Uranius Mons

Uranius Mons , ^[1] formerly Uranius Patera , is a volcano on Mars located in the Tharsis quadrangle , named after a classical albedo feature. The name "Uranius Patera" now refers only to the volcano's central caldera. ^[2] It is about three kilometers high and has shallow slopes. It belongs to the Uranius group of volcanoes in the Tharsis area. The sides of Uranius Mons consist of radial lava flows; the large caldera (90×65 km) is elongated in the southwestern direction. The surrounding plains are younger and part of the Tharsis Montes Formation of the Amazonian epoch . ^[3]

Page Revisions

Year	Metadata	Sections	Top Words	First Paragraph
2018	32608 characters 1 sections 2 paragraphs 7 images 155 internal links 3 external links	1. References	uranius 0.752 caldera 0.248 tharsis 0.245 patera 0.218 volcano 0.168 belongs 0.159 mons 0.149 southwestern 0.136 amazonian 0.111 radial 0.111 epoch 0.108 elongated 0.106 refers 0.097 montes 0.097 younger 0.095	Uranius Mons , ^[1] formerly Uranius Patera , is a volcano on Mars located in the Tharsis quadrangle , named after a classical albedo feature. The name "Uranius Patera" now refers only to the volcano's central caldera. ^[2] It is about three kilometers high and has shallow slopes. It belongs to the Uranius group of volcanoes in the Tharsis area. The sides of Uranius Mons consist of radial lava flows; the large caldera (90×65 km) is elongated in the southwestern direction. The surrounding plains are younger and part of the Tharsis Montes Formation of the Amazonian epoch . ^[3]
2017	32466 characters 1 sections 2 paragraphs 7 images 155 internal links 3 external links	1. References	uranius 0.752 caldera 0.248 tharsis 0.245 patera 0.218 volcano 0.168 belongs 0.159 mons 0.149 southwestern 0.136 amazonian 0.111 radial 0.111 epoch 0.108 elongated 0.106 refers 0.097 montes 0.097 younger 0.095	Uranius Mons , ^[1] formerly Uranius Patera , is a volcano on Mars located in the Tharsis quadrangle , named after a classical albedo feature. The name "Uranius Patera" now refers only to the volcano's central caldera. ^[2] It is about three kilometers high and has shallow slopes. It belongs to the Uranius group of volcanoes in the Tharsis area. The sides of Uranius Mons consist of radial lava flows; the large caldera (90 x 65 km) is elongated in the southwestern direction. The surrounding plains are younger and part of the Tharsis Montes Formation of the Amazonian epoch . ^[3]
2016	31550 characters 1 sections 2 paragraphs 7 images 155 internal links 3 external links	1. References	uranius 0.752 caldera 0.248 tharsis 0.245 patera 0.218 volcano 0.168 belongs 0.159 mons 0.149 southwestern 0.136 amazonian 0.111 radial 0.111 epoch 0.108 elongated 0.106 refers 0.097 montes 0.097 younger 0.095	Uranius Mons , ^[1] formerly Uranius Patera , is a volcano on Mars located in the Tharsis quadrangle , named after a classical albedo feature. The name "Uranius Patera" now refers only to the volcano's central caldera. ^[2] It is about three kilometers high and has shallow slopes. It belongs to the Uranius group of volcanoes in the Tharsis area. The sides of Uranius Mons consist of radial lava flows; the large caldera (90 x 65 km) is elongated in the southwestern direction. The surrounding plains are younger and part of the Tharsis Montes Formation of the Amazonian epoch . ^[3]
2014	31457 characters 1 sections 1 paragraphs 7 images 155 internal links 3 external links	1. References	uranius 0.752 caldera 0.248 tharsis 0.245 patera 0.218 volcano 0.168 belongs 0.159 mons 0.149 southwestern 0.136 amazonian 0.111 radial 0.111 epoch 0.108 elongated 0.106 refers 0.097 montes 0.097 younger 0.095	Uranius Mons , ^[1] formerly Uranius Patera , is a volcano on Mars located in the Tharsis quadrangle , named after a classical albedo feature. The name "Uranius Patera" now refers only to the volcano's central caldera. ^[2] It is about three kilometers high and has shallow slopes. It belongs to the Uranius group of volcanoes in the Tharsis area. The sides of Uranius Mons consist of radial lava flows; the large caldera (90 x 65 km) is elongated in the southwestern direction. The surrounding plains are younger and part of the Tharsis Montes Formation of the Amazonian epoch . ^[3]
