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Pedestal Crater in the Medusa Fossae Formation (PSP_003253_1880)

Pedestal Crater in the Medusa Fossae Formation
Pedestal Crater in the Medusa Fossae Formation (PSP_003253_1880)
Credit: NASA/JPL/University of Arizona

This image shows a pedestal crater located in a geologic unit on Mars called the Medusa Fossae Formation.

Pedestal craters are produced by differential erosion around impact craters. If the ejecta (material thrown out of the crater) is more resistant to erosion, then the crater and surrounding ejecta will be preserved while the surface is eroded nearby. This causes the ejecta blanket surrounding the crater to form a "pedestal," standing out in relief rather than gradually merging into its surroundings.

There appear to be at least two resistant layers in the material around this pedestal crater, as there are two "steps" in the topography of the pedestal. The cutout (2196x1442, 3 MB), from the long ridge near the top center of the image, shows these steps as well as possible smaller-scale layering.

Despite the detail resolved by HiRISE, it is not clear why the step-forming layers are more resistant. Much of the scene is coated with a mantle of dust which obscures details. Dark slope streaks, likely produced by small avalanches in the dust, are common here. Dust deposition and erosion are also likely the reason for the scalloped texture of mantling material in the crater.
Written by: Colin Dundas

OBSERVATION TOOLBOX
Acquisition date:06 April 2007 Local Mars time: 3:35 PM
Latitude (centered):7.7 ° Longitude (East):196.2 °
Range to target site:276.8 km (173.0 miles)Original image scale range:55.4 cm/pixel
(with 2 x 2 binning) so objects ~166 cm across are resolved
Map projected scale:50 cm/pixel and north is upMap projection:EQUIRECTANGULAR
Emission angle:1.2 ° Phase angle:58.8 °
Solar incidence angle:58 °, with the Sun about 32 ° above the horizon Solar longitude:214.3 °, Northern Autumn
For non-map projected products:
North azimuth:97 ° Sub-solar azimuth:344.2 °
F O R   M A P   P R O J E C T E D   P R O D U C T S
North azimuth:270°Sub solar azimuth158.2°

 

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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: Image: NASA/JPL/University of Arizona


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.