Week 10 references Flashcards
Plucking and bedrock communition forms a continuum:
Fractured bedrock
Pulverised bedrock
Mono-lithological diamicton
Hiemstra et al 2007
Stress (and therefore failure) is exponential towards the ice-bed interface
van der Wateren 1995
Deforming bed theory found by researching how ice streams are moving so fast in Antarctica
Alley 1986, 1987
A and B horizon tills in deforming bed theory
Boulton and Hindmarsh 1987
Boulton et al 2001
Experiment on Breidamerkurjokull, outlet of Vatnajokull SE Iceland for deforming bed theory
Boulton and Hindmarsh 1987
Ice deformation; Breidamerkurjokull till strain patterns = non-linearly viscous material
Boulton and Hindmarsh 1987
Ice deformation; perfect plastic rheology
Iverson et al 1997, 1998
Ice deformation; plastic failure at vertically migrating levels
Engelhardt and Kamb 1998
Truffet et al 1999/2000
Tulaczyk et al 2000
Ice deformation; observations of subglacial tills from paleo-ice sheet beds = plastic failure at vertically migrating levels
Evans et al 2006
O Cofaigh et al 2007
Sub-till and intra-till stratified sediments are indicative of sliding glacier bed conditions
Piotrowski and Tulaczyk 1999
Sliding and deforming bed mosaic is related to temporal and spatial variation in subglacial effective pressure (Pi-Pw)
Boulton et al 2001
Subglacial landforms form a bedform continuum
Rose 1987
Subglacial landforms are formed by different processes = distinct populations
Clark 1993
Approaches to studying subglacial landforms: morphometry
Smalley and Unwin 1968
Approaches to studying subglacial landforms: Sedimentology
Shaw et al 2000
Approaches to studying subglacial landforms: Modelling
Hindmarsh 1998
Eskers = sinuous elongate ridges of glacifluvial sand and gravel
Benn and Evans 1998
Eskers are 10s m high, 100s m wide, 1000s m long
Storrar et al 2014