Week 7 references Flashcards

(25 cards)

1
Q

Controls on erosion and form

A

Sugden and Joh 1976

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2
Q

Small landform types

A

Benn and Evans 1998

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3
Q

P-forms originally thought to be due to abrasion of plastically deforming ice

A

Dahl 1965

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4
Q

P-forms are similar to water eroded scour marks

A

Shaw 1988

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5
Q

P-forms have striae on their face so must be glacial

A

Goldthwaite 1979

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6
Q

P-forms; striae created after formation and their tortuous appearance suggests its not ice

A

Shaw 1988

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7
Q

P-forms observed with debris rich basal ice in situ

A

Boulton 1974

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8
Q

P-forms observed with ice turning corners

A

Rea and Whlley 1994

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9
Q

P-forms and fluvial features represent alternating erosion forms

A

Boulton 1974

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10
Q

Roche moutons tend to form under thin ice with fluctuating Pw

A

Sudden et al 1992

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11
Q

Bedrock structure is important in the formation of roche moutonnees

A

Sugden et al 1992

Roberts et al 2005

Lane et al 2014

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12
Q

Nye channels can be used to reconstruct subglacial meltwater drainage and equipotential contours

A

Booth and hallet 1993

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13
Q

Tunnel valleys formed by steady state meltwater drainage over deformable bed towards end of glacial stage

A

Shoemaker 1986

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14
Q

Tunnel valleys formed as time-transgressive formation close to ice margin

A

Kristensen et al 2008

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15
Q

Later meltwater channels can be used to reconstruct marginal recession and ice sheet elevation

A

Greenwood et al 2007

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16
Q

Largest pro-glacial channels from by jokulhlaups e.g. channeled scablands in Washington State, USA

A

Baker and Bunker 1985

17
Q

Streamlined hard beds

A

Eyles et al 2012/2015

Krabbendam et al 2016

18
Q

Quarrying and abrasion in rock basins and over deepening and enhanced by meltwater pressure variations

A

Hooke 1991

Kor et al 1991

19
Q

In troughs and fjords positive feedback is linked to topographic steering and erosion proportional to ice discharge

A

Jamieson et al 2008

Kessler et al 2008

20
Q

Cirques = flat-floored/overdeepened basin connected to steep back wall by concave slope

A

Benn and Evans 1998

21
Q

Types of cirques

A

Benn and Evans 1998

22
Q

Cirques develop from more than one episode of occupancy

A

Evans and Cox 1995

23
Q

Density/orientation/altitude of cirques can be used as palaeoclimate indicators

24
Q

Jakoshavn Isbrae forms landscape of areal scour and selective linear erosion

25
Recent studies of the various scales of landforms at Jakobshavn Isbrae to reconstruct ice sheet and ice stream evolution
Roberts et al 2005, 2010