Fingerprint Terrain with Sawtooth Patterns in the South Polar Ice Cap
NASA/JPL/University of Arizona

Fingerprint Terrain with Sawtooth Patterns in the South Polar Ice Cap
PSP_004820_0940  Science Theme: Polar Geology


This image shows a portion of the south polar ice cap. The ice you see here is frozen carbon dioxide rather than the frozen water you are used to here on Earth.

Even on Mars, where the temperatures are much lower than on Earth, carbon dioxide ice is a volatile substance. As it is so unstable, large amounts can sublimate (change from a solid into a gas) very quickly when heated. In this ice cap we can see icy features shrink in size by several meters per year as the ice that makes them up is removed by solar heating. Usually these icy features are almost circular as you get equal amounts of sunlight from every direction when you are at the pole.

However, in this location something strange has happened. Instead of the usual circular features we see features that are decidedly linear in shape. These sets of linear features have been dubbed "fingerprint terrain" by planetary scientists. They are seen in several locations in this ice cap and usually have a wavelength close to 90 meters (295 feet). It's hard to understand why linear features would form in this sort of environment by sublimation of ice alone. It is possible that these features are formed instead by atmospheric processes. Either the features are sand dunes covered by a thin covering of frost or they might be made up of loose ice crystals that saltate like sand grains and have collected into ripples.

It would be a huge surprise to find sand dunes in this location, just as you wouldn't expect to see sand dunes on top of the Greenland ice sheet on Earth. To confirm that they are made of carbon dioxide ice, HiRISE will image this location again at the end of the year and compare it to this image to look for changes. Icy features should show large changes, but sand dunes move much more slowly.Written by: Shane Byrne   (29 August 2007)



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Acquisition date:07 August 2007 Local Mars time: 5:31 PM
Latitude (centered):-86.2 degrees Longitude (East):308.7 degrees
Range to target site:243.9 km (152.4 miles)Original image scale range:24.4 cm/pixel (with 1 x 1 binning) so objects ~73 cm across are resolved
Map projected scale:25 cm/pixelMap projection:POLAR STEREOGRAPHIC
Emission angle:0.1 degrees Phase angle:66.2 degrees
Solar incidence angle:66 degrees, with the Sun about 24 degrees above the horizon Solar longitude:290.8 degrees, Northern Winter
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North azimuth:195 degrees Sub-solar azimuth:50.0 degrees
For map-projected products
North azimuth:218.7 degreesSub solar azimuth:134.1 degrees

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For information about NASA and agency programs on the Web, visit: http://www.nasa.gov. NASA's Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, Calif., manages the Mars Reconnaissance Orbiter for NASA's Science Mission Directorate, Washington. Lockheed Martin Space Systems is the prime contractor for the project and built the spacecraft. The HiRISE camera was built by Ball Aerospace and Technology Corporation and is operated by the University of Arizona. The image data were processed using the U.S. Geological Survey’s ISIS3 software.