- Chile Triple Junction
-
The Chile Triple Junction (or Chile Margin Triple Junction) is a geologic triple junction located on the seafloor of the Pacific Ocean off Taitao and Tres Montes Peninsula on the southern coast of Chile. Here three tectonic plates meet: the South American Plate, the Nazca Plate, and the Antarctic Plate. This triple junction is unusual in that it consists of a mid-oceanic ridge, the Chile Rise, being subducted under the South American Plate at the Peru-Chile Trench.
References
- Tectonics of South America: Chile Triple Junction
- The Chile Margin Triple Junction: Modern Analog to Ancient California?
Geology of Chile Morphology Tectonics Antarctic Plate · Atacama Fault · Chile Rise · Chile Triple Junction · Easter Plate · Juan Fernández Ridge · Liquiñe-Ofqui Fault · Nazca Plate · Nazca Ridge · Peru-Chile Trench · Scotia Plate · South American PlateOrogenies Volcanism Regional geology Institutions Lists Triple Trench Boso Triple JunctionTriple Ridge Afar Triple Junction · Azores Triple Junction · Galapagos Triple Junction · Bouvet Triple Junction · Rivera Triple Junction · Rodrigues Triple Point · Tongareva triple junctionTriple Fault Trench Trench Ridge Chile Triple JunctionFault Fault Trench Kamchatka-Aleutian Triple JunctionRidge Fault Fault Ridge Ridge Fault This tectonics article is a stub. You can help Wikipedia by expanding it.