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.
Duration: 20.0 seconds
Available formats: 1280x720 (30 fps)
QT
12 MB
640x360 (29.97 fps)
MPEG-4
3 MB
320x180 (29.97 fps)
MPEG-4
1 MB
320x240 (29.97 fps)
MPEG-4
665 KB
640x360 (29.97 fps)
MPEG-1
4 MB
512x288 (29.97 fps)
MPEG-1
3 MB
1280x720 (60 fps)
QT
535 MB
1280x720 (60 fps)
QT
5 MB
320x180
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184 KB
160x80
PNG
56 KB
80x40
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