Balcones Fault

http://dbpedia.org/resource/Balcones_Fault an entity of type: Escarpment109274152

L'escarpement de Balcones, en anglais: Balcones Fault Zone, est une zone de faille du Texas qui s'étend approximativement de la portion sud-ouest de l'État, à proximité de Del Rio jusqu'au nord de la région centrale, près de Waco. rdf:langString
La scarpata di Balcones (in inglese: Balcones Fault Zone), è una zona di faglia del Texas che si estende dalle regioni sud-occidentali dello Stato, vicino a Del Rio, fino al nord della regione centrale, vicino a Waco, approssimativamente correndo lungo la Interstate 35. rdf:langString
Balcones Escarpment är den synliga delen av en lång förkastningszon, Balcones Fault, som skapar en naturlig gräns med klippig kalkstensterräng mellan och den sydöstra kustslätten i Texas. Området karakteriseras av djupa dalgångar, underjordiska vattenvägar, och andra geologiska särdrag som möjliggör ett mycket snabbt genomflöde av vatten i området. Balcones Escarpment är ett av USA:s mest översvämningsutsatta områden när omfattande regnväder inträffar. rdf:langString
The Balcones Fault or Balcones Fault Zone is an area of largely normal faulting in the U.S. state of Texas that runs roughly from the southwest part of the state near Del Rio to the north-central region near Dallas along Interstate 35. The Balcones Fault zone is made up of many smaller features, including normal faults, grabens, and horsts. One of the obvious features is the Mount Bonnell Fault. rdf:langString
rdf:langString Balcones Fault
rdf:langString Escarpement de Balcones
rdf:langString Scarpata di Balcones
rdf:langString Balcones Escarpment
xsd:integer 317658
xsd:integer 1120417876
rdf:langString The Balcones Fault or Balcones Fault Zone is an area of largely normal faulting in the U.S. state of Texas that runs roughly from the southwest part of the state near Del Rio to the north-central region near Dallas along Interstate 35. The Balcones Fault zone is made up of many smaller features, including normal faults, grabens, and horsts. One of the obvious features is the Mount Bonnell Fault. The location of the fault zone may be related to the Ouachita Mountains, formed 300 million years ago during a continental collision. Although long since worn away in Texas, the roots of these ancient mountains still exist, buried beneath thousands of feet of sediment. These buried Ouachita Mountains may still be an area of weakness that becomes a preferred site for faulting when stress exists in the Earth's crust. The Balcones Fault has remained inactive for nearly 15 million years, with the last activity being during the Neogene period. This activity was related to subsidence of the Texas Coastal Plain, most likely from the large amount of sediment deposited on it by Texas rivers. The Balcones Fault is in one of the lowest-risk zones for earthquakes in the United States. The surface expression of the fault is the Balcones Escarpment, which forms the eastern boundary of the Texas Hill Country and the western boundary of the Texas Coastal Plain, and consists of cliffs and cliff-like structures. Subterranean features such as Wonder Cave and numerous other smaller caves are found along the fault zone. Many cities are located along this fault zone. Springs such as San Pedro Springs, Comal Springs, San Marcos Springs, Barton Springs, and Salado Springs are found in the fault zone and provide a source of fresh water and a place for human settlement. The Balcones Fault Zone is a demarcation line for certain ecological systems and species distributions, e.g., the California fan palm (Washingtonia filifera) is the only species of palm tree native to the continental United States west of the Balcones Fault.
rdf:langString L'escarpement de Balcones, en anglais: Balcones Fault Zone, est une zone de faille du Texas qui s'étend approximativement de la portion sud-ouest de l'État, à proximité de Del Rio jusqu'au nord de la région centrale, près de Waco.
rdf:langString La scarpata di Balcones (in inglese: Balcones Fault Zone), è una zona di faglia del Texas che si estende dalle regioni sud-occidentali dello Stato, vicino a Del Rio, fino al nord della regione centrale, vicino a Waco, approssimativamente correndo lungo la Interstate 35.
rdf:langString Balcones Escarpment är den synliga delen av en lång förkastningszon, Balcones Fault, som skapar en naturlig gräns med klippig kalkstensterräng mellan och den sydöstra kustslätten i Texas. Området karakteriseras av djupa dalgångar, underjordiska vattenvägar, och andra geologiska särdrag som möjliggör ett mycket snabbt genomflöde av vatten i området. Balcones Escarpment är ett av USA:s mest översvämningsutsatta områden när omfattande regnväder inträffar.
xsd:nonNegativeInteger 6981

data from the linked data cloud