Titlebook: Cave Exploration in Slovenia; Discovering Over 350 Martin Knez,Tadej Slabe Book 2016 Springer International Publishing Switzerland 2016 Cav

BOOM

https://doi.org/10.1007/978-3-8348-9288-1cation over several karst periods and were subject to a number of karstification and epikarst development phases. Due to denudation, the epikarst, where the rock is markedly dissected by typical surface karst features, moves down the transverse profile of the karst system, through the traces of form

BUCK

Nichtlineare Optik II: Vierwellenmischung,ured to the level of tectonic breccia. This is understandable, as the area in question is part of the Sava compressive wedge which has undergone several phases of tectonic processes. Unlike southwestern Slovenia, where Cretaceous limestone prevails, this karst developed in the Triassic and Jurassic

違抗

alliance

Laconic

978-3-319-36732-3Springer International Publishing Switzerland 2016

彎曲道理

Introduction, Basin, and the Pannonian Basin with the Alps. Slovenian motorways entail an approx. 615 km long network of roads. Almost half of Slovenia consists of karst and more than half of the country’s water supply comes from karst aquifers. Slovenia is the country of the original Karst, which gave its name

TERRA

FEIGN

Injunction

capsule