Highlights ► Erythraea Fossa, Mars (31.5 W, 27.3 S) is a graben near Holden crater. ► Evidence for a chain of paleolakes in Erythraea Fossa is presented. ► A hypothesis of the hydrology of the paleolakes is put forth. ► Evidence for precipitation in Erythraea Fossa is presented. ► Findings in this area are contextualized with the global martian paleoclimate.
Icarus – Elsevier
Published: May 1, 2011
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