, crystalline breccia that is similar to 14069. |
| 14071 |
|
breccia |
Sample 14071 was collected at Station C1 approximately 1.28 km ENE of LM and 100 m SE of Cone Crater. The area is locally flat with a slight southerly slope. The sample was collected amongst abundant debris ranging in size from the limit of resoution up to 75 cm. The photo-documented area was too disturbed to be able to see any intact craters. The sample was returned in documented bay 10N in ALSRC 1006. All the samples collected in the vicinity of 14071 are blocky and angular to subrounded with very rough surfaces. |
| 14072 |
rock |
basalt |
Sample 14072 was collected at Station C1 approximately 1.28 km ENE of LM and 100 m SE of Cone Crater. The area is locally flat but generally slopes slightly to the south. The area is strewn with debris which ranges in size from the limit of resoution up to 75 cm. The debris is mainly angular to subrounded. The entire area of photo documentation is too disturbed to see any intact craters. The sample was returned in documented bag 10N in ALSRC 1006. Sample is medium light gray basalt and is somewhat smooth in appearance. The shape is blocky to subrounded and the rock is extremely coherent. |
| 14073 |
rock |
|
Samples 14073, 14074, 14078, and 14079 came from the bottome of a trench taken at Station G, 230 m ESE of LM and 50 m E of North Triplet Rim Crust. The are is marked by a nearly level terrain with sparse amount of debris scattered throughout. The debris ranges in size from the limit of resolution up to 60 cm. There is a moderate abundance of subdued 20 to 50 cm craters in the area. All samples were returned in documented bag 20N in ALSRC 1006 and are very light gray, very coherent, holocrystalline, melt rocks. |
| 14074 |
rock |
|
Samples 14073, 14074, 14078, and 14079 came from the bottome of a trench taken at Station G, 230 m ESE of LM and 50 m E of North Triplet Rim Crust. The are is marked by a nearly level terrain with sparse amount of debris scattered throughout. The debris ranges in size from the limit of resolution up to 60 cm. There is a moderate abundance of subdued 20 to 50 cm craters in the area. All samples were returned in documented bag 20N in ALSRC 1006 and are very light gray, very coherent, holocrystalline, melt rocks. |
| 14075 |
rock |
|
Sample 14075 was collected at the bottom of the trench at Station G 230 m ESE of LM and 50 m E of North Triplet rim crust. The area is characterized by a nearly level regolith surface which is sparsely strewn by fragmental debris. The size of the debris varies from the limit of resolution to 60 cm. It is small, subangular, blocky rock chip of a moderately coherent fragmental rock with a moderately smooth surface. The color is a ight gray. The sample was returned I documented bag 20N in ALSRC 1006. |
| 14076 |
rock |
|
Sample 14076 was collected at the bottom of the trench at Station G, 230 m ESE of LM and 50 m E of North Triplet rim crest. Area in general is nearly level and lightly strewn with debris. The size of the debris ranges from the limit of resolution up to 60 cm. There is a moderate amount of subhedral 20 to 50 cm craters. The sample was returned in documented bag 20N in ALSRC 1006 and is medium light gray in color. |
| 14077 |
rock |
|
Sample 14077 was collected at Station G locted 230 m ESE of LM and 50 m E of North Triplet rim crust. It was collected from the bottom of the trench sample. The general area is more or less level and sparsely covered with debris. The size of the debris ranges from limit of resolution of 60 cm. The area has a moderate abundance of 20 to 50 cm craters mot of which are subdued. It was returned in documented bag 20N in ALSRC 1006 and is a very light gray holocrystalline plagioclase-rich rock and is fine-grained and inequigranular. |
| 14078 |
rock |
|
Samples 14073, 14074, 14078, and 14079 came from the bottome of a trench taken at Station G, 230 m ESE of LM and 50 m E of North Triplet Rim Crust. The are is marked by a nearly level terrain with sparse amount of debris scattered throughout. The debris ranges in size from the limit of resolution up to 60 cm. There is a moderate abundance of subdued 20 to 50 cm craters in the area. All samples were returned in documented bag 20N in ALSRC 1006 and are very light gray, very coherent, holocrystalline, melt rocks. |
| 14079 |
rock |
|
Samples 14073, 14074, 14078, and 14079 came from the bottome of a trench taken at Station G, 230 m ESE of LM and 50 m E of North Triplet Rim Crust. The are is marked by a nearly level terrain with sparse amount of debris scattered throughout. The debris ranges in size from the limit of resolution up to 60 cm. There is a moderate abundance of subdued 20 to 50 cm craters in the area. All samples were returned in documented bag 20N in ALSRC 1006 and are very light gray, very coherent, holocrystalline, melt rocks. |
| 14080 |
rock |
|
Samples 14080 and 14081 were taken from the middle of the trench at Station G 230 m ESE of LM and 50 m E of the Triplet rim crust. The general area from where the sample was taken is characterized by a nearly level terrain sparsely scattered with debris. The size of the debris varies from the limit of resolution up to 60 cm. The area is also characterized by a moderate abundance of subdued 20 to 50 cm craters and were returned in documented bay 21N in ALSRC 1006. Both are light gray in color and very fine grained. The are both polymicts and contain abundant glass. Both are friable being made up of < 1 mm rock/soil fragments bonded by glass. They could be pieces of the sample but in their present state, they cannot be fitted together. |
| 14081 |
rock |
|
Samples 14080 and 14081 were taken from the middle of the trench at Station G 230 m ESE of LM and 50 m E of the Triplet rim crust. The general area from where the sample was taken is characterized by a nearly level terrain sparsely scattered with debris. The size of the debris varies from the limit of resolution up to 60 cm. The area is also characterized by a moderate abundance of subdued 20 to 50 cm craters and were returned in documented bay 21N in ALSRC 1006. Both are light gray in color and very fine grained. The are both polymicts and contain abundant glass. Both are friable being made up of < 1 mm rock/soil fragments bonded by glass. They could be pieces of the sample but in their present state, they cannot be fitted together. |
| 14082 |
rock |
breccia |
Samples 14082/14083 are white rocks collected at Station C1, 1.24 km ENE of the LM and 17 m SE of the rim of Cone Crater. They are representative of one of the major rock types as seen in lunar photo documentation. The sample was chipped from the top of White Rock, a 1 m breccia boulder with consipicous 1 cm dark and light clasts in a very light gray matrix. This sample was placed in bag 13N and returned in ALSRC 1006. By the time it had arrived at the LRL, it had broken into two pieces and these were numbered 14082 and 14083. Sample 14082 was studied extensively by the Ibrium Consortium, from which much of this information is derived. Sample 14082/14083 is one of the white rocks. It is a polymict breccia with a very light gray matrix and darker lithic clasts. |
| 14083 |
rock |
breccia |
Samples 14082/14083 are white rocks collected at Station C1, 1.24 km ENE of the LM and 17 m SE of the rim of Cone Crater. They are representative of one of the major rock types as seen in lunar photo documentation. The sample was chipped from the top of White Rock, a 1 m breccia boulder with consipicous 1 cm dark and light clasts in a very light gray matrix. This sample was placed in bag 13N and returned in ALSRC 1006. By the time it had arrived at the LRL, it had broken into two pieces and these were numbered 14082 and 14083. Sample 14082 was studied extensively by the Ibrium Consortium, from which much of this information is derived. Sample 14082/14083 is one of the white rocks. It is a polymict breccia with a very light gray matrix and darker lithic clasts. |
| 14084 |
|
|
|
| 14140 |
|
|
|
| 14141 |
soil-general |
soil |
Samples 14140, 14141, 14142, 14143, 14144 and 14068, 14069, 14070, 14071, and 14072 were collected 3 meters from the rim of a 15 meter crater just south of Cone crater. 14141 is a surface soil identified by crew as a light gray layer, 14068 through 14072 is a sample of some surface rocks in the area. The area near the rim of Cone crater is strewn with boulders up to 3 meters. |
| 14142 |
|
|
|
| 14143 |
|
|
|
| 14144 |
|
|
|
| 14148 |
|
soil |
14145, 14146, 14147, and 14148 collected from the top of the trench; 14153, 14154, 14155, and 14156 is mixed material from the middle two layers, 14080 and 14081 below that, and 14073, 14074, 14075, 14076, 14077, 14078, and 14079 and 14149, 14150, 14151, and 14152 from the bottom of a 40 cm trench. Astronaut Shepard reports the surface fines were so loose the trench walls kept falling in and layered materials were mixed. Bottom layers have pebble in it. |
| 14149 |
|
soil |
14145, 14146, 14147, and 14148 collected from the top of the trench; 14153, 14154, 14155, and 14156 is mixed material from the middle two layers, 14080 and 14081 below that, and 14073, 14074, 14075, 14076, 14077, 14078, and 14079 and 14149, 14150, 14151, and 14152 from the bottom of a 40 cm trench. Astronaut Shepard reports the surface fines were so loose the trench walls kept falling in and layered materials were mixed. Bottom layers have pebble in it. |
| 14156 |
|
soil |
Trench sample collected at Station G 30 m NE of North Triplet crater. 14145, 14146, 14147, and 14148 collected from the top of the rench, 14153, 14154, 14155, 14156 is mixed material from the middle two layers including a thin layer of glassy pebbles, 14080 and 14081 below that, and 14073, 14074, 14075, 14076, 14077, 14078, 14079, 14149, 14150, 14151, and 14152 from the bottom of the 40 cm trench. Astronaut Shepard reports the surface fines were so loose the trench walls kept falling in the layered materials mixed. |
| 14163 |
|
soil |
14160, 14161, 14162, 14163, 14402, 14422, 14425 through 14453 collected 15 m NW of LM. Samples collected from the bottom of a 1 m crater with glass in the bottom; Astronaut Shepard identifies the crater as secondary. Sample area is level and free of large blocks. |
| 14165 |
|
|
|
| 14166 |
|
|
|
| 14167 |
|
|
|
| 14168 |
|
|
|
| 14169 |
|
breccia |
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. These samples (14169 - 14188) contain a seriate distribution of clasts as large as two centimeters across. The samples are all polymict breccias with fragmental matrices. |
| 14170 |
|
breccia |
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. These samples (14169 - 14188) contain a seriate distribution of clasts as large as two centimeters across. The samples are all polymict breccias with fragmental matrices. |
| 14171 |
|
|
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. These samples (14169 - 14188) contain a seriate distribution of clasts as large as two centimeters across. The samples are all polymict breccias with fragmental matrices. |
| 14172 |
|
|
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. These samples (14169 - 14188) contain a seriate distribution of clasts as large as two centimeters across. The samples are all polymict breccias with fragmental matrices. |
| 14173 |
|
|
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. These samples (14169 - 14188) contain a seriate distribution of clasts as large as two centimeters across. The samples are all polymict breccias with fragmental matrices. |
| 14174 |
|
|
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. These samples (14169 - 14188) contain a seriate distribution of clasts as large as two centimeters across. The samples are all polymict breccias with fragmental matrices. |
| 14175 |
|
|
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. These samples (14169 - 14188) contain a seriate distribution of clasts as large as two centimeters across. The samples are all polymict breccias with fragmental matrices. |
| 14176 |
|
|
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. These samples (14169 - 14188) contain a seriate distribution of clasts as large as two centimeters across. The samples are all polymict breccias with fragmental matrices. |
| 14177 |
|
|
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. These samples (14169 - 14188) contain a seriate distribution of clasts as large as two centimeters across. The samples are all polymict breccias with fragmental matrices. |
| 14178 |
|
|
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. These samples (14169 - 14188) contain a seriate distribution of clasts as large as two centimeters across. The samples are all polymict breccias with fragmental matrices. |
| 14179 |
|
|
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. These samples (14169 - 14188) contain a seriate distribution of clasts as large as two centimeters across. The samples are all polymict breccias with fragmental matrices. |
| 14180 |
|
|
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. These samples (14169 - 14188) contain a seriate distribution of clasts as large as two centimeters across. The samples are all polymict breccias with fragmental matrices. |
| 14181 |
|
|
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. These samples (14169 - 14188) contain a seriate distribution of clasts as large as two centimeters across. The samples are all polymict breccias with fragmental matrices. |
| 14182 |
|
|
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. These samples (14169 - 14188) contain a seriate distribution of clasts as large as two centimeters across. The samples are all polymict breccias with fragmental matrices. |
| 14183 |
|
|
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. These samples (14169 - 14188) contain a seriate distribution of clasts as large as two centimeters across. The samples are all polymict breccias with fragmental matrices. |
| 14184 |
|
|
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. These samples (14169 - 14188) contain a seriate distribution of clasts as large as two centimeters across. The samples are all polymict breccias with fragmental matrices. |
| 14185 |
|
|
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. These samples (14169-14188) contain a seriate distribution of clasts as large as two centimeters across. The samples are all polymict breccias with fragmental matrices. |
| 14186 |
|
|
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. These samples (14169-14188) contain a seriate distribution of clasts as large as two centimeters across. The samples are all polymict breccias with fragmental matrices. |
| 14187 |
|
|
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. These samples ( 14169-14188) contain a seriate distribution of clasts as large as two centimeters across. The samples are all polymict breccias with fragmental matrices. |
| 14188 |
|
|
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. These samples (14169-14188) contain a seriate distribution of clasts as large as two centimeters across. The samples are all polymict breccias with fragmental matrices. |
| 14189 |
|
|
|
| 14194 |
rock |
breccia |
Weigh bag 1031 was used on the traverse during the second EVA. Samples 14194-14201 are small rock fragments that were left in weight bag 1031 after samples 14306-14311 were removed. Their lunar location and orientation are unknown and there are no lunar surface photographs of these samples. Some of these are probably pieces broken off the larger rocks during transit. This sample is a light gray, moderately friable, polymict breccia which appears to be bounded by freshly broken surface. |
| 14195 |
rock |
|
Weigh bag 1031 was used on the traverse during the second EVA. Samples 14194-14201 are small rock fragments that were left in weight bag 1031 after samples 14306-14311 were removed. Their lunar location and orientation are unknown and there are no lunar surface photographs of these samples. Some of these are probably pieces broken off the larger rocks during transit. This sample is a coherent, medium to dark gray, fragmental rock. |
| 14196 |
rock |
|
Weigh bag 1031 was used on the traverse during the second EVA. Samples 14194-14201 are small rock fragments that were left in weight bag 1031 after samples 14306-14311 were removed. Their lunar location and orientation are unknown and there are no lunar surface photographs of these samples. Some of these are probably pieces broken off the larger rocks during transit. This sample is a friable, polymict breccia similar to 14051 or 14066. |
| 14197 |
|
|
Weigh bag 1031 was used on the traverse during the second EVA. Samples 14194-14201 are small rock fragments that were left in weight bag 1031 after samples 14306-14311 were removed. Their lunar location and orientation are unknown and there are no lunar surface photographs of these samples. Some of these are probably pieces broken off the larger rocks during transit. This sample is very fine grained and appears to be completely recrystallized. |
| 14198 |
|
|
Weigh bag 1031 was used on the traverse during the second EVA. Samples 14194-14201 are small rock fragments that were left in weight bag 1031 after samples 14306-14311 were removed. Their lunar location and orientation are unknown and there are no lunar surface photographs of these samples. Some of these are probably pieces broken off the larger rocks during transit. This sample is a crystalline rock. |
| 14199 |
rock |
basalt |
Weigh bag 1031 was used on the traverse during the second EVA. Samples 14194-14201 are small rock fragments that were left in weight bag 1031 after samples 14306-14311 were removed. Their lunar location and orientation are unknown and there are no lunar surface photographs of these samples. Some of these are probably pieces broken off the larger rocks during transit. This sample is a freshly fractured, polymict breccia. |
| 14200 |
rock |
basalt |
Weigh bag 1031 was used on the traverse during the second EVA. Samples 14194-14201 are small rock fragments that were left in weight bag 1031 after samples 14306-14311 were removed. Their lunar location and orientation are unknown and there are no lunar surface photographs of these samples. Some of these are probably pieces broken off the larger rocks during transit. This sample is a fragment of very fine grained basaltic crystalline rock. |
| 14201 |
rock |
breccia |
Weigh bag 1031 was used on the traverse during the second EVA. Samples 14194-14201 are small rock fragments that were left in weight bag 1031 after samples 14306-14311 were removed. Their lunar location and orientation are unknown and there are no lunar surface photographs of these samples. Some of these are probably pieces broken off the larger rocks during transit. This sample is a fine grained polymict breccia similar to 14042. |
| 14210 |
core |
|
|
| 14211 |
core |
|
|
| 14220 |
core |
|
|
| 14230 |
core |
soil |
Intended to be a triple core tube, but driving became hard after a tube and a quarter, and material in the top tube fell out. Area generally level and free of large blocks. This sample from the top of three stratigraphic units of core. |
| 14240 |
|
|
|
| 14250 |
|
|
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. Sample 14250 is a medium gray, blocky, subangular, moderately friable, seriate fragmental rock. |
| 14251 |
|
|
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. Sample 14251 is a medium gray, blocky, friable, fragmental rock. |
| 14252 |
rock |
|
