This image acquired on November 13, 2020 by NASAs Mars Reconnaissance Orbiter shows an area where the flowing water may have stripped away some of the rocks and soils at the bottom of the valley, leaving behind the ridge-like formations.

September 30, 2022

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Ares Vallis is a large valley that was carved billions of years ago by water flowing across the surface of Mars. This image shows an area where the flowing water may have stripped away some of the rocks and soils at the bottom of the valley, leaving behind the ridge-like formations.

In other areas of our observation, such as the smooth terrain in the middle portion of this image, the flowing water appears to have carried in and left behind rocks and soils from somewhere upstream. Scientists study landforms, rocks and soils such as these to understand how, where and when floods occurred in Mars' past.

The map is projected here at a scale of 50 centimeters (19.7 inches) per pixel. (The original image scale is 56.0 centimeters [22.0 inches] per pixel [with 2 x 2 binning]; objects on the order of 168 centimeters [66.1 inches] across are resolved.) North is up.

This is a stereo pair with ESP_066754_1935.

The University of Arizona, in Tucson, operates HiRISE, which was built by Ball Aerospace & Technologies Corp., in Boulder, Colorado. NASA's Jet Propulsion Laboratory, a division of Caltech in Pasadena, California, manages the Mars Reconnaissance Orbiter Project for NASA's Science Mission Directorate, Washington.

Credit

NASA/JPL-Caltech/University of Arizona

ENLARGE

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