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]
See also
- Denali Fault
- Rocky Mountain Trench
- Northern Cordilleran Volcanic Province
References
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Major seismically active faults of North America
(crosses national borders)
- Aleutian Trench (US–RU)
- Basin and Range Province (US–MX)
- Canadian Arctic Rift System (CA–GL)
- Cascadia subduction zone (US–CA)
- Clarendon-Linden fault system (US–CA)
- Denali Fault (US–CA)
- Northern Cordilleran Volcanic Province (CA–US)
- Puget Sound faults (US–CA)
- Rio Grande rift (US–MX)
- San Andreas Fault (US–MX)
- Southern Great Lakes Seismic Zone (US–CA)
- Tintina Fault (US–CA)
Washington and Oregon | |
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California | |
Great Basin | |
Great Plains |
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Midwest | |
Appalachian Mountains and Atlantic Coast |
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- Cayman Trough
- Chixoy-Polochic Fault
- Enriquillo–Plantain Garden fault zone (Cuba)
- Gulf of California Rift Zone
- Lesser Antilles subduction zone
- Middle America Trench (Central America)
- Motagua Fault (Central America)
- Pedro Miguel Fault
- Puerto Rico Trench
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