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. Sample 14252 is a medium gray, friable, fragmental rock. It is subround to angular, appearing to be 1/4 of a sphere. |
| 14253 |
rock |
breccia |
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. Sample 14253 is a gray, angular, block, homogeneous, crystalline breccia. |
| 14254 |
rock |
soil |
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. Sample 14254 is gray soil, adhering to frothy black glass and is highly irregular in shape. |
| 14255 |
rock |
|
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. Sample 14255 is a medium gray, subangular, blocky, friable fragmental rock. |
| 14256 |
|
|
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. |
| 14257 |
|
|
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. |
| 14258 |
|
|
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. |
| 14259 |
|
soil |
This scoop sample is part of the comprehensive sample collected 110 m WNW of LM along with 14165 through 14189, 14250 through 14289, 14298 through 14300, and 14420. All samples were collected from within a 4 m circle drawn by Astronaut Shepard. Astronaut Mitchell reports, "The number of surface rocks, or rocks compared with the number of surface fines is very small Houston. There's a few boulders lying around and there's a few blocks around some of the craters, but by and large, it's a powdery surface." |
| 14260 |
|
soil |
Surface soil sample is part of comprehensive sample collected 110 WNW of LM with 14165 through 14189, 14250 through 14289, 14298 through 14300 and 14421. All samples, including many walnut sized rocks were collected within a 4 m circle drawn by Astronaut Shepard. 14260 was collected from the top 1 cm of an undisturbed region with this circle. Area is generally level and free of boulders. |
| 14261 |
|
|
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. |
| 14263 |
|
|
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. |
| 14264 |
rock |
breccia |
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. Sample 14264 is a dark gray, blocky, tough fragmental rock, described by Phinney et al. (1975) as a vitric (matrix) breccia. |
| 14265 |
rock |
|
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. Sample 14265 is angular, with half the surface coated with dark greenish gray to black glass. The rock is a medium dark gray, coherent fragmental rock. |
| 14266 |
rock |
breccia |
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. Sample 14266 is a light medium gray, rounded, slabby, tough, fragmental matrix, polymict breccia. |
| 14267 |
rock |
breccia |
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. Sample 14267 is a blocky, angular, dark gray, tough, vitric (matrix) breccia. |
| 14268 |
rock |
breccia |
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. Sample 14268 is described by Phinney et al. (1975) as a blocky, medium dark gray, vitric (matrix) breccia. |
| 14269 |
rock |
breccia |
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. Sample 14269 is a dark medium gray, frgmental microbreccia with one rounded side. |
| 14270 |
rock |
breccia |
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. Sample 14270 is a blocky, medium greenish gray fine-grained crystalline breccia. |
| 14271 |
rock |
breccia |
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. Sample 14271 is a blocky, dark medium vitric (matrix) breccia with light gray clasts. |
| 14272 |
rock |
breccia |
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. Sample 14272 is a blocky medium dark gray coherent vitric (matrix) breccia. |
| 14273 |
rock |
breccia |
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. Sample 14273 is a medium dark gray, vitric (matrix) breccia. |
| 14274 |
rock |
breccia |
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. Sample 14274 is a light medium gray, blocky, tough, crystalline, polymict breccia. |
| 14275 |
rock |
breccia |
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. Sample 14275 is a medium light gray, blocky, polymict breccia. |
| 14276 |
rock |
|
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. Sample 14276 is a brownish-gray, blocky, coherent, medium-grained, crystalline rock. |
| 14277 |
rock |
breccia |
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. Sample 14277 is a dark gray, blocky, coherent vitric (matrix) breccia. |
| 14278 |
rock |
breccia |
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. Sample 14278 is a medium light gray, subrounded, coherent, low-grade, polymict breccia. |
| 14279 |
rock |
breccia |
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. Sample 14279 is medium light gray in color, blocky, rounded to subrounded in shape, and is a coherent, polymict breccia with a fragmented matrix. |
| 14280 |
rock |
breccia |
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. Sample 14280 is a medium dark gray, angular block of vitric (matrix) breccia. |
| 14281 |
rock |
breccia |
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. Sample 14281 is a medium dark gray, subrounded to angular block of coherent, vitric (matrix) breccia. |
| 14282 |
rock |
breccia |
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. Sample 14282 is a medium gray, friable, fragmental rock (soil breccia). |
| 14283 |
rock |
breccia |
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. Sample 14283 is a light gray, slabby, angular, coherent, crystalline, polymict breccia. |
| 14284 |
rock |
|
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. Sample 14284 is a subrounded, medium gray, coherent, fragmental rock. |
| 14285 |
rock |
breccia |
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. Sample 14285 is a light medium gray, coherent, polymict breccia. |
| 14286 |
rock |
|
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. Sample 14286 is a medium brownish-gray fragmental rock. |
| 14287 |
rock |
|
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. Sample 14287 is a medium brownish gray, coherent, fragmental rock that is blocky and angular in shape. |
| 14288 |
rock |
breccia |
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. Sample 14288 is a medium dark gray, vitric (matrix) breccia. It is blocky and angular in shpe and is coherent. |
| 14289 |
|
|
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. Sample 14288 is a medium dark gray, vitric (matrix) breccia. It is blocky and angular in shpe and is coherent. |
| 14290 |
|
soil |
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. |
| 14291 |
|
soil |
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. |
| 14292 |
|
soil |
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. |
| 14293 |
|
soil |
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. |
| 14294 |
|
breccia |
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. Weigh bag 1038 was used to hold rocks and fragments from Station H, EVA-2. The largest samples are numbered 14312-14320 and the residue is 14290-14297. Samples 14294-14297 are the largest fragments of the residue. Sample 14294 is a breccia with one rounded side and one angular side. It is grayish brown on the rounded surface and light to medium gray on the fresh surface. |
| 14295 |
rock |
breccia |
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. Weigh bag 1038 was used to hold rocks and fragments from Station H, EVA-2. The largest samples are numbered 14312-14320 and the residue is 14290-14297. Samples 14294-14297 are the largest fragments of the residue. Sample 14295 is a fine grained, polymict breccia with 5% clasts larger than 1 mm and 95% matrix grains smaller than 1 mm in size. |
| 14296 |
rock |
breccia |
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. Weigh bag 1038 was used to hold rocks and fragments from Station H, EVA-2. The largest samples are numbered 14312-14320 and the residue is 14290-14297. Samples 14294-14297 are the largest fragments of the residue. Sample 14296 is a light ray, angular, flat, polymict breccia chip. |
| 14297 |
rock |
breccia |
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. Weigh bag 1038 was used to hold rocks and fragments from Station H, EVA-2. The largest samples are numbered 14312-14320 and the residue is 14290-14297. Samples 14294-14297 are the largest fragments of the residue. Sample 14297 is a polymict breccia with an unusual clast mineralogy. |
| 14298 |
|
|
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. |
| 14299 |
|
|
The purpose of the Comprehensive Sample (14169-14188; 14250-14299) was to acquire a statistically significant set of small rock samples to petrographically characterize the distribution of rock types in the lunar regolith. The sample location was selected 100 to 125 m west of the LM. A two to three meter diameter circle was marked and all of the walnut sized rocks on the surface within the circle were collected with tongs. |
| 14300 |
|
|
|
| 14301 |
rock |
breccia |
Sample 14301 is one of two samples (14301 and 14313) collected at Station G1, 150 m east of the LM on the north rim crest of North Triplet Crater during the second EVA. According to the astronauts, the rock appeared to be similar to the other rocks in the area; these appear to be ejecta from North Triplet Crater. Except for samples dug from trenches, 14301 was the most deeply buried rock returned during the Apollo 14 mission (Swann et al., 1977). This sample was larger then anticipated, and was placed directly in weigh bag 1031 (?) by the astronauts. Sample 14301 is a moderately coherent, light medium gray, polymict breccia. It consists of at least 20% clasts larger than 1mm. |
| 14302 |
rock |
|
|
| 14303 |
rock |
breccia |
These samples (14303 and 14304) are pieces of a football-size rock collected from a location 80 m NNW of the LM during EVA 1. This rock was almost completely buried in the regolith and its orientation is unknown. Both of these samples have freshly broken surfaces. They were first identified as pieces of the same rock in March, 1977, when the models of the rock were found to fit together along their freshly broken surfaces. They share a common lithology which is especially evident along the broken surfaces. These samples were returned together in weigh bag 1027 which also contained samples 14305/302 and various smaller chips (see Phinney et al., 1975). These samples were examined in the CRA and NNPL by the PET< and 14303 was extensively distributed for scientific experimentation. Sample 14304 has been designated a posterity sample. This rock (14303) is a coherent, gray, block to subrounded breccia. |
| 14304 |
rock |
breccia |
These samples (14303 and 14304) are pieces of a football-size rock collected from a location 80 m NNW of the LM during EVA 1. This rock was almost completely buried in the regolith and its orientation is unknown. Both of these samples have freshly broken surfaces. They were first identified as pieces of the same rock in March, 1977, when the models of the rock were found to fit together along their freshly broken surfaces. They share a common lithology which is especially evident along the broken surfaces. These samples were returned together in weigh bag 1027 which also contained samples 14305/302 and various smaller chips (see Phinney et al., 1975). These samples were examined in the CRA and NNPL by the PET, and 14303 was extensively distributed for scientific experimentation. Sample 14304 has been designated a posterity sample. |
| 14305 |
rock |
breccia |
broken apart during transit to LRL and numberd 14305 / 14302 and 14303 / 14304; sample 14302 was later renumbered 14305,18. The sample is a medium gray, holocrystalline, clast rich breccia which has been well-sintered together. |
| 14306 |
rock |
breccia |
Sample 14306 is a fragmental rock collected at station G, 230 meters ESE of the lunar module (LM), and 50 meters E of the rrim crest of North Triplet Crater. It is said to be somewhat more tabular and less irregular than 60 cm boulder but similar to it in color and albedo. The lunar location and orientation are well documented. This sample is gray with ~25% white clasts and is blocky in shape. The rock is a coherent breccia. |
| 14307 |
rock |
breccia |
Breccia sample 14307 was collected during the second EVA at station G. This sample was not well-documented because its position had already been changed by the time it was collected. There are no lunar surface photographs of 14307, and its lunar orientation is only known through surface pitting. The rock was placed in documented bag 25N and returned to weigh bag 1031. This is a block, subrounded rock with an irregular surface. The color varies from white to dark gray. The rock is friable, but suffieciently strong to prevent clasts from falling out. |
| 14308 |
|
|
|
| 14309 |
rock |
breccia |
Sample 14309 was collected sometime during the second EVA. No lunar-surface photographs were made, nor are the location and orientation known. The sample was returned in weight bag 1031 with other grap samples from EVA 2. Sample 14309 is a moderately friable, vitric matrix breccia. |
| 14310 |
rock |
|
Crystalline Sample 14310 was collected during the second EVA at Station G. The collection was not well documented -- no lunar-surface photographs were made, and the orientation is known only from surface pitting. This rock is a medium, gray, blocky melt rock, which is subrounded on the pitted sides. It is fine grained and homogeneous in mineralogy. |
| 14311 |
rock |
breccia |
Breccia sample 14311 was collected during EVA 2 at station Dg. Lunar surface photographs were not taken and the orientation is estimated from surface pitting. Sample 14308 consisted of 3 pieces which PET found to have been part of 14311 and are included herein. These three pieces were renumbered 14311,26; 14311,64; and 14311,65. This sample is a gray coherent breccia which is broken into pieces along fractures. There are only a few fragments >1 mm (<5%) and the rock is mostly (95%) crystalline matrix. |
| 14312 |
rock |
breccia |
Sample 14312 is a breccia collected from the top of Turtle Rock during EVA 2 at Station H. Its lunar orientation and location were well documented. Turkle Rock is the largest of several boulders at Station H, and the two rocks on it were nicknamed "turtle eggs", and collected as samples 14312 and 14319; rock is medium gray, coherent breccia which is partly covered with glass. |
| 14313 |
rock |
breccia |
Breccia sample 14313 was collected during the second EVA at Station G1, 150 m east of LM, on north rim crest of North Triplet Crater. It was placed in documented bag 27N. Its lunar location and orientation are well documented. This is a medium light gray, coherent, fragmental breccia with a distrinctive shape due to a prominent notch produced by spalling along two sets of fractures intersecting at an angle of 150 degrees. |
| 14314 |
rock |
breccia |
Sample 14314 is a breccia sample collected during the second EVA at Station H. It was collected from the fillet below Turtle Rock, 80 meters NW of the LM. The fillet slopes 2-3 degrees to the flat regolith and has abundant rocks up to 30 cm in size distributed in it. The rock is a friable breccia, medium to light gray on its fresh surface and dark brownish gray elsewhere. Approximately 40% of the surface is glass covered. |
| 14315 |
|
breccia |
Sample 14315 is a breccia collected from Station H (North Boulder Field) during EVA 2. Its lunar location is documented as bieing 15 m SE of Turtle Rock and 70 m NW of the LM, but the lunar orientation is tentative. It was returned in weight bag 1038. This coherent, gray breccia has a rounded surface and an angular flat underside. |
| 14316 |
rock |
breccia |
Sample 14316 is a breccia collected at Station H during EVA 2. It has not been identified in lunar surface photographs, so its exact lunar location and orientation are unknown. It was returned in weigh bag 1038. This rock is a medium gray, inhomogeneous, fragmental breccia with one flat face. There is a predominance of leucocratic clasts. |
| 14317 |
rock |
breccia |
Breccia sample 14317 was collected at Station H during the second EVA but has not been identified in the North Boulder Field photographs, so its lunar location is tentative, and lunar orientation, unknown. It was returned in weigh bag 1038. This rock is a medium gray, coherent breccia. |
| 14318 |
rock |
breccia |
Breccia sample 14318 was collected from the regolith near the south end of North Boulder Field at Station H during the second EVA. It was returned in weigh bag 1038. Sample 14318 is one of the specimens chosen for study by the Imbrium Consortium, who received 14318,0. A complete set of matched thin sections, across the entire specimen was made by the Consortium (1976); This sample is a very coherent, gray, polymict breccia consisting of light gray clasts in a medium gray matrix. |
| 14319 |
rock |
breccia |
Breccia sample 14319 is the western rock from the top of Turtle Rock ("turtle eggs"). This sample as well as 14312 were collected from Turtle Rock at Station H during the second EVA and returned in weigh bag 1038. Its lunar orientation and location have been well documented. It appears to be similar to Turtle Rock and the other rocks in the area. This is alight-medium gray coherent breccia which is flat on one side and rounded on the other side. |
| 14320 |
|
breccia |
This breccia was collected from North Boulder Field from Station h during EVA 2. The sample has not been identified in lunar surface photographs so the lunar location is only tentative and the lunar orientation is unknown. Sample 14320 was returned in weight bag 1038. This is a medium gray, coherent, polymict breccia. |
| 14321 |
rock |
breccia |
largest sample returned during Apollo 14 mission; also known as "Big Bertha". This sample is the third largest sample returned by any Apollo mission. This breccia was collected during the second EVA at Station C1, near the rim of Cone Crater. A voice transcript made during the collection, as well as a more detailed discussion of the lunar environment can be found in Geological Survey Professional Paper 880 (Swann et al., 1977). The sample was returned in bag 1038. This large sample is typical of the apparently dominent rock type in the Cone Crater ejecta blanket. It is a moderately well-indurated breccia, in which predominately dark clasts are set in a lighter matrix. The relative abundance of this rock type suggests that it is probalby representative of the Fra Mauro Formation. This rock, 14321, is a partly annealed, moderately coherent polymict breccia. The blocky surface is gray with patches of black and white. |
| 14411 |
|
|
|
| 14414 |
|
|
|
| 14421 |
|
|
|
| 14426 |
rock |
breccia |
This sample is a polymict breccia which is broken into two pieces which are similar. The sample is a friable, fine grained, polymict breccia with textural and mineralogic homogeniety. |
| 14427 |
rock |
|
This sample is a fine grained clastic rock composed of white feldspar and black glass. |
| 14428 |
rock |
breccia |
Sample 14428 is a vesicular breccia with a crystalline matrix. |
| 14429 |
rock |
breccia |
Sample 14429 is a slightly vesicular polymict breccia similar to 14428. |
| 14430 |
|
breccia |
Sample 14430 is a medium to light gray, polymict breccia |
| 14431 |
rock |
|
Sample 14431 is a light gray, crystalline rock |
| 14434 |
|
|
|
| 14435 |
rock |
|
Sample 14435 is a holocrystalline, equigranular, coherent rock which appears to have been freshly broken. |
| 14436 |
rock |
|
Sample 14436 is a brownish gray sample which may be either an igneous rock or a dense, fine grained, fragmental rock. |
| 14437 |
rock |
|
Sample 14437 is a fragmental rock with all grains smaller than 1 mm and no lithic fragments. |
