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About: Athabasca Valles     Goto   Sponge   NotDistinct   Permalink

An Entity of Type : yago:Valley109468604, within Data Space : dbpedia.demo.openlinksw.com associated with source document(s)

Type: yago:WikicatValleysAndCanyonsOnMarsyago:GeologicalFormation109287968yago:NaturalDepression109366017yago:Object100002684yago:PhysicalEntity100001930yago:YagoGeoEntityyago:YagoPermanentlyLocatedEntitytelevision stationyago:Valley109468604 New Facet based on Instances of this Class

The Athabasca Valles are a late Amazonian-period outflow channel system in the central Elysium Planitia region of Mars, located to the south of the Elysium Rise. They are part of a network of outflow channels in this region that are understood to emanate from large fissures in the Martian surface rather than the chaos terrains that source the circum-Chryse outflow channels. The Athabasca Valles in particular emanate from one of the Cerberus Fossae fissures and flow downstream to the southwest, constrained to the south by a wrinkle ridge for over 100 km, before debouching into the Cerberus Palus volcanic plain. The Athabasca Valles are widely understood to be the youngest outflow channel system on the planet.