Structure of the North Polar Layered Deposits
NASA/JPL/University of Arizona

Structure of the North Polar Layered Deposits
PSP_010008_2630  Science Theme: Polar Geology
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This image shows an exposure of the north polar layered deposits (NPLD) within the northern residual ice cap. The polar layered deposits are thought to have been formed by recent climate changes on Mars, like ice ages on Earth.

Scientists are studying the NPLD to learn more about these climate changes on Mars. In many places, the NPLD layers appear to extend over large areas, suggesting that they were deposited from atmospheric suspension. If the layers in this image are horizontal and continuous, the apparent curves are caused by erosion of valleys into the NPLD. To determine whether this is the case, HiRISE has acquired two images of this location to form a stereo pair. Analysis of this stereo pair will allow the orientation and thickness of the layers to be measured across the region of stereo coverage, constraining hypotheses for their formation.

Also visible in this image are bright and dark streaks that may be caused by the redistribution of frost by winds.
Written by: Ken Herkenhoff   (12 November 2008)

This is a stereo pair with PSP_009969_2630.



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Acquisition date:14 September 2008 Local Mars time: 1:07 PM
Latitude (centered):82.9 degrees Longitude (East):40.9 degrees
Range to target site:330.4 km (206.5 miles)Original image scale range:33.1 cm/pixel (with 1 x 1 binning) so objects ~99 cm across are resolved
Map projected scale:25 cm/pixelMap projection:POLAR STEREOGRAPHIC
Emission angle:16.8 degrees Phase angle:77.4 degrees
Solar incidence angle:63 degrees, with the Sun about 27 degrees above the horizon Solar longitude:127.0 degrees, Northern Summer
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North azimuth:126 degrees Sub-solar azimuth:321.8 degrees
For map-projected products
North azimuth:229.1 degreesSub solar azimuth:66.96 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.