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Denali Fault information


Denali Fault
EtymologyDenali (mountain)
LocationBritish Columbia, Canada and Alaska, USA
Coordinates63°29′25″N 148°07′33″W / 63.4902°N 148.1257°W / 63.4902; -148.1257
Tectonics
PlateNorth American Plate
Earthquakes2002 Denali earthquake
Typestrike-slip fault
Movementdextral
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.[1]

  1. ^ Benjamin R. Edwards, James K. Russell (August 2000). "Distribution, nature, and origin of Neogene–Quaternary magmatism in the northern Cordilleran volcanic province, Canada" (PDF). Geological Society of America Bulletin. 112 (8): 1280–1295. Bibcode:2000GSAB..112.1280E. doi:10.1130/0016-7606(2000)112<1280:dnaoon>2.0.co;2. Archived from the original (PDF) on 2015-09-24. Retrieved 2009-09-27.

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Denali Fault

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The Denali Fault is a major intracontinental dextral (right lateral) strike-slip fault in western North America, extending from northwestern British Columbia...

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Denali

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topography of Denali is related to the complex structural relationships created by the right-lateral Denali Fault and Denali Fault Bend. The Denali Fault is caused...

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2002 Denali earthquake

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Washington State. The Denali-Totschunda fault is a major dextral (right lateral) strike-slip system, similar in scale to the San Andreas fault system. In Alaska...

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Northern Cordilleran Volcanic Province

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Denali fault systems, have been tectonically active since the Cretaceous period as strike-slip faults. The Denali fault to the west and the Tintina fault to...

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Epicenter

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subsurface fault rupture may be long and spread surface damage across the entire rupture zone. As an example, in the magnitude 7.9 Denali earthquake of...

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Denali National Park and Preserve

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Denali National Park and Preserve, formerly known as Mount McKinley National Park, is a national park and preserve located in Interior Alaska, United States...

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Earthquake

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ruptures on strike-slip faults, like the San Andreas Fault (1857, 1906), the North Anatolian Fault in Turkey (1939), and the Denali Fault in Alaska (2002),...

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New Madrid Seismic Zone

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The New Madrid Seismic Zone (NMSZ), sometimes called the New Madrid Fault Line, is a major seismic zone and a prolific source of intraplate earthquakes...

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List of fault zones

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This list covers all faults and fault-systems that are either geologically important[clarification needed] or connected to prominent seismic activity.[clarification...

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Totschunda Fault

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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...

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Supershear earthquake

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movement on the Kunlun fault 2002 Denali earthquake, magnitude Mw 7.9 associated with strike-slip movement on the Denali Fault 2008 Sichuan earthquake...

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Yellowstone Caldera

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from more than 800 miles (1,300 km) away, and the 2002 7.9 magnitude Denali fault earthquake 2,000 miles (3,200 km) away in Alaska that altered the activity...

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1967 Mount McKinley disaster

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Mount McKinley disaster occurred in July 1967 when seven climbers died on Denali (then still officially known as Mount McKinley) while attempting to descend...

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Alaska Range

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to the east. The range is part of the Pacific Ring of Fire, and the Denali Fault that runs along its southern edge is responsible for many major earthquakes...

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Geology of the United States

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terrane addition is the Denali Fault, which curves through south-central Alaska. The Denali Fault bends just north of Denali. The combination of the subduction...

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Tintina Fault

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Mountain Trench in the northern United States and the Kaltag Fault in Alaska. Denali Fault Rocky Mountain Trench Northern Cordilleran Volcanic Province...

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Earthquake rupture

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place on a single fault, but in many cases the rupture starts on one fault before jumping to another, sometimes repeatedly. The 2002 Denali earthquake initiated...

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Juliet Biggs

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a doctoral researcher, where she studied the earthquake cycle at the Denali Fault. During her doctoral research supervised by Barry Parsons and Tim J....

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Pebble Mine

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quakes occur on the fault on a 700-year cycle. The Lake Clark fault several hundred miles to the north is sub-parallel to the Denali fault and considered to...

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Isabel Pass

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Yukon River drainage, and to the south is the Copper River drainage. The Denali Fault approximately bisects the pass. Castner Glacier is located on its southern...

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Surface rupture

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earthquake M7.8 in Tibet, strike-slip faulting - 400 km (249 mi) 2002 Denali earthquake M7.9 in Alaska, strike-slip faulting - 340 km (211 mi) 2008 Sichuan earthquake...

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Geology of Alaska

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magmatism, rapid uplift and unroofing north of the Denali fault zone, formation of transform transgressional faults, and subduction of the pacific and Yakutat...

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Daisy Geyser

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triggered seismicity in Yellowstone National Park produced by the 2002 M 7.9 Denali fault earthquake, Alaska". Geology. 32 (6): 537–540. Bibcode:2004Geo....32...

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Susitna Glacier

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Susitna Glacier fault. Susitna River Matanuska-Susitna Valley 2002 Denali earthquake "Susitna Glacier, Alaska". NASA. "2002 Denali Fault Earthquake". Science...

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Rocky Mountain Trench

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is one of the two major fault zones paralleling the Northern Cordilleran Volcanic Province, the other being the Denali Fault in the Yukon, the U.S. state...

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Geography of Yukon

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Yukon has scattered patches of permafrost. Two major faults, the Denali Fault and the Tintina Fault have created major valleys called trenches: the Shakwak...

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Geology of Yukon

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gold skarn and copper-molybdenum deposits. To the northeast of the Denali Fault, the Dawson Range and Whitehorse suites batholith generates the gold...

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