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Wednesday, 24 September 2008 22:15 |
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Through the interaction of the topography and climate in the Park, as well as the living world, there are three major soil types in the Park: (a) humic-silicate (rankers); (b) acid brown (cambisols); and (c) ilimerised (brunipodzols, brownised cambisols). Within the areas covered by forest, i.e. molika, beech and oak forests, the acid-brown soils prevail; several varieties and different evolutionary stages can be distinguished within these soils. The humic-silicate soils are found in the sub-alpine and the alpine zone and less frequently in the forest zone. The third soil type is found in the sub-alpine zone in places overgrown by molika trees.
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Last Updated ( Saturday, 27 September 2008 20:49 )
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