Hecates Tholus: Difference between revisions
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[[Image:Hecates_Tholus.jpg|thumb|right|px|Hecates Tholus with [[cloud|clouds]]]]'''Hecates Tholus''' is a [[volcano]] in the [[Elysium Volcanic Region]]. Hecates is in the Cebrenia quadrangle. It is thought that the [[caldera]] may have had [[glacier|glaciers]] in the past.<ref>http://www.msnbc.msn/id/7209308 | [[Image:Hecates_Tholus.jpg|thumb|right|px|Hecates Tholus with [[cloud|clouds]]]]'''Hecates Tholus''' is a [[volcano]] in the [[Elysium Volcanic Region]]. Hecates is in the Cebrenia quadrangle. It is thought that the [[caldera]] may have had [[glacier|glaciers]] in the past.<ref>http://www.msnbc.msn/id/7209308</ref> Some valleys on Hecates show a parallel drainage pattern.<ref>Hugh H. Kieffer 1992. Mars. University of Arizona Press. ISBN 978-0-8165-1257-7.</ref> | ||
[[category:Volcano]] | [[category:Volcano]] | ||
Revision as of 17:02, 15 February 2018

Hecates Tholus is a volcano in the Elysium Volcanic Region. Hecates is in the Cebrenia quadrangle. It is thought that the caldera may have had glaciers in the past.[1] Some valleys on Hecates show a parallel drainage pattern.[2]
- ↑ http://www.msnbc.msn/id/7209308
- ↑ Hugh H. Kieffer 1992. Mars. University of Arizona Press. ISBN 978-0-8165-1257-7.