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About: Llano Uplift     Goto   Sponge   NotDistinct   Permalink

An Entity of Type : yago:State108654360, within Data Space : dbpedia.demo.openlinksw.com associated with source document(s)

Type: Thingplacedbo:Locationschema:Mountainschema:Placenatural placeMountaingeo:SpatialThingyago:AdministrativeDistrict108491826yago:District108552138yago:GeologicalFormation109287968yago:Location100027167yago:Object100002684yago:PhysicalEntity100001930yago:Range109403734yago:Region108630985yago:WikicatGeologicProvincesOfTexasyago:YagoGeoEntityyago:YagoLegalActorGeoyago:YagoPermanentlyLocatedEntitymountainyago:State108654360 New Facet based on Instances of this Class

The Llano Uplift is a geologically ancient, low geologic dome that is about 90 miles (140 km) in diameter and located mostly in Llano, Mason, San Saba, Gillespie, and Blanco counties, Texas. It consists of an island-like exposure of Precambrian igneous and metamorphic rocks surrounded by outcrops of Paleozoic and Cretaceous sedimentary strata. At their widest, the exposed Precambrian rocks extend about 65 miles (105 km) westward from the valley of the Colorado River and beneath a broad, gentle topographic basin drained by the Llano River. The subdued topographic basin is underlain by Precambrian rocks and bordered by a discontinuous rim of flat-topped hills. These hills are the dissected edge of the Edwards Plateau, which consist of overlying Cretaceous sedimentary strata. Within this basi