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“Unusual relief forms“ on Velebit Mt., Croatia
2010Located along the Adriatic coast, the Velebit Mt. is the largest mountain range in Croatia. As a part of extensive Dinaric karst region, it consists of a wide variety of stratigraphic units, ranging in age from Carboniferous to Quaternary. Structurally, Velebit Mt. represents an anticline built up predominantly of carbonate rocks.
Dražen, Perica +2 more
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Fluviokarst of Velebit Mt. (Croatia)
2001The origin and evolution of fluviokarst features on Velebit Mt. is conditioned by hydrogeological beds that build it. Since most of its structure is developed in permeable limestone beds fluviokarst forms are rare. Besides hydrogeological characteristics of the beds important role in their development has slope inclination.
Buzjak, Nenad, Perica, Dražen
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Cave register of North Velebit mt.
2011jeverni Velebit izrazito je krško područje, a površina terena u potpunosti je izgrađena od okršavanju podložnih karbonatnih stijena: mezozojskih vapnenaca i dolomita, te tercijarnih karbonatnih breča (Velić & Velić, 2009). Krški masiv Sjevernog Velebita omeđen je ponornim područjima rijeka Like i Gacke s istočne te obalom mora sa zapadne strane.
Stroj, Andrej +2 more
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Bizarre karst landforms on Velebit Mt.
2005Carbonate substrate of the Velebit Mt. karst favoured development of some bizarre landforms. The carbonate rocks exposed on the Velebit Mt. date from Middle Permian age (but exposed only in a small area) to Eocene-Oligocene age. The outcrops reveal varieties of limestones, calcareous dolomites, dolomites and carbonate breccias. The odd-shaped (bizarre)
Marjanac, Tihomir +2 more
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Middle Permian calcispongal cement reef on the Velebit Mt
Vijesti Hrvatskoga geološkog društva, 2000Middle Permian middle zone of black limestones exposed near Baške Oštarije on the Velebit Mt. is reinterpreted as ecological and morphological calcispongite reef. The reef framework is made of fenestellid bryozoans and calcisponges. It is possible to recognize two overgrowth generations.
Sremac, Jasenka, Marjanac, Tihomir
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Geology of the Central Velebit Mt.(Croatia)
Lička revija, 2005Velebit se u geološkom smislu, kao dio krških Dinarida i Jadranske karbonatne platforme, sastoji od sedimenata vrlo velikog raspona starosti: od karbona (oko 320 milijuna godina) pa do oligocena (oko 24 milujuna godina), ukupne debljine od gotovo 10.000 m.
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2007
Dan je popularni prikaz permske alge Mizzia Velebitana koja je prije točno 100 godina pronađena na Velebitu.
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Dan je popularni prikaz permske alge Mizzia Velebitana koja je prije točno 100 godina pronađena na Velebitu.
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Velebit Mt. Permian - Jurassic carbonates
2014U terenskom vodiču se opisuju stijene i facijesi u starosnom rasponu od srednjeg Perma do mlađe Jure koji su otkriveni na području srednjeg velebita.
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2007
The succession on Velebit Mt. provides evidence of shallow-marine deposition with several periods of emergence from the Late Carboniferous (Moscovian) to the Oligocene, when the dominant uplift phase took place. Quaternary deposits in highlands and valleys tell the story of the more recent geological history, including the Pleistocene glaciation.
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The succession on Velebit Mt. provides evidence of shallow-marine deposition with several periods of emergence from the Late Carboniferous (Moscovian) to the Oligocene, when the dominant uplift phase took place. Quaternary deposits in highlands and valleys tell the story of the more recent geological history, including the Pleistocene glaciation.
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