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Description
English: Ridges as Evidence of Fluid Alteration: Tectonic fractures within the Candor Chasma region of Valles Marineris, Mars, retain ridge-like shapes as the surrounding bedrock erodes away. This points to past episodes of fluid alteration along the fractures and reveals clues into past fluid flow and geochemical conditions below the surface. The High Resolution Imaging Science Experiment camera on NASA's Mars Reconnaissance Orbiter took this image on Dec. 2, 2006. The image is approximately 1 kilometer (0.6 mile) across. Illumination from the upper left. This view is a portion of the camera's image catalogued as PSP_001641_1735.
Date
Source http://www.nasa.gov/mission_pages/MRO/multimedia/pia09189.html
Author NASA

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Public domain This file is in the public domain in the United States because it was solely created by NASA. NASA copyright policy states that "NASA material is not protected by copyright unless noted". (See Template:PD-USGov, NASA copyright policy page or JPL Image Use Policy.)
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  • 2007-02-18 01:14 Rickyjames 330×230× (41342 bytes) NASA http://www.nasa.gov/mission_pages/MRO/multimedia/pia09189.html Ridges as Evidence of Fluid Alteration Tectonic fractures within the Candor Chasma region of Valles Marineris, Mars, retain ridge-like shapes as the surrounding bedrock erodes away. Th

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2 December 2006

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Date/TimeThumbnailDimensionsUserComment
current11:52, 18 February 2019Thumbnail for version as of 11:52, 18 February 20192,025 × 2,905 (10.2 MB)Kesäperuna100% JPEG quality from full quality TIFF.
20:51, 13 March 2009Thumbnail for version as of 20:51, 13 March 2009330 × 230 (40 KB)File Upload Bot (Magnus Manske) {{BotMoveToCommons|en.wikipedia|year={{subst:CURRENTYEAR}}|month={{subst:CURRENTMONTHNAME}}|day={{subst:CURRENTDAY}}}} {{Information |Description={{en|NASA http://www.nasa.gov/mission_pages/MRO/multimedia/pia09189.html Ridges as Evidence of Fluid Alter

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