Arcadia Planitia
Arcadia Planitia is a smooth plain with fresh lava flows and Amazonian volcanic flows on Mars . It was named by Giovanni Schiaparelli in 1882 after the Arcadia region of ancient Greece . It dates from the Amazonian period 's Arcadia formation's lava flows and small cinder cones . It includes a more recently developed large region of aeolian materials derived from periglacial processes. It is located northwest of the Tharsis region in the northern lowlands, spanning roughly the region 40-60° North and 150-180° West [1] , straddling partly in the Cebrenia quadrangle (MC-07), and partly in the Diacria one (MC-02), and centered at 47°12′N 184°18′E / 47.2°N 184.3°E . [2] Arcadia marks a transition from the thinly cratered terrain to its north and the very old cratered terrain to the south. On its east it runs into the Alba Mons volcanoes. Its elevation relative to the geodetic datum varies between 0 and -3 km. [3]
Page Revisions
| Year | Metadata | Sections | Top Words | First Paragraph |
| 2018 |
50513 characters 6 sections 10 paragraphs 12 images 200 internal links 7 external links |
arcadia 0.496 ice 0.252 gullies 0.238 expanded 0.208 184 0.207 planitia 0.152 craters 0.144 excess 0.144 47 0.120 ground 0.114 secondary 0.112 incised 0.109 amazonian 0.094 partly 0.094 gully 0.090 |
Arcadia Planitia is a smooth plain with fresh lava flows and Amazonian volcanic flows on Mars . It was named by Giovanni Schiaparelli in 1882 after the Arcadia region of ancient Greece . It dates from the Amazonian period 's Arcadia formation's lava flows and small cinder cones . It includes a more recently developed large region of aeolian materials derived from periglacial processes. It is located northwest of the Tharsis region in the northern lowlands, spanning roughly the region 40-60° North and 150-180° West [1] , straddling partly in the Cebrenia quadrangle (MC-07), and partly in the Diacria one (MC-02), and centered at 47°12′N 184°18′E / 47.2°N 184.3°E . [2] Arcadia marks a transition from the thinly cratered terrain to its north and the very old cratered terrain to the south. On its east it runs into the Alba Mons volcanoes. Its elevation relative to the geodetic datum varies between 0 and -3 km. [3] |
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| 2017 |
50713 characters 6 sections 10 paragraphs 12 images 201 internal links 8 external links |
arcadia 0.496 ice 0.252 gullies 0.238 expanded 0.208 184 0.207 planitia 0.152 craters 0.144 excess 0.144 47 0.120 ground 0.114 secondary 0.112 incised 0.109 amazonian 0.094 partly 0.094 gully 0.090 |
Arcadia Planitia is a smooth plain with fresh lava flows and Amazonian volcanic flows on Mars . It was named by Giovanni Schiaparelli in 1882 after the Arcadia region of ancient Greece . It dates from the Amazonian period 's Arcadia formation's lava flows and small cinder cones . It includes a more recently developed large region of aeolian materials derived from periglacial processes. It is located northwest of the Tharsis region in the northern lowlands, spanning roughly the region 40-60° North and 150-180° West [1] , straddling partly in the Cebrenia quadrangle (MC-07), and partly in the Diacria one (MC-02), and centered at 47°12′N 184°18′E / 47.2°N 184.3°E . [2] Arcadia marks a transition from the thinly cratered terrain to its north and the very old cratered terrain to the south. On its east it runs into the Alba Mons volcanoes. Its elevation relative to the geodetic datum varies between 0 and -3 km. [3] |
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| 2016 |
48319 characters 5 sections 9 paragraphs 13 images 205 internal links 7 external links |
arcadia 0.587 gullies 0.281 184 0.245 planitia 0.180 47 0.142 incised 0.129 amazonian 0.111 gully 0.106 flows 0.103 cratered 0.097 thinly 0.095 linux 0.095 enlarged 0.094 geodetic 0.091 proposition 0.088 |
Arcadia Planitia is a smooth plain with fresh lava flows and Amazonian volcanic flows on Mars . It was named by Giovanni Schiaparelli in 1882 after the Arcadia region of ancient Greece . It dates from the Amazonian period 's Arcadia formation's lava flows and small cinder cones . It includes a more recently developed large region of aeolian materials derived from periglacial processes. It is located northwest of the Tharsis region in the northern lowlands, spanning the region 40-60° North and 150-180° West in the Cebrenia quadrangle and centered at 47°12′N 184°18′E / 47.2°N 184.3°E . [1] Part of it is in the Diacria quadrangle . Arcadia marks a transition from the thinly cratered terrain to its north and the very old cratered terrain to the south. On its east it runs into the Alba Mons volcanoes. Its elevation relative to the geodetic datum varies between 0 and -3 km. [2] |
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| 2015 |
40862 characters 4 sections 6 paragraphs 11 images 171 internal links 6 external links |
arcadia 0.545 gullies 0.294 184 0.256 planitia 0.150 47 0.149 incised 0.135 amazonian 0.116 gully 0.111 flows 0.108 cratered 0.102 thinly 0.099 linux 0.099 enlarged 0.098 geodetic 0.095 proposition 0.092 |
