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Published byPurificación Casado Roldán Modified over 6 years ago
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Olympus Mons Mitchell Kirshner 3/11/14
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History 19th century Mariner 9 Viking Mars Global Surveyor
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Location 18.65 °N, 226.2 °W Northwest of Tharsis
23 km tall, km, km 600 km across
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Timeline MOC and THEMIS used to find that Noachian period >3.7Ga yielded global volcanism followed by vent volcanism in Tharsis, Elysium, and Circum-Hellas later just in Tharsis and Elysium Activity localized to Tharsis around 1.6Ga volcanism was active until Ma
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Effusion rate of magma supply to Kilauea and Moana Loa averages .01 km3/yr Volume is estimated to be 2.6*10^6 km^3 Using rate accumulation values given in Hawaii, it would take 130 million years to construct shield volcano
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Gravity
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Aureole Deposits Northwest East Flank failure-induced landslides
Ice-Lubricated Gravity Spreading Glacial Interactions
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Escarpment 8 km Assymetry Northwest=shallow, southeast=steep Water
Mass movement Faults
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Caldera SiO2 content Lava fountain cinders
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Magma Chamber d<16 km Estimated depth of Martian primary melts
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Atmospheric Effect Constant column density
~5 decrease in mass from bottom Low atmospheric density
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Water Deep within volcano Shielded from radiation East flank- faults
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Future Landings Difficult to study via rover 8km escarpment Parachute
Dust
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The End
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