Very Recent Impact Crater
NASA/JPL/University of Arizona

Very Recent Impact Crater
ESP_015962_1695  Science Theme: Impact Processes
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This image shows a very fresh-looking impact crater with extensive radial ejecta.

The crater was first seen in an image acquired with MRO's Context Camera (CTX). The best image of this region prior to CTX was from one of the Viking Orbiters, and the crater isn't apparent in that image. This could mean that the crater formed sometime between 1976 and 1999, or there may have been more dust on the surface in 1976 or the air may have been hazy, obscuring the crater.

Based on the HiRISE image, we suspect that the crater is more than several decades old, because at full resolution we see a textured surface that is common in dust-mantled regions of Mars, but absent in the youngest craters.
Written by: Alfred McEwen   (13 January 2010)



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Acquisition date:22 December 2009 Local Mars time: 2:42 PM
Latitude (centered):-10.6 degrees Longitude (East):254.1 degrees
Range to target site:255.9 km (159.9 miles)Original image scale range:25.6 cm/pixel (with 1 x 1 binning) so objects ~77 cm across are resolved
Map projected scale:25 cm/pixel and North is upMap projection:EQUIRECTANGULAR
Emission angle:6.7 degrees Phase angle:51.6 degrees
Solar incidence angle:46 degrees, with the Sun about 44 degrees above the horizon Solar longitude:27.1 degrees, Northern Spring
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North azimuth:97 degrees Sub-solar azimuth:32.8 degrees
For map-projected products
North azimuth:270 degreesSub solar azimuth:207.1 degrees

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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.