ILLUSTRATIONS 



Figure Page 



7^ Wave energy spectriim for tide-gage marigram at Crescent City, 



registered at the time of the Chile tsunami, May I96O 113 



75 Wave crest elevation above still water as a function of 



relative water depth and wave steepness I16 



76 Influence of resonance on wave runup on uniformly sloping -, -, „ 

 Continental Shelves 



77 Maximum heights of tsunami waves recorded at tide 

 stations along the North American seahoard from Alaska 



to Vancouver Island 119 



78 Maximum heights of tsunami waves recorded at tide 

 stations or river gaging stations in the Vancouver Island 



Region, Canada 120 



79 Maximum heights of tsunami waves recorded along the 

 Washington-Oregon coastline 122 



80 Sample tide gage records from stations along the 



Columbia River 123 



81 Analysis of tsunami wave propagation up the Columbia 



River, Washington-Oregon 12i+ 



82 Maximum runup heights of tsunami waves observed along 



the north-central California coast 127 



83 Geometrical analogy of Monterey Bay to the quadrant of 



a circular basin 129 



8U Possible modes of oscillation for Monterey Bay as a 



circular quadrant basin of uniform depth 130 



85 Marigrams recording the tsunami in Southern California waters . 133 



86 Maximum runup heights of tsunami waves (referred to MLLW) 

 measured along the coasts of the Hawaiian Islands 135 



87 Bathymetry of coastal region adjacent to Kodiak City, Kodiak . 139 



88 Location of the Kodiak Naval Station and the City of Kodiak . . lUO 



89 Map of Kodiak City and Harbor with details of the breakwaters . lUl 



90 Hypothetical marigrams for Kodiak City based on eyewitness 

 observations 1^2 



