Tintina Fault
The Tintina Fault is a large right-lateral strike-slip fault in western North America, extending from Flathead Lake, Montana to the centre of the U.S. state of Alaska.[1] It represents the Yukon continuum between the Rocky Mountain Trench in the northern United States and the Kaltag Fault in Alaska.[2]
Unlike the Denali Fault, which ruptured a 200 km (120 mi) portion of its central segment during the 2002 Denali earthquake, the Tintina Fault is considered inactive. Despite this classification, researchers noted a magnitude 5.3 right-lateral event in 1972 and a relatively young (Holocene) 14 km (8.7 mi) scarp with a maximum offset of 2.5 m (8 ft 2 in).[3]
See also
[edit]References
[edit]- ^ Connor, Cathy (2014). Roadside Geology of Alaska (2nd ed.). Missoula, Montana USA: Mountain Press Publishing Company. p. 26. ISBN 978-0-87842-619-5.
- ^ Mineral deposits of the Tanana – Yukon Uplands: A Summary Report
- ^ Yeats, R. (2012), Active Faults of the World, Cambridge University Press, pp. 37–40, ISBN 978-0521190855
Further reading
[edit]- Page, Robert A.; Plafker, George; Pulpan, Hans (1995), "Block rotation in east-central Alaska: A framework for evaluating earthquake potential?", Geology, 23 (7): 629, Bibcode:1995Geo....23..629P, doi:10.1130/0091-7613(1995)023<0629:BRIECA>2.3.CO;2
 | This British Columbia-related article is a stub. You can help Wikipedia by expanding it. |
 | This article about a Yukon location is a stub. You can help Wikipedia by expanding it. |
 | This Alaska location article is a stub. You can help Wikipedia by expanding it. |
 | This article about structural geology is a stub. You can help Wikipedia by expanding it. |