About: Cerro Prieto Fault

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The Cerro Prieto Fault is a transform fault located in far northern Baja California. It runs between the Cerro Prieto spreading center located southwest of Mexicali, and the Wagner Basin, another spreading center which lies under the Gulf of California. These spreading centers are part of the East Pacific Rise, the northern leg of which has formed the Gulf of California by steadily rifting the Baja California Peninsula away from the mainland of Mexico.

Attributes	Values
rdf:type	geo:SpatialThing
rdfs:label	Cerro Prieto Fault (en) Faglia del Cerro Prieto (it)
rdfs:comment	The Cerro Prieto Fault is a transform fault located in far northern Baja California. It runs between the Cerro Prieto spreading center located southwest of Mexicali, and the Wagner Basin, another spreading center which lies under the Gulf of California. These spreading centers are part of the East Pacific Rise, the northern leg of which has formed the Gulf of California by steadily rifting the Baja California Peninsula away from the mainland of Mexico. (en) La faglia del Cerro Prieto è una delle faglie trasformi a movimento laterale destro presenti nella parte settentrionale della Bassa California. La faglia si estende tra il centro di espansione del Cerro Prieto, a sud ovest di Mexicali e il bacino di Wagner, nella parte settentrionale del Golfo di California. La faglia fa parte della dorsale del Pacifico orientale, la cui parte settentrionale ha formato il Golfo di California, letteralmente separando la penisola di Bassa California dal Messico. (it)
geo:lat	34.049999 (xsd:float)
geo:long	-118.250000 (xsd:float)
foaf:depiction
dct:subject	Salton Trough Geology of Mexico Depressions of Mexico
Wikipage page ID	27044291 (xsd:integer)
Wikipage revision ID	1119427681 (xsd:integer)
Link from a Wikipage to another Wikipage	San Diego Salton Trough East Pacific Rise Colorado River Salton Sea Los Angeles Yuma, Arizona Pull-apart basin Baja California Province of the Californias Cerro Prieto Tijuana Alamo River Gulf of California Hypocenter Geology of Mexico Laguna Salada (Mexico) Transform fault Mexicali Mexico Depressions of Mexico Wagner Basin
sameAs	Cerro Prieto Fault Cerro Prieto Fault Cerro Prieto Fault Cerro Prieto Fault Cerro Prieto Fault
dbp:wikiPageUsesTemplate	dbt:BajaCalifornia-geo-stub dbt:Tectonics-stub dbt:Coord dbt:Location_map_many dbt:Reflist dbt:Central_America_plates
thumbnail	wiki-commons:Special:FilePath/Salton_trough_fault_overlay.svg?width=300
caption	Cierro Prieto fault and area to the north. The red lines are simplified faults. Right-lateral direction of motion of the transform fault is shown . The red rhombs are pull-apart basins; the northern one is the site of the Niland geothermal field, the southern the Cerro Prieto geothermal field. (en)
label	Gulf of California (en) Los Angeles (en) Mexicali (en) Salton Sea (en) San Diego (en) Tijuana (en) Yuma (en) Alamo River mouth (en) Cerro Prieto volcano (en) Colorado River Valley (en) Colorado River mouth (en) Laguna Salada (en)
position	left (en) right (en)
width	400 (xsd:integer)
georss:point	34.05 -118.25
has abstract	The Cerro Prieto Fault is a transform fault located in far northern Baja California. It runs between the Cerro Prieto spreading center located southwest of Mexicali, and the Wagner Basin, another spreading center which lies under the Gulf of California. These spreading centers are part of the East Pacific Rise, the northern leg of which has formed the Gulf of California by steadily rifting the Baja California Peninsula away from the mainland of Mexico. Seismic studies indicate a linear trend of hypocenters to the northwest of Cerro Prieto which is interpreted as a continuation of the Cerro Prieto Fault some 45 km to the northwest across the international border about 7 km into southern California. (en) La faglia del Cerro Prieto è una delle faglie trasformi a movimento laterale destro presenti nella parte settentrionale della Bassa California. La faglia si estende tra il centro di espansione del Cerro Prieto, a sud ovest di Mexicali e il bacino di Wagner, nella parte settentrionale del Golfo di California. La faglia fa parte della dorsale del Pacifico orientale, la cui parte settentrionale ha formato il Golfo di California, letteralmente separando la penisola di Bassa California dal Messico. Studi sismologici hanno individuato una sequenza lineare di ipocentri a nord-ovest del Cerro Prieto, interpretando ciò come una continuazione della faglia del Cerro Prieto per circa 45 km verso nord-ovest, fino ad arrivare di 7 km oltre l'attuale confine internazionale tra Messico e Stati Uniti d'America. (it)
overlay image	Salton_trough_fault_overlay.svg (en)
prov:wasDerivedFrom	wikipedia-en:Cerro_Prieto_Fault?oldid=1119427681&ns=0
page length (characters) of wiki page	4232 (xsd:nonNegativeInteger)
foaf:isPrimaryTopicOf	wikipedia-en:Cerro_Prieto_Fault
geo:geometry	POINT(-118.25 34.049999237061)
is Link from a Wikipage to another Wikipage of	List of fault zones Brawley Seismic Zone List of seismic faults in Mexico 1915 Imperial Valley earthquakes Cerro Prieto Gran Desierto de Altar Lake Cahuilla Imperial Fault Zone Wagner Basin Gulf of California Rift Zone
is foaf:primaryTopic of	wikipedia-en:Cerro_Prieto_Fault

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