A Martian starburst spider
Cool image time! The photo to the right, cropped to post here, illustrates an example of a wholly unique Martian phenomenon, that is not only unique to Mars but is also found only in its south polar regions. The image was taken on July 17, 2020 by the high resolution camera on Mars Reconnaissance Orbiter (MRO).
What we are looking at is a permanent spider formation etched into the layered deposits of ice and dirt that cover the widest area surrounding Mars’ south pole. The blue dot just north of Chasma Australe on the overview map below shows the location of these starbursts, on those layered deposits.
Each winter the poles of Mars are blanketed with a thin mantle of dry ice, generally less than six feet thick. When spring arrives and sunlight hits this mantle, it heats the ice and sand on which the mantle lies, and that warmth causes the mantle’s base to sublimate back into gas. Eventually gas pressure causes the mantle to crack at its weak points so the gas can escape. By the time summer arrives that mantle is entirely gone, all of it returning to the atmosphere as CO2 gas.
This sublimation process differs between the north and south pole, due to the different terrain found at each. In the north the mantle mostly lies on ice or sand dunes, neither of which is stable over repeated years. Thus, the mantle weak points do not occur at the exact same place each year, even though they occur at the same type of locations, such as the base and crests of dunes.
In the south however the ground is more stable, so that each year the trapped gas at the base of the mantle travels upward along the same exact paths, repeatedly etching into that ground the meandering spider patterns we see in the image above.
Think of these lines as river tributaries, except that the flow here is gas and it is upward to the surface, not downward following gravity. Moreover, in the case of these starbursts, the flow is going uphill on all sides of a small peak, until the separate flows meet at the top, where they escape.
Essentially the starbursts are vaguely reflecting the surface topography of the layered ice/dust deposit on which they sit. At this spot there several high points, and surrounding each is a starburst.
I’ve said it before, but it bears repeating: Mars is strange. Mars is alien. Mars epitomizes the universe in all its glory.
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Cool image time! The photo to the right, cropped to post here, illustrates an example of a wholly unique Martian phenomenon, that is not only unique to Mars but is also found only in its south polar regions. The image was taken on July 17, 2020 by the high resolution camera on Mars Reconnaissance Orbiter (MRO).
What we are looking at is a permanent spider formation etched into the layered deposits of ice and dirt that cover the widest area surrounding Mars’ south pole. The blue dot just north of Chasma Australe on the overview map below shows the location of these starbursts, on those layered deposits.
Each winter the poles of Mars are blanketed with a thin mantle of dry ice, generally less than six feet thick. When spring arrives and sunlight hits this mantle, it heats the ice and sand on which the mantle lies, and that warmth causes the mantle’s base to sublimate back into gas. Eventually gas pressure causes the mantle to crack at its weak points so the gas can escape. By the time summer arrives that mantle is entirely gone, all of it returning to the atmosphere as CO2 gas.
This sublimation process differs between the north and south pole, due to the different terrain found at each. In the north the mantle mostly lies on ice or sand dunes, neither of which is stable over repeated years. Thus, the mantle weak points do not occur at the exact same place each year, even though they occur at the same type of locations, such as the base and crests of dunes.
In the south however the ground is more stable, so that each year the trapped gas at the base of the mantle travels upward along the same exact paths, repeatedly etching into that ground the meandering spider patterns we see in the image above.
Think of these lines as river tributaries, except that the flow here is gas and it is upward to the surface, not downward following gravity. Moreover, in the case of these starbursts, the flow is going uphill on all sides of a small peak, until the separate flows meet at the top, where they escape.
Essentially the starbursts are vaguely reflecting the surface topography of the layered ice/dust deposit on which they sit. At this spot there several high points, and surrounding each is a starburst.
I’ve said it before, but it bears repeating: Mars is strange. Mars is alien. Mars epitomizes the universe in all its glory.
In order to remain completely independent and honest in my writing, I accept no sponsorships from big space companies or any political organizations. Nor do I depend on ads.
Instead, I rely entirely on the generosity of readers to keep Behind the Black running. You can either make a one time donation for whatever amount you wish, or you sign up for a monthly subscription ranging from $2 to $15 through Paypal, or $3 to $50 through Patreon, or any amount through Zelle.
The best method to donate or subscribe is by using Zelle through your internet bank account, since it charges no fees to you or I. You will need to give my name and email address (found at the bottom of the "About" page). What you donate is what I get.
To use Patreon, go to my website there and pick one of five monthly subscription amounts, or by making a one-time donation.
For PayPal click one of the following buttons:
If these electronic payment methods don't work for you, you can support Behind The Black directly by sending your donation by check, payable to Robert Zimmerman, to
Behind The Black
c/o Robert Zimmerman
P.O.Box 1262
Cortaro, AZ 85652
Mars has “continental sized” dust storms yearly, and a global one on average about every 6 years. Doesn’t the movement of dust change the landscape as imaged from orbit, as permanent features are covered and uncovered?
LocalFluff: The answer is yes, but only to a somewhat limited extent. The atmosphere is just not thick enough and thus cannot blow hard enough to physically change much.
See these posts for some examples however:
You will notice that most of the changes are somewhat superficial. The winds didn’t change things much besides the appearance of the ground’s top surface.
I must add that we are talking about the short term seasonal changes. Over a very long time (thousands of years) the winds can erode a lot, just as they do on Earth. It just takes longer.
In the larger scale image of the Ice cap region, I presume the zone marked “layered ice/dust” is just water ice? Or is there dry ice mixed in there too?
Brad: Click on the link under the words “south pole.” I go into some detail about the south pole. The layered deposits are exactly what I wrote, layered deposits of ice and dust mixed together. It is part of the permanent cap, but unlike the north pole, it is not covered by the purer residual permanent icecap. In the south the residual permanent ice cap covers only a small portion.
Brad: I just realized I did not answer your question. There is no dry ice in the layered deposits. The only time we see dry ice at the poles is in the winter when the CO2 in the atmosphere falls as dry ice snow to create the seasonal mantle on top of the ice.
And the Red Planet Mars Red Dust Storms that would mean Winds could mars have Winds?
Angry Red Planet of spiders