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About: Santa Ynez Mountains     Goto   Sponge   NotDistinct   Permalink

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

Type: Thingplacedbo:Locationschema:Mountainschema:Placenatural placeMountainanatomical structureyago:WikicatMountainRangesOfCaliforniayago:WikicatMountainRangesOfNorthAmericayago:WikicatMountainRangesOfSantaBarbaraCounty,Californiayago:WikicatMountainRangesOfSouthernCaliforniayago:WikicatMountainRangesOfVenturaCounty,Californiageo:SpatialThingyago:GeologicalFormation109287968yago:Mountain109359803yago:NaturalElevation109366317yago:Object100002684yago:PhysicalEntity100001930yago:Range109403734yago:YagoGeoEntityyago:YagoPermanentlyLocatedEntitymountainmountain range New Facet based on Instances of this Class

The Santa Ynez Mountains are a portion of the Transverse Ranges, part of the Pacific Coast Ranges of the west coast of North America. It is the westernmost range in the Transverse Ranges. The range is a large fault block of Cenozoic age created by the movements of the Santa Ynez Fault. A very narrow range, the Santa Ynez Mountains rise quickly on its north side and drops off equally dramatically along the range's south face along the Gaviota Coast. The Santa Ynez Mountains begin as a series of volcanic hills near Point Arguello, and gradually transitions eastward into a single, well-defined ridge extending from Gaviota Peak to Matilija Creek. The range is approximately contiguous with the Topatopa Mountains beyond to the east, which terminates abruptly at Sespe Creek.