HiRISE images

Hills, boulders, and wind
Published 6/17/2013 in Lori Fenton's Blog Author lfenton
A piece of Mars: In the lower left of the image, a small hill stands above a plain partly covered by stabilized ripples. Boulders have rolled down the hill as it slowly erodes. If these ripples aren't ever activated by the wind again, they will one day be completely buried by sediment eroded from this and other surrounding hills. (HiRISE ESP_031215_1830, NASA/JPL/University of Arizona) read more ❯

Where does martian sand come from?
Published 5/24/2013 in Lori Fenton's Blog Author lfenton
A piece of Mars: The source of dune sand on Mars is normally something of a mystery. But here on the interior wall of a small crater it appears that small gullies have eroded sediment from the wall and carried it down toward the center of the crater (toward the upper right). The bluish and tan regions are the material the gullies have transported, and the bluish sediments have formed into small aeolian ripples. The mystery is solved for this one small region of Mars: is it the same story elsewhere? (HiRISE ESP_030915_1290, NASA/JPL/University of Arizona) read more ❯

Dunes on crater bones
Published 5/2/2013 in Lori Fenton's Blog Author lfenton
A piece of Mars. The dark circle (~170 m across) in the middle of the picture is the interior of what used to be a crater. It's now almost completely eroded away, probably by the wind. Small dunes have formed on these former crater sediments -- because the dunes seem to form mostly on this circular plateau, it's likely that they're made from sand derived from the former crater sediments (and thus these dunes have not traveled far). (HiRISE ESP_030622_2060, NASA/JPL/University of Arizona) read more ❯

Modern art or windy Mars?
Published 4/16/2013 in Lori Fenton's Blog Author lfenton
A piece of Mars: Is it modern art? Well maybe it looks like it from a distance. Up close, this is reality on Mars. These are dark dunes in the southern hemisphere, awaking from a long hibernation beneath bright winter frost (a touch of which can still be seen in white patches). The wind has begun to shape the dunes, leaving crayon streaks where dust devils have swept by. Maybe we'll see those little ripples move this summer. (HiRISE ESP_030602_1080, NASA/JPL/University of Arizona) read more ❯

Giant crayons on Mars
Published 3/27/2013 in Lori Fenton's Blog Author lfenton
A piece of Mars: There are vast plains on Mars that display criss-crossing streaks like this. These are ~5 m (~16 feet) across, give or take. Did an alien drive a dune buggy all over, leaving behind tracks? Nope. These are the distinctive trails made by the passage of dust devils, which act like huge vacuum cleaners that suck up dust from the ground. The patterns of the tracks change every year as new dust devils churn away at the surface. (HiRISE ESP_030916_1250, NASA/JPL/University of Arizona) read more ❯

Dunes in the spring
Published 3/22/2013 in Lori Fenton's Blog Author lfenton
A piece of Mars: Dunes near the north and south poles get cold in the winter, just like they do on Earth. Except on Mars instead of H2O ice, it's a mix of CO2 and H2O ice (mostly CO2). In the spring the white ice slowly disappears, revealing the dark dunes underneath. (HiRISE PSP_002033_1325, NASA/JPL/University of Arizona) read more ❯

Nili Patera
Published 3/19/2013 in Lori Fenton's Blog Author lfenton
A piece of Mars: Nili Patera on Mars is an ancient volcano. Some of the old volcanic material has been blown into rather striking sand dunes. It is the first place where dunes were conclusively identified as actively moving. Here's a closeup of one of them -- the steep slip face on the downwind side indicates these dunes are moving to the lower left. This dune migrates about a meter every year. (HiRISE ESP_030210_1890, NASA/JPL/University of Arizona) read more ❯

Almost a dune
Published 3/7/2013 in Lori Fenton's Blog Author lfenton
A piece of Mars: Not all piles of windblown sand are able to form proper dunes, with a fully developed avalanche on the downwind side. Here, bluish sand tries to make its way through hilly terrain, which both traps the sand and makes it difficult for slip faces (avalanches) to form. Smaller, now stabilized dunes in the upper right were also trapped by the hills. (HiRISE ESP_030570_1440, NASA/JPL/University of Arizona) read more ❯

Those feathery bright dunes on Mars
Published 2/22/2013 in Lori Fenton's Blog Author lfenton
A piece of Mars: Some of the dunes on Mars are just plain weird. Here are some feather-shaped ones. I'm not sure anybody knows why they form these fractal shapes just yet. I don't know of anything on Earth that looks like these. (HiRISE ESP_028024_1830 NASA/JPL/University of Arizona) read more ❯

Dunes. Just dunes.
Published 2/1/2013 in Lori Fenton's Blog Author lfenton
A piece of Mars: These large dunes are located in Kaiser crater, a big crater in the southern midlatitudes. The scene is 789x592 m across. Imagine standing on one of these monsters, and seeing nothing but pristine ripples criscrossing all over the place. (HiRISE ESP_029500_1330, NASA/JPL/University of Arizona) read more ❯

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