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The Salcha Seismic Zone is a fault line in the Interior region of Alaska, United States, generally located to the east of Fairbanks.The fault runs for 65 km (40 mi) from the northern edge of the Alaska Range across the Tanana Valley to the southern end of the Yukon–Tanana Uplands and is parallel to the Fairbanks and Minto Seismic Zones located further west.
1138 Aleppo earthquake: Delfi Fault Zone: 25: Central Greece: Normal to strike-slip: Denali Fault ... Queen Charlotte-Fairweather Fault: 800: Canada and Alaska ...
According to the U.S. Geological Survey (USGS), the first magnitude 6.3 earthquake occurred just before 11 a.m. local time on Sunday in the Pacific Ocean about 70 miles southwest of Adak, Alaska ...
Tectonic map of Alaska and northwestern Canada showing main faults and historic earthquakes Denali Fault and the Denali National Park boundary. The Denali Fault is a major intracontinental dextral (right lateral) strike-slip fault in western North America, extending from northwestern British Columbia, Canada to the central region of the U.S. state of Alaska.
“Because this area has been in, or on the edge, of numerous large historical earthquakes, we are keeping close watch on it.” There are small earthquake swarms every couple of years on average in the subduction zone along the Aleutian chain. A swarm occured in May about 350 miles (550 kilometers) east of Sunday's activity, the center said.
ANCHORAGE, Alaska (AP) — The magnitude 7.0 earthquake that rattled Alaska's largest city cracked roads and collapsed highway ramps, but there were no reports of widespread catastrophic damage or ...
The Totschunda Fault is a major active dextral (right-lateral) continental strike-slip fault in southeastern Alaska. It forms a link between the Denali Fault to the northwest and the Fairweather Fault to the southeast. The northwestern end of the fault ruptured during the 2002 Denali earthquake. [1]
The 1964 Alaska earthquake, also known as the Great Alaska earthquake and Good Friday earthquake, occurred at 5:36 PM AKST on Good Friday, March 27, 1964. [2] Across south-central Alaska , ground fissures, collapsing structures, and tsunamis resulting from the earthquake caused about 131 deaths.