Miyamoto (crater)
Miyamoto is a crater lying situated within the Margaritifer Sinus quadrangle (MC-19) region of the planet Mars , west of the Plains of Meridiani . The crater is 150 kilometers (93 mi) wide. The crater's northeastern half is filled with rocks formed in the presence of water and include minerals of iron and sulfur, which likely settled on lake bottoms or in groundwater systems. In the southwestern half of the crater floor, erosion has stripped these materials away, instead revealing clays and other materials like those found in the most ancient Martian rocks. More than 3.5 billion years old, they date to the Noachian era at which time, liquid water was likely present at the surface and could have created an environment favorable to life. [1] [2]
Page Revisions
| Year | Metadata | Sections | Top Words | First Paragraph |
| 2018 |
85072 characters 3 sections 8 paragraphs 8 images 665 internal links 10 external links |
miyamoto 0.660 inverted 0.352 sites 0.148 sediments 0.145 minerals 0.133 crater 0.132 channels 0.120 clays 0.112 examine 0.102 margaritifer 0.099 channel 0.098 life 0.095 laboratory 0.095 sinus 0.094 eberswalde 0.084 |
Miyamoto is a crater lying situated within the Margaritifer Sinus quadrangle (MC-19) region of the planet Mars , west of the Plains of Meridiani . The crater is 150 kilometers (93 mi) wide. The crater's northeastern half is filled with rocks formed in the presence of water and include minerals of iron and sulfur, which likely settled on lake bottoms or in groundwater systems. In the southwestern half of the crater floor, erosion has stripped these materials away, instead revealing clays and other materials like those found in the most ancient Martian rocks. More than 3.5 billion years old, they date to the Noachian era at which time, liquid water was likely present at the surface and could have created an environment favorable to life. [1] [2] |
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| 2017 |
42527 characters 3 sections 8 paragraphs 10 images 176 internal links 9 external links |
miyamoto 0.660 inverted 0.352 sites 0.148 sediments 0.145 minerals 0.133 crater 0.132 channels 0.120 clays 0.112 examine 0.102 margaritifer 0.099 channel 0.098 life 0.095 laboratory 0.095 sinus 0.094 eberswalde 0.084 |
Miyamoto is a crater lying situated within the Margaritifer Sinus quadrangle (MC-19) region of the planet Mars , west of the Plains of Meridiani . The crater is 150 kilometers (93 mi) wide. The crater's northeastern half is filled with rocks formed in the presence of water and include minerals of iron and sulfur, which likely settled on lake bottoms or in groundwater systems. In the southwestern half of the crater floor, erosion has stripped these materials away, instead revealing clays and other materials like those found in the most ancient Martian rocks. More than 3.5 billion years old, they date to the Noachian era at which time, liquid water was likely present at the surface and could have created an environment favorable to life. [1] [2] |
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| 2016 |
40840 characters 3 sections 7 paragraphs 10 images 174 internal links 8 external links |
miyamoto 0.660 inverted 0.352 sites 0.148 sediments 0.145 minerals 0.133 crater 0.132 channels 0.120 clays 0.112 examine 0.102 margaritifer 0.099 channel 0.098 life 0.095 laboratory 0.095 sinus 0.094 eberswalde 0.084 |
Miyamoto is a crater lying situated within the Margaritifer Sinus quadrangle (MC-19) region of the planet Mars , west of the Plains of Meridiani . The crater is 150 kilometers (93 mi) wide. The crater's northeastern half is filled with rocks formed in the presence of water and include minerals of iron and sulfur, which likely settled on lake bottoms or in groundwater systems. In the southwestern half of the crater floor, erosion has stripped these materials away, instead revealing clays and other materials like those found in the most ancient Martian rocks. More than 3.5 billion years old, they date to the Noachian era at which time, liquid water was likely present at the surface and could have created an environment favorable to life. [1] [2] |
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| 2015 |
