We get to witness it—a moment in geological history unfolding in real time.
A 5-12 meter meteorite created a 150-meter-wide crater in Mars's Amazonis Planitia region, one of the largest impacts observed since NASA began Mars exploration. The impact exposed subsurface ice deposits closer to Mars's equator than ever before, a critical discovery for future human colonization plans requiring water and rocket fuel.
- Meteorite impact on December 24, 2021, in Amazonis Planitia region of Mars
- 5-12 meter meteoroid created 150-meter-wide, 21-meter-deep crater
- Impact exposed subsurface ice closer to Mars's equator than ever before documented
- InSight lander detected magnitude-4 marsquake; Mars Reconnaissance Orbiter confirmed impact via orbital imagery
NASA's InSight lander detected a magnitude-4 marsquake on December 24 that was confirmed as a meteorite impact, with orbital imagery revealing a 150-meter crater and exposed subsurface ice near Mars's equator.
On December 24th, NASA's InSight lander felt the ground shake beneath it—a magnitude-4 tremor that rippled through the Martian soil. The spacecraft's seismic instruments recorded the jolt, but the scientists studying the data faced an immediate puzzle: was this a marsquake, the kind of seismic activity that occurs naturally on rocky planets, or something else entirely?
It took months to know for certain. In February 2022, researchers working with NASA's Mars Reconnaissance Orbiter—a spacecraft that has been circling the planet for years—spotted something new on the surface: an enormous crater, roughly 150 meters across and 21 meters deep, in a region called Amazonis Planitia. By comparing images taken before and after December 24th, the team could confirm what the seismic data had suggested. A meteorite had struck Mars. The tremor InSight detected was the planet's response to impact.
The meteoroid itself was estimated to measure between 5 and 12 meters across—small enough that it would have burned up entirely in Earth's atmosphere, but large enough to survive the thin Martian air, which is only about 1 percent as dense as our own. When it hit, the collision was violent enough to excavate material from deep underground. Debris from the explosion scattered across the landscape, with some fragments traveling as far as 37 kilometers from the impact site. Most remarkably, the blast exposed chunks of subsurface ice—water ice buried beneath the Martian regolith, closer to the equator than scientists had ever documented before.
This discovery carries weight beyond the immediate scientific interest. For NASA's long-term plans to send human explorers to Mars, subsurface ice near the equator represents something precious: a source of water for drinking, for agriculture, and for producing rocket fuel. The equatorial region is already attractive to mission planners because it is warmer than other parts of the planet. Now it offered something more—the raw materials astronauts would need to survive and work there.
The impact itself ranks among the largest ever observed on Mars since NASA began exploring the planet. Older craters dot the Martian surface, some far larger, but they formed long before any spacecraft arrived to witness them. This one was different. InSight detected it in real time. The Mars Reconnaissance Orbiter captured its aftermath in photographs. Two scientific papers describing the event and its implications were published in the journal Science, offering an unprecedented record of a major impact unfolding in the modern era of Mars exploration.
Ingrid Daubar, a scientist at Brown University who leads InSight's impact science working group, called the moment historic. "It is unprecedented to find a new impact of this size," she said. "It is an exciting moment in geological history, and we get to witness it." Her colleague Liliya Posiolova, who oversees orbital operations and science at the company that built and operates the orbiter's cameras, described the first time she saw the impact imagery: the enormous crater, the exposed ice, the dramatic blast zone preserved in Martian dust. She found herself imagining what it must have been like to see the meteorite arrive, the atmospheric explosion, the debris hurled across miles of landscape.
The timing of this discovery carries a note of urgency. InSight's solar panels have accumulated dust over the months, draining the lander's power reserves. The spacecraft was expected to shut down within weeks of the October 2022 publication of these findings, ending its mission after nearly four years on the surface. Since landing in November 2018, InSight had detected 1,318 marsquakes, including several triggered by smaller meteorite impacts. But this December event was the first to produce surface waves—a type of seismic wave that ripples along the top of a planet's crust. Those waves, scientists discovered, could be used to map the structure of Mars's interior in new ways, revealing details about the composition and architecture of the planet's crustal layers.
As InSight's power faded, the data it had gathered—combined with the orbital imagery showing the crater and the exposed ice—would help scientists refine their understanding of how often large impacts occur on Mars, and how that frequency shapes the planet's geological timeline. For future explorers planning to live and work on Mars, the ice near the equator offered both a practical resource and a reminder of the dynamic, still-active world they would be entering.
Citações Notáveis
It is unprecedented to find a new impact of this size. It is an exciting moment in geological history, and we get to witness it.— Ingrid Daubar, Brown University, InSight impact science working group
The image of the impact was unlike anything I had seen before—the enormous crater, the exposed ice, the dramatic blast zone preserved in Martian dust.— Liliya Posiolova, Malin Space Science Systems
A Conversa do Hearth Outra perspectiva sobre a história
Why does it matter that this impact was detected in real time, rather than discovered years later?
Because we almost never get to see a major impact happen on another planet as it occurs. Usually we find old craters and work backward, trying to figure out when they formed. This time, we have seismic data from the moment of impact, orbital images showing the crater fresh and undisturbed, and the blast zone still visible in the dust. It's like having a complete record of the event.
The ice discovery seems to be the practical payoff here. But why is ice near the equator so much more valuable than ice elsewhere on Mars?
Warmth. The equator is the most hospitable region for human settlement—easier to generate power, easier to maintain equipment, easier to live. If you have to choose between a cold, dark location with ice and a warm location with ice, you choose the warm one. This impact essentially handed us both conditions in one place.
InSight was dying anyway. Did this discovery come at the last possible moment?
Almost exactly. The lander's power was already failing from dust accumulation. The seismic data from December was recorded and stored, but it took months to confirm what caused it. By the time the orbital images confirmed the impact and the papers were published, InSight had weeks left. It's like the mission got one final, major discovery before the lights went out.
What can seismic waves from an impact tell you that photographs alone cannot?
The waves travel through the planet's interior and bounce back. By studying how they move and change, you can map what's beneath the surface—how thick the crust is, what it's made of, where the boundaries between different layers lie. A photograph shows you the crater. Seismic data shows you the planet's skeleton.
Does this change how NASA thinks about where to land humans?
It refines the thinking. The equator was already on the list. Now there's concrete evidence of accessible ice there, which wasn't known before. It shifts the calculus from "this region is warm" to "this region is warm and has the resources we need to stay alive."