Namen knjige je predstaviti rezultate 10 let trajajočih slovensko-čeških raziskav, ko smo predvsem z različnimi paleomagnetnimi metodami intenzivno raziskovali kraške površinske in jamske sedimente v različnih geografskih in geoloških območjih Slovenije. Paleomagnetne raziskave sedimentov so prinesle presenetljive rezultate glede starosti sedimentov v jamah in na površju in s tem tudi prve podrobne informacije o starosti jam in posredno tudi našega krasa. Pri vzorčevanju sedimentov za paleomagnetne analize smo v nekaterih primerih našli fosilne ostanke favne, njihova najdba je zelo pomembna ker, smo tako lahko rezultate paleomagnetnih in magnetostratigrafskih analiz postavili v točno določen čas.

Dinarski kras je obsežno, 800 km dolgo in do 150 km široko kraško območje, ki zavzema večji del Dinarskih gora in zavzema zahodni del Slovenije. Dinarski kras se odlikuje po velikih sklenjenih površinah, izjemni pestrosti reliefnih oblik, izjemnih jamah, velikih rekah ponikalnicah in kraških izvirih. Zaradi izrazitih oblik in pojavov so se tu že zgodaj pojavili opisi krasa pa tudi znanstvena raziskovanja. V 19. stoletju, je iz imena pokrajine Kras nastal termin karst, domača imena za reliefne oblike, dolina, polje, uvala, ponor pa so postali znanstveni termini. Tu so bile odkrite in opisane tudi prve jamske živali. Kljub odkritju številnih novih kraških območij v drugačnih geoloških ali klimatskih pogojih ostaja Dinarski kras še vedno svetovno pomembno kraško področje. Dinarski kras je locus tipicus za številne oblike in pojave, je mesto intenzivnega raziskovanja, pa tudi mesto, kjer se srečujejo krasoslovci s celega sveta. Knjiga na poljudnoznanstven način opisuje osnovne karakteristike Dinarskega krasa ter karakteristične primere tipov površja z Dinarskega krasa.

Encyclopedia of Caves, Third Edition, provides detailed background information to anyone with a serious interest in caves. This includes students, both undergraduate and graduate, in the earth, biological and environmental sciences, and consultants, environmental scientists, land managers and government agency staff whose work requires them to know something about caves and the biota that inhabit them. Caves touch on many scientific interests in geology, climate science, biology, hydrology, archaeology, and paleontology, as well as more popular interests in sport caving and cave exploration. Case studies and descriptions of specific caves selected for their special features and public interest are also included. This book will appeal to these audiences by providing in-depth essays written by expert authors chosen for their expertise in their assigned subject. - Features 14 new chapters and 13 completely rewritten chapters - Contains beautifully illustrated content, with more than 500 color images of cave life and features - Provides extensive bibliographies that allow readers to access their subject of interest in greater depth

The book is the result of joint work and many years of mutual cooperation between researchers from Slovenia and Croatia. It was made as part of the transboundary project ŽIVO! Življenje – voda! (Life – Water!) (IPA CBC SI-HR 2007-2013), which involved the participation of authors from project partner institutions as well as invited authors who are famil­iar with the characteristics of the karst area of Northern Istria and the conditions there relating to drinking water supply. The monograph presents the natural features of Northern Istria, the karst and karst phenomena, karst hy­drogeology, ecology and microbiology, and highlights in particular the vulnerability of the karst to various human activities. The main focus of attention is on karst water sources. In assessing their characteristics we used available knowledge of karst water on both sides of the border and supplemented it with new research on the transboundary area in question, which was based on field measurements and sampling, and chemical, microbiological and biologi­cal analysis of water. The collected findings form the basis for planning more effective monitoring of the quality of karst water sources, their protection and consequently the improvement of their quality. First editon was published in 2015, this corrected second edition is available also in paperback (ISBN 978-961-05-0001-8). _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ Knjiga je rezultat skupnega dela in dolgoletnega medsebojnega sodelovanja raziskovalcev iz Slovenije in Hrvaške. Nastala je v sklopu čezmejnega projekta ŽIVO! Življenje – voda! (IPA CBC SI-HR 2007-2013), kjer so sodelovali tako avtorji iz inštitucij projektnih partnerjev kot vabljeni avtorji, ki poznajo značilnosti kraškega območja severne Istre in tamkajšnje razmere pri oskrbi s pitno vodo. V monografiji so predstavljene naravne danosti severne Istre, kras in kraški pojavi, kraška hidrogeologija, ekologija in mikrobiologija, posebej pa je izpostavljena ranljivost krasa na različne človekove dejavnosti. Glavna pozornost je posvečena kraškim vodnim virom. Pri oceni njihovih značilnosti smo uporabili razpoložljiva spoznanja o kraških vodah z obeh strani meje in jih dopolnili z novimi raziskavami obravnavanega čezmejnega prostora, ki so temeljile na terenskih meritvah in vzorčenju ter kemijskih, mikrobioloških in bioloških analizah vode. Zbrani izsledki so osnova za načrtovanje bolj učinkovite zaščite vodnih virov in posledično za izboljšanje njihove kakovosti. Pregledani ponatis knjige, ki je prvič izšla leta 2015, je na voljo tudi v mehki vezavi (ISBN 978-961-05-0001-8).

