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justification for its material and methods ham-
pered progress in achievingscientific engage-
ment with the environment. This kind of
physical geography (foundedeitherin the dis-
closure of spatial associations or in
the examination of human–environment
relations – the contested identities of the sub-
ject: Turner, 2002) demanded a vocabulary
and style of enquiry adapted to the scale and
scope of landscape and regional study, which
set it far apart from the other sciences, and
which, throughout the latter half of the twen-
tieth century, did not seem relevant to their
increasingly reductionist methodologies.
As regionalism itself receded from the geo-
graphical stage, the role and relations of phys-
ical geography were once more examined. By
this time, climatology, geomorphology and
ecology were all well advanced separately,
and without areal relations as a touchstone,
there were uncomfortable parallels with the
identity crisis of earlier generations:
It is clear that physical geography, however
much it overlaps with the earth sciences,
must be distinguished from disciplines
which study terrestrial phenomena for their
own sake, irrespective of their relevance to
the spatial characterisation of man’s occu-
pancy and exploitation ... (Chorley, 1971,
p. 95)
For Chorley, there were several ways forward
for physical geography to avoid increasing
divergence within geography and to ensure
‘relevance’ to science and society beyond:
common application of techniques and
methods (model-building and increasingly,
GIS); study of resources and development;
and (general) systems theory (GST), in large
part adapted from Ludwig von Bertalanffy (a
biologist). Of these, only the last topic was
new, and for Chorley, it was only this that
provided a truly integrating concept and a
widely transferable approach:
. .. systems can be visualised as three-
dimensional structures in which the very
complicated flows and relationships forming
the socio-economic spatial decision-making
systems interpenetrate the physical process-
response systems ... (ibid., p. 22)
1900
Huntington
Fleure
Bowman
Brunhes
Blache
Leploy
Rat-
zel
Chistiolm
Ripley
Matthew
Kappen
Bjerknes
Bort
Worming Monn
Darvin
L. Green
Agassiz
Peschel
Cook
Franklin
Mac-
kenzie
Living stone
Nanseon
Scott
Peary
Penok
Suess
Davis
De Mor-
ranne
Buckan
1850
Ritter
Cuvier
Humboldt
PATTERNS
URBAN
SETTLEMENT
FORECASTING
SOCIOL: GEOG
ECON: GEOG
BIO: GEOG
METEOROLOGY
CLIMATOLOGY
MORPHOLOGY
SURVEYS
EXPLORATION
ASTRON: GEOG
HIST: GEO
PHYSICAL
HUMAN
ETHNOLOGY
Varenius
Newton
Delisle
Harrison
D’Anville
1800
1750
1700
THEOCRATIC
GEO CRATIC
WEOCRATIC
physical geography 2: The ramifications of modern geography since 1700(Taylor, 1953, fig. 1, p. 4)
Gregory / The Dictionary of Human Geography 9781405132879_4_P Final Proof page 535 1.4.2009 3:20pm
PHYSICAL GEOGRAPHY