Terby (crater)
Terby is a crater on the northern edge of Hellas Planitia , Mars . It is in the Iapygia quadrangle .The 174 km diameter crater is centered at 28°S, 73°E with an elevation of −5 km. It is named after François J. Terby . It is the site of an ancient lakebed and has clay deposits. [1] Using data from Mars Global Surveyor, Mars Odyssey, Mars Express and Mars Reconnaissance Orbiter missions researchers believe Terby's layers were formed from sediments settling under water. Crater counts show this happened during the Noachian period . It used to be thought that Terby Crater contained a large delta. [2] However, newer observations have led researchers to think of the layered sequence as part of a group of layers that may have extended all the across Hellas. There is no valley large enough at the northern rim of Terby to have carried the large amount of sediments necessary to produce the layers. Other details in the layers argue against Terby containing a delta. [3] Fan deposits are some of the thickest on Mars. Hydrated minerals, including Fe/Mg phyllosilicates, have been detected in several layers. [4]
Page Revisions
| Year | Metadata | Sections | Top Words | First Paragraph |
| 2018 |
81075 characters 4 sections 9 paragraphs 11 images 655 internal links 4 external links |
terby 0.910 layers 0.205 northern 0.098 hellas 0.098 iapygia 0.098 crater 0.092 showing 0.071 reconnaissance 0.070 ctx 0.068 sediments 0.067 françois 0.062 thickest 0.060 settling 0.060 delta 0.060 174 0.053 |
Terby is a crater on the northern edge of Hellas Planitia , Mars . It is in the Iapygia quadrangle .The 174 km diameter crater is centered at 28°S, 73°E with an elevation of −5 km. It is named after François J. Terby . It is the site of an ancient lakebed and has clay deposits. [1] Using data from Mars Global Surveyor, Mars Odyssey, Mars Express and Mars Reconnaissance Orbiter missions researchers believe Terby's layers were formed from sediments settling under water. Crater counts show this happened during the Noachian period . It used to be thought that Terby Crater contained a large delta. [2] However, newer observations have led researchers to think of the layered sequence as part of a group of layers that may have extended all the across Hellas. There is no valley large enough at the northern rim of Terby to have carried the large amount of sediments necessary to produce the layers. Other details in the layers argue against Terby containing a delta. [3] Fan deposits are some of the thickest on Mars. Hydrated minerals, including Fe/Mg phyllosilicates, have been detected in several layers. [4] |
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| 2017 |
39690 characters 4 sections 9 paragraphs 14 images 161 internal links 4 external links |
terby 0.910 layers 0.205 northern 0.098 hellas 0.098 iapygia 0.098 crater 0.092 showing 0.071 reconnaissance 0.070 ctx 0.068 sediments 0.067 françois 0.062 thickest 0.060 settling 0.060 delta 0.060 174 0.053 |
Terby is a crater on the northern edge of Hellas Planitia , Mars . It is in the Iapygia quadrangle .The 174 km diameter crater is centered at 28°S, 73°E with an elevation of −5 km. It is named after François J. Terby . It is the site of an ancient lakebed and has clay deposits. [1] Using data from Mars Global Surveyor, Mars Odyssey, Mars Express and Mars Reconnaissance Orbiter missions researchers believe Terby's layers were formed from sediments settling under water. Crater counts show this happened during the Noachian period . It used to be thought that Terby Crater contained a large delta. [2] However, newer observations have led researchers to think of the layered sequence as part of a group of layers that may have extended all the across Hellas. There is no valley large enough at the northern rim of Terby to have carried the large amount of sediments necessary to produce the layers. Other details in the layers argue against Terby containing a delta. [3] Fan deposits are some of the thickest on Mars. Hydrated minerals, including Fe/Mg phyllosilicates, have been detected in several layers. [4] |
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| 2016 |
50967 characters 6 sections 12 paragraphs 15 images 163 internal links 7 external links |
terby 0.816 layers 0.200 craters 0.179 deltas 0.126 cracks 0.113 crater 0.112 delta 0.107 northern 0.088 hellas 0.088 iapygia 0.088 deposits 0.087 minerals 0.082 produced 0.066 showing 0.064 reconnaissance 0.063 |
Terby is a crater on the northern edge of Hellas Planitia , Mars . It is in the Iapygia quadrangle .The 174 km diameter crater is centered at 28°S, 73°E with an elevation of −5 km. It is named after François J. Terby . It is the site of an ancient lakebed and has clay deposits. [1] Using data from Mars Global Surveyor, Mars Odyssey, Mars Express and Mars Reconnaissance Orbiter missions researchers believe Terby's layers were formed from sediments settling under water. Crater counts show this happened during the Noachian period . It used to be thought that Terby Crater contained a large delta. [2] However, newer observations have led researchers to think of the layered sequence as part of a group of layers that may have extended all the across Hellas. There is no valley large enough at the northern rim of Terby to have carried the large amount of sediments necessary to produce the layers. Other details in the layers argue against Terby containing a delta. [3] Fan deposits are some of the thickest on Mars. Hydrated minerals, including Fe/Mg phyllosilicates, have been detected in several layers. [4] |
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| 2015 |
50966 characters 6 sections 12 paragraphs 15 images 163 internal links 7 external links |
