Fingerprint Terrain with Sawtooth Patterns in the South Polar Ice Cap
NASA/JPL-Caltech/UArizona
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  (22 August 2007)

 
Acquisition date
07 August 2007

Local Mars time
17:31

Latitude (centered)
-86.222°

Longitude (East)
308.741°

Spacecraft altitude
243.9 km (151.6 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/pixel

Map projection
Polarstereographic

Emission angle
0.1°

Phase angle
66.2°

Solar incidence angle
66°, with the Sun about 24° above the horizon

Solar longitude
290.8°, Northern Winter

For non-map projected images
North azimuth:  135°
Sub-solar azimuth:  50.3°
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non-map           (288MB)

IRB color
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non-map           (214MB)

Merged IRB
map projected  (90MB)

Merged RGB
map-projected  (83MB)

RGB color
non map           (181MB)
ADDITIONAL INFORMATION
B&W label
Color label
Merged IRB label
Merged RGB label
EDR products
HiView

NB
IRB: infrared-red-blue
RGB: red-green-blue
About color products (PDF)

Black & white is 5 km across; enhanced color about 1 km
For scale, use JPEG/JP2 black & white map-projected images

USAGE POLICY
All of the images produced by HiRISE and accessible on this site are within the public domain: there are no restrictions on their usage by anyone in the public, including news or science organizations. We do ask for a credit line where possible:
NASA/JPL-Caltech/UArizona

POSTSCRIPT
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. The HiRISE camera was built by Ball Aerospace and Technology Corporation and is operated by the University of Arizona.