Since then, Perseverance has been exploring the area in seek for proof of previous (and probably current) life – very similar to its cousin, the Curiosity rover.
This consists of acquiring samples that will probably be positioned in a cache and retrieved by a future ESA/NASA sample-return mission.
These would be the first directly-retrieved samples of Martian rock and soil that will probably be analyzed in a laboratory on Earth, that are anticipated to disclose some tantalizing bits concerning the historical past of the crimson planet.
However it seems that we need not wait on the sample-return mission for the reason that Perseverance rover is already sending some shocking information again to Earth.
In response to a brand new research by a analysis workforce led by the College of California at Los Angeles (UCLA) and the College of Oslo, Perseverance’s ground-penetrating radar detected that the rock layers beneath the crater are unusually inclined.
These unusual sections might have resulted from lava flows that slowly cooled or may very well be sedimentary deposits from an underground lake.
The analysis workforce was led by Svein-Erik Hamran, a Professor of autonomous programs and sensor applied sciences on the College of Oslo (UiO) and the Precept Investigator of the Radar Imager for Mars subsurFAce eXperiment (RIMFAX) aboard the Perseverance rover.
He was joined by researchers from UiO, UCLA, the Planetary Science Institute (PSI), Vestfonna Geophysical, the Centro de Astrobiología, the Norwegian Polar Institute, NASA’s Jet Propulsion Laboratory, and a number of universities. The paper that describes their findings just lately appeared within the journal Science Advances.
The Jezero Crater, positioned in Syrtis Main Planum between the Northern Lowlands and Southern Highlands, measures about 45 km (28 mi) in diameter and is believed to have as soon as been a lake.
This area was particularly chosen because the touchdown web site for Perseverance, which has been exploring the big deposits of rocks and clay minerals deposited at its western edge, the place water as soon as flowed into the crater.
Like Curiosity, the aim is to be taught extra concerning the durations when Mars had flowing water on its floor so scientists can get a greater thought of how (and when) it transitioned to the chilly, arid planet it’s right this moment.
As they point out of their research, the workforce consulted the primary information obtained by the Radar Imager for Mars subsurFAce eXperiment (RIMFAX), which carried out the primary rover-mounted ground-penetrating radar survey of the Martian subsurface.
This survey was performed because the rover made its preliminary 3-km (~1.85 mi) hike throughout the Jezero Crater and supplied steady information on the electromagnetic properties of the bedrock construction beneath the crater to depths of 15 meters (~49 toes) under the floor.
The ensuing radar pictures confirmed layered sequences that dip downward at angles of as much as 15 levels.
David Paige, a UCLA professor of Earth, planetary and house sciences and one of many lead researchers on the RIMFAX, defined in a current ULCA Newsroom launch:
“We had been fairly stunned to search out rocks stacked up at an inclined angle. We had been anticipating to see horizontal rocks on the crater ground. The truth that they’re tilted like this requires a extra complicated geologic historical past.
They might have been shaped when molten rock rose up in direction of the floor, or, alternatively, they might symbolize an older delta deposit buried within the crater ground.”
RIMFAX paints an image of Mars’ subsurface geology by sending bursts of radar waves into the floor, that are mirrored by rock layers and different options underground. This permits scientists to find out the shapes, densities, thickness, angles, and composition of underground objects based mostly on how radar waves are returned to the instrument.
After analyzing the information, the analysis workforce famous that layered rock was widespread all through the realm surveyed by Perseverance. Extra perplexing, additionally they discovered that the inclined areas had highly-reflective rock layers that tilt in a number of instructions.
The almost certainly rationalization for the angled layers they witnessed factors towards an igneous (molten) origin, the place the motion of magma underground deposited rock layers over time that cooled and solidified.
Nonetheless, there’s additionally the likelihood that the layers are sedimentary, a phenomenon generally present in aqueous environments on Earth.
On this case, the options outcome from water depositing materials over time, which hardens and turns into layered. As Paige mentioned, this dropped at thoughts one other acquainted Earth function:
“RIMFAX is giving us a view of Mars stratigraphy much like what you possibly can see on Earth in freeway highway cuts, the place tall stacks of rock layers are typically seen in a mountainside as you drive by.
Earlier than Perseverance landed, there have been many hypotheses concerning the actual nature and origin of the crater ground supplies. We have now been in a position to slim down the vary of potentialities, however the information we have acquired to this point recommend that the historical past of the crater ground could also be fairly a bit extra difficult than we had anticipated.”
The info collected by RIMFAX will probably be of nice worth when the samples collected by Perseverance are returned to Earth for evaluation. Figuring out what lies beneath the Jezero Crater and the way it shaped will present the mandatory context for characterizing the samples.
It will present a clearer image of how and when Mars had flowing water on its floor, for the way lengthy, and whether or not this was intermittent or not. It should additionally point out how and when Mars transitioned to the extraordinarily chilly and dry setting we see there right this moment.
However most significantly, this information might reveal if Mars was ever in a position to assist life on its floor, which might lastly reply a query people have been asking for hundreds of years!