MODELING CASCADIA TSUNAMIS INTO DISCOVERY BAY AND HOOD CANAL

2017 ◽  
Author(s):  
Carrie Garrison-Laney ◽  
◽  
Loyce M. Adams ◽  
Loyce M. Adams
Keyword(s):  
Author(s):  
F. William Simonds ◽  
Peter W. Swarzenski ◽  
Donald O. Rosenberry ◽  
Christopher D. Reich ◽  
Anthony J. Paulson

1968 ◽  
Vol 5 (04) ◽  
pp. 347-373
Author(s):  
Robert B. Harris

On 13 February 1979, the entire west span of the Hood Canal Floating Bridge sank under the action of a very severe storm. Although the significant wave height was estimated as high as 4.7 feet, wind and wave conditions during the storm were well within the design criteria of the bridge.


Radiocarbon ◽  
2015 ◽  
Vol 57 (5) ◽  
pp. 917-941 ◽  
Author(s):  
Ian Hutchinson

Surface-breaking ruptures on shallow crustal faults in the southern Puget Lowland in western Washington State about a millennium ago prompted abrupt changes in land level and triggered tsunamis in Puget Sound. The displacement on the Seattle fault most likely occurred in the 1050–1020 cal BP interval. Structures further south (the Tacoma and Olympia faults, and one or more faults in the southern Hood Canal zone) ruptured at about the same time, or slightly earlier. The low frequency of radiocarbon ages from archaeological sites in the region in the aftermath of the “millennial series” of earthquakes, when compared to bootstrapped samples from a database of 1255 ages from the Pacific Northwest as a whole, suggests that these very large earthquakes had significant socioeconomic consequences. The cultural record from coastal archaeological sites shows that although survivors camped on the shore in the aftermath, many coastal villages appear to have been abandoned, and were not reoccupied for several centuries. There is little evidence, however, to suggest that people migrated from southern Puget Sound to neighboring areas, and no evidence of social conflict in the adjacent areas that might have served as havens.


2009 ◽  
Vol 66 (6) ◽  
pp. 1296-1302 ◽  
Author(s):  
Sandra L. Parker-Stetter ◽  
John K. Horne ◽  
Mariko M. Langness

Abstract Parker-Stetter, S. L., Horne, J. K., and Langness, M. M. 2009. The influence of midwater hypoxia on nekton vertical migration. – ICES Journal of Marine Science, 66: 1296–1302. Hypoxia affects pelagic nekton, fish and large zooplankton, distributions in marine and fresh-water ecosystems. Bottom hypoxia is common, but midwater oxygen minimum layers (OMLs) may also affect nekton that undergo diel vertical migration (DVM). This study examined the response of pelagic nekton to an OML in a temperate fjord (Hood Canal, WA, USA). A 2006 study suggested that the OML created a prey refuge for zooplankton. Using acoustics (38 and 120 kHz), the 2007 night DVM patterns of nekton were quantified before (June, August) and during (September) an OML. All months had similar precrepuscular distributions (>50-m depth) of fish and invertebrates. During the September evening crepuscular period, a zooplankton layer migrated upwards (>1.5 m min−1), but the layer's rate of ascent slowed to <0.5 m min−1 when it reached the lower edge of the OML. The bottom edge of the layer then moved below the OML and remained there for 13 minutes before moving through the OML at >1.0 m min−1. As in June and August, fish in September followed the upward migration of the zooplankton layer to the surface, crossing through the OML. Our results suggest that the 2007 OML did not affect zooplankton or fish vertical distributions.


Ports 2004 ◽  
2004 ◽  
Author(s):  
Richard K. Johnson ◽  
Patrick Clarke
Keyword(s):  

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