Acta Botanica Croatica, Vol. 54 No. 1, 1995.
Izvorni znanstveni članak
Structure of Soil Cover on Dolomites of Samobor and Zumberak Hills
Branimir Mayer
; Šumarski institut Jastrebarsko
Boris Vrbek
; Šumarski institut Jastrebarsko
Sažetak
Soil on the dolomites of Samobor and Žumberak hills developed as a consequence of interaction of specific pedogenetic factors. The zone of saccharoidal Triassic dolomites is characterized by heavily dissected relief with tent-like crests with steep sloping sides and cut in "V"-shaped valleys, displaying a great density of valley network. Dolomite parent rock is poorly permeable with a shallow, fairly uniform zone of physical weathering into dolomite gravel, which results in a dominance of calcareous skeletal rendzinas on dolomite.
Ključne riječi
Hrčak ID:
160428
URI
Datum izdavanja:
31.12.1995.
Posjeta: 971 *