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Ring Mold Craters are kind of crater on the planet Mars, that look like the ring molds used in baking. They are thought to be caused by an impact into ice. The ice is covered by a layer of debris. They are found in parts of Mars that have buried ice. Laboratory experiments confirm that impacts into ice result in a "ring mold shape".
Impacts into ice warm the ice and cause it to flow into the ring mold shape. These craters are common in lobate debris aprons and lineated valley fill. Many have been found in Mamers Valles, a channel found along the dichotomy boundary in Deuteronilus Mensae. [1] [2] [3] They may be an easy way for future colonists of Mars to find water ice.
The ice is covered by a layer of debris. They are found in parts of Mars that have buried ice. The shape is caused by a rebound of the ice. Laboratory experiments confirm that impacts into ice result in a "ring mold shape". [11] [12] [13] They may be an easy way for future colonists of Mars to find water ice.
Ring mold craters are believed to be formed from asteroid impacts into ground that has an underlying layer of ice. The impact produces a rebound of the ice layer to form a "ring-mold" shape. Ring mold craters on floor of a crater, as seen by HiRISE under HiWish program Location is Ismenius Lacus quadrangle .
A Ring mold crater looks like the ring molds used in baking. Many researchers believe they are created by an impact into ice. Many researchers believe they are created by an impact into ice. The ice is covered by a layer of debris, but many impacts are strong enough to penetrate far enough to go into the ice layer.
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Much of the area in high latitudes, especially the Ismenius Lacus quadrangle, is believed to still contain enormous amounts of water ice. [ 16 ] [ 19 ] [ 21 ] In March 2010, scientists released the results of a radar study of an area called Deuteronilus Mensae that found widespread evidence of ice lying beneath a few meters of rock debris. [ 22 ]