Denali Fault

E836962

The Denali Fault is a major strike-slip fault in Alaska that accommodates significant lateral motion between tectonic plates and has produced large, damaging earthquakes.

All labels observed (2)

Label Occurrences
Denali Fault canonical 1
Denali Fault system 1

How this entity was disambiguated

Statements (45)

Predicate Object
instanceOf continental transform fault ⓘ
geologic fault ⓘ
strike-slip fault ⓘ
accommodates lateral motion between crustal blocks in Alaska ⓘ
age Cenozoic activity ⓘ
associatedWith Alaska Range orogeny ⓘ
intraplate deformation of the North American Plate ⓘ
country United States ⓘ
crosses Alaska Range ⓘ
deformationStyle horizontal shear ⓘ
displacementType lateral offset of geologic units ⓘ
earthquakeHazard capable of producing large damaging earthquakes ⓘ
formsBoundaryBetween different crustal blocks in interior Alaska ⓘ
hasEvidence linear fault scarps ⓘ
offset glacial and fluvial landforms ⓘ
seismicity alignment ⓘ
hasSegment central Denali Fault segment ⓘ
eastern Denali Fault segment ⓘ
western Denali Fault segment ⓘ
hazardTo infrastructure in interior Alaska ⓘ
length hundreds of kilometers long ⓘ
locatedIn Alaska ⓘ
United States ⓘ
maximumObservedEarthquakeMagnitude approximately 7.9 ⓘ
monitoredBy Alaska Earthquake Center ⓘ
United States Geological Survey ⓘ
movementType strike-slip ⓘ
namedAfter Denali ⓘ
orientation generally east-west trending ⓘ
partOf Alaska Range ⓘ
plateBoundaryRole accommodates part of the relative motion within the North American Plate margin system ⓘ
region interior Alaska ⓘ
relatedTo Tintina Fault system ⓘ
linked to: Totschunda Fault

Totschunda Fault ⓘ
riskCategory significant active fault in Alaska ⓘ
rupturedIn 2002 Denali earthquake ⓘ
ruptureLength2002Event hundreds of kilometers ⓘ
seismotectonicRole major source of large inland earthquakes in Alaska ⓘ
senseOfSlip right-lateral ⓘ
slipRate several millimeters per year ⓘ
studiedInDiscipline seismology ⓘ
structural geology ⓘ
tectonics ⓘ
tectonicSetting North American Plate interior ⓘ
typeOfSeismicity shallow crustal earthquakes ⓘ

How these facts were elicited

Referenced by (2)

Full triples — surface form annotated when it differs from this entity's canonical label.