Difference between revisions of "Hydrothermal vents"
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There appears to be a number of areas on mars where hydrothermal vents may have existed. | There appears to be a number of areas on mars where hydrothermal vents may have existed. | ||
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| + | Areas where hydrothermal vents may exist: | ||
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| + | * [[Mare Tyrrhenum quadrangle]] | ||
| + | * Nili Fossae region | ||
| + | * Eridania basin, ancient sea floor deposits | ||
| + | * [[Thaumasia quadrangle]] | ||
| + | * [[Phaethontis quadrangle]] | ||
| + | * | ||
Revision as of 09:47, 16 November 2020
Hydrothermal vents, either from volcanoes or meteoritic impact, are often associated with high concentrations of minerals that may be of value to Martian settlements.
There appears to be a number of areas on mars where hydrothermal vents may have existed.
Areas where hydrothermal vents may exist:
- Mare Tyrrhenum quadrangle
- Nili Fossae region
- Eridania basin, ancient sea floor deposits
- Thaumasia quadrangle
- Phaethontis quadrangle
