Layering in Central Candor Chasma
NASA/JPL-Caltech/UArizona
Layering in Central Candor Chasma
ESP_025112_1750  Science Theme: Tectonic Processes
A Context Camera 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, 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 (narration: Tre Gibbs)  (6 February 2013)

This is a stereo pair with ESP_019732_1750.
 
Acquisition date
05 December 2011

Local Mars time
14:46

Latitude (centered)
-5.180°

Longitude (East)
286.110°

Spacecraft altitude
265.6 km (165.1 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 up

Map projection
Equirectangular

Emission angle
2.3°

Phase angle
44.2°

Solar incidence angle
46°, with the Sun about 44° above the horizon

Solar longitude
39.0°, Northern Spring

For non-map projected images
North azimuth:  97°
Sub-solar azimuth:  32.9°
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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:
NASA/JPL-Caltech/UArizona

POSTSCRIPT
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. The HiRISE camera was built by Ball Aerospace and Technology Corporation and is operated by the University of Arizona.