39666 characters 3 sections 7 paragraphs 10 images 167 internal links 7 external links |
miyamoto 0.662 inverted 0.353 sites 0.148 sediments 0.146 minerals 0.133 crater 0.133 channels 0.121 clays 0.113 examine 0.102 margaritifer 0.100 channel 0.098 life 0.096 laboratory 0.095 sinus 0.094 eberswalde 0.085 |
Miyamoto is a crater lying situated within the Margaritifer Sinus quadrangle (MC-19) region of the planet Mars , west of the Plains of Meridiani . The crater is 150 kilometers (93 mi) wide. The crater's northeastern half is filled with rocks formed in the presence of water and include minerals of iron and sulfur, which likely settled on lake bottoms or in groundwater systems. In the southwestern half of the crater floor, erosion has stripped these materials away, instead revealing clays and other materials like those found in the most ancient Martian rocks. More than 3.5 billion years old, they date to the Noachian era at which time, liquid water was likely present at the surface and could have created an environment favorable to life. [1] [2] |
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| 2014 |
38855 characters 3 sections 6 paragraphs 10 images 167 internal links 6 external links |
miyamoto 0.662 inverted 0.353 sites 0.148 sediments 0.146 minerals 0.133 crater 0.133 channels 0.121 clays 0.113 examine 0.102 margaritifer 0.100 channel 0.098 life 0.096 laboratory 0.095 sinus 0.094 eberswalde 0.085 |
Miyamoto is a crater lying situated within the Margaritifer Sinus quadrangle (MC-19) region of the planet Mars , west of the Plains of Meridiani . The crater is 150 kilometers (93 mi) wide. The crater's northeastern half is filled with rocks formed in the presence of water and include minerals of iron and sulfur, which likely settled on lake bottoms or in groundwater systems. In the southwestern half of the crater floor, erosion has stripped these materials away, instead revealing clays and other materials like those found in the most ancient Martian rocks. More than 3.5 billion years old, they date to the Noachian era at which time, liquid water was likely present at the surface and could have created an environment favorable to life. [1] [2] |
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| 2013 |
37880 characters 3 sections 6 paragraphs 9 images 167 internal links 6 external links |
miyamoto 0.662 inverted 0.353 sites 0.148 sediments 0.146 minerals 0.133 crater 0.133 channels 0.121 clays 0.113 examine 0.102 margaritifer 0.100 channel 0.098 life 0.096 laboratory 0.095 sinus 0.094 eberswalde 0.085 |
Miyamoto is a crater lying situated within the Margaritifer Sinus quadrangle (MC-19) region of the planet Mars , west of the Plains of Meridiani . The crater is 150 kilometers (93 mi) wide. The crater's northeastern half is filled with rocks formed in the presence of water and include minerals of iron and sulfur, which likely settled on lake bottoms or in groundwater systems. In the southwestern half of the crater floor, erosion has stripped these materials away, instead revealing clays and other materials like those found in the most ancient Martian rocks. More than 3.5 billion years old, they date to the Noachian era at which time, liquid water was likely present at the surface and could have created an environment favorable to life. [1] [2] |
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| 2012 |
16387 characters 3 sections 6 paragraphs 5 images 23 internal links 6 external links |
miyamoto 0.670 inverted 0.357 sites 0.150 sediments 0.148 minerals 0.134 crater 0.134 channels 0.122 clays 0.114 examine 0.103 channel 0.100 life 0.097 laboratory 0.096 eberswalde 0.086 bottoms 0.084 iani 0.084 |
Miyamoto is a crater on Mars , west of the Plains of Meridiani . The crater is 150 kilometers (93 mi) wide. The crater's northeastern half is filled with rocks formed in the presence of water and include minerals of iron and sulfur, which likely settled on lake bottoms or in groundwater systems. In the southwestern half of the crater floor, erosion has stripped these materials away, instead revealing clays and other materials like those found in the most ancient Martian rocks. More than 3.5 billion years old, they date to the Noachian era at which time, liquid water was likely present at the surface and could have created an environment favorable to life. [1] [2] |