| 14438 |
rock |
|
Sample 141438 is a medium to light brownish gray, fragmental rock. |
| 14439 |
rock |
|
This sample consists of two, small, subequal pieces of a fragmental rock. |
| 14440 |
rock |
|
This sample is a blocky, angular, medium gray, holocrystalline rock with smooth, unpitted surfaces. |
| 14441 |
rock |
|
This is a medium to dark gray, coherent, fragmental rock with a pronounced conical shape. |
| 14442 |
rock |
|
Sample 14442 is a small, blocky, friable, medium gray fragment which resembles siltstone in appearance. |
| 14443 |
rock |
|
The sample is a dust covered, slightly elongated, holocrystalline rock. |
| 14444 |
rock |
|
This is a very light gray, coherent, holocrystalline rock with 4% megacrysts. |
| 14445 |
rock |
breccia |
Sample 14445 is a blocky, subangular, medium gray, hackly, polymict breccia with moderate cohesiveness. |
| 14446 |
rock |
|
This sample consists of four small chips of plagioclase-rich rock. |
| 14447 |
rock |
|
This small sample is blocky and angular in shape, it has a very hackly surface. It appears to be an agglometation of fine grained clastics that is held together with glass. |
| 14448 |
rock |
|
This sample is an agglomerate of fine grained, clastic rocks held together by spatter glass. |
| 14449 |
rock |
|
Sample 14449 is a gray, friable, freshly broken chip of clastic rock. |
| 14450 |
rock |
|
The sample is an agglomerate of friable, clastic clods bonded by dark gray to honey brown vesicular glass. |
| 14451 |
rock |
|
This sample is a very light gray, coherent, massive, inequigranular, holocrystalline rock. |
| 14452 |
rock |
|
Sample is a fine grained, gray, clastic rock. |
| 14453 |
rock |
breccia |
This is a banded, light gray, slightly flattened, breccia chip. |
Jump to Apollo:
11
12
14
16
17
|
| Apollo 15 |
| Sample Number |
Sample Type |
Lithology |
Description |
| 15000 |
|
|
|
| 15001 |
core |
|
Deep core 15001 through 15006 was taken at Station 8, 5 m southeast of the trench. Area has a smooth hummocky surface with fine grained material and rare cobble-sized fragments not visibly related to any particular crater. Astronauts report a hard layer at a depht of 35 cm at the trench; this layer may exist in the core as well. |
| 15002 |
core |
|
Deep core 15001 through 15006 was taken at Station 8, 5 m southeast of the trench. Area has a smooth hummocky surface with fine grained material and rare cobble-sized fragments not visibly related to any particular crater. Astronauts report a hard layer at a depht of 35 cm at the trench; this layer may exist in the core as well. |
| 15003 |
core |
|
Deep core 15001 through 15006 was taken at Station 8, 5 m southeast of the trench. Area has a smooth hummocky surface with fine grained material and rare cobble-sized fragments not visibly related to any particular crater. Astronauts report a hard layer at a depht of 35 cm at the trench; this layer may exist in the core as well. |
| 15004 |
core |
|
Deep core 15001 through 15006 was taken at Station 8, 5 m southeast of the trench. Area has a smooth hummocky surface with fine grained material and rare cobble-sized fragments not visibly related to any particular crater. Astronauts report a hard layer at a depht of 35 cm at the trench; this layer may exist in the core as well. |
| 15005 |
core |
|
Deep core 15001 through 15006 was taken at Station 8, 5 m southeast of the trench. Area has a smooth hummocky surface with fine grained material and rare cobble-sized fragments not visibly related to any particular crater. Astronauts report a hard layer at a depht of 35 cm at the trench; this layer may exist in the core as well. |
| 15006 |
core |
|
Deep core 15001 through 15006 was taken at Station 8, 5 m southeast of the trench. Area has a smooth hummocky surface with fine grained material and rare cobble-sized fragments not visibly related to any particular crater. Astronauts report a hard layer at a depht of 35 cm at the trench; this layer may exist in the core as well. |
| 15007 |
core |
|
Double core 15007 through 15008 was collected at Station 2, 5m SE of the large boulder on the rim of a 10m crater. Local concentrations of clods on the crater rim, but the site mostly has fine grained character. Lack of blocks suggests a mature, intensely gardened regolith. |
| 15008 |
core |
|
Double core 15007 through 15008 was collected at Station 2, 5m SE of the large boulder on the rim of a 10m crater. Local concentrations of clods on the crater rim, but the site mostly has fine grained character. Lack of blocks suggests a mature, intensely gardened regolith. |
| 15009 |
core |
|
|
| 15010 |
core |
|
Double core 15010-15011 was collected at Station 9A 20 m N of the rim of Hadley Rille. The site is level with no fresh craters apparent; fragments <20 cm are common, boulders >1m are scattered. Core area was undisturbed by footprings before sampling, even the uppermost part of the core should be undisturbed. |
| 15011 |
core |
soil |
Double core 15010-15011 was collected at Station 9A 20 m N of the rim of Hadley Rille. The site is level with no fresh craters apparent; fragments <20 cm are common, boulders >1m are scattered. Core area was undisturbed by footprings before sampling, even the uppermost part of the core should be undisturbed. |
| 15012 |
|
soil |
Soil collected with rock fragments 15260 through 15264 from the bottom of a trench dug into the south rim of a 12 m cratr at Station 6. The rim of this crater is asymmetric; the north rim is hard, granular, and littered with fragments, and the south rim is softer and smoother. |
| 15013 |
|
|
|
| 15014 |
soil-general |
|
|
| 15015 |
rock |
regolith breccia |
Coherent, glassy matrix breccia containing abundant glass balls, shards, and schlieren |
| 15016 |
|
|
|
| 15017 |
|
|
|
| 15018 |
|
|
|
| 15019 |
|
|
|
| 15020 |
|
soil |
This is the contingency sample collected 12 m west of the LM +Z footpad. The surface material here is soft and fine grained. The sample was taken on a small flat between two subdued 1 m craters. The sample sieved includes a 1.1g glass coated microbreccia, but excludes a 77 gm coherent breccia. |
| 15021 |
|
|
|
| 15024 |
|
|
|
| 15025 |
|
|
|
| 15026 |
|
|
|
| 15027 |
|
|
|
| 15028 |
|
|
|
| 15030 |
soil-general |
|
At Station 8, Astronaut Irwin dug the deep trench; samples 15030 through 15034 were taken from the bottom of the trench. The trench area is similar to the area near the ALSEP, a smooth, hummocky surface of fine grained material with rare, cobble sized fragments not visibly related to any particular crater. The trench wall was described by the astronauts as uniform, with perhaps a slight color darkening in the middle part, above a hard layer which was not penetrated, but just reached at a depth of about 35 cm. |
| 15031 |
|
|
|
| 15032 |
|
|
|
| 15033 |
|
|
|
| 15034 |
|
|
|
| 15040 |
|
|
At Station 8 Astronaut Irwin dug the deep trench; samples 15040 through 15044 were taken from the tope of the trench. The trench area is similar to the area near the ALSEP, a smooth, hummocky surface of fine grained material with rare, cobble sized fragments not visibly related to any particular crater. The trench wall was described by the astronauts as uniform, with perhaps a slight color darkening in the middle part, above a hard layer which was not penetrated, but just reached at a depth of about 35 cm. One small fresh crater occurs a few meters north of the trench, but it is too distant to add a significant layer of ejecta to the top of the trench area. |
| 15041 |
|
|
|
| 15042 |
|
|
|
| 15043 |
|
|
|
| 15044 |
|
|
|
| 15058 |
|
|
|
| 15059 |
|
breccia |
|
| 15065 |
|
|
|
| 15070 |
|
soil |
Soil 15070, rock sample 15075, and rock sample 15076 were taken from a small area about 25 m east of the rim of Elbow crater at Station 1. The samples were taken as the middle part of a three part radial sample of the ejecta blanket of Elbow crater. The soil and two rock samples were placed in the same sample bag. |
| 15071 |
|
|
|
| 15072 |
|
|
|
| 15073 |
|
|
|
| 15074 |
|
|
|
| 15075 |
|
|
|
| 15076 |
|
|
|
| 15080 |
|
|
|
| 15081 |
|
|
|
| 15082 |
|
|
|
| 15083 |
|
|
|
| 15084 |
|
|
|
| 15085 |
|
|
|
| 15086 |
|
regolith breccia |
Soil 15080 and two cobble-sized rocks, 15085 and 15086 were collected at Station 1 about 65 m east of the Elbow crater ejecta rim. This collection was the farthest from the rim of the three part radial sample of ejecta blanket. In the local area of this sample, the general ejecta blanket appears smooth with scattered cobble sized rocks. A chip from friable breccia 115086 was put through freeze-thaw cycling and ultrasonic vibration to disaggregate, then sieved. |
| 15087 |
|
|
|
| 15088 |
|
|
|
| 15090 |
|
soil |
Samples 15090 through 15093 and 15095 were collected near a large boulder at Station 2. The regolith is notable for its fine texture. Coherent fragments larger than a centimeter in diameter are scattered, and none larger than 10 cm in diameter occur within the immediate sample locality. The soil can be assumed representative of the mature, well gardened regolith composed of St. George crater ejecta plus whatever exotic components have been admixed since the St. George impact. |
| 15091 |
|
|
|
| 15092 |
|
|
|
| 15093 |
|
|
|
| 15095 |
|
|
|
| 15100 |
|
soil |
Sample was collected at the rake sample site 5m east of the large rock at Station 2. The mature fine grained regolith with a few scattered fragments up to about 10 cm in diameter is characteristic of the entire Station 2 area and presumably represents intensely gardened St. George ejecta to which some ejecta from impacts elsewhere in the Apennine Mountains and Imbrium basin have been added. |
| 15101 |
|
|
|
| 15102 |
|
|
|
| 15103 |
|
|
|
| 15104 |
|
|
|
| 15105 |
|
|
|
| 15115 |
|
|
|
| 15116 |
|
|
|
| 15117 |
|
|
|
| 15118 |
|
|
|
| 15119 |
|
|
|
| 15124 |
|
|
|
| 15125 |
|
|
|
| 15135 |
|
|
|
| 15145 |
rake |
breccia |
Olivine-normative mare basalt breccia |
| 15146 |
|
|
|
| 15147 |
|
|
|
| 15148 |
|
|
|
| 15200 |
|
soil |
Soil 15200 and fragments 15201 through 15206 were broken from the 1 m boulder at Station 2. The boulder appears to be an ejecta fragment from a relatively recent impact of another site. The boulder may have impacted at a low angle and rolled uphill onto the rim of its own secondary crater. Sample area is generally flat and free of fragments. Carrier notes that this is an unrepresenative collection of rock chips and loose soils found at the bootm of a sample bag. |
| 15201 |
|
|
|
| 15202 |
|
|
|
| 15203 |
|
|
|
| 15204 |
|
|
|
| 15205 |
|
|
|
| 15206 |
|
|
|
| 15208 |
|
|
|
| 15210 |
|
soil |
Samples 15210 through 15214 are soil samples collected from the rim of the secondary impact crater made by the large rock at Station 2. Samples 15210 through 15214 lie on the south crater rim. 15210, 15220, and 15230 are all representative of the fine grained upper part of the regolith at Station 2. Except for the large boulder itself, the immediate sample area is underlain by sub-centimeter fines with a few scattered consolidated fragments no larger than 10 cm in diameter. |
| 15211 |
|
|
|
| 15212 |
|
|
|
| 15213 |
|
|
|
| 15214 |
|
|
|
| 15220 |
|
soil |
Sample 15220 was collected from the rim of the secondary impact crater made by the large rock at Station 2, about 1 meter northeast of the large rock. Samples 15210, 15220, and 15230 are all representative of the fine grained upper part of the regolith at Station 2. Except for the large boulder itself, the immediate sample area is underlain by sub-centimeter fines with a few scattered consolidated fragments no larger than 10 cm in diameter. |
| 15221 |
|
|
|
| 15222 |
|
|
|
| 15223 |
|
|
|
| 15224 |
|
|
|
| 15230 |
|
soil |
Sample 15230 was collected at Station 2 from underneath the boulder which was rolled over by the crew. All soil samples collected at Station 2, 15210, 15220, and 15230 are representative of the fine grained upper part of the regolith at Station 2. Except for the large boulder itself, the immediate sample area is underlain by the sub centermeter fines whith a few scattered consolidated fragments no longer than 10 cm in diameter. |
| 15231 |
|
|
|
| 15232 |
|
|
|
| 15233 |
|
|
|
| 15234 |
|
|
|
| 15240 |
|
soil |
Samples 15240 through 15245 and 15250 through 15255 were collected from the floor and rim respectively of a 1m crater 20m upslope of the LRV at Station 6. The crew described the crater as a "fresh little crater" and noted a concentration of clods up to 10 cm on an otherwise smooth, fine grained surface. Approximately half of the sample collected here are pieces of glassy breccia >1cm not included as part of the soil (15245). There are only a few fragments >1cm in the area surrounding the crater, and all other craters in the area are subdued. The general slope of the area dips 10 degrees to the north. |
| 15241 |
|
|
|
| 15242 |
|
|
|
| 15243 |
|
|
|
| 15244 |
|
|
|
| 15245 |
|
|
|
| 15250 |
|
soil |
Sample collected from the east rim of a 1m crater approximately 20 m southeast and upslope from the LRV at Station 6. The crater is marked by a concentration of fragments, primarily clods up to 10 cm in diameter, on an otherwise smooth, finely granular surface. It was described by the crew as a "fresh little crater" and it is superposed on the south wall of a subdued 3 m crater which has no visible ejecta material around it. Sample 15240 is collected from the floor of the same 1 m crater. |
| 15251 |
|
|
|
| 15252 |
|
|
|
| 15253 |
|
|
|
| 15254 |
|
|
|
| 15255 |
|
|
|
| 15256 |
|
|
|
| 15257 |
|
|
|
| 15258 |
|
|
|
| 15259 |
|
|
|
| 15260 |
|
soil |
Rock sample 15012 and soil 15260 were collected from the bottom of a trench dug into the south rim of a 12 meter diameter crater 10-15 meters downslope from the LRV at Station 6. Sample 15012 was also collected at the bottom of this trench and placed in a Special Environmental Sample Container. The surface where the trench was dug is littered with fragments ranging from .5 - 2 cm size, but distinctly fewer than on the north rim of the same crater. This may have prompted the astronaut's remarks that the south rim was softer and the north rim more granular. |
| 15261 |
|
|
|
| 15262 |
|
|
|
| 15263 |
|
|
|
| 15264 |
|
|
|
| 15265 |
|
regolith breccia |
Basalt fragment colected from the rim of a 12m, subdued crater at Station 6, the furthest point east sampled on the Appennine front during this mission. This basalt fragment is probaby exotic. Fragment was disaggregated with 4480 cycles of freeze/thaw and sonic disaggregation. |
| 15266 |
|
|
|
| 15267 |
|
|
|
| 15268 |
|
|
|
| 15269 |
|
|
|
| 15270 |
|
soil |
Sample was a large soil sample collected from the compressed wheel track behind the LRV which was parked on a slope of 10-15 degres toward the north. The adjacent undisturbed soil surface appears to be typical of the coarsely granular texture at Station 6. The immediate vicinity is 5-7% covered by centimeter size clods, and is lacking in fresh craters or coherent looking rock fragments. |
| 15271 |
|
|
|
| 15272 |
|
|
|
| 15273 |
|
|
|
| 15274 |
|
|
|
| 15281 |
|
|
|
| 15282 |
|
|
|
| 15283 |
|
|
|
| 15284 |
|
|
|
| 15285 |
|
|
|
| 15286 |
|
|
|
| 15287 |
|
|
|
| 15288 |
|
|
|
| 15289 |
|
|
|
| 15290 |
|
soil |
Soil sample 15290 was collected with fine grained breccia 15295 10 to 15 meters south of the LRV. Soil 15290 includes soil from the immediate area and possible some fragments from 15295 which may have disintegrated in transit and handling into additional fines. This comminution of the breccia enriches the large size fractions of this soil and degrades the pristinity of the grain size distribution. |
| 15291 |
|
|
|
| 15292 |
|
|
|
| 15293 |
|
|
|
| 15294 |
|
|
|
| 15295 |
|
regolith breccia |
Glassy matrix regolith breccia with conspicuous white clasts and vesicular glass veins. |
| 15297 |
|
|
|
| 15298 |
|
regolith breccia |
Regolith breccia with a glassy matrix containing numerous small glass, mineral, and lithic fragments. |
| 15299 |
rock |
regolith breccia |
Regolith Breccia |
| 15300 |
rake |
soil |
15300 was collected at Spur crater at Station 7 to accompany the comprehensive rake sample; 15305 through 15308, and 15315 through 15312. The sample area has moderately abundant small fragments on and near the rim crest of Spur crater. |
| 15301 |
|
|
|
| 15302 |
|
|
|
| 15303 |
|
|
|
| 15304 |
|
|
|
| 15305 |
|
|
|
| 15306 |
|
|
|
| 15307 |
|
|
|
| 15308 |
|
|
|
| 15310 |
|
|
|
| 15311 |
|
|
|
| 15312 |
|
|
|
| 15313 |
|
|
|
| 15314 |
|
|
|
| 15315 |
|
|
|
| 15316 |
|
|
|
| 15317 |
|
|
|
| 15318 |
|
|
|
| 15319 |
|
|
|
| 15320 |
|
|
|
| 15321 |
|
|
|
| 15322 |
|
|
|
| 15323 |
|
|
|
| 15324 |
|
|
|
| 15325 |
|
|
|
| 15326 |
|
|
|
| 15327 |
|
|
|
| 15328 |
|
|
|
| 15329 |
|
|
|
| 15330 |
|
|
|
| 15331 |
|
|
|
| 15332 |
|
|
|
| 15333 |
|
|
|
| 15334 |
|
|
|
| 15335 |
|
|
|
| 15336 |
|
|
|
| 15337 |
|
|
|
| 15338 |
|
|
|
| 15339 |
|
|
|
| 15340 |
|
|
|
| 15341 |
|
|
|
| 15342 |
|
|
|
| 15343 |
|
|
|
| 15344 |
|
|
|
| 15345 |
|
|
|
| 15346 |
|
|
|
| 15347 |
|
|
|
| 15348 |
|
|
|
| 15349 |
|
|
|
| 15350 |
|
|
|
| 15351 |
|
|
|
| 15352 |
|
|
|
| 15353 |
|
|
|
| 15354 |
|
|
|
| 15355 |
|
|
|
| 15356 |
|
|
|
| 15357 |
|
|
|
| 15358 |
|
|
|
| 15359 |
|
|
|
| 15360 |
|
|
|
| 15361 |
|
|
|
| 15362 |
|
|
|
| 15363 |
|
|
|
| 15364 |
|
|
|
| 15365 |
|
|
|
| 15366 |
|
|
|
| 15367 |
|
|
|
| 15368 |
|
|
|
| 15369 |
|
|
|
| 15370 |
|
|
|
| 15371 |
|
|
|
| 15372 |
|
|
|
| 15373 |
|
|
|
| 15374 |
|
|
|
| 15375 |
|
|
|
| 15376 |
|
|
|
| 15377 |
|
|
|
| 15378 |
|
|
|
| 15379 |
|
|
|
| 15380 |
|
|
|
| 15381 |
|
|
|
| 15382 |
|
|
|
| 15383 |
|
|
|
| 15384 |
|
|
|
| 15385 |
|
|
|
| 15386 |
|
|
|
| 15387 |
|
|
|
| 15388 |
|
|
|
| 15389 |
|
|
|
| 15390 |
|
|
|
| 15391 |
|
|
|
| 15392 |
|
|
|
| 15400 |
|
soil |
Soil 15400 and green breccia 15405 were collected from the singular rounded 3 meter long boulder and from an apparent fillet developed high on the south side of the boulder. Relatively few fragments occur in the vicinity of the rock. Most are angular and lie on the fillet, but sparse fragments are found with random distribution in all directions. The samples are probably representative of the boulder and its disintegration products which may typify the composition of its fillet. |
| 15401 |
|
|
|
| 15402 |
|
|
|
| 15403 |
|
|
|
| 15404 |
|
|
|
| 15405 |
|
|
|
| 15410 |
|
soil |
Collected at Station 7 from the summit of the subdued rim crest of Spur Crater. Local surface is moderately well populated with rock fragments up to tens of centimeters across. The sample area is characterized however by the abundance of less than 1 cm size fragments. Several large fragments in the sample have been excluded from the grain size analysis. |
| 15411 |
|
|
|
| 15412 |
|
|
|
| 15413 |
|
|
|
| 15414 |
|
|
|
| 15415 |
rock |
anorthite |
Anorthite. Corse-grained, ferroan crystalline rock with complex cataclastic and metamorphic history. Pale, blocky, angular to subrounded sample, which was originally partly dust-covered. |
| 15416 |
|
|
|
| 15417 |
|
|
|
| 15418 |
|
|
|
| 15419 |
|
|
|
| 15421 |
|
|
|
| 15422 |
|
|
|
| 15423 |
|
|
|
| 15424 |
|
|
|
| 15425 |
soil-general |
|
|
| 15426 |
|
|
|
| 15427 |
|
|
|
| 15430 |
|
soil |
Sample collected at Station 7, 5 meters inside of the north rim of Spur Crater. A clod and a soil were collected together as a surface sample. The clod tended to break down and degrade the size distribution for this soil. Station 7 was moderately well populated with rock fragments up to tens of centimeters across. |
| 15431 |
|
|
|
| 15432 |
|
|
|
| 15433 |
|
|
|
| 15434 |
|
|
|
| 15435 |
|
|
