Geomorfološke značajke Ogulinsko-plaščanske zavale

master's thesis

• Title (english): Geomorphological Features of the Ogulin-Plaški Depression
• Author: Nedeljka Pejić
• Mentor: Neven Bočić (mentor)
• Committee member: Neven Bočić (predsjednik povjerenstva)
• Committee member: Nenad Buzjak (član povjerenstva)
• Committee member: Mladen Pahernik (član povjerenstva)
• Granter: University of Zagreb; Faculty of Science; (Department of Geography); Zagreb
• Defense date and country: 2013-09-30, Croatia
• Scientific / art field, discipline and subdiscipline: INTERDISCIPLINARY AREAS OF KNOWLEDGE; Geography

Abstract

Ogulinsko – plaščanska zavala zatvorena je krška depresija oblikovana u karbonatnim naslaga mezozoika, veliki dio u dolomitima trijasa i jure, dok je područje između Ogulina i Oštarija oblikovano u vapnencima donje krede. Istraživano područje zavale površine je oko 270 km2. Ima dinarski pravac pružanja i duljine je oko 35 km, dok joj širina varira između 5 i 10 km. U izradi ovog diplomskog rada korištene su metode geomorfološke analize i sinteze, metoda terenskog istraživanja te geomorfološkog kartiranja. Na temelju raščlanjenosti dna i oboda, cijela zavala se može podijeliti na sjeverni Ogulinsko-oštarijski dio i južni Modruško-plaški. Krške depresije na dnu zavale ispunjene sedimentima aluvijalnog i proluvijalnog porijekla tvore dva krška polja: Ogulinsko i Plaščansko. Na razvoj reljefa utjecali su krški, fluviokrški, padinski i fluvijalni procesi.

Abstract (english)

The Ogulin-Plaški depression is a closed karst depression built in carbonate sediments of the Mesozoic Era, a large part was built in the Triassic and Jurassic dolomites, while the area between Ogulin and Oštarije was built in the lower Cretaceous limestones. The area of the depression used in this research is about 270 km2. It has Dinaric direction and length of about 35 km, while its width varies between 5 and 10 km. Geomorphological analysis, synthesis and mapping accompanied by fiel research was applied. Based on the segmentation of the bottom and the rim, the whole depression is divided into a northern Ogulin-Oštarije part and the southern Modruš-Plaški part. The karst depressions in the bottom of the depression which are filled with sediments alluvial and sub-alluvial origin consists of two karst poljes: Ogulin polje and Plaški polje. The development of the terrain was influenced by karst, fluviokarst, fluvial, and slope processes.

• Keywords: analiza reljefa; Hrvatska; Ogulinsko-plaščanska zavala; razvoj reljefa; zavala polja u kršu
• Keywords (english): relief analysis; Croatia; The Ogulin-Plaški Depression; landscape development; karst polje
• Language: croatian
• URN:NBN: urn:nbn:hr:217:225520
• Study programme: Title: Geography; specializations in: Physical Geography with Geoecology, Spatial Planning and Regional Development, Heritage and Tourism, Geographic Information Systems; Course: Physical Geography with Geoecology; Study programme type: university; Study level: graduate; Academic / professional title: magistar/magistra geografije (magistar/magistra geografije)
• Type of resource: Text
• File origin: Born digital
• Access conditions: Closed access
• Created on: 2018-01-12 20:31:06