 Ravi Vallis and Aromatum Chaos, as seen by Viking Orbiter | |
| Coordinates | 0°12′S40°42′W / 0.2°S 40.7°W /-0.2; -40.7 |
|---|---|
Ravi Vallis is an ancientoutflow channel, the source of which originates from theAromatum Chaos depression, and is situated at the eastern end of Xanthe Terra, in theMargaritifer Sinus quadrangle (MC-19) region ofMars, located at0°12′S40°42′W / 0.2°S 40.7°W /-0.2; -40.7. The Ravi Vallis outflow channel is 205.5 km (127.7 mi) long, and starts at the northeastern end of the Aromatum Chaos depression. The channel is orientated in an easterly direction, and further down channel, Ravi Vallis divides into two; a larger northern channel, and a smaller southern channel, and is finally truncated by a fault which is located at the western margin of theHydraotes Chaos depression. Ravi Vallis was named after the Ravi River, an ancient Indian river.[1][2][3][4][5]
The Ravi Vallisoutflow channel and neighboring deep depression atAromatum Chaos, are thought to have been caused by volcano-ice interactions underneath the surface, which pierced an undergroundaquifer. This released large amounts of water, causing a catastrophic flood event, with an estimated speed of between 10 and 25 m s−1. The discharge rates from the Ravi Vallisoutflow channel are thought to have ranged from a maximum of ~30 × 106 m3 s−1 after the beginning of the flood event, to below 10 × 106 m3 s−1 in its later stages. The flood event is thought to have lasted between 2 and 10 weeks, with an estimated minimum total water volume of somewhere in the range of 11,000 to 65,000 km3.[1][2]
Intermittent volcanism and related flood events like that which occurred at Ravi Vallis, are known to have occurred in other regions of Mars, such as atKasei Valles,[6] andMangala Valles.[7][8]
