NASA’s Perseverance took this selfie at “Witch Hazel
Hill” on Jezero Crater’s rim on May 10, 2025. The small dark hole in the rock
in front of the rover is the borehole made when the rover collected the “Bell
Island” sample. The small puff of dust left of center and below the horizon
line is a dust devil.
NASA/JPL-Caltech/MSSS
NASA’s Perseverance Mars rover has uncovered evidence that a 245-foot-thick
(75-meter-thick) stack of ancient rock on the rim of Jezero Crater was built by
repeated asteroid impacts. Referred to as the “Broom Point member” by the
rover’s science team, this sequence of layered bedrock is likely more than 3.9
billion years old, making it among the oldest terrain ever examined by a Mars
rover.
Released Wednesday in the Journal of Geophysical Research: Planets, the findings offer a window into one of the most
tumultuous chapters in the history of the solar system.
“Since leaving Jezero, Perseverance
has been exploring a brand-new frontier, both geographically and geologically —
a chapter of Martian time that predates the crater itself,” said Ken Farley,
Perseverance deputy project scientist at Caltech in Pasadena, California. “On
Earth, our earliest geologic history has been fundamentally broken up,
deformed, and erased by plate tectonics. Because Mars lacks plate tectonics to
recycle its crust, this ancient record remains intact, giving us a rare glimpse
into a geological time period that doesn’t exist on our own planet.”
Reading between layers
After ascending the western rim of Jezero Crater in late 2024, Perseverance
began examining surrounding locations with its science instruments. Their data at
Broom Point revealed six distinct rock types, including breccias — rocks
composed of angular fragments — alternating with layers of fine-grained,
pulverized rock dust. Rock fragments within the breccias are pocked with
gas-bubble cavities, indicating they were once molten.
The presence of tiny, dark, glassy
beads within the layers offered an important clue about how these rocks formed.
While volcanoes can produce similar glassy droplets, they rarely occur in such
high abundance, pointing to asteroid impacts, instead, as the primary
architect. In fact, the largest beads rival those flung out by the
dinosaur-killing Chicxulub asteroid’s impact on Earth.
NASA’s Perseverance rover captured its own tracks
descending from the rim of Jezero Crater. The bright-colored rocks running from
middle left to middle right of the image, a formation dubbed the “Broom Point
member,” are likely more than 3.9 billion years old, making them among the
oldest terrain ever examined by a Mars rover.
NASA/JPL-Caltech/ASU/MSSS
The repetition of these distinct rock types multiple times throughout this
thick sequence of rock indicates that high-energy impact events happened again
and again across this region of early Mars.
“The different rock layers are a
record of variable-sized impacts occurring at different distances from where
this rock sequence was accumulating,” said Alex Jones, a Ph.D. student in
planetary geology at Imperial College London and lead author of the paper.
“Some large impacts took place very far away, some small impacts nearby. Their
debris all ended up landing here, constructing this thick section of
rock.”
How these layers formed may suggest
an interaction with water or ice. Several of the layers look like they may have
been formed by fast, ground-hugging debris flows. On Earth, these powerful,
fluidlike surges can occur when molten rock hits water or ice that instantly
flashes into steam.
Cosmic one-two punch
Some of Broom Point’s layers tilt
at angles exceeding 80 degrees — nearly vertical — which is far too steep to be
caused by the impact that created Jezero Crater.
Instead, scientists suspect a
cosmic “one-two punch” shaped this landscape long ago. First, a colossal
asteroid impact created the 1,200-mile-wide (1,900-kilometer-wide) Isidis
Basin, one of the largest impact basins on Mars, upending and tilting the once-flat
rock layers. Later, a second asteroid likely struck, forming Jezero Crater,
which measures 28 miles (45 kilometers) across. This second impact fractured
and uplifted the already-tilted rocks into the dramatic formations the rover
sees today.
To pin down exactly when these
events took place, the Perseverance team collected two core samples, dubbed
“Bell Island” and “Main River.” If a future mission were to return them to
Earth, laboratory dating could determine when and how often impacts were
occurring on early Mars — and, by extension, the infant Earth, whose own early
impact record has been erased by billions of years of plate tectonics.
“During this violent era, it wasn’t
rain or snow falling from the sky, but an almost constant barrage of molten
rock droplets and pulverized dust kicked up by asteroid impacts,” said Jones.
“If we can pin down the ages of these layers, it would be like reading a cosmic
weather report from 4 billion years ago.”
This orbital map shows the path NASA’s Perseverance
Mars rover took from its 2021 landing site in Jezero Crater to the “Broom
Point” location in mid-2025.
NASA/JPL-Caltech/MRO/HIRISE/UA/ICL
More about Perseverance
NASA’s Jet Propulsion Laboratory in
Southern California, which is managed for the agency by Caltech, built and
manages operations of the Perseverance rover on behalf of the agency’s Science
Mission Directorate in Washington, as part of NASA’s Mars Exploration Program
portfolio. Arizona State University leads the operations of the rover’s
Mastcam-Z instrument, working in collaboration with Malin Space Science Systems
in San Diego, on the design, fabrication, testing, and operation of the
cameras. SuperCam is led by Los Alamos National Laboratory in New Mexico, where
the instrument’s Body Unit was developed. The rover’s SHERLOC (Scanning
Habitable Environments with Raman and Luminescence for Organics and Chemicals)
instrument was built at NASA JPL, and its WATSON (Wide Angle Topographic Sensor
for Operations and eNgineering) camera was built at Malin Space Science
Systems.
For more information on NASA’s Perseverance, visit: https://science.nasa.gov/mission/mars-2020-perseverance
Source: NASA’s Perseverance Rover Reads Record of Ancient Mars Impacts - NASA



