The youngest flood lava on Mars, flowing past a crater
Cool image time! The photo to the right, rotated, cropped, reduced to post here, was taken on December 3, 2022 by the high resolution camera on Mars Reconnaissance Orbiter (MRO).
The title given to this image by the MRO science team is “Upstream Edge of Crater in Athabasca Valles.” The crater itself is a pedestal crater, uplifted from the surrounding terrain because it was more resistant to erosion.
The material to the east of the crater’s rim definitely appears to have flow characteristics, but is it wet mud, glacial ice, or lava?
To figure this out we need as always some context. The latitude, 8 degrees north, immediately eliminates mud or glacial material. This location is in the dry equatorial regions of Mars, where no near surface ice has yet been found. Thus, the flow features are likely hardened lava.
What direction however was the flow? Was it flowing to the north, widening as it moved past the pedestal crater? Or was it to the south, narrowing as it pushed past that crater? To answer this question we need to widen our view.
The image to the right, rotated, cropped, and reduced to post here, was taken by MRO’s context camera on March 31, 2012, and shows this entire crater plus the surrounding region. The white rectangle indicates the area covered by the photo above.
The visual evidence, though still somewhat uncertain, suggests the lava had been flowing from the northeast to the southwest. For example, the teardrop shape of the aprons around both craters both suggest the flow was to the southwest. Furthermore, as the flow moved south it pushed through a gap in a ridge to flow to the south and southeast as well. The mesas in this area also have shapes that suggest the flow is to the south.
The overview map below tells us that this flow is near the head of what scientists have labeled the Athabasca Valles flood lava, as indicated by the dark blue area. According to this 2008 paper [pdf]:
Athabasca Valles is an outflow channel system located in north-central Elysium Planitia. It emerges full-born from the westernmost major fissure segment of the Cerberus Fossae, stretches southwest for 300 km, and empties into the Cerberus Palus basin. Previous work has shown that, despite the erosional appearance of its gross morphology, the entire channel system (including its banks) is coated with a veneer of lava. The lava is exceedingly thin in proximal Athabasca Valles and gradually thickens in the downstream direction, transitioning from a material unit that drapes the substrate topography to one that submerges it near the terminus of the channel system.
The most straightforward interpretation of these observations is that a fissure eruption at the head of Athabasca Valles flooded the down-slope terrain with lava, and then, as the eruption waned, the lava receded from the channels and drained downstream into Cerberus Palus where it ponded.
Athabasca is also thought to be the youngest such flood lava event on Mars, the eruption occurring about 600 million years ago and in just a matter of a few weeks — because lava is thought to flow much faster in Mars’ weak gravity — poured out enough material to cover an area about the size of Great Britain.
Today’s picture is near the head of Athabasca, where the hardened lava flow is thinnest. Thus, it did not bury the crater, but merely rushed past, possibly as it did so contributing to the erosion that left this crater upraised.
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Cool image time! The photo to the right, rotated, cropped, reduced to post here, was taken on December 3, 2022 by the high resolution camera on Mars Reconnaissance Orbiter (MRO).
The title given to this image by the MRO science team is “Upstream Edge of Crater in Athabasca Valles.” The crater itself is a pedestal crater, uplifted from the surrounding terrain because it was more resistant to erosion.
The material to the east of the crater’s rim definitely appears to have flow characteristics, but is it wet mud, glacial ice, or lava?
To figure this out we need as always some context. The latitude, 8 degrees north, immediately eliminates mud or glacial material. This location is in the dry equatorial regions of Mars, where no near surface ice has yet been found. Thus, the flow features are likely hardened lava.
What direction however was the flow? Was it flowing to the north, widening as it moved past the pedestal crater? Or was it to the south, narrowing as it pushed past that crater? To answer this question we need to widen our view.
The image to the right, rotated, cropped, and reduced to post here, was taken by MRO’s context camera on March 31, 2012, and shows this entire crater plus the surrounding region. The white rectangle indicates the area covered by the photo above.
The visual evidence, though still somewhat uncertain, suggests the lava had been flowing from the northeast to the southwest. For example, the teardrop shape of the aprons around both craters both suggest the flow was to the southwest. Furthermore, as the flow moved south it pushed through a gap in a ridge to flow to the south and southeast as well. The mesas in this area also have shapes that suggest the flow is to the south.
The overview map below tells us that this flow is near the head of what scientists have labeled the Athabasca Valles flood lava, as indicated by the dark blue area. According to this 2008 paper [pdf]:
Athabasca Valles is an outflow channel system located in north-central Elysium Planitia. It emerges full-born from the westernmost major fissure segment of the Cerberus Fossae, stretches southwest for 300 km, and empties into the Cerberus Palus basin. Previous work has shown that, despite the erosional appearance of its gross morphology, the entire channel system (including its banks) is coated with a veneer of lava. The lava is exceedingly thin in proximal Athabasca Valles and gradually thickens in the downstream direction, transitioning from a material unit that drapes the substrate topography to one that submerges it near the terminus of the channel system.
The most straightforward interpretation of these observations is that a fissure eruption at the head of Athabasca Valles flooded the down-slope terrain with lava, and then, as the eruption waned, the lava receded from the channels and drained downstream into Cerberus Palus where it ponded.
Athabasca is also thought to be the youngest such flood lava event on Mars, the eruption occurring about 600 million years ago and in just a matter of a few weeks — because lava is thought to flow much faster in Mars’ weak gravity — poured out enough material to cover an area about the size of Great Britain.
Today’s picture is near the head of Athabasca, where the hardened lava flow is thinnest. Thus, it did not bury the crater, but merely rushed past, possibly as it did so contributing to the erosion that left this crater upraised.
The support of my readers through the years has given me the freedom and ability to analyze objectively the ongoing renaissance in space, as well as the cultural changes -- for good or ill -- that are happening across America. Four years ago, just before the 2020 election I wrote that Joe Biden's mental health was suspect. Only in this year has the propaganda mainstream media decided to recognize that basic fact.
Fourteen years ago I wrote that SLS and Orion were a bad ideas, a waste of money, would be years behind schedule, and better replaced by commercial private enterprise. Even today NASA and Congress refuse to recognize this reality.
In 2020 when the world panicked over COVID I wrote that the panic was unnecessary, that the virus was apparently simply a variation of the flu, that masks were not simply pointless but if worn incorrectly were a health threat, that the lockdowns were a disaster and did nothing to stop the spread of COVID. Only in the past year have some of our so-called experts in the health field have begun to recognize these facts.
Your help allows me to do this kind of intelligent analysis. I take no advertising or sponsors, so my reporting isn't influenced by donations by established space or drug companies. Instead, I rely entirely on donations and subscriptions from my readers, which gives me the freedom to write what I think, unencumbered by outside influences.
Please consider supporting my work here at Behind the Black.
You can support me either by giving a one-time contribution or a regular subscription. There are five ways of doing so:
1. Zelle: This is the only internet method that charges no fees. All you have to do is use the Zelle link at your internet bank and give my name and email address (zimmerman at nasw dot org). What you donate is what I get.
2. Patreon: Go to my website there and pick one of five monthly subscription amounts, or by making a one-time donation.
3. A Paypal Donation:
5. Donate by check, payable to Robert Zimmerman and mailed to
Behind The Black
c/o Robert Zimmerman
P.O.Box 1262
Cortaro, AZ 85652
You can also support me by buying one of my books, as noted in the boxes interspersed throughout the webpage or shown in the menu above. And if you buy the books through the ebookit links, I get a larger cut and I get it sooner.
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