Layering in Central Candor Chasma
NASA/JPL/University of Arizona

Layering in Central Candor Chasma
ESP_025112_1750  Science Theme: Tectonic Processes
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A Context Camera (CTX) image of this area shows faulted layered deposits near the contact between the layered deposits and wall rock.

At HiRISE resolution, we may be able to discern any structural relationships, which may yield insight into relative age of these layered deposits and faulting to basin formation. As part of a stereo pair (linked below), we can measure bedding and fault orientations.

This observation is in an area of high hematite abundance. On Earth, hematite is a mineral formed in an aqueous environment. Its presence on Mars can help us understand what the past environment was like that formed it.

This caption is based on the original science rationale.

Written by: HiRISE Science Team   (6 February 2013)

This is a stereo pair with ESP_019732_1750.



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Acquisition date:05 December 2011 Local Mars time: 2:46 PM
Latitude (centered):-5.180 degrees Longitude (East):286.110 degrees
Range to target site:265.6 km (166.0 miles)Original image scale range:26.6 cm/pixel (with 1 x 1 binning) so objects ~80 cm across are resolved
Map projected scale:25 cm/pixel and North is upMap projection:EQUIRECTANGULAR
Emission angle:2.3 degrees Phase angle:44.2 degrees
Solar incidence angle:46 degrees, with the Sun about 44 degrees above the horizon Solar longitude:39.0 degrees, Northern Spring
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North azimuth:97 degrees Sub-solar azimuth:32.9 degrees
For map-projected products
North azimuth:270 degreesSub solar azimuth:207.4 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.