- Chile Rise
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The Chile Rise or Chile Ridge is an oceanic ridge, a tectonic divergent plate boundary between the Nazca and Antarctic Plates. Its eastern end is the Chile Triple Junction where the Chile Rise is being subducted below the South American Plate in the Peru-Chile Trench.[1] It runs westward to a triple point south of the Juan Fernández Microplate where it intersects the East Pacific Rise.
References
- ^ Russo, R.M.; Vandecar, John C.; Comte, Diana; Mocanu, Victor I.; Gallego, Alejandro; Murdie, Ruth E. (2010). "Subduction of the Chile Ridge: Upper mantle structure and flow". GSA Today: 4. doi:10.1130/GSATG61A.1.
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 Mid-ocean ridges Present American-Antarctic · Chile · East Pacific · Explorer · Gakkel · Gorda · Juan de Fuca · Mid-Atlantic · Pacific–Antarctic · Central Indian · Southeast Indian · Southwest IndianFormer This tectonics article is a stub. You can help Wikipedia by expanding it.