G E O L O F G Y O T A N N E D M M T I R N E A R P A E L D I N N O D G U E S R T R O Tracking Prehistoric Cascadia Tsunami Deposits at Nestucca Bay, Oregon, USA I E S 1 937 1 2 1 o PHYSICAL PROPERTIES OF SAND 120 Robert C. Witter , Eileen Hemphill-Haley , and Roger Hart 130 o 125 o Queen Charlotte Three tsunamis triggered by fault INTRODUCTION. 1 2 BRITISH AB A N1 Sandy Deposit C N5 Sandy Deposit COLUMBIA Oregon Department of Geology and Mineral Industries Consulting Micropaleontology North South North South great earthquakes on the Cascadia subduction zone have 10 10 10 100 16 ND-B2, 107-110 cm Upton-06, 162-165 cm Upton -19, 116-118 cm Vancouver 50o o N1 sand N5 sandy mud, upper layer N5 sandy mud 50 S t N4 sandy layer N4 sandy layer r a Coastal Field Office, P.O. Box 1033, Newport, OR 97365 1871 Pickett Road 12 it % Volume % Volume Explorer o inundated Nestucca Bay, Oregon over the past 2000 years. m) River channel 0 0 0 f N5 sandy layer G Vancouver μ e CANADA ( Plate Island o 50 8 0 100 200 300 400 500 600 700 800 900 1000 0 100 200 300 400 500 600 700 800 900 0 100 200 300 400 500 600 700 800 900 1000 Continental rg i U.S.A. C a o size n
[email protected] McKinleyville, CA 95519 10 10 1000 10 ti WASHINGTON 4 n Mean particle S e The primary evidence includes layers of sandy sediment that Thickness (cm) LN-02, 43-45 cm Upton-06, 168-172 cm Upton-24, 96-98 cm e n N5 sandy layer a t w a shelf l N5 sandy mud a 0 0 N1 sandy mud N5 sandy mud, lower layer r s d lo p Seattle 0 500 1000 1500 0 500 1000 1500 e % Volume Puget North % Volume e 0 0 0 d bury tidal marshes submerged by earthquake-related Distance south of Little Nestucca River (m) Distance south of Little Nestucca River (m) Sound g America 0 100 200 300 400 500 600 700 800 900 1000 0 100 200 300 400 500 600 700 800 900 1000 0 100 200 300 400 500 600 700 800 900 1000 e Grays Harbor Plate Particle size (μm) Particle size (μm) o Willapa f 10 Bay subsidence.