Volcanic regions: Tharsis Bulge, Elysium Planitia — areas of potential residual geological heat
Mars is geologically less active than Earth but not dead. MAVEN discovered ongoing volcanic-style chemistry, and Tharsis and Elysium show geological ages of <100 million years in some areas. InSight's HP³ heat probe (despite not penetrating deeply enough) measured heat flow suggesting Mars has cooled significantly. For practical ISRU purposes, geothermal power on Mars is theoretical — nuclear fission power is more reliable. However, subsurface brines or hydrothermal vents near Tharsis remain astrobiologically interesting.
If accessible — geothermal could power crewed outposts without nuclear or solar dependence
Reality Check
InSight detected very low heat flux (~21 mW/m² near Elysium Planitia) — far below economically viable geothermal extraction; Mars may be too geologically cold for practical geothermal
Confidence: medium · Last verified 2026-06-01
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