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Starburst Channels
Starburst Channels
Starburst Channels   (PSP_003443_0980)
Credit: NASA/JPL/University of Arizona

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

Translucent carbon dioxide ice covers the polar regions of Mars seasonally. It is warmed and sublimates (evaporates) from below, and escaping gas carves a numerous channel morphologies.

In this example the channels form a "starburst" pattern, radiating out into feathery extensions. The center of the pattern is being buried with dust and new darker dust fans ring the outer edges. This may be an example of an expanding morphology, where new channels are formed as the older ones fill and are no longer efficiently channeling the subliming gas out.


OBSERVATION TOOLBOX
Acquisition date:21 April 2007 Local Mars time: 4:52 PM
Latitude (centered):-81.8 ° Longitude (East):76.2 °
Range to target site:247.1 km (154.4 miles)Original image scale range:24.7 cm/pixel
(with 1 x 1 binning) so objects ~74 cm across are resolved
Map projected scale:25 cm/pixelMap projection:POLAR STEREOGRAPHIC
Emission angle:1.1 ° Phase angle:69.9 °
Solar incidence angle:71 °, with the Sun about 19 ° above the horizon Solar longitude:223.4 °, Northern Autumn
For non-map projected products:
North azimuth:119 ° Sub-solar azimuth:33.1 °
For map projected products:
North azimuth:346.189°Sub solar azimuth270.585°
 

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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.