nstantaneous and historical temperature effects on a-pinene
GIS
utilization in determining the limits between low morphological units
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Author Details
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SorinAvram
(Corresponding author)
Geography
Department, University
of Craiova,
Str.Al.I.Cuza,
nr. 13, Craiova,
Romania
e-mail:
asorin@clicknet.ro
AlinaVladut
Geography Department, University of Craiova, Str.Al.I.Cuza,
nr. 13, Craiova,
Romania
GheorgheCurcan
Geography Department, University of Craiova, Str.Al.I.Cuza,
nr. 13, Craiova,
Romania
SanduBoengiu
Geography Department, University of Craiova, Str.Al.I.Cuza,
nr. 13, Craiova,
Romania
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Publication Data
Paper received:
08
October 2010
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Revised
received:
07
July 2011
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Accepted:
30 July 2011
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Abstract
The limit between low
morphological units is quite difficult to be established due to the fact that
the lithological, elevation and/or structure
differences are hardly visible. Thus, the contact between piedmont and plain
units is represented, in many cases, by areas where limits are hard to be
drawn. In order to establish the way geographic information system (GIS) may
contribute to the determination of the aforementioned limits, we used the
situation of the limit between the Getic Piedmont
and the Romanian plain and compared the obtained results to examples from
other areas with different formation and evolution conditions. Presently, the
Getic Piedmont undergoes a modelling
process as valleys widen, torrential enlargements laterally advance, and
slope denudation develop, which make difficult to establish a clear southern
limit. The fan texture of the valleys, their age, the flowing direction, as
well as the differences of altitude, lithology, and
structure disposal represent the main elements when establishing
limits even in the case of GIS analysis. The drawing of thematic layers
rendering elements such as hydrographic system, hypsometry, DEM on a
traditional cartographic support, orthophotoplans,
satellite images, for a better interpretation of the geomorphologic aspects
allow a more objective attempt of reconstructing the morphological limits.
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Key
words
Geomorphologic limit,
Geographic information system (GIS), Getic Piedmont