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    Denali Fault

    Strike-Slip Fault · United States of America, Canada

    The Denali Fault is a strike-slip fault, where the two blocks slide horizontally past each other. Its mapped traces are about 2,650 km long in the United States of America and Canada. It lies within the North American Plate, which deforms under the push of neighbouring plates. Its slip rate is estimated between 0.2 and 5 mm per year depending on the section. Since 1900, 2 major earthquakes have occurred within 30 km of its trace.

    Type
    Strike-Slip Fault
    Mapped Length
    ≈ 2,650 km
    Slip Rate
    0.2 – 5 mm per year
    Countries
    United States of America, Canada
    Plates
    North American Plate

    Major Earthquakes Within 30 km

    Deadly or magnitude 7+ earthquakes recorded by NOAA, most recent first.

    Sources: GEM Global Active Faults (Styron et Pagani, 2020), CC BY-SA 4.0, catalogue GEM Faulted Earth · NOAA NCEI · Bird (2003), PB2002 · Wikidata