NASA’s InSight Lander Detects Stunning Meteoroid Impact on Mars

Mars impact crater

Boulder-sized blocks of water ice can be seen around the rim of an impact crater on Mars, as viewed by the High-Resolution Imaging Science Experiment (HiRISE) camera onboard NASA’s Mars Reconnaissance Orbiter. The crater was formed December 24, 2021, by a meteoroid strike in the Amazonis Planitia region. Credit: NASA/JPL-Caltech/University of Arizona.

NASA’s InSight lander recorded a magnitude 4 marsquake December 24, 2021, but scientists learned later the cause of that quake: a meteoroid strike estimated to be one of the biggest seen on Mars since NASA began exploring the cosmos. What’s more, the meteoroid excavated boulder-sized chunks of ice buried closer to the martian equator than ever found before, a discovery with implications for NASA’s plans to send astronauts to the Red Planet.

Scientists determined the quake resulted from a meteoroid impact when they looked at before-and-after images from NASA’s Mars Reconnaissance Orbiter (MRO) and spotted a new, yawning crater. Offering a rare opportunity to see how a large impact shook the ground on Mars, the event and its effects were detailed in two papers published October 27, 2022, in the journal Science.

The meteoroid is estimated to have spanned 5 to 12 meters (16 to 39 feet), small enough that it would have burned up in Earth’s atmosphere, but not in Mars’ thin atmosphere, which is just 1% as dense as our planet’s. The impact, which occurred in a region called Amazonis Planitia, blasted a crater roughly 150 meters (492 feet) across and 21 meters (70 feet) deep. Some of the ejecta thrown by the impact flew as far as 37 kilometers (23 miles) away.

With images and seismic data documenting the event, this is believed to be one of the largest craters ever witnessed forming any place in the solar system. Many larger craters exist on the Red Planet, but they are significantly older and predate any Mars mission.

“It’s unprecedented to find a fresh impact of this size,” said Ingrid Daubar of Brown University, who leads InSight’s Impact Science Working Group. “It’s an exciting moment in geologic history, and we got to witness it.”

InSight studied the planet’s crust, mantle, and core. Seismic waves are key to the mission and have revealed the size, depth, and composition of Mars’ inner layers. Since landing in November 2018, InSight detected 1,318 marsquakes, including several caused by smaller meteoroid impacts.

But the quake resulting from the December 2021 impact was the first observed to have surface waves, a kind of seismic wave that ripples along the top of a planet’s crust. The second of the two Science papers related to the big impact describes how scientists use these waves to study the structure of Mars’ crust.

In late 2021, InSight scientists reported to the rest of the team they had detected a major marsquake on December 24. The crater was first spotted February 11, 2022, by scientists working at Malin Space Science Systems (MSSS), which built and operates two cameras onboard MRO. The Context Camera (CTX) provides black-and-white, medium-resolution images, while the Mars Color Imager (MARCI) produces daily maps of the entire planet, allowing scientists to track large-scale weather changes like the recent regional dust storm that further diminished InSight’s solar power.

The impact’s blast zone was visible in MARCI data that allowed the team to pin down a 24-hour period within which the impact occurred. These observations correlated with the seismic epicenter, conclusively demonstrating that a meteoroid impact caused the large December 24 marsquake.

“The image of the impact was unlike any I had seen before, with the massive crater, the exposed ice, and the dramatic blast zone preserved in the martian dust,” said Liliya Posiolova, who leads the Orbital Science and Operations Group at MSSS. “I couldn’t help but imagine what it must have been like to witness the impact, the atmospheric blast, and debris ejected miles downrange.”

Establishing the rate at which craters appear on Mars is critical for refining the planet’s geologic timeline. On older surfaces, such as those of Mars and our Moon, there are more craters than on Earth; on our planet, the processes of erosion and plate tectonics erase older features from the surface.

New craters also expose materials below the surface. In this case, large chunks of ice scattered by the impact were viewed by MRO’s High-Resolution Imaging Science Experiment (HiRISE) color camera.

Subsurface ice will be a vital resource for astronauts, who could use it for a variety of needs, including drinking water, agriculture, and rocket propellant. Buried ice has never been spotted this close to the martian equator, which, as the warmest part of Mars, is an appealing location for astronauts.

For more information, visit https://mars.nasa.gov/insight/.