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卡斯卡迪亞隱沒帶自加拿大溫哥華島一路延伸至加州北部,為萬德夫卡(Juan de Fuca)板塊隱沒到北美大陸板塊之下的區域。高芬格指出:「正是這些高摩擦的(板塊)接觸帶,造成對人類最直接的威脅。」
他與研究團隊發現,強震不僅影響北方地區,也可能波及更南方的聖安地列斯斷層,唡條斷層在加州門多西諾角(Cape Mendocino)附近交會,這也是地震學家特別關注的區域。