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Some Gullies on Mars Could Be Tracks of Sliding Dry Ice
Some Gullies on Mars Could Be Tracks of Sliding Dry Ice (click to enlarge)
 
 

Some Gullies on Mars Could Be Tracks of Sliding Dry Ice

These examples of one distinctive type of Martian gullies, called "linear gullies," are on a dune in Matara Crater, seen at different times of year to observe changes. The observations support a new hypothesis that chunks of frozen carbon dioxide, also known as "dry ice," may create linear gullies. In early Martian spring at some latitudes, dry-ice blocks may glide down sandy slopes on self-generated cushions of sublimating carbon-dioxide gas, plowing the grooves as they go and sometimes leaving pits where they stop sliding and sublimate away.

The three images were taken by the High Resolution Imaging Science Experiment (HiRISE) camera on NASA's Mars Reconnaissance Orbiter, of a site at 49.4 degrees south latitude, 34.7 degrees east longitude. The top image is from Mars southern-hemisphere early summer. The middle image is from the start of spring not quite two Martian years later. The white arrow points out a frost block, which appears very bright against the defrosting dune surface. The bottom image is from later the same spring. Black arrows indicate regions where new channels and pits appeared during the intervening seasons since the top image was taken. The scale bar is 50 m (55 yards).

The three images are excerpts from HiRISE observations catalogued as ESP_013834_1300 (taken 9 July 2009); ESP_029038_1305 (taken 6 Oct. 2012) and ESP_029961_1305 (taken 17 Dec. 2012).

The University of Arizona Lunar and Planetary Laboratory operates HiRISE, which was built by Ball Aerospace & Technologies Corp., Boulder, Colo. NASA's Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the Mars Reconnaissance Orbiter for NASA's Science Mission Directorate in Washington. Lockheed Martin Space Systems, Denver, built the orbiter.

Credit: NASA/JPL-Caltech/University of Arizona



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Last Updated: 11 Jun 2013