Northern Appalachians Seismic Zone
The Northern Appalachians Seismic Zone is an active seismic zone in the Appalachian Mountains of eastern North America, extending from New Brunswick southwards into New England and Boston.[1] Both the seismic zone and the resultant Appalachian Mountains were created by the collision of two tectonic plates about 440–480 million years ago during the middle Ordovician Period.[2]
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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
45°N 70°W / 45°N 70°W / 45; -70
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