Pregled bibliografske jedinice broj: 870041
Structure of Soil Cover on Dolomites of Samobor and Zumberak Hills
Structure of Soil Cover on Dolomites of Samobor and Zumberak Hills // Acta botanica Croatica, 54 (1995), 1; 141-149 (recenziran, članak, znanstveni)
CROSBI ID: 870041 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Structure of Soil Cover on Dolomites of Samobor and Zumberak Hills
Autori
Mayer, Branimir ; Vrbek, Boris
Izvornik
Acta botanica Croatica (0365-0588) 54
(1995), 1;
141-149
Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni
Ključne riječi
soil cover ; Žumberak ; Samobor ; dolomites
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.
Izvorni jezik
Engleski
Znanstvena područja
Geologija, Šumarstvo
POVEZANOST RADA
Ustanove:
Hrvatski šumarski institut, Jastrebarsko