Accession Number : AD0647272
Title : SLIDING OF NON-TEMPERATE GLACIERS.
Descriptive Note : Research rept.,
Corporate Author : COLD REGIONS RESEARCH AND ENGINEERING LAB HANOVER N H
Personal Author(s) : Weertman,J.
Report Date : DEC 1966
Pagination or Media Count : 10
Abstract : It is shown that the temperature gradient normal to the bed is an important parameter in determining whether sliding can or cannot occur in a glacier whose bottom surface is at the melting point. Only if a large temperature gradient exists will sliding be prevented. Since the temperature gradient of a glacier whose bottom surface is at the melting point is expected to be small, it is concluded that sliding usually will occur in such a glacier even if obstacles in the bed may protrude into cold ice. (Author)
Descriptors : (*GLACIERS, MOTION), MELTING, CREEP, VELOCITY, FRICTION, SHEAR STRESSES, THERMAL PROPERTIES
Subject Categories : Snow, Ice and Permafrost
Distribution Statement : APPROVED FOR PUBLIC RELEASE