Geomorfološke značajke zavale Oštarijskog polja u kršu
The Baške Oštarije karst polje is stretching out at the direction E - W at lenght of 3,75 km, while the width is varying from 0,25 to 2,0 km. It divides central from the south part of the Velebit mountain and it is formed at the contact of two orographic wholes. Besides karst and fluvio-karst proces...
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| Veröffentlicht in: | Geoadria 2017-01, Vol.7 (2), p.23-34 |
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| container_title | Geoadria |
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| creator | Perica, Dražen Bognar, Andrija Lozić, Sanja |
| description | The Baške Oštarije karst polje is stretching out at the direction E - W at lenght of 3,75 km, while the width is varying from 0,25 to 2,0 km. It divides central from the south part of the Velebit mountain and it is formed at the contact of two orographic wholes. Besides karst and fluvio-karst processes, the derasion and periglacial processes have been most expressed at the relief formation. The water which flows down from edge parts of polje has great importance in relief formation because of its corrosional aggressivity. |
| doi_str_mv | 10.15291/geoadria.87 |
| format | Article |
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It divides central from the south part of the Velebit mountain and it is formed at the contact of two orographic wholes. Besides karst and fluvio-karst processes, the derasion and periglacial processes have been most expressed at the relief formation. The water which flows down from edge parts of polje has great importance in relief formation because of its corrosional aggressivity. </description><subject>Baške Oštarije karst polje</subject><subject>derasion and periglacial processes and relief forms</subject><subject>derazijski i periglacijalni procesi i reljefni oblici</subject><subject>fluvio-karst</subject><subject>fluvio-krški</subject><subject>karst</subject><subject>krški</subject><subject>Oštarijsko polje u kršu</subject><subject>Velebit</subject><subject>Velebit mountain</subject><issn>1331-2294</issn><issn>1848-9710</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2017</creationdate><recordtype>article</recordtype><recordid>eNo9kE1OwzAUhC0EEqWw4wDZQ4qf7SQ2O1TRglSpm-6tV9cu-SmubIoEd-AQuQu5F4EAq_k0mpnFEHIJdAIZU3CztR43ocSJLI7ICKSQqSqAHvfMOaSMKXFKzmKsKM3zDNiI3M6t3_ngfOO7trbJ-zN-fmD1TfiKjU2WXfuCoaxi7bfJ3jcVJoekDl17OCcnDptoL351TFaz-9X0IV0s54_Tu0VqAKBI18ahNUYwk62ZAMqYFErmgkllpDAsd1yg44iZzJRVlGdGgrCFsWojneJjcjXMPgWDtd6HcofhTXss9eDEYGyPWuWM9unrIW2CjzFY918Aqn9O0n8naVnwL4pGX0c</recordid><startdate>20170111</startdate><enddate>20170111</enddate><creator>Perica, Dražen</creator><creator>Bognar, Andrija</creator><creator>Lozić, Sanja</creator><general>Hrvatsko geografsko društvo - Zadar, Odjel za geografiju, Sveučilište u Zadru</general><scope>AAYXX</scope><scope>CITATION</scope><scope>VP8</scope></search><sort><creationdate>20170111</creationdate><title>Geomorfološke značajke zavale Oštarijskog polja u kršu</title><author>Perica, Dražen ; Bognar, Andrija ; Lozić, Sanja</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c1117-bcfaecc42c5b241022849864289c84c26f34af3aa5859e9035c814e7ce9d8f93</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>hrv ; eng</language><creationdate>2017</creationdate><topic>Baške Oštarije karst polje</topic><topic>derasion and periglacial processes and relief forms</topic><topic>derazijski i periglacijalni procesi i reljefni oblici</topic><topic>fluvio-karst</topic><topic>fluvio-krški</topic><topic>karst</topic><topic>krški</topic><topic>Oštarijsko polje u kršu</topic><topic>Velebit</topic><topic>Velebit mountain</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Perica, Dražen</creatorcontrib><creatorcontrib>Bognar, Andrija</creatorcontrib><creatorcontrib>Lozić, Sanja</creatorcontrib><collection>CrossRef</collection><collection>Hrcak: Portal of scientific journals of Croatia</collection><jtitle>Geoadria</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Perica, Dražen</au><au>Bognar, Andrija</au><au>Lozić, Sanja</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Geomorfološke značajke zavale Oštarijskog polja u kršu</atitle><jtitle>Geoadria</jtitle><date>2017-01-11</date><risdate>2017</risdate><volume>7</volume><issue>2</issue><spage>23</spage><epage>34</epage><pages>23-34</pages><issn>1331-2294</issn><eissn>1848-9710</eissn><coden>GEOAFZ</coden><abstract>The Baške Oštarije karst polje is stretching out at the direction E - W at lenght of 3,75 km, while the width is varying from 0,25 to 2,0 km. It divides central from the south part of the Velebit mountain and it is formed at the contact of two orographic wholes. Besides karst and fluvio-karst processes, the derasion and periglacial processes have been most expressed at the relief formation. The water which flows down from edge parts of polje has great importance in relief formation because of its corrosional aggressivity. </abstract><pub>Hrvatsko geografsko društvo - Zadar, Odjel za geografiju, Sveučilište u Zadru</pub><doi>10.15291/geoadria.87</doi><tpages>12</tpages><oa>free_for_read</oa></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 1331-2294 |
| ispartof | Geoadria, 2017-01, Vol.7 (2), p.23-34 |
| issn | 1331-2294 1848-9710 |
| language | hrv ; eng |
| recordid | cdi_hrcak_primary_oai_hrcak_srce_hr_9620 |
| source | DOAJ Directory of Open Access Journals; EZB-FREE-00999 freely available EZB journals |
| subjects | Baške Oštarije karst polje derasion and periglacial processes and relief forms derazijski i periglacijalni procesi i reljefni oblici fluvio-karst fluvio-krški karst krški Oštarijsko polje u kršu Velebit Velebit mountain |
| title | Geomorfološke značajke zavale Oštarijskog polja u kršu |
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