|
| 15436 |
|
|
|
| 15437 |
|
|
|
| 15445 |
|
|
|
| 15455 |
|
|
|
| 15459 |
|
|
|
| 15465 |
|
|
|
| 15466 |
|
glassy impact melt breccia |
|
| 15467 |
|
|
|
| 15468 |
|
|
|
| 15469 |
|
|
|
| 15470 |
|
soil |
Soil 15470 and basalts 15475, 15476 and gabbro 15495 were collected at Station 4, 28 m southeast of the rim crest of Dune crater. The surface surrounding the samples has a moderate cover of fragments, small craters in the sample area are sparse. Two large fragments in the sample were excluded from grain size analysis. |
| 15471 |
|
|
|
| 15472 |
|
|
|
| 15473 |
|
|
|
| 15474 |
|
|
|
| 15475 |
|
|
|
| 15476 |
|
|
|
| 15477 |
|
|
|
| 15478 |
|
|
|
| 15485 |
|
|
|
| 15486 |
|
|
|
| 15487 |
|
|
|
| 15495 |
|
|
|
| 15498 |
rock |
regolith breccia |
A coherent, glassy matrix breccia with components mainly of mare derivation, including basalt fragments and glass. |
| 15499 |
|
|
|
| 15500 |
|
soil |
Collected at Station 9, Scarp crater. This surface sample was collected 10 m from the rim of a 10 meter diameter fresh crater. The surface is saturated with "raindrop depressions" and fragments less than 1 cm in diameter. |
| 15501 |
|
|
|
| 15502 |
|
|
|
| 15503 |
|
|
|
| 15504 |
|
|
|
| 15505 |
|
|
|
| 15506 |
|
|
|
| 15507 |
|
|
|
| 15508 |
|
|
|
| 15514 |
|
|
|
| 15515 |
|
|
|
| 15516 |
|
|
|
| 15528 |
|
|
|
| 15529 |
|
|
|
| 15530 |
|
soil |
15530 was collected with a suite of rocks, fragments, and cores at Station 9A. The soil sample was taken about 20 m east of the rim of Hadley Rille, its exact location has not been identified on the surface photographs. The ground slopes gently from the sample site toward the rim of Hadley Rille; rock fragments on the surface become increasingly abundant as the rille rim is approached. |
| 15531 |
|
|
|
| 15532 |
|
|
|
| 15533 |
|
|
|
| 15534 |
|
|
|
| 15535 |
|
|
|
| 15536 |
|
|
|
| 15537 |
|
|
|
| 15538 |
|
|
|
| 15545 |
|
|
|
| 15546 |
|
|
|
| 15547 |
|
|
|
| 15548 |
|
|
|
| 15555 |
|
|
|
| 15556 |
|
|
|
| 15557 |
|
|
|
| 15558 |
rock |
regolith breccia |
Regolith breccia derived mainly from mare components |
| 15560 |
|
|
|
| 15564 |
|
|
|
| 15565 |
|
regolith breccia |
Regolith breccia fragments ranging from friable to coherent |
| 15568 |
|
|
|
| 15577 |
|
|
|
| 15595 |
|
|
|
| 15596 |
|
|
|
| 15597 |
|
|
|
| 15598 |
|
|
|
| 15600 |
|
soil |
This comprehensive soil was collected at Station 9A to accompany the rake samples 20 m northeast of the rim of Hadley Rille. The surface around the sample is smoth, level, and locally free of rock fragments greater tha 5 cm across. The general vicinity is littered with fragments commonly up to 20 cm across and a few sparse scattered boulders greater than a meter across. |
| 15601 |
|
|
|
| 15602 |
|
|
|
| 15603 |
|
|
|
| 15604 |
|
|
|
| 15605 |
|
|
|
| 15606 |
|
|
|
| 15607 |
|
|
|
| 15608 |
|
|
|
| 15609 |
|
|
|
| 15610 |
|
|
|
| 15611 |
|
|
|
| 15612 |
rake |
|
|
| 15613 |
rake |
|
|
| 15614 |
rake |
|
|
| 15615 |
rake |
|
|
| 15616 |
rake |
|
|
| 15617 |
rake |
|
|
| 15618 |
rake |
|
|
| 15619 |
rake |
|
|
| 15620 |
rake |
|
|
| 15621 |
rake |
|
|
| 15622 |
rake |
|
|
| 15623 |
rake |
|
|
| 15624 |
rake |
|
|
| 15625 |
rake |
|
|
| 15626 |
rake |
|
|
| 15627 |
rake |
|
|
| 15628 |
rake |
|
|
| 15629 |
rake |
|
|
| 15630 |
rake |
|
|
| 15631 |
rake |
|
|
| 15632 |
rake |
|
|
| 15633 |
rake |
|
|
| 15634 |
rake |
|
|
| 15635 |
rake |
|
|
| 15636 |
rake |
|
|
| 15637 |
rake |
|
|
| 15638 |
rake |
|
|
| 15639 |
rake |
|
|
| 15640 |
rake |
|
|
| 15641 |
rake |
|
|
| 15642 |
rake |
|
|
| 15643 |
rake |
|
|
| 15644 |
rake |
|
|
| 15645 |
rake |
|
|
| 15646 |
rake |
|
|
| 15647 |
rake |
|
|
| 15648 |
rake |
|
|
| 15649 |
rake |
|
|
| 15650 |
rake |
|
|
| 15651 |
rake |
|
|
| 15652 |
rake |
|
|
| 15653 |
rake |
|
|
| 15654 |
rake |
|
|
| 15655 |
rake |
|
|
| 15656 |
rake |
|
|
| 15657 |
rake |
|
|
| 15658 |
rake |
|
|
| 15659 |
rake |
|
|
| 15660 |
rake |
|
|
| 15661 |
rake |
|
|
| 15662 |
rake |
|
|
| 15663 |
rake |
|
|
| 15664 |
rake |
|
|
| 15665 |
rake |
|
|
| 15666 |
rake |
|
|
| 15667 |
rake |
|
|
| 15668 |
rake |
|
|
| 15669 |
rake |
|
|
| 15670 |
rake |
|
|
| 15671 |
rake |
|
|
| 15672 |
rake |
|
|
| 15673 |
rake |
|
|
| 15674 |
rake |
|
|
| 15675 |
rake |
|
|
| 15676 |
rake |
|
|
| 15677 |
rake |
|
|
| 15678 |
rake |
|
|
| 15679 |
rake |
|
|
| 15680 |
rake |
|
|
| 15681 |
rake |
|
|
| 15682 |
rake |
|
|
| 15683 |
rake |
|
|
| 15684 |
rake |
|
|
| 15685 |
rake |
|
|
| 15686 |
rake |
|
|
| 15687 |
rake |
|
|
| 15688 |
rake |
|
|
| 15689 |
rake |
|
|
| 15695 |
|
|
|
| 15696 |
|
|
|
| 15697 |
|
|
|
| 15698 |
|
|
|
| 15933 |
|
|
|
| 15952 |
|
|
|
Jump to Apollo:
11
12
14
15
17
|
| Apollo 17 |
| Sample Number |
Sample Type |
Lithology |
Description |
| 17508 |
|
|
|
Jump to Apollo:
11
12
14
15
16
17
|
| Apollo 15 |
| Sample Number |
Sample Type |
Lithology |
Description |
Jump to Apollo:
11
12
14
15
17
|
| Apollo 16 |
| Sample Number |
Sample Type |
Lithology |
Description |
| 36576 |
|
|
|
| 60001 |
core |
|
|
| 60002 |
core |
|
|
| 60003 |
core |
|
|
| 60004 |
core |
|
|
| 60005 |
core |
|
|
| 60006 |
core |
soil |
Deep core contining samples 60001 through 60007 was drilled at the ALSEP site about 175 m southwest of the LM and 25 m south of the ALSEP central station. The sample area is generally flat with blocks up to 10-15 cm abundant. Deep drill area has the least compacted soil and the highest density of craters in the area. Core stems went easily into the surface. |
| 60007 |
core |
|
Deep core contining samples 60001 through 60007 was drilled at the ALSEP site about 175 m southwest of the LM and 25 m south of the ALSEP central station. The sample area is generally flat with blocks up to 10-15 cm abundant. Deep drill area has the least compacted soil and the highest density of craters in the area. Core stems went easily into the surface. |
| 60009 |
core |
soil |
Drive Tube 60009/60010 was taken at Station 10 bout 100 meters southwest of the LM. Samples were taken from the rim of a subdued 60 cm crater. Fragments on the surface are mostly pear sized; none are larger than a few cm. Grain sizes >1mm may have been handled less so friable fragments would be less likely to break apart. |
| 60010 |
core |
soil |
Drive Tube 60009/60010 was taken at Station 10 bout 100 meters southwest of the LM. Samples were taken from the rim of a subdued 60 cm crater. Fragments on the surface are mostly pear sized; none are larger than a few cm. Grain sizes >1mm may have been handled less so friable fragments would be less likely to break apart. |
| 60013 |
core |
|
|
| 60014 |
core |
|
|
| 60015 |
rock |
anorthite |
Coherent, very light gray, shock-melted and cataclastic anorthosite; largely coated with vesicular glass up to 1 cm thick |
| 60016 |
|
fragmental breccia |
This is a friable breccia disaggregated with 1362 freeze - thaw cycles. The breccia was collected 15 meters southwest of the LM. The sample area was fairly flat with fragments up to 20 cm in the area. Craters >3cm are sparse near the sample environment. The surface is relatively unpitted and smooth. |
| 60017 |
|
|
|
| 60018 |
|
|
|
| 60019 |
|
|
|
| 60025 |
rock |
anorthite |
Coarse-grained, moderately shocked, pristine cataclastic ferroan anorthosite |
| 60030 |
|
|
|
| 60031 |
|
|
|
| 60032 |
|
|
|
| 60033 |
|
|
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| 60034 |
|
|
|
| 60035 |
|
|
|
| 60050 |
|
soil |
Scooped soil from the ALSEP site, approximately 170 meters south-southwest of the LM and 50 meters south-southeast of the ALSEP central station. Sample contains friable white breccias described by the crew as "caliche - like." Sample area contains abundant fragments <15cm. The soil is light colored and loose in the crater wall and rim. This soil was taken from the loose material on the rim of a 5 meter crater. |
| 60051 |
|
|
|
| 60052 |
|
|
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| 60053 |
|
|
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| 60054 |
|
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| 60055 |
|
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| 60056 |
|
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| 60057 |
|
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| 60058 |
|
|
|
| 60059 |
|
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|
| 60070 |
|
|
|
| 60075 |
|
|
|
| 60095 |
rock |
green glass vitrophyres |
Fractured spheroid of yellow-green to light brown glass |
| 60110 |
|
|
|
| 60115 |
rock |
breccia |
Glass-bonded polymict breccia |
| 60130 |
|
|
|
| 60135 |
|
|
|
| 60210 |
|
|
|
| 60215 |
|
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| 60230 |
|
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|
| 60235 |
|
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| 60250 |
|
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| 60255 |
|
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|
| 60270 |
|
|
|
| 60275 |
|
|
|
| 60310 |
|
|
|
| 60315 |
|
|
|
| 60330 |
|
|
|
| 60335 |
|
impact melt breccia |
|
| 60500 |
|
soil |
60500 was collected 5 meters southeast of Station 10 approximately 100 meters southwest of the LM. The sample accompanies rake sample 60510. The surrounding area is level with 2-3 cm pebbles exposed on the surface. |
| 60501 |
rake |
soil |
|
| 60502 |
rake |
soil |
|
| 60503 |
rake |
soil |
|
| 60504 |
rake |
soil |
|
| 60510 |
rake |
|
|
| 60511 |
rake |
|
|
| 60512 |
rake |
|
|
| 60513 |
rake |
|
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| 60514 |
rake |
|
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| 60515 |
rake |
|
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| 60516 |
rake |
|
|
| 60517 |
rake |
|
|
| 60518 |
rake |
|
|
| 60519 |
rake |
|
|
| 60520 |
rake |
|
|
| 60521 |
rake |
|
|
| 60522 |
rake |
|
|
| 60523 |
rake |
|
|
| 60524 |
rake |
|
|
| 60525 |
rake |
|
|
| 60526 |
rake |
|
|
| 60527 |
rake |
|
|
| 60528 |
rake |
|
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| 60529 |
rake |
|
|
| 60530 |
rake |
|
|
| 60531 |
rake |
|
|
| 60532 |
rake |
|
|
| 60533 |
rake |
|
|
| 60534 |
rake |
|
|
| 60535 |
rake |
|
|
| 60600 |
rake |
soil |
|
| 60601 |
rake |
soil |
|
| 60602 |
rake |
soil |
|
| 60603 |
rake |
soil |
|
| 60604 |
rake |
soil |
|
| 60610 |
rake |
|
|
| 60611 |
rake |
|
|
| 60612 |
rake |
|
|
| 60613 |
rake |
|
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| 60614 |
rake |
|
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| 60615 |
rake |
|
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| 60616 |
rake |
|
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| 60617 |
rake |
|
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| 60618 |
rake |
|
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| 60619 |
rake |
|
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| 60620 |
|
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| 60621 |
rake |
|
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| 60622 |
rake |
|
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| 60623 |
rake |
|
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| 60624 |
rake |
|
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| 60625 |
rake |
|
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| 60626 |
rake |
|
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| 60627 |
rake |
|
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| 60628 |
rake |
|
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| 60629 |
rake |
|
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| 60630 |
rake |
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| 60631 |
rake |
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| 60632 |
rake |
|
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| 60633 |
rake |
|
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| 60634 |
rake |
|
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| 60635 |
rake |
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| 60636 |
rake |
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| 60637 |
rake |
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| 60638 |
rake |
|
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| 60639 |
rake |
|
|
| 60640 |
rake |
|
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| 60641 |
rake |
|
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| 60642 |
rake |
|
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| 60643 |
rake |
|
|
| 60644 |
rake |
|
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| 60645 |
rake |
|
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| 60646 |
rake |
|
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| 60647 |
rake |
|
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| 60648 |
rake |
|
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| 60649 |
rake |
|
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| 60650 |
rake |
|
|
| 60651 |
rake |
|
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| 60652 |
rake |
|
|
| 60653 |
rake |
|
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| 60654 |
rake |
|
|
| 60655 |
rake |
|
|
| 60656 |
rake |
|
|
| 60657 |
rake |
|
|
| 60658 |
rake |
|
|
| 60659 |
rake |
|
|
| 60660 |
rake |
|
|
| 60661 |
rake |
|
|
| 60662 |
rake |
|
|
| 60663 |
rake |
|
|
| 60664 |
rake |
|
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| 60665 |
rake |
|
|
| 60666 |
rake |
|
|
| 60667 |
rake |
|
|
| 60668 |
rake |
|
|
| 60669 |
rake |
|
|
| 60670 |
rake |
|
|
| 60671 |
rake |
|
|
| 60672 |
rake |
|
|
| 60673 |
rake |
|
|
| 60674 |
rake |
|
|
| 60675 |
rake |
|
|
| 60676 |
rake |
|
|
| 60677 |
rake |
|
|
| 60678 |
rake |
|
|
| 60679 |
rake |
|
|
| 61015 |
|
|
|
| 61016 |
|
|
|
| 61130 |
|
|
|
| 61135 |
|
|
|
| 61140 |
|
soil |
Surface sample collected 30 meters northeast of Plum crater as part of a radial sample sequence (with 61180, 61500, and 61160) Station 1. Site level with fragments <4 cm are common and >4 cm are absent. Craters <50 cm are common and larger ones are sparse, most craters in the area are subdued but one is sharp with a radial raised rim. |
| 61141 |
|
|
|
| 61142 |
|
|
|
| 61143 |
|
|
|
| 61144 |
|
|
|
| 61150 |
|
|
|
| 61155 |
|
|
|
| 61156 |
rock |
impact melt breccia |
Tough, medium gray, poikilitic impact melt that has been thermally metamorphosed |
| 61160 |
|
soil |
This surface sample was collected 10 meters Northeast of the rim of Plum crater as part of a radial sample sequence (with 61180, 61500, and 61140). It was collected from a spot disturbed by a footprint. The site is level with fragments <2 cm common and >2 cm sparse. A .75 m boulder is 2 meters north of the sample. |
| 61161 |
|
|
|
| 61162 |
|
|
|
| 61163 |
|
|
|
| 61164 |
|
|
|
| 61170 |
|
|
|
| 61175 |
|
fragmental breccia |
Friable breccia 61175 was collected with 61160 10 meters northeast of the rim of Plum crater at Station 1. The breccia was disaggregated by 4964 freeze - thaw cycles. There were two 5 cm fragments in the immediate sample area, including sample 61175. Craters greater than 2 meters in the sample area are sparse. |
| 61180 |
|
soil |
Surface sample collected at Station 1 on the rim of Plum crater and on the rim of a smaller, 10 meter crater. Innermost of a radial sample sequence with 61500, 61160, and 61140. The site is level until there is a break at Plum crater, fragments <2 cm are common, >10 cm are sparse. Craters <10 cm are dense and craters <1 meter are common. Some of the larger craters are subdued and some are sharp. |
| 61181 |
|
|
|
| 61182 |
|
|
|
| 61183 |
|
|
|
| 61184 |
|
|
|
| 61190 |
|
|
|
| 61195 |
|
|
|
| 61220 |
|
soil |
Trench samples taken from the east rim of Plum crater at Station 1. 61220 is from the bottom of the trench and 61240 is from the top. This sample includes several rock chips. .5-2 cm fragments are common near the sample site. Soil color is listed as light olive gray but mission transcripts state, "I just had a good scoopful, and I lost it. Let me dig out a little - another little trench. There she be. Coming up all white. That's all that's in there John." |
| 61221 |
soil <1 mm |
soil |
|
| 61222 |
|
|
|
| 61223 |
|
|
|
| 61224 |
|
|
|
| 61225 |
|
|
|
| 61226 |
|
|
|
| 61240 |
|
soil |
Trench samples taken from the east rim of Plum crater at Station 1. 61220 is from the bottom of the trench and 61240 is from the top. This sample includes several rock chips. .5-2 cm fragments are common near the sample site. Soil color is listed as light olive gray but mission transcripts state, "I just had a good scoopful, and I lost it. Let me dig out a little - another little trench. There she be. Coming up all white. That's all that's in there John." |
| 61241 |
|
|
|
| 61242 |
|
|
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| 61243 |
|
|
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| 61244 |
|
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| 61245 |
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| 61246 |
|
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| 61247 |
|
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| 61248 |
|
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| 61249 |
|
|
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| 61255 |
|
|
|
| 61280 |
|
|
|
| 61281 |
|
|
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| 61282 |
|
|
|
| 61283 |
|
|
|
| 61284 |
|
|
|
| 61290 |
|
|
|
| 61295 |
|
|
|
| 61500 |
|
soil |
Surface sample about 30 m east of Flag crater and one about 40 m north-northeast of Plum crater at Station 1. This is part of a radial sample sequence with 61180, 61160, and 61140. The site is level with fragments 1-10 cm sparse and none larger in the area. Craters <3 m are common; most are subdued but one has a sharp rim. |
| 61501 |
|
|
|
| 61502 |
|
|
|
| 61503 |
|
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|
| 61504 |
|
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| 61505 |
|
|
|
| 61510 |
|
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| 61515 |
|
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| 61516 |
|
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| 61517 |
|
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| 61518 |
|
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| 61519 |
|
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| 61525 |
|
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| 61526 |
|
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| 61527 |
|
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| 61528 |
|
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| 61529 |
|
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| 61535 |
|
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| 61536 |
|
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| 61537 |
|
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| 61538 |
|
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| 61539 |
|
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| 61545 |
|
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| 61546 |
|
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| 61547 |
|
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| 61548 |
|
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| 61549 |
|
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| 61555 |
|
|
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| 61556 |
|
|
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| 61557 |
|
|
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| 61558 |
|
|
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| 61559 |
|
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|
| 61565 |
|
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| 61566 |
|