Arcadia Planitia is a smooth plain with fresh lava flows and Amazonian volcanic flows on Mars . It was named by Giovanni Schiaparelli in 1882 after the Arcadia region of ancient Greece . It dates from the Amazonian period 's Arcadia formation's lava flows and small cinder cones . It includes a more recently developed large region of aeolian materials derived from periglacial processes. It is located northwest of the Tharsis region in the northern lowlands, spanning the region 40-60° North and 150-180° West in the Cebrenia quadrangle and centered at 47°12′N 184°18′E / 47.2°N 184.3°E . [1] Part of it is in the Diacria quadrangle . Arcadia marks a transition from the thinly cratered terrain to its north and the very old cratered terrain to the south. On its east it runs into the Alba Mons volcanoes. Its elevation relative to the geodetic datum varies between 0 and -3 km. [2] |
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| 2013 |
31932 characters 3 sections 2 paragraphs 8 images 162 internal links 4 external links |
arcadia 0.569 192 0.297 46 0.206 amazonian 0.161 flows 0.150 cratered 0.141 thinly 0.138 linux 0.138 geodetic 0.133 proposition 0.128 materials 0.127 thawing 0.125 cinder 0.118 periglacial 0.116 lava 0.112 |
Arcadia Planitia is a smooth plain with fresh lava flows and Amazonian volcanic flows on Mars . It was named by Giovanni Schiaparelli in 1882 after the Arcadia region of ancient Greece . It dates from the Amazonian period 's Arcadia formation's lava flows and small cinder cones . It includes a more recently developed large region of aeolian materials derived from periglacial processes. It is located northwest of the Tharsis region in the northern lowlands, spanning the region 40-60° North and 150-180° West in the Cebrenia quadrangle and centered at 46°42′N 192°00′E / 46.7°N 192.0°E . Arcadia marks a transition from the thinly cratered terrain to its north and the very old cratered terrain to the south. On its east it runs into the Alba Mons volcanoes. Its elevation relative to the geodetic datum varies between 0 and -3 km. [1] |
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| 2012 |
10638 characters 3 sections 3 paragraphs 4 images 21 internal links 4 external links |
arcadia 0.569 192 0.297 46 0.206 amazonian 0.161 flows 0.150 cratered 0.141 thinly 0.138 linux 0.138 geodetic 0.133 proposition 0.128 materials 0.127 thawing 0.125 cinder 0.118 periglacial 0.116 lava 0.112 |
Arcadia Planitia is a smooth plain with fresh lava flows and Amazonian volcanic flows on Mars . It was named by Giovanni Schiaparelli in 1882 after the Arcadia region of ancient Greece . It dates from the Amazonian period 's Arcadia formation's lava flows and small cinder cones . It includes a more recently developed large region of aeolian materials derived from periglacial processes. It is located northwest of the Tharsis region in the northern lowlands, spanning the region 40-60° North and 150-180° West in the Cebrenia quadrangle and centered at 46°42′N 192°00′E / 46.7°N 192.0°E . Arcadia marks a transition from the thinly cratered terrain to its north and the very old cratered terrain to the south. On its east it runs into the Alba Mons volcanoes. Its elevation relative to the geodetic datum varies between 0 and -3 km. [1] |
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| 2011 |
10676 characters 3 sections 3 paragraphs 4 images 22 internal links 4 external links |
arcadia 0.569 192 0.297 46 0.206 amazonian 0.161 flows 0.150 cratered 0.141 thinly 0.138 linux 0.138 geodetic 0.133 proposition 0.128 materials 0.127 thawing 0.125 cinder 0.118 periglacial 0.116 lava 0.112 |
Arcadia Planitia is a smooth plain with fresh lava flows and Amazonian volcanic flows on Mars . It was named by Giovanni Schiaparelli in 1882 after the Arcadia region of ancient Greece . It dates from the Amazonian period 's Arcadia formation's lava flows and small cinder cones . It includes a more recently developed large region of aeolian materials derived from periglacial processes. It is located northwest of the Tharsis region in the northern lowlands, spanning the region 40-60° North and 150-180° West in the Cebrenia quadrangle and centered at 46°42′N 192°00′E / 46.7°N 192.0°E . Arcadia marks a transition from the thinly cratered terrain to its north and the very old cratered terrain to the south. On its east it runs into the Alba Mons volcanoes. Its elevation relative to the geodetic datum varies between 0 and -3 km. [1] |
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| 2010 |
10676 characters 3 sections 3 paragraphs 4 images 22 internal links 4 external links |
arcadia 0.569 192 0.297 46 0.206 amazonian 0.161 flows 0.150 cratered 0.141 thinly 0.138 linux 0.138 geodetic 0.133 proposition 0.128 materials 0.127 thawing 0.125 cinder 0.118 periglacial 0.116 lava 0.112 |
