Ring mold crater
A Ring mold crater is a kind of crater on the planet Mars that looks like the ring molds used in baking. They are believed 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." They are also bigger than other craters in which an asteroid impacted solid rock. 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.
Page Revisions
| Year | Metadata | Sections | Top Words | First Paragraph |
| 2018 |
80861 characters 3 sections 16 paragraphs 13 images 643 internal links 1 external links |
mold 0.772 ring 0.429 hiwish 0.210 hirise 0.150 craters 0.138 ice 0.135 program 0.111 ismenius 0.092 view 0.082 lacus 0.080 undergoes 0.071 shape 0.063 crater 0.056 debris 0.054 image 0.050 |
A Ring mold crater is a kind of crater on the planet Mars that looks like the ring molds used in baking. They are believed 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." They are also bigger than other craters in which an asteroid impacted solid rock. 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. |
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| 2017 |
38859 characters 3 sections 15 paragraphs 16 images 151 internal links 1 external links |
mold 0.766 ring 0.427 hiwish 0.220 hirise 0.157 craters 0.145 ice 0.130 program 0.116 ismenius 0.096 view 0.086 lacus 0.083 undergoes 0.074 shape 0.066 debris 0.056 image 0.053 crater 0.052 |
Ring Mold Craters are a kind of crater on the planet Mars , that look like the ring molds used in baking. They are believed 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." They are also bigger than other craters in which an asteroid impacted solid rock. 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. |
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| 2016 |
33525 characters 3 sections 9 paragraphs 10 images 150 internal links 1 external links |
mold 0.742 ring 0.424 ice 0.189 hiwish 0.145 craters 0.135 hirise 0.114 undergoes 0.108 shape 0.095 ismenius 0.093 debris 0.082 lacus 0.081 image 0.077 program 0.077 baking 0.070 insulate 0.070 |
Ring Mold Craters are a kind of crater on the planet Mars , that look like the ring molds used in baking. They are believed 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." They are also bigger than other craters in which an asteroid impacted solid rock. 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. |
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| 2015 |
34991 characters 3 sections 9 paragraphs 11 images 154 internal links 1 external links |
mold 0.742 ring 0.424 ice 0.189 hiwish 0.145 craters 0.135 hirise 0.114 undergoes 0.108 shape 0.095 ismenius 0.093 debris 0.082 lacus 0.081 image 0.077 program 0.077 baking 0.070 insulate 0.070 |
Ring Mold Craters are a kind of crater on the planet Mars , that look like the ring molds used in baking. They are believed 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." They are also bigger than other craters in which an asteroid impacted solid rock. 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. |
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| 2013 |
8564 characters 2 sections 5 paragraphs 4 images 12 internal links 0 external links |
mold 0.657 ring 0.405 ice 0.279 shape 0.169 debris 0.144 baking 0.124 insulate 0.124 molds 0.120 mamers 0.120 image 0.109 footprint 0.107 craters 0.106 impacts 0.099 deuteronilus 0.093 lineated 0.089 |
Ring Mold Craters are kind of crater on the planet Mars , that look like the ring molds used in baking. They are believed 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." They are also bigger than other craters in which an asteroid impacted solid rock. 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. |
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| 2011 |
5382 characters 1 sections 3 paragraphs 2 images 5 internal links 0 external links |
mold 0.573 ring 0.378 ice 0.292 shape 0.165 baking 0.162 molds 0.157 mamers 0.157 image 0.142 footprint 0.141 impacts 0.130 debris 0.126 deuteronilus 0.122 lineated 0.117 dichotomy 0.116 mensae 0.109 |
Ring Mold Craters are kind of crater on the planet Mars , that look like the ring molds used in baking. They are believed 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." They are also bigger than other craters in which an asteroid impacted solid rock. 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. |
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| 2010 |
5571 characters 2 sections 3 paragraphs 2 images 3 internal links 0 external links |
mold 0.576 ring 0.380 ice 0.294 shape 0.166 baking 0.163 molds 0.158 mamers 0.158 image 0.143 footprint 0.141 impacts 0.130 debris 0.127 deuteronilus 0.123 lineated 0.118 dichotomy 0.117 mensae 0.109 |
Ring Mold Craters look like the ring molds used in baking. They are believed 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." They are also bigger than other craters in which an asteroid impacted solid rock. 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. |