Mars: The Terrain of Margaritifer Chaos PIA02340
The jumbled and broken terrain in the picture is known as chaotic terrain. Chaotic terrain was first observed in Mariner 6 and 7 images of Mars more than 30 years ago, and is thought to result from collapse after material--perhaps water or ice--was removed from the subsurface by events such as the formation of giant flood channels.
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Image Credit: NASA/JPL/Malin Space Science Systems  

The jumbled and broken terrain in the picture is known as chaotic terrain. Chaotic terrain was first observed in Mariner 6 and 7 images of Mars more than 30 years ago, and is thought to result from collapse after material--perhaps water or ice--was removed from the subsurface by events such as the formation of giant flood channels. The region shown here is named `Margaritifer Chaos'. The high resolution view covers a small portion of the Margaritifer Chaos at 1.8 meters per pixel. The area shown is 3 km across. Uplands are lumpy with small bright outcrops of bedrock. Lowlands or valleys in the chaotic terrain have floors covered by light-toned windblown d rifts. This image is typical of the very highest-resolution views of the equatorial latitudes of Mars. Both pictures are illuminated from the left/upper left, north is toward the top.  
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