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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

https://hrcak.srce.hr/160428

Datum izdavanja:

31.12.1995.

Podaci na drugim jezicima: hrvatski

Posjeta: 1.412 *