2013	30634 characters 1 sections 1 paragraphs 6 images 155 internal links 3 external links	1. References	uranius 0.752 caldera 0.248 tharsis 0.245 patera 0.218 volcano 0.168 belongs 0.159 mons 0.149 southwestern 0.136 amazonian 0.111 radial 0.111 epoch 0.108 elongated 0.106 refers 0.097 montes 0.097 younger 0.095	Uranius Mons , ^[1] formerly Uranius Patera , is a volcano on Mars located in the Tharsis quadrangle , named after a classical albedo feature. The name "Uranius Patera" now refers only to the volcano's central caldera. ^[2] It is about three kilometers high and has shallow slopes. It belongs to the Uranius group of volcanoes in the Tharsis area. The sides of Uranius Mons consist of radial lava flows; the large caldera (90 x 65 km) is elongated in the southwestern direction. The surrounding plains are younger and part of the Tharsis Montes Formation of the Amazonian epoch . ^[3]
2012	9518 characters 1 sections 2 paragraphs 2 images 11 internal links 3 external links	1. References	uranius 0.752 caldera 0.248 tharsis 0.245 patera 0.218 volcano 0.168 belongs 0.159 mons 0.149 southwestern 0.136 amazonian 0.111 radial 0.111 epoch 0.108 elongated 0.106 refers 0.097 montes 0.097 younger 0.095	Uranius Mons , ^[1] formerly Uranius Patera , is a volcano on Mars located in the Tharsis quadrangle , named after a classical albedo feature. The name "Uranius Patera" now refers only to the volcano's central caldera. ^[2] It is about three kilometers high and has shallow slopes. It belongs to the Uranius group of volcanoes in the Tharsis area. The sides of Uranius Mons consist of radial lava flows; the large caldera (90 x 65 km) is elongated in the southwestern direction. The surrounding plains are younger and part of the Tharsis Montes Formation of the Amazonian epoch . ^[3]
2011	5033 characters 1 sections 2 paragraphs 2 images 10 internal links 0 external links	1. References	uranius 0.616 tharsis 0.335 patera 0.298 belongs 0.217 southwestern 0.186 shields 0.174 caldera 0.169 amazonian 0.151 radial 0.151 epoch 0.148 elongated 0.145 montes 0.132 younger 0.129 shallow 0.125 volcano 0.115	Uranius Patera is a volcano on Mars located in the Tharsis quadrangle . It is about three kilometers high and has shallow slopes. It belongs to Uranius group of volcanoes in the Tharsis area. Side of Uranius Patera consist of radial lava flows with few low shields with the large caldera (90 x 65 km) which is elongated in the southwestern direction. The surrounding plains are younger and part of the Tharsis Montes Formation in Amazonian epoch . ^[1]
2010	5032 characters 1 sections 2 paragraphs 2 images 10 internal links 0 external links	1. References	uranius 0.617 tharsis 0.335 patera 0.299 belongs 0.217 southwestern 0.186 shields 0.174 caldera 0.169 amazonian 0.151 radial 0.151 epoch 0.148 elongated 0.145 montes 0.132 younger 0.129 shallow 0.125 volcano 0.115	Uranius Patera is a volcano on Mars located in the Tharsis quadrangle . It is about 3 kilometers high and it has shallow slopes. It belongs to Uranius group of volcanoes in the Tharsis area. Side of Uranius Patera consist of radial lava flows with few low shields with the large caldera (90 x 65 km) which is elongated in the southwestern direction. The surrounding plains are younger and part of the Tharsis Montes Formation in Amazonian epoch . ^[1]
2009	4966 characters 1 sections 2 paragraphs 2 images 9 internal links 0 external links	1. References	uranius 0.617 tharsis 0.335 patera 0.299 belongs 0.217 southwestern 0.186 shields 0.174 caldera 0.169 amazonian 0.151 radial 0.151 epoch 0.148 elongated 0.145 montes 0.132 younger 0.129 shallow 0.125 volcano 0.115	Uranius Patera is a volcano on Mars located in the Tharsis quadrangle. It is about 3 kilometers high and it has shallow slopes. It belongs to Uranius group of volcanoes in the Tharsis area. Side of Uranius Patera consist of radial lava flows with few low shields with the large caldera (90 x 65 km) which is elongated in the southwestern direction. The surrounding plains are younger and part of the Tharsis Montes Formation in Amazonian epoch . ^[1]