Accession Number : ADA337542
Title : Stratigraphic Studies in the Snow and Firn of the Greenland Ice Sheet
Descriptive Note : Research rept
Corporate Author : SNOW ICE AND PERMAFROST RESEARCH ESTABLISHMENT WILMETTE IL
Personal Author(s) : Benson, Carl S.
PDF Url : ADA337542
Report Date : AUG 1996
Pagination or Media Count : 182
Abstract : The Greenland ice sheet is treated as a monomineralic rock formation, primarily metamorphic, but with a sedimentary veneer of snow and firn. The sedimentary part is perennial above the firn line, and the classical methods of stratigraphy and sedimentation can be profitably applied to it. During a 4-yr period 146 pit studies and 288 supplementary Rammsonde profiles were made along 1100 miles of over snow traverse (Fig. I). Temperature, density, ram hardness, and grain size were measured in the strata exposed in each pit. Stratification of snow results from variations in the conditions of deposition and is emphasized by subsequent diagenesis. Summer layers are coarser grained and have generally lower density and hardness values than winter layers; they may also show evidence of surface melt. The onset of fall is usually identified by an abrupt increase in density and hard ness accompanied by a decrease in grain size. This stratigraphic discontinuity is used as the annual reference plane.
Descriptors : *SNOW, *LAND ICE, GRAIN SIZE, STRATIGRAPHY, STRATIFICATION, HARDNESS, SEDIMENTATION, GREENLAND.
Subject Categories : Snow, Ice and Permafrost
Distribution Statement : APPROVED FOR PUBLIC RELEASE