Boulton, G. and Lunn, R.J. and Vidstrand, P. and Zatsepin, S. (2007) Subglacial drainage by groundwater-channel coupling, and the origin of esker systems: part 1 - glaciological observations. Quaternary Science Reviews, 26 (7-8). pp. 1067-1090. ISSN 0277-3791Full text not available in this repository. Request a copy from the Strathclyde author
This work is presented in two parts. Part I presents observations on the coupling between subglacial channel flow and groundwater flow in determining subglacial hydraulic regime and creating eskers from an Icelandic glacier that is suggested as an analogue for many parts of Pleistocene ice sheets. Part II develops a theory of perennial subglacial stream flow and the origin of esker systems, and models the evolution of the subglacial stream system and associated groundwater flow in a glacier of the type described in Part I. It is suggested that groundwater flow may be the predominant mechanism whereby meltwater at the glacier bed finds its way to the major subglacial streams that discharge water to glacier margins.
|Keywords:||subglacial drainage, groundwater-channel coupling, aesker systems, glaciological observations, civil engineering, Engineering (General). Civil engineering (General), Global and Planetary Change, Ecology, Evolution, Behavior and Systematics, Geology|
|Subjects:||Technology > Engineering (General). Civil engineering (General)|
|Department:||Faculty of Engineering > Civil and Environmental Engineering|
|Depositing user:||Strathprints Administrator|
|Date Deposited:||07 Sep 2009 11:10|
|Last modified:||22 Mar 2017 10:09|