Martian Crater May Once Have Held Groundwater-Fed Lake
This view of layered
rocks on the floor of McLaughlin Crater shows sedimentary rocks that
contain spectroscopic evidence for minerals formed through interaction
with water. The High Resolution Imaging Science Experiment (HiRISE)
camera on NASA's Mars Reconnaissance Orbiter recorded the image. Image
Credit: NASA/JPL-Caltech/Univ. of Arizona› Full image and caption
|
January 20, 2013
The new information comes from researchers analyzing spectrometer data from NASA's Mars Reconnaissance Orbiter, which looked down on the floor of McLaughlin Crater. The Martian crater is 57 miles (92 kilometers) in diameter and 1.4 miles (2.2 kilometers) deep. McLaughlin's depth apparently once allowed underground water, which otherwise would have stayed hidden, to flow into the crater's interior.
More - Link >>> http://www.jpl.nasa.gov/news/news.php?release=2013-028&cid=release_2013-028
Sources: Jet Propulsion Laboratory, NASA.
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