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| 2011 |
15537 characters 3 sections 6 paragraphs 4 images 23 internal links 6 external links |
miyamoto 0.670 inverted 0.357 sites 0.150 sediments 0.148 minerals 0.134 crater 0.134 channels 0.122 clays 0.114 examine 0.103 channel 0.100 life 0.097 laboratory 0.096 eberswalde 0.086 bottoms 0.084 iani 0.084 |
Miyamoto is a crater on Mars , west of the Plains of Meridiani . The crater is 150 kilometers (93 mi) wide. The crater's northeastern half is filled with rocks formed in the presence of water and include minerals of iron and sulfur, which likely settled on lake bottoms or in groundwater systems. In the southwestern half of the crater floor, erosion has stripped these materials away, instead revealing clays and other materials like those found in the most ancient Martian rocks. More than 3.5 billion years old, they date to the Noachian era at which time, liquid water was likely present at the surface and could have created an environment favorable to life. [1] [2] |
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| 2010 |
12184 characters 2 sections 6 paragraphs 4 images 20 internal links 4 external links |
miyamoto 0.669 inverted 0.357 sites 0.150 sediments 0.147 minerals 0.134 crater 0.134 channels 0.122 clays 0.114 examine 0.103 channel 0.100 life 0.097 laboratory 0.096 eberswalde 0.086 bottoms 0.084 iani 0.084 |
Miyamoto is a crater on Mars , west of the Plains of Meridiani . The crater is 150 kilometers (93 miles) wide. The crater's northeastern half is filled with rocks formed in the presence of water and include minerals of iron and sulfur, which likely settled on lake bottoms or in groundwater systems. In the southwestern half of the crater floor, erosion has stripped these materials away, instead revealing clays and other materials like those found in the most ancient Martian rocks. More than 3.5 billion years old, they date to the Noachian era at which time, liquid water was likely present at the surface and could have created an environment favorable to life. [1] [2] |
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| 2009 |
11468 characters 2 sections 5 paragraphs 4 images 19 internal links 4 external links |
miyamoto 0.623 inverted 0.222 sites 0.186 sediments 0.183 clays 0.141 crater 0.136 examine 0.128 minerals 0.125 channel 0.124 laboratory 0.119 eberswalde 0.106 bottoms 0.104 iani 0.104 holden 0.102 eroded 0.100 |
Miyamoto is a crater on Mars , west of the Plains of Meridiani . The crater is 150 kilometers (93 miles) wide. The crater's northeastern half is filled with rocks formed in the presence of water and include minerals of iron and sulfur, which likely settled on lake bottoms or in groundwater systems. In the southwestern half of the crater floor, erosion has stripped these materials away, instead revealing clays and other materials like those found in the most ancient Martian rocks. More than 3.5 billion years old, they date to the Noachian era at which time, liquid water was likely present at the surface and could have created an environment favorable to life. [1] [2] |
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| 2008 |
7636 characters 1 sections 2 paragraphs 3 images 17 internal links 1 external links |
miyamoto 0.489 bottoms 0.245 southwestern 0.205 stripped 0.198 northeastern 0.194 half 0.186 revealing 0.180 settled 0.178 materials 0.174 clays 0.167 rocks 0.165 favorable 0.164 era 0.152 meridiani 0.146 noachian 0.145 |
Miyamoto is a crater on Mars , west of the Plains of Meridiani . The crater is 150 kilometers (93 miles) wide. The crater's northeastern half is filled with rocks formed in the presence of water and include minerals of iron and sulfur, which likely settled on lake bottoms or in groundwater systems. In the southwestern half of the crater floor, erosion has stripped these materials away, instead revealing clays and other materials like those found in the most ancient Martian rocks. More than 3.5 billion years old, they date to the Noachian era at which time, liquid water was likely present at the surface and could have created an environment favorable to life. [1] [2] |