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master's thesis
Geomorfološke značajke miljevačkog dijela Sjevernodalmatinske krške zaravni
2019. urn:nbn:hr:162:165333
Grcić, Ivana
University of Zadar
Department of Geography

Cite this document

Grcić, I. (2019). Geomorfološke značajke miljevačkog dijela Sjevernodalmatinske krške zaravni (Master's thesis). Zadar: University of Zadar. Retrieved from https://urn.nsk.hr/urn:nbn:hr:162:165333

Grcić, Ivana. "Geomorfološke značajke miljevačkog dijela Sjevernodalmatinske krške zaravni." Master's thesis, University of Zadar, 2019. https://urn.nsk.hr/urn:nbn:hr:162:165333

Grcić, Ivana. "Geomorfološke značajke miljevačkog dijela Sjevernodalmatinske krške zaravni." Master's thesis, University of Zadar, 2019. https://urn.nsk.hr/urn:nbn:hr:162:165333

Grcić, I. (2019). 'Geomorfološke značajke miljevačkog dijela Sjevernodalmatinske krške zaravni', Master's thesis, University of Zadar, accessed 03 April 2025, https://urn.nsk.hr/urn:nbn:hr:162:165333

Grcić I. Geomorfološke značajke miljevačkog dijela Sjevernodalmatinske krške zaravni [Master's thesis]. Zadar: University of Zadar; 2019 [cited 2025 April 03] Available at: https://urn.nsk.hr/urn:nbn:hr:162:165333

I. Grcić, "Geomorfološke značajke miljevačkog dijela Sjevernodalmatinske krške zaravni", Master's thesis, University of Zadar, Zadar, 2019. Available at: https://urn.nsk.hr/urn:nbn:hr:162:165333

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Metadata
TitleGeomorfološke značajke miljevačkog dijela Sjevernodalmatinske krške zaravni
Title (english)Geomorphological characteristics of the Miljevci plateau in the area of the Notrh Dalmatian karst plateau
AuthorIvana Grcić
MentorNina Lončar (mentor)
Committee memberDražen Perica (predsjednik povjerenstva)
Committee memberMarica Mamut (član povjerenstva)
Committee memberNina Lončar (član povjerenstva)
GranterUniversity of Zadar
(Department of Geography)
Zadar
Defense date and country2019-03-19, Croatia
Scientific / art field,
discipline and subdiscipline		INTERDISCIPLINARY AREAS OF KNOWLEDGE
Geography
Physical Geography
Abstract
Miljevačko područje dio je Sjevernodalmatinske krške zaravni. Nalazi se u trokutu između rijeke Krke, Čikole i planine Promine, a zauzima površinu od 264,89 km2. Geomorfološkom analizom obuhvaćena su morfometrijska i morfogenetska obilježja reljefa. Na temelju izračunatih vrijednosti hipsometrije, nagiba padina i vertikalne raščlanjenosti reljefa uočeno je da je krška zaravan najzastupljenija u hipsometrijskom razredu 200-300 m/nv (74,93%) s prevladavajućim nagibima padina 0-5° (78,27%) na... More zaravnjenom terenu i slabo raščlanjenim ravnicama (0-30 m/km2). U vezu sa morfometrijskim parametrima reljefa dovedene su i ponikve – dijagnostički oblik krškog reljefa. Kartirano je 286 ponikava. Prosječna gustoća iznosi 1 pon/km2 što ovo područje svrstava u prostor s neznatnom gustoćom prema dosadašnjim istraživanjima ponikava na teritoriju RH. Statističkom analizom prostornog rasporeda i distribucije ponikava ustanovljen je vrlo visok stupanj povezanosti ponikava sa prevladavajućim morfometrijskim kategorijama. U okviru endokrškog reljefa uočena je zastupljenost speleoloških objekata jednostavne morfologije i malih dimenzija. S obzirom na vrstu objekata na istraživanom području prevladavaju jamski objekti (64%). Najviše speleoloških objekata nalazi se na zaravni (56%), u istim morfometrijskim kategorijama kao i ponikve. 40% speleoloških objekata nalazi se u kanjonu Čikole i Krke gdje prevladavaju špiljski objekti za razliku od jama koje su više zastupljene na zaravni. Uz morfometrijska obilježja reljefa analizirana su i strukturnogeomorfološka i egzogeomorfološka obilježja. Uz dominantni krški reljef, na istraživanom području izdvojeni su još fluvijalni, fluviokrški, padinski i antropogeni morfogenetski tip reljefa. Less
Abstract (english)
Miljevci plateau is part of the North-Dalmatian karst plateau. It's situated between Krka river, Čikola river and mountain Promina with total area of the 264,89 km2. As a part of the geomorphological analysis, morphometric and morphogenetic characteristics were distinguished. Based on calculated values of the hypsometry, slope and vertical relief dissection it’s noticed that most prominent occurrence of karst plateau is linked with the areas ranging 200-300 meters of altitude (74,93%),... More slope inclination 0-5° (78,27%) and plain relief and weakly dissected plains (0-30 m/km2). Further more, dolines are considered as diagnostic forms of karst. The influence of morphometric parameters on the spatial distribution of the dolines are analysed as well. A total of 286 dolines has been identified in the researched area. According to the recent investigation of doline density on territory of Croatia, this area is classified in area with very low doline density since Miljevci plateau has just 1 doline/km2. A high degree of connection among dolines and prevailing geomorphometric categories is established. Moreover, speleological objects with simple morphology and small dimensions are most frequent. Considering a type of the speleological objects, pits prevail in this area. Most speleological object are found on the plateau (56%) in the same morphometric categories as dolines. 40% of the speleological object are found in canyon of the Čikola and Krka river where caves prevails unlike the pits which are more represented on the plateau. Beside morphometric features of the terrain this paper analyses structural-morphologic and exogeomorphologic characteristics. Along karst relief, fluvial, fluvio-karst, slope and anthropogenic morphogenetic types of the relief formation are determined too. Less
Keywords
Keywords (english)
Languagecroatian
URN:NBNurn:nbn:hr:162:165333
Study programmeTitle: Applied Geography (single major)
Study programme type: university
Study level: graduate
Academic / professional title: magistar/magistra geografije (magistar/magistra geografije)
Type of resourceText
File originBorn digital
Access conditionsAccess restricted to students and staff of home institution
Terms of useLicence In copyright icon
Created on2019-09-09 07:17:34
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