Articles | Volume 21, issue 6
Nat. Hazards Earth Syst. Sci., 21, 1971–1982, 2021
Nat. Hazards Earth Syst. Sci., 21, 1971–1982, 2021

Research article 30 Jun 2021

Research article | 30 Jun 2021

Assessing local impacts of the 1700 CE Cascadia earthquake and tsunami using tree-ring growth histories: a case study in South Beach, Oregon, USA

Robert P. Dziak et al.

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Cited articles

Atwater, B., Satoko, M. R., Satake, K., Yoshinobu, T., Kazue, U., and Yamaguchi, D. K.: The orphan tsunami of 1700-Japanese clues t a parent earthquake in the North America, US Geol. Survey Professional Paper 1707, US Geological Survey, Reston, Virginia, USA, p. 14, 2006. 
Atwater, B. F.: Geologic evidence for earthquakes during the past 2000 years along the Copalis River, southern coastal Washington, J. Geophys. Res., 97, 1901–1919, 1992. 
Atwater, B. F. and Yamaguchi, D. K.: Sudden, probably coseismic submergence of Holocene trees and grass in coastal Washington State, Geology, 19, 706–709, 1991. 
Atwater, B. F., Tuttle, M. P., Schweig, E. S., Rubin, E. S., Yamaguchi, D. K., and Hemphill-Haley, E.: Earthquake recurrence inferred from paleoseismology, Dev. Quatern. Sci., 1, 331–350, 2003. 
Black, B. A., Dunham, J. B., Blundon, B. W., Brim-Box, J., and Tepley, A. J.: Long-term growth-increment chronologies reveal diverse influences of climate forcing on freshwater and forest biota in the Pacific Northwest, Global Change Biol., 21, 594–604, 2015. 
Short summary
On 26 January 1700 CE, a massive earthquake and tsunami struck the US Pacific Northwest west coast. The tsunami caused severe damage to coastal forests in Washington State. However, evidence of the impact on coastal Oregon trees has been difficult to find. We present some of the first evidence of tree-ring growth changes caused by the 1700 tsunami from an old-growth Douglas-fir stand located in South Beach, Oregon. We also present a tsunami inundation model of the 1700 earthquake.
Final-revised paper