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About: San Rafael Swell     Goto   Sponge   NotDistinct   Permalink

An Entity of Type : yago:WikicatRegionsOfUtah, within Data Space : dbpedia.org associated with source document(s)

Type: Thingplacedbo:Locationschema:Mountainschema:Placenatural placeworkMountaingeo:SpatialThingyago:Area108497294yago:GeologicalFormation109287968yago:Location100027167yago:Object100002684yago:PhysicalEntity100001930yago:Range109403734yago:Region108630039yago:Region108630985yago:YagoGeoEntityyago:YagoLegalActorGeoyago:YagoPermanentlyLocatedEntitymountainyago:WikicatProtectedAreasOfEmeryCounty,Utahyago:WikicatRegionsOfUtah New Facet based on Instances of this Class

The San Rafael Swell is a large geologic feature located in south-central Utah, United States about 16 miles (26 km) west of Green River. The San Rafael Swell, measuring approximately 75 by 40 miles (121 by 64 km), consists of a giant dome-shaped anticline of sandstone, shale, and limestone that was pushed up during the Paleocene Laramide Orogeny 60–40 million years ago. Since that time, infrequent but powerful flash floods have eroded the sedimentary rocks into numerous valleys, canyons, gorges, mesas, buttes, and badlands. The swell is part of the Colorado Plateau physiographic region.