terby 0.816 layers 0.200 craters 0.179 deltas 0.126 cracks 0.113 crater 0.112 delta 0.107 northern 0.088 hellas 0.088 iapygia 0.088 deposits 0.087 minerals 0.082 produced 0.066 showing 0.064 reconnaissance 0.063 |
Terby is a crater on the northern edge of Hellas Planitia , Mars . It is in the Iapygia quadrangle .The 174 km diameter crater is centered at 28°S, 73°E with an elevation of −5 km. It is named after François J. Terby . It is the site of an ancient lakebed and has clay deposits. [1] Using data from Mars Global Surveyor, Mars Odyssey, Mars Express and Mars Reconnaissance Orbiter missions researchers believe Terby's layers were formed from sediments settling under water. Crater counts show this happened during the Noachian period . It used to be thought that Terby Crater contained a large delta. [2] However, newer observations have led researchers to think of the layered sequence as part of a group of layers that may have extended all the across Hellas. There is no valley large enough at the northern rim of Terby to have carried the large amount of sediments necessary to produce the layers. Other details in the layers argue against Terby containing a delta. [3] Fan deposits are some of the thickest on Mars. Hydrated minerals, including Fe/Mg phyllosilicates, have been detected in several layers. [4] |
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| 2014 |
49621 characters 5 sections 12 paragraphs 15 images 162 internal links 7 external links |
terby 0.760 craters 0.217 layers 0.202 deltas 0.152 cracks 0.136 crater 0.118 iapygia 0.107 deposits 0.105 minerals 0.100 northern 0.085 impact 0.084 deposited 0.084 produced 0.079 reconnaissance 0.076 ctx 0.074 |
Terby is a crater on the northern edge of Hellas Planitia , Mars . It is in the Iapygia quadrangle .The 174 km diameter crater is centered at 28°S, 73°E with an elevation of −5 km. It is named after François J. Terby . It is the site of an ancient lakebed and has clay deposits. [1] Using data from Mars Global Surveyor, Mars Odyssey, Mars Express and Mars Reconnaissance Orbiter missions researchers believe Terby's layers were formed from sediments settling under water. Crater counts show this happened during the Noachian period . Fan deposits are some of the thickest on Mars. Hydrated minerals, including Fe/Mg phyllosilicates, have been detected in several layers. [2] |
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| 2013 |
30530 characters 2 sections 6 paragraphs 10 images 157 internal links 3 external links |
terby 0.896 layers 0.199 hellas 0.140 françois 0.132 174 0.113 lakebed 0.106 iapygia 0.105 mounds 0.089 crater 0.089 73 0.084 hirise 0.072 clay 0.067 filled 0.062 elevation 0.061 centered 0.060 |
Terby is a crater on the northern edge of Hellas Planitia , Mars . The 174 km diameter crater is centered at 28°S, 73°E with an elevation of −5 km. It is named after François J. Terby . It is the site of an ancient lakebed and has clay deposits. [1] |
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| 2011 |
9181 characters 2 sections 6 paragraphs 6 images 13 internal links 3 external links |
terby 0.896 layers 0.199 hellas 0.140 françois 0.132 174 0.113 lakebed 0.106 iapygia 0.105 mounds 0.089 crater 0.089 73 0.084 hirise 0.072 clay 0.067 filled 0.062 elevation 0.061 centered 0.060 |
Terby is a crater on the northern edge of Hellas Planitia , Mars . The 174 km diameter crater is centered at 28°S, 73°E with an elevation of −5 km. It is named after François J. Terby . It is the site of an ancient lakebed and has clay deposits. [1] |
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| 2010 |
8324 characters 2 sections 5 paragraphs 5 images 12 internal links 3 external links |
terby 0.879 layers 0.187 hellas 0.165 françois 0.156 174 0.133 lakebed 0.125 iapygia 0.123 crater 0.105 73 0.099 hirise 0.085 clay 0.079 filled 0.073 elevation 0.072 centered 0.071 basin 0.068 |
Terby is a crater on the northern edge of Hellas Planitia , Mars . The 174 km diameter crater is centered at 28°S, 73°E with an elevation of −5 km. It is named after François J. Terby . It is the site of an ancient lakebed and has clay deposits. [1] |
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| 2009 |
7996 characters 2 sections 5 paragraphs 5 images 13 internal links 3 external links |
terby 0.870 layers 0.185 hellas 0.163 françois 0.154 gallery 0.142 174 0.132 lakebed 0.124 iapygia 0.122 crater 0.104 73 0.098 hirise 0.084 clay 0.078 filled 0.073 elevation 0.071 centered 0.070 |
Terby is a crater on the northern edge of Hellas Planitia , Mars . The 174 km diameter crater is centered at 28°S, 73°E with an elevation of −5 km. It is named after François J. Terby . It is the site of an ancient lakebed and has clay deposits. |
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| 2008 |
5167 characters 1 sections 1 paragraphs 2 images 12 internal links 3 external links |
terby 0.722 françois 0.319 174 0.273 lakebed 0.257 73 0.202 hellas 0.169 clay 0.161 elevation 0.147 centered 0.145 planitia 0.130 edge 0.124 28 0.118 northern 0.102 deposits 0.100 ancient 0.097 |
Terby is a crater on the northern edge of Hellas Planitia , Mars . The 174 km diameter crater is centered at 28°S, 73°E with an elevation of −5 km. It is named after François J. Terby . It is the site of an ancient lakebed and has clay deposits. |
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| 2007 |
4245 characters 0 sections 1 paragraphs 2 images 11 internal links 0 external links |
terby 0.795 françois 0.352 lakebed 0.283 73 0.223 clay 0.178 elevation 0.162 28 0.130 deposits 0.110 ancient 0.106 site 0.104 crater 0.047 5 0.047 named 0.031 mars 0.012 |
Terby is a crater on Mars at 28°S, 73°E with an elevation of −5 km, named after François J. Terby . It is the site of an ancient lakebed and has clay deposits. |