Geochemical Creation of Methane

  • Released Thursday, January 15, 2009

Conceptual animation depicting how geochemical processes during the course of Mars' history may have produced the methane plumes now seen in Mars' atmosphere. Here, through a process called serpentinization, methane is generated as part of a reaction involving the conversion of liquid water (seen seeping into the planet's crust), iron oxide, and carbon dioxide energized by the planet's internal heat into serpentine minerals.

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Please give credit for this item to:
NASA/Goddard Space Flight Center

Release date

This page was originally published on Thursday, January 15, 2009.
This page was last updated on Wednesday, May 3, 2023 at 1:54 PM EDT.


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