Hephaestus Fossae
The Hephaestus Fossae are a system of troughs and channels in the Amenthes quadrangle of Mars, with a location centered at 21.1 N and 237.5 W. They are 604 km long and were named after a classical albedo feature name. [1] The fossae have been tentatively identified as outflow channels , but their origin and evolution remain ambiguous. [2] It has been proposed that water may have been released into the troughs as a catastrophic flood due to subsurface ice melting following a large bolide impact. [3]
Page Revisions
| Year | Metadata | Sections | Top Words | First Paragraph |
| 2018 |
70726 characters 2 sections 1 paragraphs 3 images 646 internal links 3 external links |
bolide 0.331 604 0.302 troughs 0.289 hephaestus 0.284 237 0.277 fossae 0.271 ambiguous 0.242 tentatively 0.242 amenthes 0.235 channels 0.197 flood 0.181 catastrophic 0.179 outflow 0.143 melting 0.142 evolution 0.140 |
The Hephaestus Fossae are a system of troughs and channels in the Amenthes quadrangle of Mars, with a location centered at 21.1 N and 237.5 W. They are 604 km long and were named after a classical albedo feature name. [1] The fossae have been tentatively identified as outflow channels , but their origin and evolution remain ambiguous. [2] It has been proposed that water may have been released into the troughs as a catastrophic flood due to subsurface ice melting following a large bolide impact. [3] |
|
| 2017 |
29345 characters 2 sections 1 paragraphs 6 images 152 internal links 3 external links |
bolide 0.331 604 0.302 troughs 0.289 hephaestus 0.284 237 0.277 fossae 0.271 ambiguous 0.242 tentatively 0.242 amenthes 0.235 channels 0.197 flood 0.181 catastrophic 0.179 outflow 0.143 melting 0.142 evolution 0.140 |
The Hephaestus Fossae are a system of troughs and channels in the Amenthes quadrangle of Mars, with a location centered at 21.1 N and 237.5 W. They are 604 km long and were named after a classical albedo feature name. [1] The fossae have been tentatively identified as outflow channels , but their origin and evolution remain ambiguous. [2] It has been proposed that water may have been released into the troughs as a catastrophic flood due to subsurface ice melting following a large bolide impact. [3] |
|
| 2016 |
27205 characters 1 sections 1 paragraphs 6 images 151 internal links 2 external links |
bolide 0.331 604 0.302 troughs 0.289 hephaestus 0.284 237 0.277 fossae 0.271 ambiguous 0.242 tentatively 0.242 amenthes 0.235 channels 0.197 flood 0.181 catastrophic 0.179 outflow 0.143 melting 0.142 evolution 0.140 |
The Hephaestus Fossae are a system of troughs and channels in the Amenthes quadrangle of Mars, with a location centered at 21.1 N and 237.5 W. They are 604 km long and were named after a classical albedo feature name. [1] The fossae have been tentatively identified as outflow channels , but their origin and evolution remain ambiguous. [2] It has been proposed that water may have been released into the troughs as a catastrophic flood due to subsurface ice melting following a large bolide impact. [3] |
|
| 2014 |
27210 characters 1 sections 1 paragraphs 6 images 151 internal links 2 external links |
bolide 0.331 604 0.302 troughs 0.289 hephaestus 0.284 237 0.277 fossae 0.271 ambiguous 0.242 tentatively 0.242 amenthes 0.235 channels 0.197 flood 0.181 catastrophic 0.179 outflow 0.143 melting 0.142 evolution 0.140 |
The Hephaestus Fossae are a system of troughs and channels in the Amenthes quadrangle of Mars, with a location centered at 21.1 N and 237.5 W. It is 604 km long and was named after a classical albedo feature name. [1] The fossae have been tentatively identified as outflow channels , but their origin and evolution remain ambiguous. [2] It has been proposed that water may have been released into the troughs as a catastrophic flood due to subsurface ice melting following a large bolide impact. [3] |
