Geomorphology - 1 Flashcards

1
Q

What is geomorphology

A

An ancient discipline

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2
Q

What is Aristotle’s idea

A

Idea of changing places land and sea

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3
Q

18th and 19th Century believed …

A

In the instantaneous creation of Earth and its features

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4
Q

Playfair

A

1802

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5
Q

1802

A

Playfair

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6
Q

Playfair, 1802

A

Landforms shaped by slow continuous flow of water eroding land

Uniformitarianism

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7
Q

Lyell

A

1830

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8
Q

1830

A

Lyell

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9
Q

Lyell, 1830

A

Principles of geology

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10
Q

Berhadi

A

1832

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11
Q

Bernhadi, 1832

A

First evidence of glaciation

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12
Q

Darwin

A

Social, economic and hillslope evolution

Idea that things evolve over time

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13
Q

William Morris Davis

A

1889

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14
Q

Davis, 1889

A

Created the geographical cycle
- youth, maturity, old, peneplain

Approach refined over the next 50 year’s

Doesn’t involve the concept of climate change

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15
Q

Powell

A

1875

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16
Q

Powell, 1875

A

Created the concept of base level, the lowest elevation at which a stream can erode

17
Q

Gilbert

A

1877

18
Q

Gilbert, 1877

A

Developed the description of weathering and erosion

Identified steady state model and concept of equilibrium

19
Q

1941

A

Bagnold

20
Q

Bagnold, 1941

A

Developed equations used for the physics of landscapes

Sediment transportation

21
Q

Horton

A

1945

22
Q

Horton, 1945

A

Horntons law - stream orders and channels

Hydro physical approach to morphology

23
Q

Strahler

A

1952

24
Q

Strahler, 1952

A

Dynamics basis of geomorphology

25
Q

1964

A

Leopold

26
Q

Leopold, 1964

A

Fluvial processes in geomorphology

27
Q

Process - response approach

A

Explains functional relationships between geomorphical processes and landforms

Gilbert, 1950

28
Q

Hack, 1975

A

Dynamic equilibrium model

Idea that landscape always adjusts

29
Q

Legacy of process - response approach has been largely to:

3 points

A

1) build up a database of process observations and rates
2) develop simple models for predictions of short term changes
3) generate ideas about stability and instability in geomorphic systems

30
Q

Before 1950s

A

Historical approaches
- just a narrative

Present is the key to the past

31
Q

Post 1950s

A

Development process of geomorphology

Understanding of times and scales

32
Q

Tooth

A

2009

No current successful promotion of geomorphology

Ipcc, 2007 missed valuable links between geomorphic and climate change

Increased links with applied sciences = policy and planning

E.g. slope failure and engineers

33
Q

Church

A

2010

Development in understanding is influential in reorientation of geomorphical timescales e.g absolute dating methods

Need to construct law other theories of sediment fluxes on timescales

Cosmogenic isotopes date time, exposure, weathering and residence times of sediments

34
Q

Orme

A

2013

Idea that climate change needs to be incorporated into the Davison cycle, identifying related changes

Importance in understanding how fluvial systems and erosion are affected, in underpinning the Davison model and reduction to peneplain