3284 KB32 KB198520252013Kodelja, BlažMorris, MalindiStepišnik, UrošStepišnik, UrošŽebre, Manjaštevilka:39str. 157-170ISSN:0354-0596COBISSID:53581666URN:URN:NBN:SI:doc-QWJVCX3KslZnanstvena založba Filozofske fakulteteDela - Oddelek za geografijo Filozofske fakultete v Ljubljanigeomorfologijageomorphologyledena dobaledenikipleistocenSloveniaSlovenijaTrnovo Forest PlateauTrnovski gozdSledovi pleistocenske poledenitve na Trnovskem gozdu|Trnovski gozd is a high karst plateau situated in the Dinaric Mountains of western Slovenia which was modified by glacial action in the Pleistocene. With our research we concluded that slopes with northern exposure and the footslope of the highest ridge of Golaki had an glacier up to 180 m thick with an area of 4.8 km2. Several outlet glaciers were found to have been drifting over a steep escarpment from the plateau to the valleys of Belca, Trebuša and on the Hudo polje plateau. There was no evidence of glaciation on southern exposed slopes. The equilibrium line altitude was established via the accumulation-area ratio method on an elevation of 1240 mTrnovski gozd je visoka kraška planota na dinarskem krasu zahodne Slovenije, ki so jov pleistocenu preoblikovali tudi ledeniški procesi. Ugotovili smo, da je severna pobočja in podnožje najvišjega osrednjega grebena Golaki pokrival ledenik s površino 4,8 km2 in največjo debelino okoli 180 m. V več odtočnih ledenikih je padal preko strme reliefne stopnje v dolini Belce in Trebuše ter na Hudo polje. Prisojna pobočja Golakov niso bila poledenela. Z metodama deleža akumulacijskega dela ledenika ter zgornje meje bočnih moren smo izračunali ravnovesno mejo ledenikov na višini 1240 mTEXTznanstveno časopisjejournalsSlovenian National E-content AggregatorNational and University Library of SloveniaUniverza v Ljubljani, Filozofska fakulteta