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| 61567 |
|
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|
| 61568 |
|
|
|
| 61569 |
|
|
|
| 61575 |
|
|
|
| 61576 |
|
|
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| 61577 |
|
|
|
| 62230 |
|
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| 62231 |
|
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|
| 62232 |
|
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| 62233 |
|
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| 62234 |
|
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| 62235 |
|
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| 62236 |
|
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| 62237 |
|
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| 62238 |
|
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|
| 62240 |
|
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| 62241 |
|
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| 62242 |
|
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| 62243 |
|
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| 62244 |
|
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| 62245 |
|
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| 62246 |
|
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| 62247 |
|
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| 62248 |
|
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| 62249 |
|
|
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| 62250 |
|
|
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| 62255 |
|
|
|
| 62270 |
|
|
|
| 62275 |
|
|
|
| 62280 |
|
soil |
Soil 62280 and angular coherent breccia 62295 were collected together about 20 meters northwest of the LRV at Station 2. The sample area is on the south slope of Buster crater, fragments are mostly 5 cm or less, and craters are mostly 5-10 cm. There was a light colored material on the surface of the soil, but none of this high albedo material was found below the surface. |
| 62281 |
|
|
|
| 62282 |
|
|
|
| 62283 |
|
|
|
| 62284 |
|
|
|
| 62285 |
|
|
|
| 62286 |
|
|
|
| 62287 |
|
|
|
| 62288 |
|
|
|
| 62289 |
|
|
|
| 62290 |
|
|
|
| 62295 |
|
impact melt breccia |
|
| 62305 |
|
|
|
| 62315 |
|
|
|
| 62566 |
|
|
|
| 62567 |
|
|
|
| 63320 |
|
soil |
Part of a suit of samples collected at Shadow Rock, Station 13. Two soils were collected; 63320 from the shadowed region of Shadow Rock and 63340, a control sample collected below 63320. On the southeast slope on the flank of North Ray crater, the sample area has abundant 5-10 cm cobbles with scattered blocks up to 5 meters in size. Abundant .5-1 meter craters in the immediate area. 63320 is probably the fine grained ejecta from North Ray crater. If Shadow Rock was ejected from North Ray crater, these samples have been virtually undisturbed since the North Ray event. |
| 63321 |
|
soil |
|
| 63322 |
|
soil |
|
| 63323 |
|
soil |
|
| 63324 |
|
soil |
|
| 63335 |
|
|
|
| 63340 |
|
soil |
Part of a suit of samples collected at Shadow Rock, Station 13. Two soils were collected; 63320 from the shadowed region of Shadow Rock and 63340, a control sample collected below 63320. On the southeast slope on the flank of North Ray crater, the sample area has abundant 5-10 cm cobbles with scattered blocks up to 5 meters in size. Abundant .5-1 meter craters in the immediate area. 63320 is probably the fine grained ejecta from North Ray crater. If Shadow Rock was ejected from North Ray crater, these samples have been virtually undisturbed since the North Ray event. |
| 63341 |
|
soil |
|
| 63342 |
|
soil |
|
| 63343 |
|
soil |
|
| 63344 |
|
soil |
|
| 63355 |
|
|
|
| 63500 |
|
soil |
This reference soil collected at Station 13, 5 meters west of Shadow Rock refers to rake sample 63510 collected at the same site and shadow soils 63320 and 63340 collected under the overhang of Shadow Rock. The sample area contains small rocks (2-10 cm) which cover 5% of the surface, fines are less compacted than soil at North Ray crater. Random 1-2 meter fresh to subdued craters are found in the local area. No crater is recognizable in the immediate sample area. |
| 63501 |
|
|
|
| 63502 |
|
|
|
| 63503 |
|
|
|
| 63504 |
|
|
|
| 63505 |
|
|
|
| 63506 |
|
|
|
| 63507 |
|
|
|
| 63508 |
|
|
|
| 63509 |
|
|
|
| 63515 |
|
|
|
| 63520 |
rake |
|
|
| 63521 |
rake |
|
|
| 63522 |
rake |
|
|
| 63523 |
rake |
|
|
| 63524 |
rake |
|
|
| 63525 |
rake |
|
|
| 63526 |
rake |
|
|
| 63527 |
rake |
|
|
| 63528 |
rake |
|
|
| 63529 |
rake |
|
|
| 63530 |
rake |
|
|
| 63531 |
rake |
|
|
| 63532 |
rake |
|
|
| 63533 |
rake |
|
|
| 63534 |
rake |
|
|
| 63535 |
rake |
|
|
| 63536 |
rake |
|
|
| 63537 |
rake |
|
|
| 63538 |
rake |
|
|
| 63539 |
rake |
|
|
| 63540 |
rake |
|
|
| 63541 |
rake |
|
|
| 63542 |
rake |
|
|
| 63543 |
rake |
|
|
| 63544 |
rake |
|
|
| 63545 |
rake |
|
|
| 63546 |
rake |
|
|
| 63547 |
rake |
|
|
| 63548 |
rake |
|
|
| 63549 |
rake |
|
|
| 63550 |
rake |
|
|
| 63551 |
rake |
|
|
| 63552 |
rake |
|
|
| 63553 |
rake |
|
|
| 63554 |
rake |
|
|
| 63555 |
rake |
|
|
| 63556 |
rake |
|
|
| 63557 |
rake |
|
|
| 63558 |
rake |
|
|
| 63559 |
rake |
|
|
| 63560 |
rake |
|
|
| 63561 |
rake |
|
|
| 63562 |
rake |
|
|
| 63563 |
rake |
|
|
| 63564 |
rake |
|
|
| 63565 |
rake |
|
|
| 63566 |
rake |
|
|
| 63567 |
rake |
|
|
| 63568 |
rake |
|
|
| 63569 |
rake |
|
|
| 63570 |
rake |
|
|
| 63571 |
rake |
|
|
| 63572 |
rake |
|
|
| 63573 |
rake |
|
|
| 63574 |
rake |
|
|
| 63575 |
rake |
|
|
| 63576 |
rake |
|
|
| 63577 |
rake |
|
|
| 63578 |
rake |
|
|
| 63579 |
rake |
|
|
| 63580 |
rake |
|
|
| 63581 |
rake |
|
|
| 63582 |
rake |
|
|
| 63583 |
rake |
|
|
| 63584 |
rake |
|
|
| 63585 |
rake |
|
|
| 63586 |
rake |
|
|
| 63587 |
rake |
|
|
| 63588 |
rake |
|
|
| 63589 |
rake |
|
|
| 63590 |
rake |
|
|
| 63591 |
rake |
|
|
| 63592 |
rake |
|
|
| 63593 |
rake |
|
|
| 63594 |
rake |
|
|
| 63595 |
rake |
|
|
| 63596 |
rake |
|
|
| 63597 |
rake |
|
|
| 63598 |
rake |
|
|
| 63756 |
|
|
|
| 64001 |
core |
soil |
Core drilled on Stone Mountain at Station 4, within one crater diameter of a 15 meter subdued doublet crater. The deep sections of the core may contain the best samples of typical Descartes material. The sample area has a 10-15 degree slope to the northwest. There are a few scattered cobbles 5-10 cm. Scattered craters .5 to several meters in diameter are common in the general area, there is a .5 meter crater just southwest of the drive tube. |
| 64002 |
core |
soil |
Drive tube 64001 / 64002 collected on Stone Mountain at Station 4, within one crater diameter of a 15 meter subdued doublet crater. The deep sections of the core may contain the best samples of typical Descartes material. The sample area has a 10-15 degree slope to the northwest. There are a few scattered cobbles 5-10 cm. Scattered craters .5 to several meters in diameter are common in the general area, there is a .5 meter crater just southwest of the drive tube. |
| 64420 |
|
soil |
Soil 64420 was collected with breccia 64475 at Station 4A near Cinco B crater, 5 meters from the LRV on the floor of a subdued 15 meter crater. The soil was taken from the bottom of a 25 cm trench. At the sample area, 5-10 cm pebbles are abundant, 20-40 cm cobbles are common and meter size blocks are sparsely scattered. Scattered craters up to several meters in size are common in the general area. This regolith is probably South Ray ejecta mixed with underlying Descartes material. |
| 64421 |
|
|
|
| 64422 |
|
|
|
| 64423 |
|
|
|
| 64424 |
|
|
|
| 64425 |
|
|
|
| 64430 |
|
|
|
| 64435 |
|
|
|
| 64450 |
|
|
|
| 64455 |
|
impact melt breccia |
|
| 64470 |
|
|
|
| 64475 |
|
|
|
| 64476 |
|
|
|
| 64477 |
|
|
|
| 64478 |
|
|
|
| 64500 |
rake |
soil |
Soil 64500 and rake 64510 were collected at Station 4A in the vicinity of Cinco B crater, near the rim of a subdued 15 meter crater. The sample area slopes 10-15 degrees to the northwest off Stone Mountain, surface fragments up to 10 cm are abundant, up to 40 cm are common, up to 1 meter sparse. Scattered craters .5 to several meters are in the general area, very subdued and barely visible smaller craters are in the local area. The gray surface is underlain by a white layer. |
| 64501 |
rake |
|
|
| 64502 |
rake |
|
|
| 64503 |
rake |
|
|
| 64504 |
rake |
|
|
| 64505 |
rake |
|
|
| 64506 |
rake |
|
|
| 64507 |
rake |
|
|
| 64508 |
rake |
|
|
| 64509 |
rake |
|
|
| 64510 |
rake |
|
|
| 64511 |
rake |
|
|
| 64512 |
rake |
|
|
| 64513 |
rake |
|
|
| 64514 |
rake |
|
|
| 64515 |
rake |
|
|
| 64516 |
rake |
|
|
| 64517 |
rake |
|
|
| 64518 |
rake |
|
|
| 64519 |
rake |
|
|
| 64520 |
rake |
|
|
| 64521 |
rake |
|
|
| 64522 |
rake |
|
|
| 64523 |
rake |
|
|
| 64525 |
rake |
|
|
| 64530 |
rake |
|
|
| 64531 |
rake |
|
|
| 64532 |
rake |
|
|
| 64533 |
rake |
|
|
| 64534 |
rake |
|
|
| 64535 |
rake |
|
|
| 64536 |
rake |
|
|
| 64537 |
rake |
|
|
| 64538 |
rake |
|
|
| 64539 |
rake |
|
|
| 64540 |
rake |
|
|
| 64541 |
rake |
|
|
| 64542 |
rake |
|
|
| 64543 |
rake |
|
|
| 64544 |
rake |
|
|
| 64545 |
rake |
|
|
| 64546 |
rake |
|
|
| 64547 |
rake |
|
|
| 64548 |
rake |
|
|
| 64549 |
rake |
|
|
| 64550 |
rake |
|
|
| 64551 |
rake |
|
|
| 64552 |
rake |
|
|
| 64553 |
rake |
|
|
| 64554 |
rake |
|
|
| 64555 |
rake |
|
|
| 64556 |
rake |
|
|
| 64557 |
rake |
|
|
| 64558 |
rake |
|
|
| 64559 |
rake |
|
|
| 64560 |
rake |
|
|
| 64561 |
rake |
|
|
| 64562 |
rake |
|
|
| 64563 |
rake |
|
|
| 64564 |
rake |
|
|
| 64565 |
rake |
|
|
| 64566 |
rake |
|
|
| 64567 |
rake |
|
|
| 64568 |
rake |
|
|
| 64569 |
rake |
|
|
| 64570 |
rake |
|
|
| 64571 |
rake |
|
|
| 64572 |
rake |
|
|
| 64573 |
rake |
|
|
| 64574 |
rake |
|
|
| 64575 |
rake |
|
|
| 64576 |
rake |
|
|
| 64577 |
rake |
|
|
| 64578 |
rake |
|
|
| 64579 |
rake |
|
|
| 64580 |
rake |
|
|
| 64581 |
rake |
|
|
| 64582 |
rake |
|
|
| 64583 |
rake |
|
|
| 64584 |
rake |
|
|
| 64585 |
rake |
|
|
| 64586 |
rake |
|
|
| 64587 |
rake |
|
|
| 64588 |
rake |
|
|
| 64589 |
rake |
|
|
| 64800 |
|
soil |
Surface soil 64800 accompanies rake 64810, collected at Station 4B on the rim of a 20 meter crater. Blocks and cobbles cover 80-90% of the northeast wall of the main crater, elsewhere the surface is relatively smooth with scattered cobbles. The fines are loose, numerous small crates are found in the sample area. |
| 64801 |
|
|
|
| 64802 |
|
|
|
| 64803 |
|
|
|
| 64804 |
|
|
|
| 64810 |
rake |
|
|
| 64811 |
rake |
|
|
| 64812 |
rake |
|
|
| 64813 |
rake |
|
|
| 64814 |
rake |
|
|
| 64815 |
rake |
|
|
| 64816 |
rake |
|
|
| 64817 |
rake |
|
|
| 64818 |
rake |
|
|
| 64819 |
rake |
|
|
| 64820 |
rake |
|
|
| 64821 |
rake |
|
|
| 64822 |
rake |
|
|
| 64823 |
rake |
|
|
| 64824 |
rake |
|
|
| 64825 |
rake |
|
|
| 64826 |
rake |
|
|
| 64827 |
rake |
|
|
| 64828 |
rake |
|
|
| 64829 |
rake |
|
|
| 64830 |
rake |
|
|
| 64831 |
rake |
|
|
| 64832 |
rake |
|
|
| 64833 |
rake |
|
|
| 64834 |
rake |
|
|
| 64835 |
rake |
|
|
| 64836 |
rake |
|
|
| 64837 |
rake |
|
|
| 65015 |
rock |
other |
Poikilitic Impact Melt |
| 65016 |
|
|
|
| 65030 |
|
|
|
| 65035 |
|
|
|
| 65050 |
|
|
|
| 65055 |
|
impact melt breccia |
|
| 65056 |
|
|
|
| 65070 |
|
|
|
| 65075 |
|
|
|
| 65090 |
|
|
|
| 65095 |
|
|
|
| 65315 |
|
|
|
| 65325 |
|
|
|
| 65326 |
rake |
anorthite |
Moderately coherent cataclastic anorthosite |
| 65327 |
|
|
|
| 65328 |
|
|
|
| 65329 |
|
|
|
| 65335 |
|
|
|
| 65336 |
|
|
|
| 65337 |
|
|
|
| 65338 |
|
|
|
| 65339 |
|
|
|
| 65345 |
|
|
|
| 65346 |
|
|
|
| 65347 |
|
|
|
| 65348 |
|
|
|
| 65349 |
|
|
|
| 65355 |
|
|
|
| 65356 |
|
|
|
| 65357 |
rake |
impact melt breccia |
Light gray, coherent, poikilitic impact melt |
| 65358 |
|
|
|
| 65359 |
|
|
|
| 65365 |
|
|
|
| 65366 |
|
|
|
| 65500 |
|
soil |
Soil 65500 accompanies rake sample 65510 collected at Station 5 near the rim of a 20 meter crater. The sample area has no blocks larger tha 30 cm, it is a mostly sandy surface. The fines are loose with a gray surface and whitish subsurface. Numerous small craters are superposed on the 20 meter crater. Friable clods are included in the sample. |
| 65501 |
rake |
|
|
| 65502 |
rake |
|
|
| 65503 |
rake |
|
|
| 65504 |
rake |
|
|
| 65510 |
rake |
|
|
| 65511 |
rake |
|
|
| 65512 |
rake |
|
|
| 65513 |
rake |
|
|
| 65514 |
rake |
|
|
| 65515 |
rake |
|
|
| 65516 |
rake |
|
|
| 65517 |
rake |
|
|
| 65518 |
rake |
|
|
| 65519 |
rake |
|
|
| 65520 |
rake |
|
|
| 65521 |
rake |
|
|
| 65522 |
rake |
|
|
| 65523 |
rake |
|
|
| 65524 |
rake |
|
|
| 65525 |
rake |
|
|
| 65526 |
rake |
|
|
| 65527 |
rake |
|
|
| 65528 |
rake |
|
|
| 65529 |
rake |
|
|
| 65530 |
rake |
|
|
| 65531 |
rake |
|
|
| 65532 |
rake |
|
|
| 65533 |
rake |
|
|
| 65534 |
rake |
|
|
| 65535 |
rake |
|
|
| 65536 |
rake |
|
|
| 65537 |
rake |
|
|
| 65538 |
rake |
|
|
| 65539 |
rake |
|
|
| 65540 |
rake |
|
|
| 65541 |
rake |
|
|
| 65542 |
rake |
|
|
| 65543 |
rake |
|
|
| 65544 |
rake |
|
|
| 65545 |
rake |
|
|
| 65546 |
rake |
|
|
| 65547 |
rake |
|
|
| 65548 |
rake |
|
|
| 65549 |
rake |
|
|
| 65550 |
rake |
|
|
| 65551 |
rake |
|
|
| 65552 |
rake |
|
|
| 65553 |
rake |
|
|
| 65554 |
rake |
|
|
| 65555 |
rake |
|
|
| 65556 |
rake |
|
|
| 65557 |
rake |
|
|
| 65558 |
rake |
|
|
| 65559 |
rake |
|
|
| 65560 |
rake |
|
|
| 65561 |
rake |
|
|
| 65562 |
rake |
|
|
| 65563 |
rake |
|
|
| 65564 |
rake |
|
|
| 65565 |
rake |
|
|
| 65566 |
rake |
|
|
| 65567 |
rake |
|
|
| 65568 |
rake |
|
|
| 65569 |
rake |
|
|
| 65570 |
rake |
|
|
| 65571 |
rake |
|
|
| 65572 |
rake |
|
|
| 65573 |
rake |
|
|
| 65574 |
rake |
|
|
| 65575 |
rake |
|
|
| 65576 |
rake |
|
|
| 65577 |
|
|
|
| 65578 |
rake |
|
|
| 65579 |
rake |
|
|
| 65580 |
rake |
|
|
| 65581 |
rake |
|
|
| 65582 |
rake |
|
|
| 65583 |
rake |
|
|
| 65584 |
rake |
|
|
| 65585 |
rake |
|
|
| 65586 |
rake |
|
|
| 65587 |
rake |
|
|
| 65588 |
rake |
|
|
| 65700 |
|
soil |
65700 and 65900 are surface soils to accompany the rake samples at Station 5. Samples were collected on the interior wall of a 20 meter crater, very close to the rim. The sample area has a mostly sandy surface with no large blocks nearby. Fines in the area are extremely loose. |
| 65702 |
rake |
|
|
| 65703 |
rake |
|
|
| 65704 |
rake |
|
|
| 65710 |
rake |
|
|
| 65711 |
rake |
|
|
| 65712 |
rake |
|
|
| 65713 |
rake |
|
|
| 65714 |
rake |
|
|
| 65715 |
rake |
|
|
| 65716 |
rake |
|
|
| 65717 |
rake |
|
|
| 65718 |
rake |
|
|
| 65719 |
rake |
|
|
| 65720 |
rake |
|
|
| 65721 |
rake |
|
|
| 65722 |
rake |
|
|
| 65723 |
rake |
|
|
| 65724 |
rake |
|
|
| 65725 |
rake |
|
|
| 65726 |
rake |
|
|
| 65727 |
rake |
|
|
| 65728 |
rake |
|
|
| 65729 |
rake |
|
|
| 65730 |
rake |
|
|
| 65731 |
rake |
|
|
| 65732 |
rake |
|
|
| 65733 |
rake |
|
|
| 65734 |
rake |
|
|
| 65735 |
rake |
|
|
| 65736 |
rake |
|
|
| 65737 |
rake |
|
|
| 65738 |
rake |
|
|
| 65739 |
rake |
|
|
| 65740 |
rake |
|
|
| 65741 |
rake |
|
|
| 65742 |
rake |
|
|
| 65743 |
rake |
|
|
| 65744 |
rake |
|
|
| 65745 |
rake |
|
|
| 65746 |
rake |
|
|
| 65747 |
rake |
|
|
| 65748 |
rake |
|
|
| 65749 |
rake |
|
|
| 65750 |
rake |
|
|
| 65751 |
rake |
|
|
| 65752 |
rake |
|
|
| 65753 |
rake |
|
|
| 65754 |
rake |
|
|
| 65755 |
rake |
|
|
| 65756 |
rake |
|
|
| 65757 |
rake |
|
|
| 65758 |
rake |
|
|
| 65759 |
rake |
|
|
| 65760 |
rake |
|
|
| 65761 |
rake |
|
|
| 65762 |
rake |
|
|
| 65763 |
rake |
|
|
| 65764 |
rake |
|
|
| 65765 |
rake |
|
|
| 65766 |
rake |
|
|
| 65767 |
rake |
|
|
| 65768 |
rake |
|
|
| 65769 |
rake |
|
|
| 65770 |
rake |
|
|
| 65771 |
rake |
|
|
| 65772 |
rake |
|
|
| 65773 |
rake |
|
|
| 65774 |
rake |
|
|
| 65775 |
rake |
|
|
| 65776 |
rake |
|
|
| 65777 |
rake |
|
|
| 65778 |
rake |
|
|
| 65779 |
rake |
|
|
| 65780 |
rake |
|
|
| 65781 |
rake |
|
|
| 65782 |
rake |
|
|
| 65783 |
rake |
|
|
| 65784 |
rake |
|
|
| 65785 |
rake |
|
|
| 65786 |
rake |
|
|
| 65787 |
rake |
|
|
| 65788 |
rake |
|
|
| 65789 |
rake |
|
|
| 65790 |
rake |
|
|
| 65791 |
rake |
|
|
| 65792 |
rake |
|
|
| 65793 |
rake |
|
|
| 65794 |
rake |
|
|
| 65795 |
rake |
|
|
| 65900 |
|
soil |
65900 is a surface soil to accompany the rake samples at Station 5. Samples were collected on the interior wall of a 20 meter crater, very close to the rim. The sample area has a mostly sandy surface with no large blocks nearby. Fines in the area are extremely loose. |
| 65901 |
|
|
|
| 65903 |
|
|
|
| 65904 |
|
|
|
| 65905 |
|
|
|
| 65906 |
|
|
|
| 65907 |
|
|
|
| 65915 |
|
|
|
| 65916 |
|
|
|
| 65920 |
rake |
|
|
| 65925 |
rake |
|
|
| 65926 |
rake |
|
|
| 65927 |
rake |
|
|
| 66030 |
|
soil |
66030 is a soil collected with an 8 cm breccia. It is supposed that the breccia is local ejecta, but the source crater is not obvious. Both the soil and the breccia were on a 10 meter crater rim at Station 6 near the base of Stone Mountain. In the sample area, 15-30 cm blocks are relatively common, soil is relatively firm compared to the looser regolith at Stations 4 and 5. Craters in the area are mostly <5 meters. |
| 66031 |
|
|
|
| 66032 |
|
|
|
| 66033 |
|
|
|
| 66034 |
|
|
|
| 66035 |
|
|
|
| 66036 |
|
|
|
| 66037 |
|
|
|
| 66040 |
|
soil |
Soils 66040 and 66030 and breccia 66055 were collected at the same location at Station 6. It is supposed that the breccia is local ejecta, but the source crater is not obvious. Both the soils and the breccia were on a 10 meter crater rim near the base of Stone Mountain. In the sample area 15-30 cm blocks are relatively common, soil is relatively firm compared to the looser regolith at Stations 4 and 5. Craters in the area are mostly <5 meters. |
| 66041 |
|
|
|
| 66042 |
|
|
|
| 66043 |
|
|
|
| 66044 |
|
|
|
| 66050 |
|
|
|
| 66055 |
|
|
|
| 66070 |
|
|
|
| 66075 |
|
fragmental breccia |
Friable breccia collected on the southwest wall of a 10 meter crater at the base of Stone Mountain, at Station 6. The breccia was disaggregated with 4400 freeze / thaw cycles (but no sonic disaggregation). The site slopes 10 degrees to the northwest, with scattered fragments up to 50 cm in the nearby area. .5-1 meter craters are common at the collection site. |
| 66080 |
|
soil |
Soil 66080 collected with fragment 66085 were taken at Station 6 along the west rim of a 10 meter diameter crater at the base of Stone Mountain. Cobbles 5-15 cm are widely distributed in the surrounding area with a few scattered blocks up to 50 cm. Craters <5 meters are common. The soil collected is unique for that site, it is described as an indurated clod of white impact ejecta; possibly from South Ray crater. |
| 66081 |
|
|
|
| 66082 |
|
|
|
| 66083 |
|
|
|
| 66084 |
|
|
|
| 66085 |
|
|
|
| 66086 |
|
|
|
| 66090 |
|
|
|
| 66095 |
|
|
|
| 66236 |
|
|
|
| 67015 |
|
|
|
| 67016 |
|
|
|
| 67020 |
|
|
|
| 67025 |
|
|
|
| 67035 |
rock |
fragmental breccia |
Very friable, light matrix breccia |
| 67050 |
|
|
|
| 67055 |
|
|
|
| 67070 |
|
|
|
| 67075 |
|
|
|
| 67090 |
|
|
|
| 67095 |
|
impact melt breccia |
|
| 67110 |
|
|
|
| 67115 |
|
|
|
| 67215 |
|
|
|
| 67235 |
|
|
|
| 67410 |
|
|
|
| 67415 |
|
|
|
| 67430 |
|
|
|
| 67435 |
|
|
|
| 67450 |
|
|
|
| 67455 |
|
|
|
| 67460 |
|
|
|
| 67461 |
|
|
|
| 67462 |
|
|
|
| 67463 |
|
|
|
| 67464 |
|
|
|
| 67475 |
|
|
|
| 67480 |
|
soil |
Reference soil 67840 accompanies rake sample 67510; both were taken on the southeast rim of North Ray crater, at Station 11 in the area of the white breccia boulders. The sample area is in a local north-south swale, the surface is soft and fine; fragments greater than 10 cm are sparse and the crew reported "sinking in on the slopes about 6 inches." |
| 67481 |
|
|
|
| 67482 |
|
|
|
| 67483 |
|
|
|
| 67484 |
|
|
|
| 67485 |
|
|
|
| 67486 |
|
|
|
| 67487 |
|
|
|
| 67488 |
|
|
|
| 67489 |
|
|
|
| 67495 |
|
|
|
| 67510 |
rake |
|
|
| 67511 |
