MORAVIAN GEOGRAPHICAL REPORTS - Institute of Geonics ...
MORAVIAN GEOGRAPHICAL REPORTS - Institute of Geonics ...
MORAVIAN GEOGRAPHICAL REPORTS - Institute of Geonics ...
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MoraVian geographical reports 4/2010, Vol. 18<br />
SW territory (forests) and in the vicinity <strong>of</strong> the cities<br />
(arable land). Areas under a greater human impact are<br />
located in the north near the Levoča city; these areas<br />
neighbour with the areas <strong>of</strong> zero intensity (Fig. 11 –<br />
see cover p. 3). This area was originally used as forest<br />
and later as arable land. Extensification prevails in<br />
the E and central S part <strong>of</strong> the territory. These areas<br />
were mostly used as arable land and later as forests or<br />
grasslands. The whole study area is transected with<br />
lines representing extensification or intensification.<br />
However, these lines are mostly results <strong>of</strong> map sources<br />
inaccuracy and represent a spatial shift <strong>of</strong> grasslands<br />
following rivers and streams.<br />
5. Conclusion<br />
The long term land use development survey <strong>of</strong> the<br />
lower Spiš region uncovered several land use change<br />
trends. The most visible trend in the land use is<br />
the decrease <strong>of</strong> arable land since the second half <strong>of</strong><br />
the 20 th century. The trend is mostly in progress in the<br />
contact zone between arable land and forest where due<br />
to land abandonment the arable land is overgrowing<br />
with the secondary succession. It is also reflected in<br />
the land use change intensity where the most intensive<br />
changes are situated at the perimeter <strong>of</strong> the basin in<br />
the contact zone between forest and arable land.<br />
The land use intensification occurred in the N basin<br />
part, where forests were changed to arable land or<br />
grasslands. Extensification was in progress mostly due<br />
the conversion <strong>of</strong> arable land into forest or grassland<br />
especially in the higher situated parts <strong>of</strong> the basin and<br />
steeper slopes <strong>of</strong> its mountain borders. The comparison<br />
<strong>of</strong> land use development and its main trends in the<br />
lower Spiš region and neighbouring regions or in<br />
18<br />
Categories (number <strong>of</strong> changes) 0 1 – 2 3 – 4 5 – 6 7 – 8 9 – 16<br />
Ratio 33.4% 21.8% 21.4% 16.0% 4.3% 3.2%<br />
Tab. 3: Absolute intensity <strong>of</strong> land use change<br />
Trend <strong>of</strong> land use change Ratio<br />
Extensification 18.2%<br />
Unchanged or restored land use form 67.1%<br />
Intensification 14.7%<br />
Tab. 4: Relative intensity <strong>of</strong> land use<br />
References:<br />
similar landscapes (basins surrounded by mountains<br />
or plateaus, Olah et al., 2006, 2010) unveiled several<br />
similarities as follows:<br />
a)<br />
b)<br />
c)<br />
d)<br />
e)<br />
basic urban/agriculture/forest division <strong>of</strong> basin<br />
landscape was stabilised already before the 1st studied time horizon (18th century),<br />
extensification <strong>of</strong> land use (increase <strong>of</strong> grasslands,<br />
shrubs and forests) since 1950s,<br />
rapid urbanisation since the 1900s but mainly since<br />
the 1950s,<br />
the most stable land use categories occupy the most<br />
suitable parts (geomorphology, soil and hydrology),<br />
the most land use dynamic zones are situated<br />
on the transition <strong>of</strong> main plains-hills-mountains<br />
geomorphological zones.<br />
While the main trends are almost identical for all<br />
compared regions, they differ in quantity (more<br />
dynamic landscape in the High Tatras) or in the<br />
occurrence <strong>of</strong> special factors (water scarcity on<br />
karst plateaus and slopes and wetlands in the basin<br />
bottoms in the Slovak Karst). The second part <strong>of</strong><br />
the picture is the socioeconomic development <strong>of</strong> the<br />
region. Flourishing medieval times contributed to<br />
the region’s development and conversely the shift<br />
<strong>of</strong> the new development in the 20 th cent. to the<br />
western part <strong>of</strong> the region somehow contributed to<br />
the preservation <strong>of</strong> the unique landscape. However,<br />
for the future preservation and development <strong>of</strong> the<br />
region the thoughtful regional management based on<br />
a sustainable use <strong>of</strong> landscape is crucial. The results<br />
<strong>of</strong> this study could be applied in understanding the<br />
landscape response to human activities.<br />
Acknowledgements<br />
This article was supported by the Science Grant<br />
Foundation VEGA project No. 01/0026/08 “Land<br />
use development and its relation to the landscape<br />
ecological complex's elements” and project<br />
No. 1/0557/10 “Changing landscape conditions<br />
and anthropogenic impact indicators”.<br />
BOLTIŽIAR, M. (2004): Analýza zmien krajinnej štruktúry Belianskych Tatier v rokoch 1949 – 1998 aplikáciou výsledkov<br />
DPZ a GIS. In: Štúdie o Tatranskom národnom parku, Vol. 7, No. 40, Marmota Press, Poprad, p. 483 – 491.<br />
BOLTIŽIAR, M. (2007): Štruktúra vysokohorskej krajiny Tatier. Veľkomierkové mapovanie, analýza a hodnotenie zmien<br />
aplikáciou údajov diaľkového prieskumu zeme. UKF FPV Nitra, SAV Ústav krajinnej ekológie, Slovenský národný komitét<br />
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