Reevaluation of tsunami formation by debris avalanche at Augustine Volcano, Alaska
Debris avalanches entering the sea at Augustine Volcano, Alaska have been proposed as a mechanism for generating tsunamis. Historical accounts of the 1883 eruption of the volcano describe 6- to 9-meter-high waves that struck the coastline at English Bay (Nanwalek), Alaska about 80 kilometers east of Augustine Island. These accounts are often cited as proof that volcanigenic tsunamis from Augustine Volcano are significant hazards to the coastal zone of lower Cook Inlet. This claim is disputed because deposits of unequivocal tsunami origin are not evident at more than 50 sites along the lower Cook Inlet coastline where they might be preserved. Shallow water (
Citation Information
| Publication Year | 2000 |
|---|---|
| Title | Reevaluation of tsunami formation by debris avalanche at Augustine Volcano, Alaska |
| Authors | C. Waythomas |
| Publication Type | Article |
| Publication Subtype | Journal Article |
| Series Title | Pure and Applied Geophysics |
| Index ID | 70022816 |
| Record Source | USGS Publications Warehouse |