I've been in the business for 20 years and the way skilled labor has been treated up until very recently drove a ton of people away from the industry. It is believed capable of generating earthquakes of at least magnitude 7, and there is evidence of such a quake approximately 1,000 years ago, possibly the same earthquake documented on the Seattle Fault 24 miles (38km) to the north. Geologic map of southwestern Washington (GM-34). The discovery was an alarm bell for engineers and emergency planners. The Straight Creek Fault is a major structure in the North Cascades, but has not been active for over 30 million years. Just four miles (6km) south the city of Oak Harbor straddles several stands of the Utsalady Point Fault (UPF) as they head roughly east-southeast towards Utsalady Point at the north end of Camano Island. Olympia VA Clinic at VA Puget Sound health care, 253-583-2621 This is the Puget Lowland. Modeling a Magnitude 7.2 Earthquake on the Seattle Fault Zone in TTY Relay 711. According to the Washington state Department of Natural Resources, more than 1,000 earthquakes happen in Washington state each year! There is evidence that the Tacoma Fault connects with the White River River Fault (WRF) via the EPZ and Federal Way, under the Muckleshoot Basin (see map),[137] and thence to the Naches River Fault. [74], Early Eocene igneous units in the area appear to be part of a 49- to 44- Ma magmatic belt that appeared just after the arrival of Siletzia, and possibly associated with that event. [102] Or the Crescent margin may simply (and quietly) just run south-southeast under Seattle to the WRZ. But their significance to the Puget Sound area is unknown. Curiously, the extension of line "B" north of the OWL is approximately the eastern limit of Puget Sound seismicity, the rest of southwestern Washington and the North Cascades being relatively aseismic (see the seismicity map, above). (Their model of the Black Hills Uplift is analogous with their "wedge" model of the Seattle Uplift, discussed above, but in the opposite direction. NW-striking black lines are right-lateral bedrock faults thought to be subsidiary to Dar- rington-Devils Mountain fault zone (Dragovich and DeOme, 2006). Let's make your home safer The Puget Sound faults under the heavily populated Puget Sound region (Puget Lowland) of Washington state form a regional complex of interrelated seismogenic (earthquake-causing) geologic faults. [58], Paleoseismological studies of the SWIF are scant. [2] All this is at risk of earthquakes from three sources:[3]. Earthquakes occur nearly every day in Washington. (A) Map of the Seattle fault zone (SFZ) in the central Puget Sound (A tsunami generated by a quake on the offshore Cascadia Subduction Zone would be . [183] While the towns of Centralia and Chehalis in rural Lewis County may seem distant (about 25 miles) from Puget Sound, this is still part of the Puget Lowland, and these faults, the local geology, and the underlying tectonic basement seem to be connected with that immediately adjacent to Puget Sound.

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