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    Fairweather Fault

    Strike-Slip Fault · United States of America

    The Fairweather Fault is a strike-slip fault, where the two blocks slide horizontally past each other. Its mapped traces are about 770 km long in the United States of America. It marks the boundary between the Pacific Plate and the North American Plate. Its slip rate is estimated at 5 mm per year. Since 1900, 4 major earthquakes have occurred within 30 km of its trace.

    Type
    Strike-Slip Fault
    Mapped Length
    ≈ 770 km
    Slip Rate
    5 mm per year
    Countries
    United States of America
    Plates
    Pacific Plate, 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