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Dao Vallis

Dao Vallis is a valley on Mars that appears to have been carved by water. It runs southwestward into Hellas Planitia from the southern slopes of the volcano Hadriacus Mons, and has been identified as an outflow channel. It and its tributary, Niger Vallis, extend for about 1,200 km (750 mi).

Origin
Dao Vallis begins near a large volcano, Hadriacus Mons, so it is thought to have received water when hot magma melted huge amounts of ice in the frozen ground. Much of this water may have been released in very large "outburst floods". The partially circular depressions on the left side of the channel in the image below suggests that groundwater sapping also contributed water more gradually. Image:Dao Vallis.JPG|Section of Dao Vallis, as seen by THEMIS. Click on image to see relationship of Dao Vallis to other nearby features. ==See also==
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