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Water on Mars Okyama University 2007. 06. 18
Water on Mars Okyama University Akos Kereszturi, PHD Collegium Budapest Eotvos Lorand University of Sciences Hungarian Astronomical Association
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Change of our veiw on ancient Mars
Bone dry planet (Mariner-9)...
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Change of our veiw on ancient Mars
…ancient channels (Viking probes)...
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Change of our veiw on ancient Mars
…sometimes lakes (MGS)...
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Change of our veiw on ancient Mars
…with a great northern ocean (MGS, MEX).
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H2O budget Original H2O budget: Signs of liquid water:
channels, valleys ocean shorelines clay minerals sediments deposited in water theoretical models Original H2O budget: m global coverage
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The poposed ancient ocean
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Channels by surface runoff or sapping
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Global cooling, surface freezing
Realtive small planetary mass: small radioactive heat source early stopped dinamo weak gravity fast atmospheric loss decreasing greenhouse effect decreasing volcanism only early global tectonism decreasing global temperature formation of cryosphere
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Water break up, outflow channels
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Favourable periods for liquid water
South Polar Cap - Argyre - Uzboi channel system sedimentary delta lake sediments
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Channel network water source
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H2O distribution today Almost all H2O is frozen:
60-80 % subsurface permafrost 10-30 % polar cap and polar sediments 0,1-0,01 % atmosphere
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Signs of water today? - Gullies?
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Slope straks?
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DDS „seepages”?
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Possible conditions for water today
very rarely who knows…
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