The Kamchatka-Aleutian triple junction is a triple junction of tectonic plates of the Fault-Fault-Trench type where the Pacific Plate, the Okhotsk Plate, and the North American Plate meet. [1] It is located east of the Kamchatka Mys peninsula and west of Bering Island. Meiji Seamount is located to the southeast of the junction.
In the Kamchatka-Aleutian junction, the Kuril–Kamchatka Trench meets the Aleutian Trench. The former is a subduction zone while the latter is a transform fault in its western part.
References
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^ Christoph Gaedicke, Boris Baranov, Nokolay Seliverstov, Dmitry Alexeiev, Nikolay Tsukanov, Ralf Freitag (2000). "Structure of an active arc-continent collision area: the Aleutian–Kamchatka junction". Tectonophysics. 325 (1–2): 63–85.
Bibcode:
2000Tectp.325...63G.
doi:
10.1016/S0040-1951(00)00131-1.
{{ cite journal}}: CS1 maint: multiple names: authors list ( link)
56°12′N 163°30′E / 56.2°N 163.5°E
| Triple Trench | |
|---|---|
| Triple Ridge | |
| Triple Fault | |
| Trench Trench Ridge | |
| Fault Fault Trench | |
| Ridge Fault Fault | |
| Ridge Trench Fault | |
| See also | |