Arcadia Planitia is a smooth plain with fresh lava flows and Amazonian volcanic flows on Mars . It was named by Giovanni Schiaparelli in 1882 after the Arcadia region of ancient Greece . It dates from the Amazonian period 's Arcadia formation's lava flows and small cinder cones . It includes a more recently developed large region of aeolian materials derived from periglacial processes. It is located northwest of the Tharsis region in the northern lowlands, spanning the region 40-60° North and 150-180° West in the Cebrenia quadrangle and centered at 46°42′N 192°00′E / 46.7°N 192.0°E . Arcadia marks a transition from the thinly cratered terrain to its north and the very old cratered terrain to the south. On its east it runs into the Alba Mons volcanoes. Its elevation relative to the geodetic datum varies between 0 and -3 km. [1] |
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| 2009 |
10676 characters 3 sections 3 paragraphs 4 images 22 internal links 4 external links |
arcadia 0.569 192 0.297 46 0.206 amazonian 0.161 flows 0.150 cratered 0.141 thinly 0.138 linux 0.138 geodetic 0.133 proposition 0.128 materials 0.127 thawing 0.125 cinder 0.118 periglacial 0.116 lava 0.112 |
Arcadia Planitia is a smooth plain with fresh lava flows and Amazonian volcanic flows on Mars . It was named by Giovanni Schiaparelli in 1882 after the Arcadia region of ancient Greece . It dates from the Amazonian period 's Arcadia formation's lava flows and small cinder cones . It includes a more recently developed large region of aeolian materials derived from periglacial processes. It is located northwest of the Tharsis region in the northern lowlands, spanning the region 40-60° North and 150-180° West in the Cebrenia quadrangle and centered at 46°42′N 192°00′E / 46.7°N 192.0°E . Arcadia marks a transition from the thinly cratered terrain to its north and the very old cratered terrain to the south. On its east it runs into the Alba Mons volcanoes. Its elevation relative to the geodetic datum varies between 0 and -3 km. [1] |
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| 2008 |
10738 characters 3 sections 2 paragraphs 4 images 24 internal links 4 external links |
arcadia 0.569 192 0.297 46 0.206 amazonian 0.161 flows 0.150 cratered 0.141 thinly 0.138 linux 0.138 geodetic 0.133 proposition 0.128 materials 0.127 thawing 0.125 cinder 0.118 periglacial 0.116 lava 0.112 |
Arcadia Planitia is a smooth plain with fresh lava flows and Amazonian volcanic flows on Mars . It was named by Giovanni Schiaparelli in 1882 after the Arcadia region of ancient Greece . It dates from the Amazonian period 's Arcadia formation's lava flows and small cinder cones . It includes a more recently developed large region of aeolian materials derived from periglacial processes. It is located northwest of the Tharsis region in the northern lowlands, spanning the region 40-60° North and 150-180° West in the Cebrenia quadrangle and centered at 46°42′N 192°00′E / 46.7°N 192.0°E . Arcadia marks a transition from the thinly cratered terrain to its north and the very old cratered terrain to the south. On its east it runs into the Alba Mons volcanoes. Its elevation relative to the geodetic datum varies between 0 and -3 km. [1] |
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| 2007 |
8868 characters 3 sections 2 paragraphs 2 images 24 internal links 3 external links |
arcadia 0.513 192 0.322 46 0.223 amazonian 0.175 flows 0.162 cratered 0.153 thinly 0.149 proposition 0.139 materials 0.137 thawing 0.135 cinder 0.128 periglacial 0.126 lava 0.121 1882 0.121 region 0.121 |
Arcadia Planitia is a smooth plain with fresh lava flows and Amazonian volcanic flows on Mars . It was named by Giovanni Schiaparelli in 1882 after the Arcadia region of ancient Greece . It dates from the Amazonian period 's Arcadia formation's lava flows and small cinder cones . It includes a more recently developed large region of aeolian materials derived from periglacial processes. It is located northwest of the Tharsis region in the northern lowlands, spanning the region 40-60° North and 150-180° West in the Cebrenia quadrangle and centered at 46°42′N 192°00′E / 46.7°N 192.0°E . Arcadia marks a transition from the thinly cratered terrain to its north and the very old cratered terrain to the south. On its east it runs into the Alba Patera volcanoes. Its elevation relative to the datum varies between 0 and -3 km. [1] |
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| 2006 |
7820 characters 3 sections 3 paragraphs 2 images 24 internal links 2 external links |
arcadia 0.564 amazonian 0.192 flows 0.179 cratered 0.168 thinly 0.165 proposition 0.153 materials 0.151 thawing 0.148 cinder 0.141 periglacial 0.138 lava 0.134 1882 0.133 region 0.133 alba 0.123 finds 0.118 |
Arcadia Planitia is a smooth plain with fresh lava flows and Amazonian volcanic flows on Mars . It was named by Giovanni Schiaparelli in 1882 after the Arcadia region of ancient Greece . It dates from the Amazonian period 's Arcadia formation's lava flows and small cinder cones . It includes a more recently developed large region of aeolian materials derived from periglacial processes. It is located northwest of the Tharsis region in the northern lowlands, spanning the region 40-60° North and 150-180° West in the Cebrenia quadrangle. Arcadia marks a transition from the thinly cratered terrain to its north and the very old cratered terrain to the south. On its east it runs into the Alba Patera volcanoes. Its elevation relative to the datum varies between 0 and -3 km. [1] |