Introduction to the Dinaric Karst

Dinaric karst is expansive, 800 km long and up to 150 km wide area of karst, which extends over majority of Dinaric mountains and therefore also over the southwestern part of Slovenia. Dinaric karst is an important karst area with remarkable caves, big sinking streams and abundant karst springs. Wel...

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collection Directory of Open Access Books
description Dinaric karst is expansive, 800 km long and up to 150 km wide area of karst, which extends over majority of Dinaric mountains and therefore also over the southwestern part of Slovenia. Dinaric karst is an important karst area with remarkable caves, big sinking streams and abundant karst springs. Well-expresed karst phenomena of Dinaric karst lead to early descriptions and karstological investigations. During the 19th century, a term karst was for the first time used for description of specific area without a superficial drainage system. Some Slavic words for relief forms (doline, polje, uvala, ponor) became world-wide terms. Dinaric karst is also a place of first descriptions of troglobionts. In spite of many other karst areas investigated all over the world Dinaric karst still remains one of the most important karst areas. Dinaric karst is locus tipicus of many features and phenomena. It is place of deep scientific investigation and also the place, where karstologists from all over the globe meet together. Publication in popular science language describes the basic characteristics of Dinaric karst and Slovene examples of relief types in the Dinaric karst area.
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spelling doab-20.500.12854ir-800792024-03-23T14:58:30Z Introduction to the Dinaric Karst Zupan Hajna, Nadja Mihevc, Andrej Prelovšek, Mitja Dinaric karst Dinarski kras thema EDItEUR::1 Place qualifiers::1D Europe::1DX Southeast Europe thema EDItEUR::R Earth Sciences, Geography, Environment, Planning::RB Earth sciences::RBG Geology, geomorphology and the lithosphere::RBGD Geomorphology and geological surface processes Dinaric karst is expansive, 800 km long and up to 150 km wide area of karst, which extends over majority of Dinaric mountains and therefore also over the southwestern part of Slovenia. Dinaric karst is an important karst area with remarkable caves, big sinking streams and abundant karst springs. Well-expresed karst phenomena of Dinaric karst lead to early descriptions and karstological investigations. During the 19th century, a term karst was for the first time used for description of specific area without a superficial drainage system. Some Slavic words for relief forms (doline, polje, uvala, ponor) became world-wide terms. Dinaric karst is also a place of first descriptions of troglobionts. In spite of many other karst areas investigated all over the world Dinaric karst still remains one of the most important karst areas. Dinaric karst is locus tipicus of many features and phenomena. It is place of deep scientific investigation and also the place, where karstologists from all over the globe meet together. Publication in popular science language describes the basic characteristics of Dinaric karst and Slovene examples of relief types in the Dinaric karst area. 2022-04-01T11:46:28Z 2022-04-01T11:46:28Z 2010 book ONIX_20220401_9789612541989_177 9789612541989 https://directory.doabooks.org/handle/20.500.12854/80079 eng image/jpeg Attribution-NonCommercial-NoDerivatives 4.0 International https://zalozba.zrc-sazu.si/p/240 https://omp.zrc-sazu.si/zalozba/catalog/view/711/3000/1320-1 ZRC SAZU, Založba ZRC 10.3986/9789612541989 Dinaric karst is expansive, 800 km long and up to 150 km wide area of karst, which extends over majority of Dinaric mountains and therefore also over the southwestern part of Slovenia. Dinaric karst is an important karst area with remarkable caves, big sinking streams and abundant karst springs. Well-expresed karst phenomena of Dinaric karst lead to early descriptions and karstological investigations. During the 19th century, a term karst was for the first time used for description of specific area without a superficial drainage system. Some Slavic words for relief forms (doline, polje, uvala, ponor) became world-wide terms. Dinaric karst is also a place of first descriptions of troglobionts. In spite of many other karst areas investigated all over the world Dinaric karst still remains one of the most important karst areas. Dinaric karst is locus tipicus of many features and phenomena. It is place of deep scientific investigation and also the place, where karstologists from all over the globe meet together. Publication in popular science language describes the basic characteristics of Dinaric karst and Slovene examples of relief types in the Dinaric karst area. 10.3986/9789612541989 013302f9-95d5-488d-83b2-a050c348c14f 9789612541989 71 Ljubljana open access
spellingShingle Dinaric karst
Dinarski kras
thema EDItEUR::1 Place qualifiers::1D Europe::1DX Southeast Europe
thema EDItEUR::R Earth Sciences, Geography, Environment, Planning::RB Earth sciences::RBG Geology, geomorphology and the lithosphere::RBGD Geomorphology and geological surface processes
Introduction to the Dinaric Karst
title Introduction to the Dinaric Karst
title_full Introduction to the Dinaric Karst
title_fullStr Introduction to the Dinaric Karst
title_full_unstemmed Introduction to the Dinaric Karst
title_short Introduction to the Dinaric Karst
title_sort introduction to the dinaric karst
topic Dinaric karst
Dinarski kras
thema EDItEUR::1 Place qualifiers::1D Europe::1DX Southeast Europe
thema EDItEUR::R Earth Sciences, Geography, Environment, Planning::RB Earth sciences::RBG Geology, geomorphology and the lithosphere::RBGD Geomorphology and geological surface processes
topic_facet Dinaric karst
Dinarski kras
thema EDItEUR::1 Place qualifiers::1D Europe::1DX Southeast Europe
thema EDItEUR::R Earth Sciences, Geography, Environment, Planning::RB Earth sciences::RBG Geology, geomorphology and the lithosphere::RBGD Geomorphology and geological surface processes
url ONIX_20220401_9789612541989_177