Spatial Patterns of Glacial Erosion at a Valley Scale Derived from Terrestrial Cosmogenic 10BE and 26Al Concentrations in Rock

Fabel, Frederick; Harbor, John; Dahms, Dennis; James, Allan; Elmore, David; Horn, Linda; Daley, Kelly; Steele, Charles

Cultural advice

The Australian National University acknowledges, celebrates and pays our respects to the Ngunnawal and Ngambri people of the Canberra region and to all First Nations Australians on whose traditional lands we meet and work, and whose cultures are among the oldest continuing cultures in human history.

Aboriginal and Torres Strait Islander peoples are advised that ANU Library collections may include images, names, voices, and other representations of deceased persons.

Material in the collection may contain terms, language or views that reflect the period in which the item was created and may be considered inappropriate today.

Spatial Patterns of Glacial Erosion at a Valley Scale Derived from Terrestrial Cosmogenic 10BE and 26Al Concentrations in Rock

Date

2004

Authors

Fabel, Frederick

Harbor, John

Dahms, Dennis

James, Allan

Elmore, David

Horn, Linda

Daley, Kelly

Steele, Charles

Publisher

Blackwell Publishing Ltd

Abstract

The fundamentally geographic issue of the amounts and spatial patterns of erosion necessary to produce classic glacial landforms such as U-shaped valleys has been debated by scientists for over a century. Terrestrial cosmogenic nuclide (TCN) measurements