The Tintina Fault is a large right-lateral strike-slip fault in western North America, extending from northwestern British Columbia, Canada to the centre of the U.S. state of Alaska. It represents the Yukon continuum between the Rocky Mountain Trench in the northern United States and the Kaltag Fault in Alaska.^[1]

References

North America
(crosses national borders)

Canada

United States

Washington and Oregon	Brothers Fault Zone Olympic–Wallowa Lineament Puget Sound (Seattle Fault, Tacoma Fault) Walker Lane
California	Calaveras Fault Garlock Fault Hayward Fault Zone Mendocino Fracture Zone Newport–Inglewood Fault Puente Hills Fault Rose Canyon Fault San Jacinto Fault Zone (Elsinore Fault Zone)
Great Basin	Independence Valley fault system Moab Fault Teton Fault Wasatch Fault
Great Plains	Central Oklahoma Fault Zone Humboldt Fault Long Point–Eureka Heights fault system Meers Fault Nemaha Fault Zone Wilzetta Fault
Midwest	Marianna Fault New Madrid Seismic Zone Sandwich Fault Zone Wabash Valley Seismic Zone
Appalachian Mountains and Atlantic Coast	Aiken–Augusta Fault Eastern Tennessee Seismic Zone Middleton Place–Summerville Seismic Zone (Woodstock Fault) Northern Appalachians Seismic Zone Ramapo Fault Virginia Seismic Zone

Caribbean and Mexico

See also