File:Garni crater Mars HiRISE Sep2015.jpg

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English: Original file description by NASA: Dark narrow streaks, called "recurring slope lineae", emanate from the walls of Garni Crater on Mars, in this view constructed from observations by the High Resolution Imaging Science Experiment (HiRISE) camera on NASA's Mars Reconnaissance Orbiter.

The dark streaks here are up to few hundred yards, or meters, long. They are hypothesized to be formed by flow of briny liquid water on Mars.

The image was produced by first creating a 3-D computer model (a digital terrain map) of the area based on stereo information from two HiRISE observations, and then draping an image over the land-shape model. The vertical dimension is exaggerated by a factor of 1.5 compared to horizontal dimensions. The draped image is a red waveband (monochrome) product from HiRISE observation ESP_031059_1685, taken on March 12, 2013 at 11.5 degrees south latitude, 290.3 degrees east longitude. Other image products from this observation are at http://hirise.lpl.arizona.edu/ESP_031059_1685.

The University of Arizona, Tucson, operates HiRISE, which was built by Ball Aerospace & Technologies Corp., Boulder, Colorado. NASA's Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the Mars Reconnaissance Orbiter Project and Mars Science Laboratory Project for NASA's Science Mission Directorate, Washington.
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来源 NASA, image-feature
作者 NASA/JPL-Caltech/Univ. of Arizona

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Public domain 本文件完全由NASA创作,在美国属于公有领域。根据NASA的版权方针,NASA的材料除非另有声明否则不受版权保护。(参见Template:PD-USGov/zhNASA版权方针页面JPL图片使用方针。)
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当前2015年10月1日 (四) 02:162015年10月1日 (四) 02:16版本的缩略图1,041 × 541(98 KB)Rfassbind{{Information |Description={{en|1=''Original file description by NASA:'' Dark narrow streaks, called "recurring slope lineae", emanate from the walls of {{w|Garni Crater}} on {{w|Mars}}, in this view constructed from observations by the High Resolution...

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