Processes on a glacier-dominated coast, Alaska
Zeitschrift fur Geomorphologie, Supplementband
By: Bruce F. Molnia
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Abstract
The 500 km long Gulf of Alaska coastline between Cape Suckling and Cape Spencer can be characterized by constant rapid change in an environment of glaciers, stormy climate, high relief, and extreme oceanographic parameters. During a more than 200-year history of observation, bays have completely filled with sediment, new bays have appeared, glaciers have advanced and retreated as much as 40 km, streams have been captured, and spits have grown as much as 10 km in length, earthquakes have uplifted the coast as much as 15 m, and in general, few features have been static. More than 250 km of coastline have undergone erosion and retreat, with maximum retreat exceeding 4 km at Icy Bay.
Study Area
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Processes on a glacier-dominated coast, Alaska |
| Series title | Zeitschrift fur Geomorphologie, Supplementband |
| Volume | 57 |
| Issue | 4 |
| Year Published | 1985 |
| Language | English |
| Publisher | Schweizerbart Science Publishers |
| Contributing office(s) | Earth Resources Observation and Science (EROS) Center |
| Description | 13 p. |
| First page | 141 |
| Last page | 153 |
| Country | United States |
| State | Alaska |
| Other Geospatial | Gulf of Alaska |
| Online Only (Y/N) | N |
| Additional Online Files (Y/N) | N |
| Google Analytic Metrics | Metrics page |