A thick and syrupy flow on Mars
Click for full image.
Cool image time! The photo above, rotated, cropped, and reduced to post here, was taken on March 5, 2022 by the high resolution camera on Mars Reconnaissance Orbiter (MRO). It shows what the scientists label as a “viscous flow feature,” which is another way of saying the flow was thick and syrupy.
Nor is such a flow unusual in this area of Mars. It is located in a region of chaos terrain dubbed Protonilus Mensae, which is also the central mensae region in the 2,000-mile-long strip in the northern mid-latitudes of Mars I label glacier country. The overview map above of Protonilus Mensae — covering about 500 miles in width — shows how common such flows are in this place. The black rectangles mark the locations of other cool images I have featured, as follows:
- 1. Buried glaciers flowing off of Martian mesa
- 2. Brain Terrain on Mars
- 3. How to spot a glacier on Mars
- 4. Glacier country on Mars
- 5. Revisiting Mars’ glacier country
- 6. Back to Mars’ glacier country
- 7. A cracking Martian glacier?
- 8. Ice-filled craters in Mars’ glacier country?
The red rectangle indicates the location of today’s cool image.
The glacial aspect of everything in this region is even more emphasized by the wider view provided by MRO’s context camera below.
Click for full image.
North is now to the top of the photo. The large flow in the middle of this picture is the same flow in the high resolution image above.
Notice how this flow has eaten away at a large portion of its mesa. Notice also the numerous other similar flows along that same north-facing slope. Everything here appears impregnated with water ice, which over time and the cyclical swings in the red planet’s rotational tilt get alternatively heated and cooled. During periods of heating the ice sublimates away, the ground becomes structurally weaker, and these flows occur. During cooling the ice hardens, and the flows stop. Scientists presently think we are in the latter situation, though this is not yet confirmed with great certainty.
The global map below gives us a planet-wide context. The two hatched lines at 30 degrees north and south indicate the closest to the equator such glacial features have been identified. The areas outlined in white mark regions like Protonilus Mensae — which is located in the northern mid-latitudes — where such glacial features dominate.
Click for high resolution version.
Readers!
Please consider supporting my work here at Behind the Black. Your support allows 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. 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. Only now does it appear that Washington might finally 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.
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.
Click for full image.
Cool image time! The photo above, rotated, cropped, and reduced to post here, was taken on March 5, 2022 by the high resolution camera on Mars Reconnaissance Orbiter (MRO). It shows what the scientists label as a “viscous flow feature,” which is another way of saying the flow was thick and syrupy.
Nor is such a flow unusual in this area of Mars. It is located in a region of chaos terrain dubbed Protonilus Mensae, which is also the central mensae region in the 2,000-mile-long strip in the northern mid-latitudes of Mars I label glacier country. The overview map above of Protonilus Mensae — covering about 500 miles in width — shows how common such flows are in this place. The black rectangles mark the locations of other cool images I have featured, as follows:
- 1. Buried glaciers flowing off of Martian mesa
- 2. Brain Terrain on Mars
- 3. How to spot a glacier on Mars
- 4. Glacier country on Mars
- 5. Revisiting Mars’ glacier country
- 6. Back to Mars’ glacier country
- 7. A cracking Martian glacier?
- 8. Ice-filled craters in Mars’ glacier country?
The red rectangle indicates the location of today’s cool image.
The glacial aspect of everything in this region is even more emphasized by the wider view provided by MRO’s context camera below.
Click for full image.
North is now to the top of the photo. The large flow in the middle of this picture is the same flow in the high resolution image above.
Notice how this flow has eaten away at a large portion of its mesa. Notice also the numerous other similar flows along that same north-facing slope. Everything here appears impregnated with water ice, which over time and the cyclical swings in the red planet’s rotational tilt get alternatively heated and cooled. During periods of heating the ice sublimates away, the ground becomes structurally weaker, and these flows occur. During cooling the ice hardens, and the flows stop. Scientists presently think we are in the latter situation, though this is not yet confirmed with great certainty.
The global map below gives us a planet-wide context. The two hatched lines at 30 degrees north and south indicate the closest to the equator such glacial features have been identified. The areas outlined in white mark regions like Protonilus Mensae — which is located in the northern mid-latitudes — where such glacial features dominate.
Click for high resolution version.
Readers!
Please consider supporting my work here at Behind the Black. Your support allows 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. 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. Only now does it appear that Washington might finally 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.
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.
Local name: The Tongue