|
| 2013 |
27210 characters 1 sections 1 paragraphs 6 images 151 internal links 2 external links |
bolide 0.332 604 0.303 troughs 0.290 hephaestus 0.285 237 0.277 fossae 0.272 ambiguous 0.243 tentatively 0.243 cebrenia 0.222 channels 0.197 flood 0.182 catastrophic 0.180 outflow 0.143 melting 0.142 evolution 0.141 |
The Hephaestus Fossae are a system of troughs and channels in the Cebrenia quadrangle of Mars, with a location centered at 21.1 N and 237.5 W. It is 604 km long and was named after a classical albedo feature name. [1] The fossae have been tentatively identified as outflow channels , but their origin and evolution remain ambiguous. [2] It has been proposed that water may have been released into the troughs as a catastrophic flood due to subsurface ice melting following a large bolide impact. [3] |
|
| 2012 |
5861 characters 1 sections 2 paragraphs 2 images 8 internal links 2 external links |
bolide 0.332 604 0.303 troughs 0.290 hephaestus 0.285 237 0.277 fossae 0.272 ambiguous 0.243 tentatively 0.243 cebrenia 0.222 channels 0.197 flood 0.182 catastrophic 0.180 outflow 0.143 melting 0.142 evolution 0.141 |
Hephaestus Fossae is a system of troughs and channels in the Cebrenia quadrangle of Mars, with a location centered at 21.1 N and 237.5 W. It is 604 km long and was named after a classical albedo feature name. [1] The Fossae have been tentatively identified as outflow channels , but their origin and evolution remain ambiguous. [2] It has been proposed that water may have been released into the troughs as a catastrophic flood due to subsurface ice melting following a large bolide impact. [3] |
|
| 2011 |
5861 characters 1 sections 2 paragraphs 2 images 8 internal links 2 external links |
bolide 0.332 604 0.303 troughs 0.290 hephaestus 0.285 237 0.277 fossae 0.272 ambiguous 0.243 tentatively 0.243 cebrenia 0.222 channels 0.197 flood 0.182 catastrophic 0.180 outflow 0.143 melting 0.142 evolution 0.141 |
Hephaestus Fossae is a system of troughs and channels in the Cebrenia quadrangle of Mars, with a location centered at 21.1 N and 237.5 W. It is 604 km long and was named after a classical albedo feature name. [1] The Fossae have been tentatively identified as outflow channels , but their origin and evolution remain ambiguous. [2] It has been proposed that water may have been released into the troughs as a catastrophic flood due to subsurface ice melting following a large bolide impact. [3] |
|
| 2010 |
5045 characters 1 sections 2 paragraphs 2 images 6 internal links 2 external links |
hephaestus 0.554 604 0.295 237 0.270 fossae 0.265 picture 0.225 cebrenia 0.215 fossa 0.206 void 0.189 trough 0.168 melted 0.165 underground 0.142 centered 0.130 subsurface 0.122 classical 0.122 geology 0.120 |
Hephaestus Fossae is a trough in the Cebrenia quadrangle of Mars, with a location centered at 21.1 N and 237.5 W. It is 604 km long and was named after a classical albedo feature name. [1] In this region, there is a channel systems possibly created by water flow. It was proposed, that water source was subsurface ice melted by large impact. [2] |
|
| 2009 |
4523 characters 1 sections 2 paragraphs 2 images 6 internal links 1 external links |
hephaestus 0.587 604 0.313 237 0.286 fossae 0.281 picture 0.239 cebrenia 0.228 fossa 0.219 void 0.200 trough 0.178 underground 0.150 centered 0.138 classical 0.129 geology 0.127 moving 0.110 lies 0.108 |
Hephaestus Fossae is a trough in the Cebrenia quadrangle of Mars, with a location centered at 21.1 N and 237.5 W. It is 604 km long and was named after a classical albedo feature name. [1] |