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Martian Water Ben Farley University of Massachusetts, Amherst December 1, 2003.

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Presentation on theme: "Martian Water Ben Farley University of Massachusetts, Amherst December 1, 2003."— Presentation transcript:

1 Martian Water Ben Farley University of Massachusetts, Amherst December 1, 2003

2 Overview Water on Mars? What’s left? Where did it go? What does it mean?

3 Water on Mars?

4 Martian Oceans –Northern Hemisphere is topographically lower than Southern Hemisphere –Wrinkle ridges in North appear to be smoothed –North is mostly lower Hesperian in age, while South is Noachian

5 Water on Mars? Martian Oceans –Arabia GEL of 599 m –Deuteronilus GEL of 130 m –Vasitas Borealis Formation GEL of 156 m Vasitas Borealis Formation

6 Water on Mars? Fluvial Features –Teardrop islands –Gullies –Outflow Channels

7 What’s left? Gullies –97% located between ±30-60º latitude –Consistent with groundwater stable beneath megaregolith –Not consistent with Mellon and Jakosky model Polar Caps –GEL of 20-30 meters

8 What’s left? Hydrogen enriched soil

9 Where did it go? GEL of 20-30 meters in polar caps GEL of 50 meters escaped atmosphere GEL of 80 meters unaccounted for

10 Where did it go? Volatile rich deposits Ground water (sub-megaregolith)

11 What does it mean? There is water on Mars now There probably was an Ocean on Mars during the Noachian period


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