A Martian lava flood plain
Cool image time! The photo to the right, cropped to post here, was taken by the high resolution camera on Mars Reconnaissance Orbiter (MRO) on March 2, 2020, and shows some inexplicable shallow pits and depressions in the middle of a relatively flat and featureless plain.
Make sure you click on the image to see the full photo. Though the plain looks remarkably smooth, a handful of dark splotches are scattered about, almost all of which occur on top of small craters.
What causes these depressions? The MRO team calls this “Landforms near Cerberus Tholi.” Cereberus Tholi is a a collection of several indistinct and relatively small humps that scientists think might be shield volcanoes.
More clues come from the overall context.
The location of this image is indicated by the white cross in the overview map on the right. As you can see, it is located in the middle of Mars’s volcano country, with the giant volcanoes Elysium Mons to the north and Olympus Mons to the east. To the south is the vast volcanic ash deposit dubbed Medusae Fossae, covering a region about as big as India. Just to the west is the edge of the what some scientists propose is the youngest lava field on Mars [pdf], dubbed the Athabasca Valles flood lava.
Furthermore, the darkened craters also suggest the existence of volcanic vents. To the right is the largest crater, about as wide as a football field. The dark material that the prevailing winds seem to be scattering to the west could be ash deposits. It could also be material from below ground, released at a volcanic vent.
All this superficial data suggest that we are looking at a volcanic flood plain, now extinct but once very active, as were all the volcanic features in this part of Mars. Data suggests the age of the Cereberus Tholi shields to be about 600 million years old, though the Athabasca Valles flood plain is thought to be much younger, between 500,000 to 10 million years old.
So what caused the depressions. The pdf paper about the Athabasca Valles lava flood plain gives one clue:
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.
This model is concordant with all of the available data, including the superposition and crosscutting relationships seen in the rootless cones (pseudocraters) that pepper the floor of Athabasca Valles. Thus, the flood lava that now occupies Athabasca Valles deflated, rather than inflated, in its proximal reaches before solidifying.
If I understand this interpretation correctly, this lava field, just on the outer edge of the Athabasca Valles flood plain, was thick enough to cover all of the underlying topography. As it solidified it “deflated”, producing the crater vents we see, similar to the convection bubbles you sees when you simmer tomato sauce. During that deflation the random depressions could have also formed, vaguely reflecting the underlying topography.
This interpretation could be very wrong. For example, this image is on the edge of Athabasca Valles, but it might not be part of it, which means the theory above would not apply to it.
Despite these uncertainties, it does appear that we are looking at a type of volcanic feature, produced millions of years ago and sitting relatively unchanged since then.
Readers!
Every February I run a fund-raising drive during my birthday month. This year I celebrate my 72nd birthday, and hope and plan to continue writing and posting on Behind the Black for as long as I am able.
I hope my readers will support this effort. As I did in my November fund-raising drive, I am offering autographed copies of my books for large donations. Donate $250 and you can have a choice of the hardback of either Genesis: the Story of Apollo 8 or Conscious Choice: The origins of slavery in America and why it matters today and for our future in outer space. Donate $200 and you can get an autographed paperback copy of either. IMPORTANT! If you donate enough to get a book, please email me separately to tell me which book you want and the address to mail it to.
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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.
You can support me either by giving a one-time contribution or a regular subscription. There are four ways of doing so:
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Cool image time! The photo to the right, cropped to post here, was taken by the high resolution camera on Mars Reconnaissance Orbiter (MRO) on March 2, 2020, and shows some inexplicable shallow pits and depressions in the middle of a relatively flat and featureless plain.
Make sure you click on the image to see the full photo. Though the plain looks remarkably smooth, a handful of dark splotches are scattered about, almost all of which occur on top of small craters.
What causes these depressions? The MRO team calls this “Landforms near Cerberus Tholi.” Cereberus Tholi is a a collection of several indistinct and relatively small humps that scientists think might be shield volcanoes.
More clues come from the overall context.
The location of this image is indicated by the white cross in the overview map on the right. As you can see, it is located in the middle of Mars’s volcano country, with the giant volcanoes Elysium Mons to the north and Olympus Mons to the east. To the south is the vast volcanic ash deposit dubbed Medusae Fossae, covering a region about as big as India. Just to the west is the edge of the what some scientists propose is the youngest lava field on Mars [pdf], dubbed the Athabasca Valles flood lava.
Furthermore, the darkened craters also suggest the existence of volcanic vents. To the right is the largest crater, about as wide as a football field. The dark material that the prevailing winds seem to be scattering to the west could be ash deposits. It could also be material from below ground, released at a volcanic vent.
All this superficial data suggest that we are looking at a volcanic flood plain, now extinct but once very active, as were all the volcanic features in this part of Mars. Data suggests the age of the Cereberus Tholi shields to be about 600 million years old, though the Athabasca Valles flood plain is thought to be much younger, between 500,000 to 10 million years old.
So what caused the depressions. The pdf paper about the Athabasca Valles lava flood plain gives one clue:
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.
This model is concordant with all of the available data, including the superposition and crosscutting relationships seen in the rootless cones (pseudocraters) that pepper the floor of Athabasca Valles. Thus, the flood lava that now occupies Athabasca Valles deflated, rather than inflated, in its proximal reaches before solidifying.
If I understand this interpretation correctly, this lava field, just on the outer edge of the Athabasca Valles flood plain, was thick enough to cover all of the underlying topography. As it solidified it “deflated”, producing the crater vents we see, similar to the convection bubbles you sees when you simmer tomato sauce. During that deflation the random depressions could have also formed, vaguely reflecting the underlying topography.
This interpretation could be very wrong. For example, this image is on the edge of Athabasca Valles, but it might not be part of it, which means the theory above would not apply to it.
Despite these uncertainties, it does appear that we are looking at a type of volcanic feature, produced millions of years ago and sitting relatively unchanged since then.
Readers!
Every February I run a fund-raising drive during my birthday month. This year I celebrate my 72nd birthday, and hope and plan to continue writing and posting on Behind the Black for as long as I am able.
I hope my readers will support this effort. As I did in my November fund-raising drive, I am offering autographed copies of my books for large donations. Donate $250 and you can have a choice of the hardback of either Genesis: the Story of Apollo 8 or Conscious Choice: The origins of slavery in America and why it matters today and for our future in outer space. Donate $200 and you can get an autographed paperback copy of either. IMPORTANT! If you donate enough to get a book, please email me separately to tell me which book you want and the address to mail it to.
Please consider supporting my work here at Behind the Black. My analysis of space, politics, and culture, taken from the perspective of an historian, is almost always on the money and ahead of the game. For example, in 2020 I correctly predicted that the COVID 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. Every one of those 2020 conclusions has turned out right.
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.
You can support me either by giving a one-time contribution or a regular subscription. There are four 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 or subscription:
4. 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.
Geologists and volcanologists would kill to personally ground exploring that. Rovers are good but I bet a human could do in 8 hours what the rover could do in month.