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Lizard-Skin Surface Texture
Lizard-Skin Surface Texture
Lizard-Skin Surface Texture  (PSP_003730_0945)
Credit: NASA/JPL/University of Arizona

This caption is part of a December 2007 AGU presentation "Spring at the South Pole of Mars."

The south polar region of Mars is covered seasonally with translucent carbon dioxide ice. In the spring gas subliming (evaporating) from the underside of the seasonal layer of ice bursts through weak spots, carrying dust from below with it, to form numerous dust fans aligned in the direction of the prevailing wind.

The dust gets trapped in the shallow grooves on the surface, helping to define the small-scale structure of the surface. The surface texture is reminiscent of lizard skin.


OBSERVATION TOOLBOX
Acquisition date:14 May 2007 Local Mars time: 6:04 PM
Latitude (centered):-85.2 ° Longitude (East):181.5 °
Range to target site:248.5 km (155.3 miles)Original image scale range:24.9 cm/pixel
(with 1 x 1 binning) so objects ~75 cm across are resolved
Map projected scale:25 cm/pixelMap projection:POLAR STEREOGRAPHIC
Emission angle:7.0 ° Phase angle:63.7 °
Solar incidence angle:69 °, with the Sun about 21 ° above the horizon Solar longitude:237.5 °, Northern Autumn
For non-map projected products:
North azimuth:172 ° Sub-solar azimuth:36.3 °
For map projected products:
North azimuth:91.5085°Sub solar azimuth358.634°

 

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P O S T S C R I P T

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.