Case Studies from the Dinaric Karst of Slovenia

More documents

Recommendations

Info

Andrej Mihevc, Mitja Prelovšek, Nadja Zupan Hajna (Eds.)INTRODUCTION TO THE DINARIC KARSTEditors / Uredniki:Language review / Jezikovni pregled:Photos / Fotografije:Cartography / Kartografija:Design and graphic art / Oblikovanjein grafična ureditev:Published by / Izdal in založil:Represented by / Zanj:Andrej Mihevc, Mitja Prelovšek, Nadja Zupan HajnaCarolyn L. RamseyAuthors of chapters, if not otherwise mentionedMitja PrelovšekMitja PrelovšekInštitut za raziskovanje krasa ZRC SAZU, Postojna /Karst Research Institute at ZRC SAZU, PostojnaTadej SlabePrinted by / Tisk:Printrun / Naklada:Collegium Graphicum d.o.o., Ljubljana300 copies / izvodovPostojna, junij 2010The publication was published within the Karst UndergroundProtection project which is financially supported by the Slovenia-Croatia Operational Programme 2007-2013.Knjiga je bila izdana v okviru projekta Karst UndergorundProtection financiranega iz Operativnega programa IPA Slovenija-Hrvaška 2007-2013.CIP - Kataložni zapis o publikacijiNarodna in univerzitetna knjižnica, Ljubljana911:551.44INTRODUCTION to the Dinaric Karst / edited by Andrej Mihevc,Mitja Prelovšek, Nadja Zupan Hajna ; [photos authors of chapters ;cartography Mitja Prelovšek]. - Postojna : Inštitut za raziskovanjekrasa ZRC SAZU = Karst Research Institute at ZRC SAZU, 2010ISBN 978-961-254-198-91. Mihevc, Andrej, 1952-251366400
Introduction to theDinaric KarstEdited by:Andrej MihevcMitja PrelovšekNadja Zupan HajnaPostojna, junij 2010
Page 4 and 5: ContentsGeographical Position and G
Page 7 and 8: Fig. 2: Coastal part of Dinaric kar
Page 9 and 10: ogy started. In 1531 a lawyer from
Page 11 and 12: include numerous data and general o
Page 13 and 14: GeologyNadja Zupan HajnaThe Dinaric
Page 15 and 16: ceous. The final disintegration of
Page 17 and 18: Fig. 11: Locations of Jelar Breccia
Page 19 and 20: ClimateMitja PrelovšekThe Dinaric
Page 21 and 22: 311 mm/a; Zaninović 2008) and incr
Page 23 and 24: 24Fig. 16: Spatial distribution of
Page 25 and 26: ocks (such as Eocene flysch, Lower
Page 27 and 28: absent. Downstreamparts of the cany
Page 29 and 30: GeomorphologyAndrej MihevcIn folk l
Page 31 and 32: long. They are smoother especially
Page 33 and 34: is now depositing. Best known are t
Page 35 and 36: Structural poljes are dominated by
Page 37 and 38: Fig. 28: Typical dolines of Dinaric
Page 39 and 40: the disintegrated collapsed rock at
Page 41 and 42: on Northern Velebit, where three ca
Page 43 and 44: Land UseNadja Zupan Hajna, Andrej M
Page 45 and 46: for ‘bare limestone desert’ -th
Page 47 and 48: Fig. 38: Grančarevo dam in the upp
Page 49 and 50: KrasThe Kras is a distinct plateau,
Page 51 and 52: in this part of the Kras (Mihevc 20
Page 53 and 54:
dolomite barrier along the Idrija w
Page 55 and 56:
of Dolenjska (Gams, 1974; Kranjc, 1
Page 57 and 58:
Fig. 44: Blind valleys of Matarsko
Page 59 and 60:
ly several dozen meters deep. Shaft
Page 61 and 62:
smaller than the higher ones. The r
Page 63 and 64:
tion in the Divaški kras (Mihevc 1
Page 65 and 66:
Use of Karst and its ProtectionThe
Page 67 and 68:
Gams, I., Vrišer, I. (Eds.), 1998:
Page 69 and 70:
lems.- Dela 38, Raziskovalni center
show all

Case Studies from the Dinaric Karst of Slovenia

Create successful ePaper yourself

Delete template?

Save as template?