This image, captured on 27 March 2008, reveals unprecedented detail of an enigmatic feature on the Martian surface.

With a scale of 56 centimeters per pixel (about two feet), the image shows the upper reaches of an outflow channel in Ares Valles. Outflow channels are the sites where massive catastrophic releases of a fluid, presumably water, poured out of the subsurface in flooding events on orders of magnitude larger than anything we have ever witnessed on Earth.

The image, oriented diagonal to the channel, just covers the channel from bank to bank. It is near the release point for the water—a jumbled region called chaotic terrain to the south. Impact craters on the channel provide a means of estimating the age of the flooding event, although the channel bottom may be covered by younger materials such as lava. There are also sand dunes in relatively low areas that formed long after the flooding had ceased.

The Mars Pathfinder landed to the northwest of here in 1997 (see PSP_001890_1995).
Written by: Andrea Philippoff

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: Image: NASA/JPL/University of Arizona

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.