rake |
|
|
| 67512 |
rake |
|
|
| 67513 |
rake |
|
|
| 67514 |
rake |
|
|
| 67515 |
rake |
|
|
| 67516 |
rake |
|
|
| 67517 |
rake |
|
|
| 67518 |
rake |
|
|
| 67519 |
rake |
|
|
| 67520 |
rake |
|
|
| 67521 |
rake |
|
|
| 67522 |
rake |
|
|
| 67523 |
rake |
|
|
| 67524 |
rake |
|
|
| 67525 |
rake |
|
|
| 67526 |
rake |
|
|
| 67527 |
rake |
|
|
| 67528 |
rake |
|
|
| 67529 |
rake |
|
|
| 67530 |
rake |
|
|
| 67531 |
rake |
|
|
| 67532 |
rake |
|
|
| 67533 |
rake |
|
|
| 67534 |
rake |
|
|
| 67535 |
rake |
|
|
| 67536 |
rake |
|
|
| 67537 |
rake |
|
|
| 67538 |
rake |
|
|
| 67539 |
rake |
|
|
| 67540 |
rake |
|
|
| 67541 |
rake |
|
|
| 67542 |
rake |
|
|
| 67543 |
rake |
|
|
| 67544 |
rake |
|
|
| 67545 |
rake |
|
|
| 67546 |
rake |
|
|
| 67547 |
rake |
|
|
| 67548 |
rake |
|
|
| 67549 |
rake |
|
|
| 67550 |
rake |
|
|
| 67551 |
rake |
|
|
| 67552 |
rake |
|
|
| 67553 |
rake |
|
|
| 67554 |
rake |
|
|
| 67555 |
rake |
|
|
| 67556 |
rake |
|
|
| 67557 |
rake |
|
|
| 67558 |
rake |
|
|
| 67559 |
rake |
|
|
| 67560 |
rake |
|
|
| 67561 |
rake |
|
|
| 67562 |
rake |
|
|
| 67563 |
rake |
|
|
| 67564 |
rake |
|
|
| 67565 |
rake |
|
|
| 67566 |
rake |
|
|
| 67567 |
rake |
|
|
| 67568 |
rake |
|
|
| 67569 |
rake |
|
|
| 67570 |
rake |
|
|
| 67571 |
rake |
|
|
| 67572 |
rake |
|
|
| 67573 |
rake |
|
|
| 67574 |
rake |
|
|
| 67575 |
rake |
|
|
| 67576 |
rake |
|
|
| 67600 |
rake |
soil |
Reference soil 67600, rake soil 67610, and fragment 67605 were all taken on the southeast rim of North Ray crater. The sample area is in the bottom of "Little Hollow" a few meters from the white breccia boulder. Fragments 10 cm or smaller are common here, no craters are visible and the surface is moderately firm, boot prints are often deeper than 1 cm at this site. The soil is probably derived from North Ray crater ejecta. |
| 67601 |
rake |
soil |
|
| 67602 |
rake |
soil |
|
| 67603 |
rake |
soil |
|
| 67604 |
rake |
soil |
|
| 67605 |
rake |
soil |
|
| 67610 |
rake |
|
|
| 67611 |
rake |
|
|
| 67612 |
rake |
|
|
| 67613 |
rake |
|
|
| 67614 |
rake |
|
|
| 67615 |
rake |
|
|
| 67616 |
rake |
|
|
| 67617 |
rake |
|
|
| 67618 |
rake |
|
|
| 67619 |
rake |
|
|
| 67620 |
rake |
|
|
| 67621 |
rake |
|
|
| 67622 |
rake |
|
|
| 67623 |
rake |
|
|
| 67624 |
rake |
|
|
| 67625 |
rake |
|
|
| 67626 |
rake |
|
|
| 67627 |
rake |
|
|
| 67628 |
rake |
|
|
| 67629 |
rake |
|
|
| 67630 |
rake |
|
|
| 67631 |
rake |
|
|
| 67632 |
rake |
|
|
| 67633 |
rake |
|
|
| 67634 |
rake |
|
|
| 67635 |
rake |
|
|
| 67636 |
rake |
|
|
| 67637 |
rake |
|
|
| 67638 |
rake |
|
|
| 67639 |
rake |
|
|
| 67640 |
rake |
|
|
| 67641 |
rake |
|
|
| 67642 |
rake |
|
|
| 67643 |
rake |
|
|
| 67644 |
rake |
|
|
| 67645 |
rake |
|
|
| 67646 |
rake |
|
|
| 67647 |
rake |
|
|
| 67648 |
rake |
|
|
| 67649 |
rake |
|
|
| 67650 |
rake |
|
|
| 67651 |
rake |
|
|
| 67652 |
rake |
|
|
| 67653 |
rake |
|
|
| 67654 |
rake |
|
|
| 67655 |
rake |
|
|
| 67656 |
rake |
|
|
| 67657 |
rake |
|
|
| 67658 |
rake |
|
|
| 67659 |
rake |
|
|
| 67660 |
rake |
|
|
| 67661 |
rake |
|
|
| 67662 |
rake |
|
|
| 67663 |
rake |
|
|
| 67664 |
rake |
|
|
| 67665 |
rake |
|
|
| 67666 |
rake |
|
|
| 67667 |
rake |
|
|
| 67668 |
rake |
|
|
| 67669 |
rake |
|
|
| 67670 |
rake |
|
|
| 67671 |
rake |
|
|
| 67672 |
rake |
|
|
| 67673 |
rake |
|
|
| 67674 |
rake |
|
|
| 67675 |
rake |
|
|
| 67676 |
rake |
|
|
| 67685 |
|
|
|
| 67686 |
|
|
|
| 67687 |
|
|
|
| 67688 |
|
|
|
| 67695 |
|
|
|
| 67696 |
|
|
|
| 67697 |
|
|
|
| 67700 |
rake |
soil |
Reference soil 67700, fragments in the soil numbered 67705 through 67708, and rake sample 67710 were taken at Station 11 at the southeast rim of North Ray crater. The surface gently slopes to the northeast, fragments smaller than 10 cm are common. The crew described the surface as hard, possibly on top of a large white rock. The rake would not penetrate. There is one 50 cm secondary crater in the center of the rake sample. |
| 67701 |
rake |
soil |
|
| 67702 |
rake |
soil |
|
| 67703 |
rake |
soil |
|
| 67704 |
rake |
soil |
|
| 67705 |
rake |
soil |
|
| 67706 |
rake |
soil |
|
| 67707 |
rake |
soil |
|
| 67708 |
rake |
soil |
|
| 67710 |
rake |
soil |
Reference soil 67700, fragments in the soil numbered 67705 through 67708, and rake sample 67710 were taken at Station 11 at the southeast rim of North Ray crater. The surface gently slopes to the northeast, fragments smaller than 10 cm are common. The crew described the surface as hard, possibly on top of a large white rock. The rake would not penetrate. There is one 50 cm secondary crater in the center of the rake sample. |
| 67711 |
rake |
|
|
| 67712 |
rake |
soil |
|
| 67713 |
rake |
soil |
|
| 67714 |
rake |
soil |
|
| 67715 |
rake |
|
|
| 67716 |
rake |
|
|
| 67717 |
rake |
|
|
| 67718 |
rake |
|
|
| 67719 |
rake |
|
|
| 67720 |
rake |
|
|
| 67721 |
rake |
|
|
| 67722 |
rake |
|
|
| 67723 |
rake |
|
|
| 67724 |
rake |
|
|
| 67725 |
rake |
|
|
| 67726 |
rake |
|
|
| 67727 |
rake |
|
|
| 67728 |
rake |
|
|
| 67729 |
rake |
|
|
| 67730 |
rake |
|
|
| 67731 |
rake |
|
|
| 67732 |
rake |
|
|
| 67733 |
rake |
|
|
| 67734 |
rake |
|
|
| 67735 |
rake |
|
|
| 67736 |
rake |
|
|
| 67737 |
rake |
|
|
| 67738 |
rake |
|
|
| 67739 |
rake |
|
|
| 67740 |
rake |
|
|
| 67741 |
rake |
|
|
| 67742 |
rake |
|
|
| 67743 |
rake |
|
|
| 67744 |
rake |
|
|
| 67745 |
rake |
|
|
| 67746 |
rake |
|
|
| 67747 |
rake |
|
|
| 67748 |
rake |
|
|
| 67749 |
rake |
|
|
| 67750 |
rake |
|
|
| 67751 |
rake |
|
|
| 67752 |
rake |
|
|
| 67753 |
rake |
|
|
| 67754 |
rake |
|
|
| 67755 |
rake |
|
|
| 67756 |
rake |
|
|
| 67757 |
rake |
|
|
| 67758 |
rake |
|
|
| 67759 |
rake |
|
|
| 67760 |
rake |
|
|
| 67761 |
rake |
|
|
| 67762 |
rake |
|
|
| 67763 |
rake |
|
|
| 67764 |
rake |
|
|
| 67765 |
rake |
|
|
| 67766 |
rake |
|
|
| 67767 |
rake |
|
|
| 67768 |
rake |
|
|
| 67769 |
rake |
|
|
| 67770 |
rake |
|
|
| 67771 |
rake |
|
|
| 67772 |
rake |
|
|
| 67773 |
rake |
|
|
| 67774 |
rake |
|
|
| 67775 |
rake |
|
|
| 67776 |
rake |
|
|
| 67910 |
|
|
|
| 67915 |
|
|
|
| 67930 |
|
|
|
| 67935 |
|
|
|
| 67936 |
|
|
|
| 67937 |
|
|
|
| 67940 |
|
soil |
Soil 67940 came from the "east-west crack" along with fragments 67945 through 67948 and reference soil 67960 at the House Rock area of Station 11. 67940 was collected from the east-west crack between House Rock and South Boulder; the sample was not permanently shadowed. |
| 67941 |
|
|
|
| 67942 |
|
|
|
| 67943 |
|
|
|
| 67944 |
|
|
|
| 67945 |
|
|
|
| 67946 |
|
|
|
| 67947 |
|
|
|
| 67948 |
|
|
|
| 67950 |
|
|
|
| 67955 |
|
|
|
| 67956 |
|
|
|
| 67957 |
|
|
|
| 67960 |
|
|
|
| 67975 |
rock |
fragmental breccia |
Irregularly shaped rock with approximately equal amounts of pale gray, fragmental, friable breccia and a coating of frothy, clast-rich glass. |
| 67976 |
|
|
|
| 68001 |
core |
|
|
| 68002 |
core |
|
|
| 68030 |
|
|
|
| 68035 |
|
|
|
| 68110 |
|
|
|
| 68115 |
|
|
|
| 68120 |
|
|
|
| 68121 |
|
|
|
| 68122 |
|
|
|
| 68123 |
|
|
|
| 68124 |
|
|
|
| 68410 |
|
|
|
| 68415 |
|
impact melt breccia |
|
| 68416 |
|
impact melt breccia |
|
| 68500 |
|
soil |
Soil 68500 accompanied rake sample 68510 at Station 8, on the north rim of a 10-15 meter crater in the vicinity of visible rays from South Ray crater. Astronauts reported several glass fragments scattered over the surface in this area, some reflecting red and green in the sunlight. The sample area is generally free of large rocks. |
| 68501 |
soil-general |
|
|
| 68502 |
rake |
|
|
| 68503 |
rake |
|
|
| 68504 |
rake |
|
|
| 68505 |
rake |
|
|
| 68510 |
rake |
|
|
| 68511 |
rake |
|
|
| 68512 |
rake |
|
|
| 68513 |
rake |
|
|
| 68514 |
rake |
|
|
| 68515 |
rake |
|
|
| 68516 |
rake |
|
|
| 68517 |
rake |
|
|
| 68518 |
rake |
|
|
| 68519 |
rake |
|
|
| 68520 |
rake |
|
|
| 68521 |
rake |
|
|
| 68522 |
rake |
|
|
| 68523 |
rake |
|
|
| 68524 |
rake |
|
|
| 68525 |
rake |
|
|
| 68526 |
rake |
|
|
| 68527 |
rake |
|
|
| 68528 |
rake |
|
|
| 68529 |
rake |
|
|
| 68530 |
rake |
|
|
| 68531 |
rake |
|
|
| 68532 |
rake |
|
|
| 68533 |
rake |
|
|
| 68534 |
rake |
|
|
| 68535 |
rake |
|
|
| 68536 |
rake |
|
|
| 68537 |
rake |
|
|
| 68815 |
rock |
|
|
| 68820 |
|
|
|
| 68821 |
|
|
|
| 68822 |
|
|
|
| 68823 |
|
|
|
| 68824 |
|
|
|
| 68825 |
|
|
|
| 68840 |
|
soil |
This is a reference soil collected 35 meters east of a 15 meter diameter crater and 6 meters north of the boulder from which "fillet" soil 68820 is taken. Fragments larger than 1 meter in the sample area are sparse, the soil is loose, and craters larger than 5 cm are sparse. |
| 68841 |
|
|
|
| 68842 |
|
|
|
| 68843 |
|
|
|
| 68844 |
|
|
|
| 68845 |
|
|
|
| 68846 |
|
|
|
| 68847 |
|
|
|
| 68848 |
|
|
|
| 69001 |
|
|
|
| 69003 |
|
|
|
| 69004 |
|
|
|
| 69920 |
|
|
|
| 69921 |
|
|
|
| 69922 |
|
|
|
| 69923 |
|
|
|
| 69924 |
|
|
|
| 69930 |
|
|
|
| 69935 |
|
|
|
| 69940 |
|
soil |
69920 and 69940 are in the shadow of a .5 meter boulder. 69920 is a "skim" sample and 69940 is a "scoop" sample from several cm below the surface. Both soils were collected at Station 9, 15 meters north of a 40 meter crater. Large fragments are relatively sparse at the sample site, surface is relatively firm, craters 5-30 cm are common but larger ones are sparse. |
| 69941 |
|
|
|
| 69942 |
|
|
|
| 69943 |
|
|
|
| 69944 |
|
|
|
| 69945 |
|
|
|
| 69950 |
|
|
|
| 69955 |
|
|
|
| 69960 |
|
soil |
69960 was collected at Station 9 from under a .5 meter boulder after it had been rolled over. It is part of a "surface sampler" including soils 69920, 69940, and 69960 and fragments 69003, 69004, and 66935. Large fragments are relatively sparse at the sample site, surface is relatively firm, craters 5-30 cm are common but larger ones are sparse. |
| 69961 |
|
soil |
|
| 69962 |
|
soil |
|
| 69963 |
|
soil |
|
| 69964 |
|
soil |
|
| 69965 |
|
soil |
|
Jump to Apollo:
11
12
14
15
16
|
| Apollo 17 |
| Sample Number |
Sample Type |
Lithology |
Description |
| 70001 |
core |
|
|
| 70002 |
core |
|
|
| 70003 |
core |
|
|
| 70004 |
core |
|
|
| 70005 |
core |
|
|
| 70006 |
core |
|
|
| 70007 |
|
soil |
|
| 70008 |
core |
soil |
70001-70009 are the segments of the deep core drilled at the ALSEP site 180 meters west of the LM. The sample area is flat, level and has 2-3% block cover. Craters 10 cm to 1 meter in size are common, fines are coherent below 3-4 cm. Drill penetration to 3.2 meters alternated between easy and difficult. The bottom 20 cm were very difficult to drill. The base material is cohesive, fragmental. |
| 70009 |
core |
soil |
|
| 70017 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 70018 |
rock |
breccia |
Clastic Matrix Breccia; no research has been conducted upon this sample |
| 70019 |
rock |
breccia |
Soil Breccia - Agglutinate |
| 70035 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 70075 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 70130 |
|
|
|
| 70131 |
|
|
|
| 70132 |
|
|
|
| 70133 |
|
|
|
| 70134 |
|
|
|
| 70135 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt, |
| 70136 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 70137 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 70138 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 70139 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 70140 |
|
|
|
| 70141 |
|
|
|
| 70142 |
|
|
|
| 70143 |
|
|
|
| 70144 |
|
|
|
| 70145 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 70146 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 70147 |
rock |
high-Ti mare basalt |
Clast-Rich Impact Melt |
| 70148 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 70149 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 70150 |
|
|
|
| 70151 |
|
|
|
| 70152 |
|
|
|
| 70153 |
|
|
|
| 70154 |
|
|
|
| 70155 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 70156 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 70157 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 70160 |
|
soil |
This is a fillet soil near the ALSEP central station, 180 meters west of the LM, at the base of a 1.5 meter boulder. Sample area has about 2-5% rock cover. Fines are darker when disturbed and compaction is greater in the fillet. |
| 70161 |
soil <1 mm |
soil |
|
| 70165 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 70170 |
|
|
|
| 70175 |
rock |
breccia |
Glass-Rich Microbreccia |
| 70180 |
|
soil |
This surface soil was collected 3 meters from the deep core site on the rim of an 8 meter blocky crater at the ALSEP. The sample area is flat and level with 2-3% block cover. Craters 10 cm to 1 meter in size are common, the fines are rather loose at the sample site on the rim of a .5 meter crater. This soil was collected with 70185, an 8 cm vuggy basalt. |
| 70181 |
|
|
|
| 70182 |
|
|
|
| 70183 |
|
|
|
| 70184 |
|
|
|
| 70185 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 70215 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 70250 |
|
|
|
| 70255 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 70270 |
|
|
|
| 70275 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 70295 |
rock |
breccia |
Dark Matrix Breccia |
| 70310 |
|
|
|
| 70311 |
|
|
|
| 70312 |
|
|
|
| 70313 |
|
|
|
| 70314 |
|
|
|
| 70315 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 70320 |
|
|
|
| 70321 |
|
|
|
| 70322 |
|
|
|
| 70323 |
|
|
|
| 70324 |
|
|
|
| 71030 |
|
|
|
| 71031 |
|
|
|
| 71032 |
|
|
|
| 71033 |
|
|
|
| 71034 |
|
|
|
| 71035 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 71036 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 71037 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 71040 |
|
soil |
71040 is a surface soil that was collected along with 6 chips in the shadow of "tombstone rock" at Station 1A. Soil 71060 was collected at the same site at a depth of 5-6 cm. Tombstone Rock is on the inner side of the southwest rim of a 10 meter blocky crater. The sample area is broadly rolling and dominated by ejecta. Local craters up to 2 meters in size are common, and the fines are fairly compact. |
| 71041 |
|
|
|
| 71042 |
|
|
|
| 71043 |
|
|
|
| 71044 |
|
|
|
| 71045 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 71046 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 71047 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 71048 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 71049 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 71050 |
|
|
|
| 71055 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 71060 |
|
soil |
71060 is a soil sample collected 5-6 cm below the surface in the shadow of "tombstone rock" at Station 1A. It was collected with 13 chips. Tombstone Rock is on the inner side of the southwest rim of a 10 meter blocky crater. The sample area is broadly rolling and dominated by ejecta. Local craters up to 2 meters in size are common, and the fines are faily compact. |
| 71061 |
|
|
|
| 71062 |
|
|
|
| 71063 |
|
|
|
| 71064 |
|
|
|
| 71065 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 71066 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 71067 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 71068 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 71069 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 71075 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 71085 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 71086 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 71087 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 71088 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 71089 |
|
|
|
| 71090 |
|
|
|
| 71091 |
|
|
|
| 71092 |
|
|
|
| 71093 |
|
|
|
| 71094 |
|
|
|
| 71095 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 71096 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 71097 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 71130 |
|
|
|
| 71131 |
soil <1 mm |
|
|
| 71135 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 71136 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 71150 |
|
|
|
| 71155 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 71156 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 71157 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 71170 |
|
|
|
| 71175 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 71500 |
|
soil |
Soil 71500 and 6 rock fragments were collected at Station 1A 15 meters northeast of the rim of a blocky 10 meter crater. It was collected as the reference to rake sample 71520 - 71597. The sample area is flat and essentially free of large fragments. The fines are fairly compact, there are 3 .5 meter craters in the sample area. The soil is scooped from the edge of a subdued crater in an area mostly free of surface rocks and small craters. |
| 71501 |
|
|
|
| 71502 |
|
|
|
| 71503 |
|
|
|
| 71504 |
|
|
|
| 71505 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 71506 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 71507 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 71508 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 71509 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 71515 |
rock |
other |
Glass-Bonded Agglutinate |
| 71520 |
|
|
|
| 71521 |
|
|
|
| 71522 |
|
|
|
| 71523 |
|
|
|
| 71524 |
|
|
|
| 71525 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 71526 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 71527 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 71528 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 71529 |
|
|
|
| 71530 |
|
|
|
| 71531 |
|
|
|
| 71532 |
|
|
|
| 71533 |
|
|
|
| 71534 |
|
|
|
| 71535 |
|
|
|
| 71536 |
|
|
|
| 71537 |
|
|
|
| 71538 |
|
|
|
| 71539 |
|
|
|
| 71540 |
|
|
|
| 71541 |
|
|
|
| 71542 |
|
|
|
| 71543 |
|
|
|
| 71544 |
|
|
|
| 71545 |
|
|
|
| 71546 |
|
|
|
| 71547 |
|
|
|
| 71548 |
|
|
|
| 71549 |
|
|
|
| 71550 |
|
|
|
| 71551 |
|
|
|
| 71552 |
|
|
|
| 71553 |
|
|
|
| 71554 |
|
|
|
| 71555 |
|
|
|
| 71556 |
|
|
|
| 71557 |
rock |
high-Ti mare basalt |
|
| 71558 |
|
|
|
| 71559 |
|
|
|
| 71560 |
|
|
|
| 71561 |
|
|
|
| 71562 |
|
|
|
| 71563 |
|
|
|
| 71564 |
|
|
|
| 71565 |
|
|
|
| 71566 |
|
|
|
| 71567 |
|
|
|
| 71568 |
|
|
|
| 71569 |
|
|
|
| 71570 |
|
|
|
| 71571 |
|
|
|
| 71572 |
|
|
|
| 71573 |
|
|
|
| 71574 |
|
|
|
| 71575 |
|
|
|
| 71576 |
|
|
|
| 71577 |
|
|
|
| 71578 |
|
|
|
| 71579 |
|
|
|
| 71580 |
|
|
|
| 71581 |
|
|
|
| 71582 |
|
|
|
| 71583 |
|
|
|
| 71584 |
|
|
|
| 71585 |
|
|
|
| 71586 |
|
|
|
| 71587 |
|
|
|
| 71588 |
|
|
|
| 71589 |
|
|
|
| 71590 |
|
|
|
| 71591 |
|
|
|
| 71592 |
|
|
|
| 71593 |
|
|
|
| 71594 |
|
|
|
| 71595 |
|
|
|
| 71596 |
rake |
high-Ti mare basalt |
high-Ti mare basalt |
| 71597 |
|
|
|
| 72130 |
|
|
|
| 72131 |
|
|
|
| 72132 |
|
|
|
| 72133 |
|
|
|
| 72134 |
|
|
|
| 72135 |
rock |
breccia |
Microbreccia |
| 72140 |
|
soil |
This soil was collected during the LRV traverse between Station 1 and 2 on the "prong" or very faint extension of the white mantle of a crater rim. The sample area is undulating, and fragments greater than 10 cm are rare. The ground surface is patterned in a "raindrop" texture. This sample is very cohesive. |
| 72141 |
soil <1 mm |
|
|
| 72145 |
rock |
breccia |
Polymict Microbreccia; original all remains; no subsamples have been prepared and no work has been conducted in this Catalog (Oct 1993) |
| 72150 |
|
soil |
This sample is document bag residue left in the bag which contained 72155, a 420 gm basalt. The basalt and the residue were collected during an LRV traverse on Tortilla flat between SEP and Station 2. The sample area is flat with sparse fragments. The sampling and handling procedures make this data very suspect. |
| 72155 |
rock |
basalt |
Basalt |
| 72160 |
|
|
|
| 72161 |
|
|
|
| 72162 |
|
|
|
| 72163 |
|
|
|
| 72164 |
|
|
|
| 72210 |
|
|
|
| 72215 |
