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Clanek obravnava zakrasevanje ob narivnem kontaktu dolomita in apnenca v Idrijskem Logu in Kosevniku. Ob narivnem stiku se je oblikoval neke vrste kontaktni kras. V dolomitu je povrsinska kraska oblikovanost slabse izražena, v krednih apnencih pa so nastale stevilne vrtace, brezna in požiralniki. Brezna v apnencih in vrtace v dolomitu kažejo genetsko povezanost na narivni kontakt, freaticne oblike pa so nastajale globoko pod narivnim pokrovom. The paper discusses karstification along the thrust contact between dolomite and limestone at Idrijski Log and Kosevnik (west-central Slovenia). Thrust contact induced the formation of a specific contact karst assemblage. Karst morphology is less strongly expressed within the dolomite, whereas the limestones are deeply karstified, with many dolines, shafts and sinkholes. Shafts in limestone and dolines in dolomite show genetic relationship with the thrust contact, whereas preserved fragments of phreatic features originated deep beneath the thrust plane.

Karstification along the Thrust Contact between the Dolomite and Limestone in Idrijski log and Koševnik (Idrijsko, Slovenia)