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The Seattle fault zone is a 4- to 7-km-wide east-trending fault zone that extends from the Cascade Range foothills on the east across the Puget Lowland to Hood Canal, crossing Lake Sammamish, Lake Washington, Puget Sound, Bainbridge Island, and the Kitsap Peninsula. Various strands of the fault zone lie largely concealed beneath the major population centers of Seattle, Bellevue, and Bremerton. It forms the northern boundary of a belt of bedrock exposures that cross much of the Puget Lowland. The depth to bedrock north of the fault zone is as much as 1 km (Yount and others, 1985 #4746; Johnson and others, 1999 #4729). The fault zone has been imaged on seismic-reflection profiles collected in Puget Sound and adjacent waterways (Yount and Gower, 1991 #4744; Johnson and others, 1994 #4730; Pratt and others, 1997 #4737; Johnson and others, 1999 #4729), correlates with large gravity and magnetic anomalies (Danes and nine others, 1965 #4723; Blakely and others, 2002 #4716), and is represented by a prominent velocity anomaly on tomographic models (Brocher and others, 2001 #4718; Calvert and others, 2001 #4722). These data indicate the zone consists of three or more south-dipping thrust faults that form the structural boundary between the Seattle uplift on the south and the Seattle basin on the north. Blakely and others (2002 #4716) have named three of these structures the frontal fault, the Blakely Harbor fault, and the Orchard Point fault. Nelson and others (2003 #5868) termed the 'frontal fault' the 'Seattle fault.' The Seattle fault zone also includes north-dipping reverse or thrust faults, such as the Toe Jam Hill fault (Nelson and others, 2000 #4733; 2002 #4736; 2003 #5868), which forms a complex scarp in densely forested terrain on Bainbridge Island. Slip on both south- and north-dipping faults within the zone probably is associated with offset on a south-dipping master fault (e.g.
, Pratt and others, 1997 #4737) at depth. Surface-deforming earthquakes have occurred on the Seattle fault zone in the latest Holocene, most recently about 1040–910 cal yr BP, (A.D. 900–930) as summarized by Nelson and others (2014 #7675).