Tintina Fault
The Tintina Fault is a large right-lateral strike-slip fault in western North America, extending from northwestern British Columbia, Canada to the centre of the U.S. state of Alaska. It represents the Yukon continuum between the Rocky Mountain Trench in the northern United States and the Kaltag Fault in Alaska.[1]
See also
- Denali Fault
- Rocky Mountain Trench
- Northern Cordilleran Volcanic Province
References
- ^ Mineral deposits of the Tanana - Yukon Uplands: A Summary Report
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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 | |
|---|---|
| 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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