Week 10 references Flashcards

1
Q

Plucking and bedrock communition forms a continuum:

Fractured bedrock

Pulverised bedrock

Mono-lithological diamicton

A

Hiemstra et al 2007

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2
Q

Stress (and therefore failure) is exponential towards the ice-bed interface

A

van der Wateren 1995

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3
Q

Deforming bed theory found by researching how ice streams are moving so fast in Antarctica

A

Alley 1986, 1987

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4
Q

A and B horizon tills in deforming bed theory

A

Boulton and Hindmarsh 1987

Boulton et al 2001

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5
Q

Experiment on Breidamerkurjokull, outlet of Vatnajokull SE Iceland for deforming bed theory

A

Boulton and Hindmarsh 1987

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6
Q

Ice deformation; Breidamerkurjokull till strain patterns = non-linearly viscous material

A

Boulton and Hindmarsh 1987

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7
Q

Ice deformation; perfect plastic rheology

A

Iverson et al 1997, 1998

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8
Q

Ice deformation; plastic failure at vertically migrating levels

A

Engelhardt and Kamb 1998

Truffet et al 1999/2000

Tulaczyk et al 2000

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9
Q

Ice deformation; observations of subglacial tills from paleo-ice sheet beds = plastic failure at vertically migrating levels

A

Evans et al 2006

O Cofaigh et al 2007

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10
Q

Sub-till and intra-till stratified sediments are indicative of sliding glacier bed conditions

A

Piotrowski and Tulaczyk 1999

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11
Q

Sliding and deforming bed mosaic is related to temporal and spatial variation in subglacial effective pressure (Pi-Pw)

A

Boulton et al 2001

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12
Q

Subglacial landforms form a bedform continuum

A

Rose 1987

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13
Q

Subglacial landforms are formed by different processes = distinct populations

A

Clark 1993

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14
Q

Approaches to studying subglacial landforms: morphometry

A

Smalley and Unwin 1968

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15
Q

Approaches to studying subglacial landforms: Sedimentology

A

Shaw et al 2000

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16
Q

Approaches to studying subglacial landforms: Modelling

A

Hindmarsh 1998

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17
Q

Eskers = sinuous elongate ridges of glacifluvial sand and gravel

A

Benn and Evans 1998

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18
Q

Eskers are 10s m high, 100s m wide, 1000s m long

A

Storrar et al 2014

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19
Q

Eskers can be deposited in beads of deposition in less than 24 hours

A

Burke et al 2008

20
Q

The main types of esker

A

Arren and Ashley 1994

21
Q

Concertina esker concept

A

Knudsen 1995

Brennand 2000

22
Q

Crevasse-fill ridges are related to glacier surges

A

Sharp 1985

23
Q

Crevasse-fill ridges aka geometric ridge

A

Bennett and Glasser 1996

24
Q

Some flutes may be erosional

25
Formation of flute from sediment deforming into the lower pressure cavity down ice from an obstacle
Boulton 1976
26
Sub types of flutes
Benn and Evans 1996
27
Drumlins recently found growing under Antarctica
King et al 2007 Smith et al 2007
28
Drumlins can cross cut
Clark 1995
29
Drumlins have a range of internal sediment types
Stokes et al 2011
30
Drumlins - subglacial till deformation
Boulton 1987
31
Drumlins - catastrophic subglacial meltwater floods
Shaw et al 1989
32
Drumlins - instability theory
Stokes et al 2016
33
Key of subglacial till deformation = even without resistant cores, instabilities develop in deforming till
Hindmarsh 1998 Clark 2010
34
Where does the water come from for catastrophic meltwater flood drumlins?
Clarke et al 2005
35
Drumlins - erodent layer hypothesis
Eyles et al 2016
36
First reported and named MGSL in early 1990s
Clarks 1993
37
Initial mechanism of MSGL
Clark 1993
38
MSGL have recently been found under Rutford Ice Stream W Antarctica using radar/seismic data
King et al 2009
39
MSGL could also be relating to groove ploughing
Clark et al 2003
40
MSGL could be meltwater surges
Shaw et al 2008
41
Rogen moraine genesis - shearing/stacking of subglacial sediment
Ayleswroth and Shilts 1989 Bouchard 1989
42
Rogen moraine genesis; subglacial megafloods
Fisher and Shaw 1992
43
Rogen moraine genesis; fracturing theory based on jigsaw pattern
Hättestrand and Kleman 1997
44
Who systematically quantified the characteristics of rogen moraines
Dunlop and Clark 2002
45
Drumlins, MSGLs and flutes are related in a bedform continuum
Stokes et al 2013 Aartio 1977 Rose and Later 1977 Rose 1987 Ely et al 2016