HiRISE | Impact Crater Filled with Layered Deposits (PSP_001410

NASA/JPL/University of Arizona

Impact Crater Filled with Layered Deposits
PSP_001410_2210 Science Theme: Sedimentary/Layering Processes

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This image shows an impact crater in Utopia Planitia, in the northern hemisphere of Mars, that is filled with layered material.

The layered character of these deposits is consistent with episodic deposition. Each distinct layer represents a period of sediment deposition. The layers are parallel to each other, indicating that deposition occurred by material settling onto the surface, rather than being blown across the surface in sand dunes.

The hummocky texture of these deposits suggests that volatiles (such as carbon dioxide ice) are mixed in with the rocky sediment.
Written by: Chris Okubo (11 December 2009)

This is a stereo pair with PSP_002175_2210.

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Acquisition date:	14 November 2006	Local Mars time:	3:22 PM
Latitude (centered):	40.8 degrees	Longitude (East):	99.5 degrees
Range to target site:	295.9 km (184.9 miles)	Original image scale range:	from 29.6 cm/pixel (with 1 x 1 binning) to 59.2 cm/pixel (with 2 x 2 binning)
Map projected scale:	25 cm/pixel and North is up	Map projection:	EQUIRECTANGULAR
Emission angle:	1.7 degrees	Phase angle:	47.5 degrees
Solar incidence angle:	49 degrees, with the Sun about 41 degrees above the horizon	Solar longitude:	135.2 degrees, Northern Summer
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North azimuth:	97 degrees	Sub-solar azimuth:	352.0 degrees
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North azimuth:	270 degrees	Sub solar azimuth:	167.3 degrees

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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

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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.