| Summary: | Examines an assessment of fast-receding glaciers situated around costal Glacier Bay, Alaska, by glaciologists from Ohio State University. The study focuses on how the glaciers deposit silt as they retreat, primarily by inserting dye below the glacier into the water table in order to trace the flow pattern and rate of glacial runoff. Title of clip supplied by cataloger. Narrator: Paul Herlinger Content focuses on: Alaska, Mountains, Glaciers To order a reproduction, inquire about permissions, or for information about prices, see: http://www.lib.washington.edu/specialcollections/services/reproduction/reproduction
|
|---|