rock |
impact melt breccia |
aphanitic impact melt breccia |
| 72220 |
|
|
|
| 72221 |
|
|
|
| 72222 |
|
|
|
| 72223 |
|
|
|
| 72224 |
|
|
|
| 72230 |
|
|
|
| 72235 |
rock |
impact melt breccia |
aphanitic impact melt breccia, sample was given name "Dying Dog" during processing, contains plutonic KREEP norite |
| 72240 |
|
soil |
This soil was collected at Station 2, near the base of South Massif. The upper 4 cm of soil was collected from under a .7 meter breccia boulder which was rolled over by the crew. 72440 was from the upper 4 cm of the soil, and 72460 was a skim sample. The area was too disturbed after rolling the boulder over to compare well with the undisturbed fines, but generally it appears similar. The sample area is a strewn boulder field with loose fines. |
| 72241 |
|
|
|
| 72242 |
|
|
|
| 72243 |
|
|
|
| 72244 |
|
|
|
| 72250 |
|
|
|
| 72255 |
rock |
impact melt breccia |
aphanitic impact melt breccia |
| 72260 |
|
|
|
| 72261 |
|
|
|
| 72262 |
|
|
|
| 72263 |
|
|
|
| 72264 |
|
|
|
| 72270 |
|
|
|
| 72275 |
rock |
breccia |
fragmental polymict breccia, |
| 72310 |
|
|
|
| 72315 |
rock |
impact melt breccia |
micropokilitic impact melt breccia |
| 72320 |
|
soil |
72320 was collected at Station 2, near the base of the South Massif. This "shadowed soil" collected about 20 cm under the east - west overhang of a 2 meter diameter boulder. The sample area is a strewn boulder field with boulders up to 2 meters across common. Craters up to 10 cm are abundant in the immediate sample area. The soil probably does not have as complex an exposure history as rake sample 72500 because of the protection from the rock overhang. |
| 72321 |
|
|
|
| 72322 |
|
|
|
| 72323 |
|
|
|
| 72324 |
|
|
|
| 72330 |
|
|
|
| 72335 |
rock |
impact melt breccia |
Micropoikilitic impact melt breccia |
| 72350 |
|
|
|
| 72355 |
rock |
impact melt breccia |
Micropoikilitic impact melt breccia |
| 72370 |
|
|
|
| 72375 |
rock |
impact melt breccia |
Micropoikilitic impact melt breccia |
| 72390 |
|
|
|
| 72395 |
rock |
impact melt breccia |
Micropoikilitic impact melt breccia |
| 72410 |
|
|
|
| 72415 |
rock |
dunite |
Cataclastic dunite, homogeneous |
| 72416 |
rock |
dunite |
Cataclastic Dunite, has never been dissected or allocated for study |
| 72417 |
rock |
dunite |
Cataclastic Dunite, pale yellowish to greenish gray (5Y 8/1 to 5 GY 8/1) |
| 72418 |
rock |
dunite |
Cataclastic Dunite, has never been dissected or allocated for study |
| 72430 |
|
|
|
| 72431 |
|
|
|
| 72432 |
|
|
|
| 72433 |
|
|
|
| 72434 |
|
|
|
| 72435 |
rock |
impact melt breccia |
Micropoikilitic Impact Melt Breccia, can be assumed to have formed during the Serenitatis event, has major and trace element chemistry similar to other Apollo 17 low-K Fra Mauro impacat melts |
| 72440 |
|
soil |
This soil was collected at Station 2, near the base of South Massif. The upper 4 cm of soil was collected from a .7 meter breccia boulder which was rolled over by the crew. 72440 was from the upper 4 cm of the soil, and 72460 was a skim sample. The area was too disturbed after rolling the boulder over to compare well with the undisturbed fines, but generally it appears similar. The sample area is a strewn boulder field with loose fines. |
| 72441 |
|
|
|
| 72442 |
|
|
|
| 72443 |
|
|
|
| 72444 |
|
|
|
| 72460 |
|
soil |
72460 was collected at Station 2, near the base of South Massif. It was a skim sample which was collected from under a .7 meter breccia boulder which was rolled over by the crew. 72440 was from the upper 4 cm of the soil, and 72460 was a skim sample. The area was too disturbed after rolling the boulder over to compare well with the undisturbed fines, but generally it appears similar. The sample area is a strewn boulder field with loose fines. |
| 72461 |
|
|
|
| 72462 |
|
|
|
| 72463 |
|
|
|
| 72464 |
|
|
|
| 72500 |
|
soil |
Soil 72500 and rake sample 72530-72559 were collected at Station 2 near the base of South Massif a few meters from the rim of Nansen crater. Boulders up to 2 meters are common in the general area, but fragments larger than 25 cm are sparse in the raked area. The soil was sampled to a depth of 4 cm. |
| 72501 |
|
|
|
| 72502 |
|
|
|
| 72503 |
|
|
|
| 72504 |
|
|
|
| 72505 |
rock |
impact melt breccia |
Impact Melt Breccia (?) |
| 72530 |
|
|
|
| 72531 |
|
|
|
| 72532 |
|
|
|
| 72533 |
|
|
|
| 72534 |
|
|
|
| 72535 |
rock |
impact melt breccia |
Microsubophitic Impact Melt Breccia, its chemistry is similar to the common low-K Fra Mauro melts that dominate the Apollo 17 highlands samples |
| 72536 |
rock |
impact melt breccia |
Microsubophitic Impact Melt Breccia, its chemistry is imilar to the common low-K Fra Mauro melts that dominate the Apollo 17 highlands samples |
| 72537 |
rock |
impact melt breccia |
Impact Melt Breccia (?), identification is uncertain because it has never been allocated or dissected |
| 72538 |
rock |
impact melt breccia |
Impact Melt Breccia (?), identification is uncertain because it has never been allocated or dissected |
| 72539 |
rock |
breccia |
Microsubophitic Impact Melt Breccia (?), its chemistry is similar to te common low-K Fra Mauro melts that dominate the Apollo 17 highlands samples |
| 72540 |
|
|
|
| 72541 |
|
|
|
| 72542 |
|
|
|
| 72543 |
|
|
|
| 72544 |
|
|
|
| 72545 |
rock |
breccia |
Impact Melt Breccia (?), sample has never been allocated or dissected |
| 72546 |
rock |
breccia |
Impact Melt Breccia (?), sample has never been allocated or dissected |
| 72547 |
rock |
impact melt breccia |
Impact Melt Breccia (?), sample has never been allocated or dissected |
| 72548 |
rock |
impact melt breccia |
Micropoikilitic Impact Melt Breccia, its chemistry is similar to the common low-K Fra Mauro melts that dominate the Apollo 17 highlands samples |
| 72549 |
rock |
impact melt breccia |
Micropoikilitic Impact Melt Breccia, chemistry is similar to the common low-K Fra Mauro melts that dominate the Apollo 17 highlands samples |
| 72550 |
|
|
|
| 72551 |
|
|
|
| 72552 |
|
|
|
| 72553 |
|
|
|
| 72554 |
|
|
|
| 72555 |
rock |
impact melt breccia |
Impact Melt Breccia (?), has never been allocated or dissected |
| 72556 |
rock |
impact melt breccia |
Impact Melt Breccia (?), has never been allocated or dissected |
| 72557 |
rock |
impact melt breccia |
Impact Melt Breccia (?), has never been dissected or allocated |
| 72558 |
rock |
impact melt breccia |
Micropoikilitic Impact Melt Breccia |
| 72559 |
rock |
other |
Granoblastic Impactite |
| 72700 |
|
soil |
Soil 72700 and rake samples 72735-38 were collected at Station 2 in a light mantle unit near the base of South Massif slightly upslope from Nansen crater. The area has an undulating slope towards the southeast, fragments up to 3 cm are sparsely distributed in the rake area, and craters up to 5 meters are common in the general area. The sample was collected to a depth of 5 cm. |
| 72701 |
|
|
|
| 72702 |
|
|
|
| 72703 |
|
|
|
| 72704 |
|
|
|
| 72705 |
rock |
impact melt breccia |
Impact Melt Breccia |
| 72730 |
|
|
|
| 72735 |
rock |
impact melt breccia |
Impact Melt Breccia (High-K) |
| 72736 |
rock |
impact melt breccia |
Micropoikilitic Impact Melt Breccia, chemistry is similar to the common low-K Fra Mauro melts that dominate the Apollo 17 highlands samples, |
| 72737 |
rock |
impact melt breccia |
Impact Melt Breccia (?) |
| 72738 |
rock |
impact melt breccia |
Microsubophitic Impact Melt Breccia |
| 73001 |
|
|
|
| 73002 |
|
|
|
| 73120 |
|
soil |
Surface sample 73120 was collected near trench sample 73140 at Station 2A, about 750 meters north-northeast of Station 2 at the base of South Massif on the light mantle deposits. The site is generally level, with fragments >5cm sparse and craters >10 cm sparse. |
| 73124 |
|
|
|
| 73130 |
|
|
|
| 73131 |
|
|
|
| 73132 |
|
|
|
| 73134 |
|
|
|
| 73140 |
|
soil |
This is a trench sample collected to a depth of 15 cm near surface sample 73120 at Station 2A, about 750 meters north-northeast of Station 2 at the base of South Massif on the light mantle deposits. The site is generally level, with fragments >5cm sparse and craters >10 cm sparse. |
| 73141 |
|
|
|
| 73142 |
|
|
|
| 73143 |
|
|
|
| 73144 |
|
|
|
| 73145 |
rock |
impact melt breccia |
Impact Melt Breccia (?), medium dark gray (N4), homogeneous |
| 73146 |
rock |
anorthite |
Cataclastic Troctolitic Anorthosite, very light gray (N8), homogenous |
| 73150 |
|
|
|
| 73151 |
|
|
|
| 73153 |
|
|
|
| 73154 |
|
|
|
| 73155 |
rock |
impact melt breccia |
Impact Melt Breccia, medium dark gray (N4) in color, rather heterogeneous |
| 73156 |
rock |
impact melt breccia |
Impact Melt Breccia or Granoblastic Impactite, light gray and homogeneous |
| 73210 |
|
|
|
| 73211 |
|
|
|
| 73212 |
|
|
|
| 73213 |
|
|
|
| 73214 |
|
|
|
| 73215 |
rock |
impact melt breccia |
Aphanitic Impact Melt Breccia, polymict breccia, |
| 73216 |
rock |
impact melt breccia |
Impact Melt Breccia, tan to olive gray (5Y 5/1) |
| 73217 |
rock |
impact melt breccia |
Impact Melt Breccia, bulk groundmass may be the low-K Fra Mauro basalt composition common at the Apollo 17 landing site, |
| 73218 |
rock |
impact melt breccia |
Impact Melt Breccia, greenish-gray gray (5GY 6/1) angular breccia; its chemical composition might be similar to the common low-K Fra Mauro basalt impact melts common at the site, originally described as anorthositic. |
| 73219 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt, medium dark gray (N4), the only mare basalt as an individual rock fragment from the South Massif or landslide |
| 73220 |
|
soil |
This is a skim sample from the top 1 cm of trench (73240 is from the bottom). The trench is on the rim of a 10 meter crater in light mantle deposits at Station 3. The site slopes 7 degrees to the east, 1-10 cm fragments are common and >10 cm fragments are sparse. |
| 73221 |
|
|
|
| 73222 |
|
|
|
| 73223 |
|
|
|
| 73224 |
|
|
|
| 73225 |
rock |
impact melt breccia |
Impact Melt Breccia (?), light gray (N5), contains plagioclases, possibly a ranoblastic impactite |
| 73230 |
|
|
|
| 73235 |
rock |
impact melt breccia |
Aphanitic Impact Melt Brecia, medium light gray (N6) with mottling |
| 73240 |
|
soil |
This is a trench sample from the upper part of a 15 cm deep trench containing a medium gray surface layer and a 3 cm light gray layer just below the surface. It was collected at Station 3 with skim sample 73220 on the rim of a 10 meter crater in the light mantle. The site slopes 7 degrees to the east, 1-10 cm fragments are common and >10 cm fragments are sparse. |
| 73241 |
|
|
|
| 73242 |
|
|
|
| 73243 |
|
|
|
| 73244 |
|
|
|
| 73245 |
rock |
other |
Granoblastic Impactite (?); medium gray (N6), probably feldspathic granulite with a little adhering light brownish gray regolith breccia |
| 73250 |
|
|
|
| 73255 |
rock |
impact melt breccia |
Aphanitic Impact Melt Breccia, essentally an agglomeritic bomb with abundant clasts |
| 73260 |
|
soil |
This is a trench sample from part of the "marbled zone" 5-10 cm below the surface. It may also include some material from the small patch of light material visible in the pre-sampling photographs. It was collected at Station 3 with skim sample 73220 on the rim of a 10 meter crater in the light mantle. The site slopes 7 degrees to the east, 1-10 cm fragments are common and >10 cm fragments are sparse. |
| 73261 |
|
|
|
| 73262 |
|
|
|
| 73263 |
|
|
|
| 73264 |
|
|
|
| 73270 |
|
|
|
| 73275 |
rock |
impact melt breccia |
Micropoikilitic Impact Melt Breccia, lclast-bearing, with chemical composition similar to the low-K Fra Mauro melts common at the site and generally presumed to represent the Serentatis impact melt, is light gray in color.. |
| 73280 |
|
soil |
This is a trench sample from about 5-10 cm below the surface. It appears to be similar to the light gray material just below the surface. It was collected at Station 3 with skim sample 73220 on the rim of a 10 meter crater in the light mantle. The site slopes 7 degrees to the east, 1-10 cm fragments are common and >10 cm fragments are sparse. |
| 73281 |
|
|
|
| 73282 |
|
|
|
| 73283 |
|
|
|
| 73284 |
|
|
|
| 73285 |
rock |
breccia |
Glass-Coated Polymict Breccia, medium light gray (N6), |
| 74001 |
core |
soil |
Drive tube 74001/74002 was collected at the south rim of 120 meter Shorty crater, at Station 4. The cored material is unusually compact. The core contains orange and red colored soil with nearly vertical contacts. The site is near the low place in the crater rim crest. The fragment population is viable. Craters up to several meters in diameter are scattered near the sample site. The core is almost entirely without coarse fines. |
| 74002 |
core |
soil |
Drive tube 74001/74002 was collected at the south rim of 120 meter Shorty crater, at Station 4. The cored material is unusually compact. The core contains orange and red colored soil with nearly vertical contacts. The site is near the low place in the crater rim crest. The fragment population is viable. Craters up to several meters in diameter are scattered near the sample site. The core is almost entirely without coarse fines. |
| 74110 |
|
|
|
| 74111 |
|
|
|
| 74112 |
|
|
|
| 74113 |
|
|
|
| 74114 |
|
|
|
| 74115 |
rock |
regolith breccia |
Friable Regolith Breccia, light gray polymict breccia |
| 74116 |
rock |
regolith breccia |
Friable Regolith Breccia, light gray polymict breccia |
| 74117 |
rock |
regolith breccia |
Friable Regolith Breccia, light gray polymict breccia |
| 74118 |
rock |
regolith breccia |
Friable Regolith Breccia, light gray polymict breccia |
| 74119 |
rock |
regolith breccia |
Friable Regolith Breccia, light gray polymict breccia |
| 74120 |
|
soil |
This surface soil was collected from the LRV while traversing over light mantle deposits between Stations 3 and 4. The site is undulating, yet regionally level with fragments >10 cm sparse. Craters <1 meter are abundant, but craters >1 meter are sparse. |
| 74124 |
|
|
|
| 74220 |
|
soil |
Considered to be a clod of friable material taken 6-8 cm deep in a trench from Station 4, on the rim of 120 meter Shorty crater. The site is near the low place in the crater rim crest. The fragments population is highly variable, craters up to several meters in diameter are common. The particles larger than 1 mm are mostly friable clumps that disagregated during sieving. Any discontinuity is probably due to the fact that the sizes <1 mm were sieved and the sizes >1 mm were hand picked. |
| 74221 |
|
|
|
| 74222 |
|
|
|
| 74223 |
|
|
|
| 74224 |
|
|
|
| 74235 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 74240 |
|
soil |
This is gray soil that was bordering the meter wide band of reddish soil (74240 is southwest of the colored soil and 74260 is to the northeast) at Station 4 on the rim of Shorty crater. The site is near the low place in the crater rim crest. The fragment population is highly variable, and craters up to several meters in diameter are common. |
| 74245 |
rock |
basalt |
Aphanitic High-Ti Basalt |
| 74246 |
rock |
breccia |
Soil Breccia |
| 74247 |
rock |
basalt |
High-Ti Basalt |
| 74248 |
rock |
basalt |
High-Ti Basalt |
| 74249 |
rock |
basalt |
High-Ti Basalt |
| 74250 |
|
|
|
| 74255 |
rock |
basalt |
High-Ti Basalt |
| 74260 |
|
soil |
This is gray soil that was bordering the meter wide band of reddish soil (74240 is southwest of the colored soil and 74260 is to the northeast) at Station 4 on the rim of Shorty crater. The site is near the low place in the crater rim crest. The fragment population is highly variable, and craters up to several meters in diameter are common. |
| 74275 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 74285 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 74286 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 74287 |
rock |
high-Ti mare basalt |
High-It Mare Basalt |
| 75010 |
|
|
|
| 75015 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 75030 |
|
|
|
| 75035 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 75050 |
|
|
|
| 75055 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 75060 |
|
soil |
This is a mantling soil that was collected from a 1 cm depression on a 3 meter boulder, at Station 5, the southwest rim of Camelot crater. The site has an undulating slope with cobbles and boulders covering 30% of the surface. The soil contains two rock chips, 75065-66. |
| 75061 |
|
|
|
| 75062 |
|
|
|
| 75063 |
|
|
|
| 75064 |
|
|
|
| 75065 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 75066 |
rock |
breccia |
Glassy Breccia |
| 75070 |
|
|
|
| 75075 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 75080 |
|
soil |
This is a surface soil sample from a site on the regolith surface a few meters from sample 75060 at Station 5 on the southwest rim of Camelot crater. The sample area is undulating with cobbles and boulders covering 30% of the surface. |
| 75081 |
|
|
|
| 75082 |
|
|
|
| 75083 |
|
|
|
| 75084 |
|
|
|
| 75085 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 75086 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 75087 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 75088 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 75089 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 75110 |
|
soil |
This sample was collected during LRV traverse #7, from the apex of Victory crater on the inner slope of the crater rim. The site has pebbles to 1 meter size boulders covering 2-3% of the surface. The fragments appear to be randomly scattered, but there is a slight concentration on the rims of small craters. |
| 75111 |
|
|
|
| 75112 |
|
|
|
| 75113 |
|
|
|
| 75114 |
|
|
|
| 75115 |
rock |
high-Ti mare basalt |
Light olive gray subrounded, fine-grained basalt, with an equigranular fabric and several penetrative fractures. |
| 75120 |
|
|
|
| 75121 |
|
|
|
| 75122 |
|
|
|
| 75123 |
|
|
|
| 75196 |
|
|
|
| 75210 |
|
soil |
This soil was collected during LRV traverse #8, between Victory and Horatio craters in an area of dark mantle between the small craters. The area is flat with scattered craters less than 5 meters in diameter. Clods <10 cm are found on the rims of fresh craters. "Raindrops" are present on the surface of the sample area. |
| 75224 |
|
|
|
| 75701 |
rake |
|
|
| 76001 |
|
|
|
| 76015 |
rock |
impact melt breccia |
Vesicular Micropoikilitic Impact Melt Breccia; chipped off top corner of Block 5 of big boulder at Station 6; summarized by Spudis/Ryder (1981) that boulder is from the melt sheet or ejecta blanket from the Serenitatus impact event |
| 76035 |
rock |
impact melt breccia |
Nonvesicular Impact Melt Breccia |
| 76036 |
rock |
impact melt breccia |
Impact Melt Breccia; sample has not been studied at time of this Catalog (Aug 1994) but is apparently similar to and probably piece of 76035. |
| 76037 |
soil-general |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 76055 |
rock |
impact melt breccia |
Impact Melt Breccia; appears to be older than Station 6 Boulder and other Serenitatus impact melts; may be a separate sample of Serenitatus melt sheet from high on North Massif. |
| 76120 |
|
|
|
| 76121 |
|
|
|
| 76122 |
|
|
|
| 76123 |
|
|
|
| 76124 |
|
|
|
| 76130 |
|
|
|
| 76131 |
|
|
|
| 76132 |
|
|
|
| 76133 |
|
|
|
| 76134 |
|
|
|
| 76135 |
rake |
impact melt breccia |
Vesicular Poikilitic Impact Melt Breccia |
| 76136 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 76137 |
rock |
impact melt breccia |
Poikilitic Impacat Melt Breccia; sample has not been studied at time of this Catalog (Aug 1994) |
| 76210 |
|
|
|
| 76215 |
rock |
impact melt breccia |
Vesicular Micropoikilitic Impact Melt Breccia |
| 76230 |
|
|
|
| 76235 |
rock |
other |
