Landforms Flashcards

1
Q

what are the phases of the historical study of landforms?

A

Phase 1 - exploration of the world (to mid 19th century)
phase 2 - establishment of the discipline - early theories of environmentalism (late 19th century)
phase 3 - dominance of regonal geography (detailed area descriptions - early 20th century)
phase 4 - emergence of human and physical geog - mid 20th century)
phase 5 - physical, integrated and human geography (late 20th century)

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2
Q

what was physical geography before 1800?

A
  • Ancient Greeks and Romans were concerned with topographic descriptions of places and maps
  • Dark Age Europe merely relied on Greek and Roman texts and rejected anything against the teachings of the church
  • Arab geographers were pioneering fieldwork
  • Chinese triangulation techniques for mapping
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3
Q

The Renaissance 15th and 16th Centuries

A
  • Renewed interest in geographical knowledge of the ancients due to issues of exploration, patriotism and colonization
  • Period of major invention and discovery
  • Time keeping, mapping and printing
  • Importance began to be placed on real-world experience (triumph of experience over authority was central at that time)
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4
Q

what is catastrophism and when was it around as a theory?

A

until 1830s

Ascribes the origin of Earth’s landforms to one or more “catastrophic” themes:

  • instantaneous formation during Creation
  • formation after Noah’s Flood
  • earthquake and volcanic activity
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5
Q

who was George Cuvier and what did he explain?

A

(1769-1832)
french anatomist and paleontologist, explained the patterns of extinction and faunal succession observed in the fossil record.

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6
Q

who translated cuvier’s work and linked it with the biblical flood?

A

Robert Jameson (1774-1854)

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7
Q

whats uniformitarianism and when was it around?

A

1830-1930+
also termed gradialism
‘the present is key to the past’ - coined by William Whewell in a review of Lyell’s book
natural processes shape landforms through gradual changes over long periods of time.

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8
Q

uniformitarianism does not include…

A

the role of catastrophic events. eg volcanic eruptions, meteorite impacts, massive floods.

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9
Q

Coming from the Romantic school of thought, WHO believed that “…nature is perfect till man deforms it with care”

A

Alexander von Humboldt (1769-1859)

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10
Q

Who extended uniformitarianism to biology (evoloution) and wrote the book ‘origin of species’ (1859) stating humans and animals were not that different at all?>

A

Charles Darwin (1809-1882)

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11
Q

who suggested the cycle of erosion?

A

William Morris Davies (1850-1934)

compatible with uniformitarianism

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12
Q

what is the davisian cycle of erosion?

A

1890-1950,
a) young uplifted stage with very limited incision
b) mature stage with deep valley incision and complex topography
c) old eroded landscape with few geographic features
stages = structure, process, time

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13
Q

what was the glacial theory?

A

1840 - louis agassiz
multiple glaciations
most of northern america, n europe, n asia had been covered in ice sheets later termed the pleistocene

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14
Q

who wrote ‘The Great Ice Age and its Relationship to the Antiquity of Man’

A

James Geike, 1874

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15
Q

who was Grove Karl Gilbert?

A

(1843-1918)

  • American geologist who joined the famous ‘Powell Survey’ in Rocky Mountain Region in 1874
  • Recognized importance of describing physical processes and systems of laws (using quantitative methods)
  • Proposed concept of dynamic equilibrium
  • Detailed analysis of fluvial processes in his work ‘Geology of the Henry Mountains’ (1877)
  • Gilbert’s ideas did not become popular until 1950s
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16
Q

when was the quantitative revoloution?

A
1950s, a period of global moderntiy (science driving society)
Arthur Strahler (1918-2002) argued the need for physically-based real-world measurements (opposed to Davis)
Move towards quantitative and statistical approaches
17
Q

what is the ‘Strahler Stream Order’

A

1952, a system developed for classifying streams according to the power of their tributaries

18
Q

what is the ‘equilibrium concept’

A

Hack 1960 realised -

  • Rather than a single long Davisian erosion process there is a more dynamic set of processes (non-cyclic)
  • Rejuvenated Gilbert’s concepts of dynamic equilibrium
  • often depends where and when you measure something as to whether it shows equilibrium
19
Q

what are the 3 timescales of equilibrium?

A

(a) dynamic equilibrium, 10,000 years (cyclic time);
b) steady-state equilibrium, 100 years (Graded time);
(c) static equilibrium, 0.1 years (static time)

20
Q

who proposed the climatic geomorphology?

A

Julius Büdel (1903-1983)

21
Q

what are the 3 types of geomorphology?

A
- Historical geomorphology
Catastrophism and Uniformitarianism
- Process geomorphology
Gilbert and Strahler
- Climatic geomorphology
Büdel
22
Q

what sociologist tried to distinguish science from religion?

A

Auguste Comte (1820s)

23
Q

response to large events depends on….

A

the time since the last event (relaxation time)

  • a large flood event may carry less sediment because a first flood flushed it all out
  • ecosystem disturbance causes species to decline - needs sufficient time to recover to original levels.
  • environmental response to a particular event depends on the sensitivity of the particular environment.
24
Q

historical overview - what hapenned in 1950s?

A

Quantitative revolution (positivist science)

25
Q

historical overview - what hapenned in 1970s?

A

cause - effect relationships became the focus

26
Q

historical overview - what hapenned in 1990s?

A

realism (importance of case studies) proposed alternative to the problems of positivism