An Entity of Type: mountain, from Named Graph: http://dbpedia.org, within Data Space: dbpedia.org

The Wichita Mountains are located in the southwestern portion of the U.S. state of Oklahoma. It is the principal relief system in the Southern Oklahoma Aulacogen, being the result of a failed continental rift. The mountains are a northwest-southeast trending series of rocky promontories, many capped by 500 million-year old granite. These were exposed and rounded by weathering during the Pennsylvanian & Permian Periods. The eastern end of the mountains offers 1,000 feet (305 m) of topographic relief in a region otherwise dominated by gently rolling grasslands.

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dbo:abstract
  • Las montañas Wichita están localizadas en el sudoeste del estado de Oklahoma, en los Estados Unidos.​ Es el sistema de alivio principal en el , siendo el resultado de una fractura continental fallida. Las montañas son una serie de promontorios rocosos con tendencia noroeste-sureste, muchos coronados por granito de 500 millones de años. Estos fueron expuestos y redondeados por la intemperie durante los períodos Pensilvano & Pérmico. El extremo este de las montañas ofrece 305 m. de relieve topográfico en una región que de otro modo estaría dominada por pastizales suavemente ondulados. Las montañas albergan numerosos ranchos de trabajo y operaciones de canteras, el , casas recreativas y campamentos y parques pintorescos. , sede de la , ocupa una gran parte del extremo sureste de las montañas. (es)
  • Les montagnes Wichita (en anglais Wichita Mountains) se trouvent dans le Sud-Ouest de l'État de l'Oklahoma aux États-Unis. Elles tirent leur nom d'une ancienne tribu amérindienne. En général, la montagne a une altitude comprise entre 120 et 300 mètres, et le point culminant est le Haley Peak (756 mètres). (fr)
  • The Wichita Mountains are located in the southwestern portion of the U.S. state of Oklahoma. It is the principal relief system in the Southern Oklahoma Aulacogen, being the result of a failed continental rift. The mountains are a northwest-southeast trending series of rocky promontories, many capped by 500 million-year old granite. These were exposed and rounded by weathering during the Pennsylvanian & Permian Periods. The eastern end of the mountains offers 1,000 feet (305 m) of topographic relief in a region otherwise dominated by gently rolling grasslands. The mountains are home to numerous working ranches and quarry operations, the state reformatory, recreational homes and campsites, and scenic parklands. Fort Sill, home of the U.S. Army Field Artillery School, occupies a large portion of the southeastern end of the mountains. (en)
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  • Haley Peak (en)
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  • northwest-southeast (en)
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  • Color digital elevation map of southwestern Oklahoma; the Wichita Mountains are highlighted (en)
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  • Topographic-NatAtlas-SW-OK.jpg (en)
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  • Wichita Mountains (en)
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  • Ouachita orogeny (en)
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  • Elk Mountain, OK.jpg (en)
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  • Elk Mountain, in the eastern Wichita Mountains (en)
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  • Oklahoma (en)
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  • Les montagnes Wichita (en anglais Wichita Mountains) se trouvent dans le Sud-Ouest de l'État de l'Oklahoma aux États-Unis. Elles tirent leur nom d'une ancienne tribu amérindienne. En général, la montagne a une altitude comprise entre 120 et 300 mètres, et le point culminant est le Haley Peak (756 mètres). (fr)
  • Las montañas Wichita están localizadas en el sudoeste del estado de Oklahoma, en los Estados Unidos.​ Es el sistema de alivio principal en el , siendo el resultado de una fractura continental fallida. Las montañas son una serie de promontorios rocosos con tendencia noroeste-sureste, muchos coronados por granito de 500 millones de años. Estos fueron expuestos y redondeados por la intemperie durante los períodos Pensilvano & Pérmico. El extremo este de las montañas ofrece 305 m. de relieve topográfico en una región que de otro modo estaría dominada por pastizales suavemente ondulados. (es)
  • The Wichita Mountains are located in the southwestern portion of the U.S. state of Oklahoma. It is the principal relief system in the Southern Oklahoma Aulacogen, being the result of a failed continental rift. The mountains are a northwest-southeast trending series of rocky promontories, many capped by 500 million-year old granite. These were exposed and rounded by weathering during the Pennsylvanian & Permian Periods. The eastern end of the mountains offers 1,000 feet (305 m) of topographic relief in a region otherwise dominated by gently rolling grasslands. (en)
rdfs:label
  • Wichita Mountains (en)
  • Montañas Wichita (es)
  • Montagnes Wichita (fr)
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  • Wichita Mountains (en)
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