| Athabasca Vallis Streamlined "Islands"
Tremendous floods carved these tear drop-shaped landforms in
Athabasca Vallis in the Cerberus region, south of the Elysium volcanoes.
The orientation of the streamlined forms indicate that the fluid flowed from
the right/upper right toward the left/lower left (from the northeast to the
southwest). Similar features occur in central and eastern Washington in the
northwestern United States. The examples in Washington formed when
massive amounts of water rushed across the landscape, scouring a
"channeled scabland" during the last Ice Age, roughly
12,000-13,000 years ago. The features on Mars are much older; while the
absolute age cannot be determined, the small impact craters with rayed
ejecta patterns on the flood surfaces indicate it must be much, much older
than the flood landscape in Washington. This is a mosaic of six Mars Global
Surveyor (MGS) Mars Orbiter Camera (MOC) images acquired in 1999
through 2002. Illumination is from the left. The mosaic covers an area
11.9 km (7.4 mi) by 13.0 km (8.1 mi). The full-size mosaic has a resolution
of 4 meters (13 ft) per pixel.
Images Credit: NASA/JPL/Malin Space Science Systems
Caption by: K. S. Edgett and M. C. Malin, MSSS
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