College of Sciences Campus Box 8208 Department of Marine Earth & Atmospheric Sciences 1125 Jordan Hall 2800 Faucette Drive meas.ncsu.edu Raleigh, NC 27695-8208 Final Technical Report May 31, 2017 USGS Award Number: G15AP00091 Title of Award: Establishing a High-Resolution Post-Glacial Chronology of Surface Rupture on the Lake Creek—Boundary Creek Fault, Puget Sound Region, Washington State Authors & Affiliations: Karl W. Wegmanna, Elana L. Leitholdb, and DelWayne R. Bohnenstiehlc Department of Marine, Earth, and Atmospheric Sciences North Carolina State University 2800 Faucette Drive Raleigh, NC 27695-8208 a E-mail:
[email protected]; Tel: 919-515-0380; Fax: 919-513-8812 b E-mail:
[email protected]; Tel: 919-515-7282; Fax: 919-513-8812 c E-mail:
[email protected]; Tel: 919-515-7449; Fax: 919-513-8812 Term Covered by Award: Start: July 1, 2015 End: February 28, 2017 Abstract: The Lake Creek–Boundary Creek fault and the Sadie Creek splay fault are similar to a number of steeply dipping crustal faults in the Puget Sound region exhibiting evidence for latest Pleistocene-Holocene surface rupture that accommodate north-south contraction and clockwise rotation of the Cascadia forearc in western Washington. The fault zone trends directly beneath Lake Crescent, which occupies a deep, glacially-scoured valley in Olympic National Park. There is direct physical evidence for surface ground rupture along at least 56 km of the fault zone both beneath Lake Crescent as well as to the west and east of the lake. Large Holocene landslide scarps surround the lake, and swath bathymetric data demonstrate that these failures deposited large masses of material into the lake itself.