Feldspathic Granulitic Impactite; may have broken further in sample bag including samples 76230, 76235, 236, 237, 238, 239, 305, 306 and 307 (Heiken et al., 1973; Phinney, 1981) |
| 76236 |
rock |
other |
Feldspathic Granulitic Impactite; part of 76235 |
| 76237 |
rock |
other |
Feldspathic Granulitic Impactite, part of 76235 |
| 76238 |
rake |
other |
Feldspathic Granulitic Impactite; part of 76235. |
| 76239 |
rock |
other |
Feldspathic Granulitic Impactite; part of 76235 |
| 76240 |
|
|
|
| 76241 |
|
|
|
| 76242 |
|
|
|
| 76243 |
|
|
|
| 76244 |
|
|
|
| 76245 |
|
impact melt breccia |
Impact Melt Breccia |
| 76246 |
|
impact melt breccia |
Impact Melt Breccia |
| 76250 |
|
|
|
| 76255 |
rock |
impact melt breccia |
Banded Impact Melt Breccia; has large clast of crushed norite |
| 76260 |
|
soil |
This surface soil was collected at Station 6 on the south slope of the North Massif. It has a large boulder nearby which casts a permanent shadow on 76240: 76260 and 76280 are just outside the limit of the overhang. 76260 is a 2 cm skim and 76280 is a 5 cm scoop. The area slopes 11 degrees to the south with scattered fragments <6cm. |
| 76261 |
|
|
|
| 76262 |
|
|
|
| 76263 |
|
|
|
| 76264 |
|
|
|
| 76265 |
rock |
impact melt breccia |
Impact Melt Breccia |
| 76270 |
|
|
|
| 76275 |
rock |
impact melt breccia |
Impact Melt Breccia; sample has not been well studied (Aug 1994) |
| 76280 |
|
soil |
This surface soil was collected at Station 6 on the south slope of the North Massif. It has a large boulder nearby which casts a permanent shadow on 76240: 76260 and 76280 are just outside the limit of the overhang. 76260 is a 2 cm skim and 76280 is a 5 cm scoop. The area slopes 11 degrees to the south with scattered fragments <6cm. |
| 76281 |
|
|
|
| 76282 |
|
|
|
| 76283 |
|
|
|
| 76284 |
|
|
|
| 76285 |
rock |
breccia |
Agglutinate of Dark Matrix Breccia Fragments; soil in area was collected as comparison with 76245, which was permanently shadowed. |
| 76286 |
rock |
impact melt breccia |
Impact Melt Breccia |
| 76290 |
|
|
|
| 76295 |
rock |
impact melt breccia |
Impact Melt Breccia |
| 76305 |
rock |
other |
Feldspathic Granulitic Impactites, part of 76235 |
| 76306 |
rock |
other |
Feldspathic Granulitic Impactites, part of 76235 |
| 76307 |
rock |
other |
Feldspathic Granulitic Impactites, part of 76235 |
| 76310 |
|
|
|
| 76315 |
rock |
impact melt breccia |
Micropoikilitic Impact Melt Breccia |
| 76320 |
|
soil |
Surface soil collected at Station 6 on flat face of boulder 1. The site slopes 10 degrees to the north with fragments up to 5 cm scattered about. A few 5-10 cm crataers are found in the area. |
| 76335 |
rock |
troctolite |
Cataclastic Troctolite |
| 76500 |
|
soil |
Reference soil 76500 and rake soil 76530-76577 were collected at Station 6, 25 meters west of the boulder cluster on the ejecta blanket of a 10 meter crater. The site slopes 11 degrees to the south with 1-10 cm fragments scattered randomly. One large 10 meter crater and many <30 cm craters are found at the site. |
| 76501 |
|
|
|
| 76502 |
|
|
|
| 76503 |
|
|
|
| 76504 |
|
|
|
| 76505 |
|
impact melt breccia |
Micropoikilitic Impact Melt Breccia |
| 76506 |
|
regolith breccia |
Dark Matrix Regolith Breccia |
| 76530 |
|
|
|
| 76535 |
rake |
troctolite |
Troctolite, random sample as part of rake sample at Station 6 |
| 76536 |
rake |
troctolite |
Crushed Troctolite |
| 76537 |
rake |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 76538 |
rake |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 76539 |
rake |
high-Ti mare basalt |
Aphanitic High-Ti Mare Basalt |
| 76540 |
|
|
|
| 76541 |
|
|
|
| 76542 |
|
|
|
| 76543 |
|
|
|
| 76544 |
|
|
|
| 76545 |
rake |
regolith breccia |
Dark Matrix Regolith Breccia |
| 76546 |
|
|
|
| 76547 |
|
|
|
| 76548 |
rake |
regolith breccia |
Dark Matrix Regolith Breccia |
| 76549 |
|
|
|
| 76550 |
|
|
|
| 76551 |
|
|
|
| 76552 |
|
|
|
| 76553 |
|
|
|
| 76554 |
|
|
|
| 76555 |
rake |
impact melt breccia |
Micropoikilitic Impact Melt Breccia |
| 76556 |
rake |
impact melt breccia |
Micropoikilitic Impact Melt Breccia |
| 76557 |
rake |
impact melt breccia |
Micropoikilitic Impact Melt Breccia |
| 76558 |
rake |
impact melt breccia |
Imact Melt Breccia |
| 76559 |
rake |
impact melt breccia |
Poikilitic Impact Melt Breccia |
| 76560 |
|
|
|
| 76561 |
|
|
|
| 76562 |
|
|
|
| 76563 |
|
|
|
| 76564 |
|
|
|
| 76565 |
rake |
regolith breccia |
Dark Matrix Regolith Breccia |
| 76566 |
rake |
regolith breccia |
Dark Matrix Regolith Breccia |
| 76567 |
rake |
regolith breccia |
Light Matrix Regolith Breccia |
| 76568 |
rake |
high-Ti mare basalt |
Aphanitic High-Ti Mare Basalt |
| 76569 |
rake |
impact melt breccia |
Aphanitic Impact Melt Breccia |
| 76570 |
|
|
|
| 76571 |
|
|
|
| 76572 |
|
|
|
| 76573 |
|
|
|
| 76574 |
|
|
|
| 76575 |
rake |
impact melt breccia |
Feldspathic Impact Melt Breccia |
| 76576 |
rake |
impact melt breccia |
Micropoikilitic Impact Melt Breccia |
| 76577 |
rake |
impact melt breccia |
Poikilitic Impact Melt Breccia |
| 77017 |
rock |
other |
Poikilitic Anorthsitic Gabbo, annealed, feldspathic breccia |
| 77035 |
rock |
impact melt breccia |
Micropoikilitic Impact Melt Breccia |
| 77070 |
|
|
|
| 77075 |
rock |
norite |
Impact Melt Dike in Cataclastic Norite |
| 77076 |
|
|
|
| 77077 |
rock |
norite |
Cataclastic Norite with Black Veinlets |
| 77110 |
|
|
|
| 77115 |
rock |
impact melt breccia |
Micropoikilitic Impact Melt Breccia |
| 77130 |
|
|
|
| 77135 |
rock |
impact melt breccia |
Vesicular Poikilitic Impact Melt Rock |
| 77215 |
rock |
norite |
Cataclastic Norite (41 or more pieces) |
| 77510 |
|
|
|
| 77511 |
|
|
|
| 77512 |
|
|
|
| 77513 |
|
|
|
| 77514 |
|
|
|
| 77515 |
rake |
impact melt breccia |
Poikilitic Impact Melt Breccia |
| 77516 |
rake |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 77517 |
rake |
breccia |
Unique Fragmental Breccia; sample 77517 is exotic to Apollo 17 site, contining mineral fragments of pink aluminous spinel, aluminous enstatite, and forsterite. |
| 77518 |
rake |
impact melt breccia |
Micropoikilitic Impact Melt Breccia |
| 77519 |
rake |
impact melt breccia |
Micropoikilitic Impact Melt Breccia |
| 77525 |
rake |
impact melt breccia |
Impact Melt Breccia |
| 77526 |
rake |
impact melt breccia |
Impact Melt Breccia |
| 77535 |
rake |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 77536 |
rake |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 77537 |
rake |
impact melt breccia |
Impact Melt Breccia |
| 77538 |
rake |
breccia |
Unusual Fragmental Breccia |
| 77539 |
rake |
impact melt breccia |
Poikilitic Impact Melt Breccia |
| 77545 |
rake |
impact melt breccia |
Poikilitic Impact Melt Breccia |
| 78120 |
|
|
|
| 78121 |
|
|
|
| 78122 |
|
|
|
| 78123 |
|
|
|
| 78124 |
|
|
|
| 78130 |
|
|
|
| 78135 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 78150 |
|
|
|
| 78155 |
rock |
other |
Feldspathic Granulitic Impactite; sample itself may have been projectile that made "pit crater"; may be exotic to site; |
| 78220 |
|
soil |
Soil collected from beneath a .5 meter gabbroic boulder at Station 8, near the base of Sculptured Hills, south of Wessex Cleft. The site slopes moderately steeply to the southwest, with scattered pebbles, clods, small rocks and one boulder. The surface is saturated with 1 cm craters, larger craters are present but not abundant. |
| 78221 |
|
|
|
| 78222 |
|
|
|
| 78223 |
|
|
|
| 78224 |
|
|
|
| 78230 |
|
|
|
| 78231 |
|
|
|
| 78232 |
|
|
|
| 78233 |
|
|
|
| 78234 |
|
|
|
| 78235 |
rock |
norite |
Shocked Norite |
| 78236 |
rock |
norite |
Shocked Norite, piece of norite 78235 |
| 78237 |
|
|
|
| 78238 |
rock |
norite |
Shocked Norite, piece from norite 78235 |
| 78250 |
|
|
|
| 78255 |
rock |
norite |
Shocked Norite |
| 78420 |
|
soil |
This is part of trench sequence at Station 8 at the base of Sculptured Hills south of Wessex Cleft. 78420 is at the bottom of a 25 cm trench, 78440 is at a depth of 6-15 cm, 78460 is at a depth of 1-6 cm, and 78480 is from the upper 1 cm. The site has a moderate slope to the southwest, a few pebbles and clods <5 cm are found, and the area is saturated with 1 cm craters. There are a few larger craters in the area. |
| 78421 |
|
|
|
| 78422 |
|
|
|
| 78423 |
|
|
|
| 78424 |
|
|
|
| 78440 |
|
|
|
| 78441 |
|
|
|
| 78442 |
|
|
|
| 78443 |
|
|
|
| 78444 |
|
|
|
| 78460 |
|
soil |
This is part of trench sequence at Station 8 at the base of Sculptured Hills south of Wessex Cleft. 78420 is at the bottom of a 25 cm trench, 78440 is at a depth of 6-15 cm, 78460 is at a depth of 1-6 cm, and 78480 is from the upper 1 cm. The site has a moderate slope to the southwest, a few pebbles and clods <5 cm are found, and the area is saturated with 1 m craters. There are a few larger craters in the area. |
| 78461 |
|
|
|
| 78462 |
|
|
|
| 78463 |
|
|
|
| 78464 |
|
|
|
| 78465 |
rock |
breccia |
Soil Breccia |
| 78480 |
|
soil |
This is part of trench sequence at Station 8 at the base of Sculptured Hills south of Wessex Cleft. 78420 is at the bottom of a 25 cm trench, 78440 is at a depth of 6-15 cm, 78460 is at a depth of 1-6 cm, and 78480 is from the upper 1 cm. The site has a moderate slope to the southwest, a few pebbles and clods <5 cm are found, and the area is saturated with 1 cm craters. There are a few larger craters in the area. |
| 78481 |
|
|
|
| 78482 |
|
|
|
| 78483 |
|
|
|
| 78484 |
|
|
|
| 78500 |
|
soil |
This is a surface sample to accompany rake sample 78525-599, collected near the rim of a subdued 15 meter crater at the base of Sculptured Hills, south of Wessex Cleft. The site has a moderate slope to the southwest with scattered pebbles, clods, and small rocks. |
| 78501 |
|
|
|
| 78502 |
|
|
|
| 78503 |
|
|
|
| 78504 |
|
|
|
| 78505 |
|
high-Ti mare basalt |
High-Ti Mare Basalt |
| 78506 |
|
high-Ti mare basalt |
High-Ti Mare Basalt |
| 78507 |
|
high-Ti mare basalt |
High-Ti Mare Basalt |
| 78508 |
|
breccia |
Light Matrix Soil Breccia |
| 78509 |
|
high-Ti mare basalt |
High-Ti Mare Basalt |
| 78510 |
|
|
|
| 78511 |
|
|
|
| 78512 |
|
|
|
| 78513 |
|
|
|
| 78514 |
|
|
|
| 78515 |
|
breccia |
Dark Matrix Breccia |
| 78516 |
|
breccia |
Dark Matrix Soil Breccia |
| 78517 |
|
other |
Friable White Cataclasite |
| 78518 |
|
breccia |
Dark Matrix Soil Breccia |
| 78525 |
rake |
other |
Agglutinate |
| 78526 |
rake |
green glass vitrophyres |
Green Glass Vitrophyre |
| 78527 |
rake |
breccia |
Granulitic Noritic Breccia |
| 78528 |
|
basalt |
Basalt |
| 78530 |
|
|
|
| 78535 |
rake |
breccia |
Dark Matrix Breccia |
| 78536 |
rake |
breccia |
Dark Matrix Breccia |
| 78537 |
rake |
breccia |
Dark Matrix Breccia |
| 78538 |
rake |
breccia |
Dark Matrix Breccia |
| 78539 |
rake |
breccia |
Dark Matrix Breccia |
| 78540 |
|
|
|
| 78541 |
|
|
|
| 78542 |
|
|
|
| 78543 |
|
|
|
| 78544 |
|
|
|
| 78545 |
rake |
breccia |
Dark Matrix Breccia |
| 78546 |
rake |
breccia |
Dark Matrix Breccia |
| 78547 |
rake |
breccia |
Dark Matrix Soil Breccia |
| 78548 |
rake |
other |
Soil Clod, friable soil breccia |
| 78549 |
rake |
other |
Soil Clod, friable soil breccia |
| 78550 |
|
|
|
| 78551 |
|
|
|
| 78552 |
|
|
|
| 78553 |
|
|
|
| 78554 |
|
|
|
| 78555 |
rake |
breccia |
Soil Breccia |
| 78556 |
rake |
breccia |
Dark Matrix Soil Breccia |
| 78557 |
rake |
breccia |
Dark Matrix Soil Breccia |
| 78558 |
rake |
breccia |
Dark Matrix Soil Breccia |
| 78559 |
rake |
breccia |
Dark Matrix Soil Breccia |
| 78560 |
|
|
|
| 78561 |
|
|
|
| 78563 |
|
|
|
| 78564 |
|
|
|
| 78565 |
rake |
breccia |
Dark Matrix Soil Breccia |
| 78566 |
rake |
breccia |
Dark Matrix Soil Breccia |
| 78567 |
rake |
breccia |
Dark Matrix Soil Breccia |
| 78568 |
rake |
breccia |
Breccia, coherent soil breccia |
| 78569 |
rake |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 78570 |
|
|
|
| 78571 |
|
|
|
| 78572 |
|
|
|
| 78573 |
|
|
|
| 78574 |
|
|
|
| 78575 |
rake |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 78576 |
rake |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 78577 |
rake |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 78578 |
rake |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 78579 |
rake |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 78580 |
|
|
|
| 78581 |
|
|
|
| 78582 |
|
|
|
| 78583 |
|
|
|
| 78584 |
|
|
|
| 78585 |
rake |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 78586 |
rake |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 78587 |
rake |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 78588 |
rake |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 78589 |
rake |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 78590 |
|
|
|
| 78591 |
|
|
|
| 78592 |
|
|
|
| 78593 |
|
|
|
| 78594 |
|
|
|
| 78595 |
rake |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 78596 |
rake |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 78597 |
rake |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 78598 |
rake |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 78599 |
rake |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 79001 |
core |
soil |
Double drive tube 79001/79002 was taken 2 meters from two 1 meter craters on the southeast flank of the Van Serg crater ejecta blanket, at Station 9. The site has a gentle slope to the southeast away from Van Serg crater. Fragments 2-20 cm cover 3% of the surface. Astronauts report that driving the first core was easy. The second one was a little tougher, and then it got very hard at the end. >1mm particles were hand picked and not sieved, where they would have broken down, so there is a discontinuity in the size distribution caused by the lab procesures. |
| 79002 |
core |
soil |
Double drive tube 79001/79002 was taken 2 meters from two 1 meter craters on the southeast flank of the Van Serg crater ejecta blanket, at Station 9. The site has a gentle slope to the southeast away from Van Serg crater. Fragments 2-20 cm cover 3% of the surface. Astronauts report that driving the first core was easy. The second one was a little tougher, and then it got very hard at the end. >1mm particles were hand picked and not sieved, where they would have broken down, so there is a discontinuity in the size distribution caused by the lab procesures. |
| 79035 |
rock |
breccia |
friable breccia |
| 79110 |
|
|
|
| 79115 |
rock |
breccia |
Medium Gray Soil Breccia; described as a lumpy, generally fine-grained, friable basalt, with intense platy fracturing, particularly on the west face (Apollo 17 Lunar Sample Information Catalog, 1973) |
| 79120 |
|
|
|
| 79121 |
|
|
|
| 79122 |
|
|
|
| 79123 |
|
|
|
| 79124 |
|
|
|
| 79125 |
rock |
breccia |
Microbreccia; As no work has been conducted on this sample, it is still intact as of this catalog (Oct 1993) |
| 79130 |
|
|
|
| 79135 |
rock |
breccia |
Polymict Matrix Breccia |
| 79155 |
rock |
other |
Partially Glass-Coated Gabbro |
| 79170 |
|
|
|
| 79175 |
rock |
other |
Glass-Bonded Agglutinate |
| 79190 |
|
|
|
| 79195 |
rock |
breccia |
Breccia, friable, basalt |
| 79215 |
rock |
breccia |
Metabreccia |
| 79220 |
|
soil |
79220 is part of a trench sequence (79220 depth 0-2cm, 79240 depth 2-7 cm, 79260 depth 7-17 cm) taken from the southwest flank of the Van Serg crater ejecta blanket near Station 9. The uppermost 7 cm of the trench is gray, below that is a light gray or white layer. The site has a gently southeast slope away from Van Serg crater. Fragments 2-20 cm cover 3% of the surface. Two fresh 1 meter craters are found near the trench. |
| 79221 |
|
|
|
| 79222 |
|
|
|
| 79223 |
|
|
|
| 79224 |
|
|
|
| 79225 |
rock |
breccia |
Friable Microbreccia; As of this Catalog (Oct 1993), original sample remains intact; no work has been conducted. |
| 79226 |
rock |
breccia |
Friable Microbreccia; as of this Catalog (Oct 1993), original sample remains intact; no work has been conducted. |
| 79227 |
|
soil |
Clod; after separation from the soil sample, this sample disaggregated to soil-like material and was not described |
| 79228 |
|
soil |
Clod; After separation from the soil sample, this sample disaggregated to soil-like material and was not described. |
| 79240 |
|
soil |
79220 is part of a trench sequence (79220 depth 0-2cm, 79240 depth 2-7 cm, 79260 depth 7-17 cm) taken from the southwest flank of the Van Serg crater ejecta blanket near Station 9. The uppermost 7 cm of the trench is gray, below that is a light gray or white layer. The site has a gently southeast slope away from Van Serg crater. Fragments 2-20 cm cover 3% of the surface. Two fresh 1 meter craters are found near the trench. |
| 79241 |
|
|
|
| 79242 |
|
|
|
| 79243 |
|
|
|
| 79244 |
|
|
|
| 79245 |
rock |
other |
High Grade Metaclastic; The original sample remains intact at time of the Catalog (Oct 1993); no work has been conducted. |
| 79260 |
|
soil |
79220 is part of a trench sequence (79220 depth 0-2cm, 79240 depth 2-7 cm, 79260 depth 7-17 cm) taken from the southwest flank of the Van Serg crater ejecta blanket near Station 9. The uppermost 7 cm of the trench is gray, below that is a light gray or white layer. The site has a gently southeast slope away from Van Serg crater. Fragments 2-20 cm cover 3% of the surface. Two fresh 1 meter craters are found near the trench. |
| 79261 |
|
|
|
| 79262 |
|
|
|
| 79263 |
|
|
|
| 79264 |
|
|
|
| 79265 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 79510 |
|
soil |
This surface sample was collected 2 meters east of the large boulder where 79120 was collected. Both samples were taken from the southeast rim of Van Serg crater, Station 9. There is no slope at the rim crest, fragments 2-30 cm cover 10% of the surface, the largest boulder in the area is 1.5 meters. Craters are negligible on the Van Serg crater rim. |
| 79511 |
|
|
|
| 79512 |
|
|
|
| 79513 |
|
|
|
| 79514 |
|
|
|
| 79515 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 79516 |
rock |
high-Ti mare basalt |
High-Ti Mare Basalt |
| 79517 |
rock |
breccia |
Dark Matrix Breccia; the orignal sample remains intact as of the Catalog (Oct 1993) and no wrk has been conducted. |
| 79518 |
rock |
breccia |
Dark Matrix Breccia; original sample remains intact as of this Catalog (Oct 1993); no work has been conducted |
| 79519 |
rock |
breccia |
Dark Matrix Breccia; orignal sample remains intact as of this Catalog (Oct 1993); no work has been conducted |
| 79520 |
|
|
|
| 79521 |
|
|
|
| 79522 |
|
|
|
| 79523 |
|
|
|
| 79524 |
|
|
|
| 79525 |
rock |
breccia |
Dark Matrix Breccia; original sample remains intact as of this Catalog (Oct 1993); no work has been conducted |
| 79526 |
rock |
breccia |
Dark Matrix Breccia; original sample remains intack as of this Catalog (Oct 1993); no work has been conducted |
| 79527 |
rock |
breccia |
Dark Matrix Breccia; original sample remains intact as of this Catalog (Oct 1993); no work has been conducted |
| 79528 |
rock |
breccia |
Dark Matrix Breccia; original sample remains intact as of this Catalog (Oct 1993); no work has been conducted |
| 79529 |
rock |
breccia |
Dark Matrix Breccia; original sample remains intact as of this Catalog (Oct 1993); no work has been conducted |
| 79530 |
|
|
|
| 79531 |
|
|
|
| 79532 |
|
|
|
| 79533 |
|
|
|
| 79534 |
|
|
|
| 79535 |
rock |
breccia |
Dark Mtarix Breccia; original sample remains intact as of this Catalog (Oct 1993); no work has been conducted |
| 79536 |
rock |
breccia |
Dark Matrix Breccia; the original sample remains intact as of this Catalog (Oct 1993); no work has been conducted |
| 79537 |
rock |
breccia |
Dark Matrix Breccia; original sample remains intact as of this Catalog (Oct 1993); no work has been conducted |
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