Lyot Crater
The northern plains are generally flat and smooth with few craters. However, a few large craters do stand out. The giant impact crater, Lyot, is easy to see in the northern part of Ismenius Lacus. Lyot Crater is the deepest point in Mars's northern hemisphere. One image below of Lyot Crater Dunes shows a variety of interesting forms: dark dunes, light-toned deposits, and Dust Devil Tracks. Dust devils, which resemble miniature tornados create the tracks by removing a thin, but bright deposit of dust to reveal the darker underlying surface. Light-toned deposits are widely believed to contain minerals formed in water. Research, published in June 2010, described evidence for liquid water in Lyot crater in the past.
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Lyot Crater Gullies, as seen by HiRISE.
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Lyot Crater Channel, as seen by CTX. Water-carved channels have been spotted in Lyot Crater; the curved line may be one. Click on image for a better view.
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Channels in Lyot Crater as seen by HiRISE.
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Lyot Crater Dunes, as seen by HiRISE. Click on image to see light-toned deposits and dust devil tracks.
Read more about this topic: Ismenius Lacus Quadrangle
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“Give me a condor’s quill! Give me Vesuvius’ crater for an inkstand!”
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