This thesis addresses karst development in a terrain characterized by a highly complex geological and geomorphological evolution. It tackles the extent and complexity of both epigenic and hypogenic karst development, based on morphological analyses of caves, combined with analyses and datations of cave sediments and their correlation to regional geological and geomorphological evolution. Hypogenic karst registered is mainly the result of hydrothermal speleogenesis due to increased geothermal gradient in connection with nearby Pliocene-Pleistocene volcanic centers, with occurrence of sulfuric acid speleogenesis and ghost-rock weathering due to local geological or lithological control. Epigenic speleogenesis is strongly controlled by base level oscillations, with also examples of deep phreatic (now fossil) caves connected to regional base level rise, and per-ascensum speleogenesis. Another important finding is the constraining of the timing of Mariovo Lake draining in the Pleistocene, an important event in order to understand the geomorphological evolution in Macedonia, as it led to the onset of fluvial development and incision of valleys, shaping most of the present morphology.

This volume combines review and solicited contributions, related to scientific studies of Division I of IAGA presented at its Scientific Assembly in Sopron in 2009. The book is aimed at intermediate to advanced readers dealing with the Earth’s magnetic field generation, its historical records in rocks and geological formations - including links to geodynamics and magnetic dating, with magnetic carriers in earth materials, electromagnetic induction and conductivity studies of the Earth interior with environmental applications of rock magnetism and electromagnetism. The aim of the book is to provide an overview of recent advances and future challenges in these particular fields of research.

Speleothems (mineral deposits that formed in caves) are currently giving us some of the most exciting insights into environments and climates during the Pleistocene ice ages and the subsequent Holocene rise of civilizations. The book applies system science to Quaternary environments in a new and rigorous way and gives holistic explanations the relations between the properties of speleothems and the climatic and cave setting in which they are found. It is designed as the ideal companion to someone embarking on speleothem research and, since the underlying science is very broad, it will also be invaluable to a wide variety of others. Students and professional scientists interested in carbonate rocks, karst hydrogeology, climatology, aqueous geochemistry, carbonate geochemistry and the calibration of climatic proxies will find up-to-date reviews of these topics here. The book will also be valuable to Quaternary scientists who, up to now, have lacked a thorough overview of these important archives. Additional resources for this book can be found at: www.wiley.com/go/fairchild/speleothem.

The Carpatho-Balkan Geomorphological Commission and the International Association of Geomorphologists (IAG) Carpatho-Balkan-Dinaric Regional Working Group, promote networking between researchers and the exchange of research experience. Following a brief introduction into the geology, climate, hydrology and land cover of the Carpatho-Balkan-Dinaric region, the book provides detailed information on research applying both traditional and innovative techniques and summarizes contemporary knowledge on recent geomorphic processes. It also presents studies of exogenic geomorphic processes from each country. The chapters on Poland, the Czech Republic, Slovakia, Ukraine, Hungary, Romania, Slovenia, Croatia, Serbia, Bulgaria and Macedonia examine the geomorphic processes in shaping the topography of each country. This volume also examines key geomorphic processes influencing land use and economic activities as well as contributions discussing processes under climate change.

Australian Landscapes provides an up-to-date statement on the geomorphology of Australia. Karst, desert, bedrock rivers, coasts, submarine geomorphology, biogeomorphology and tectonics are all covered, aided by the latest geochronological techniques and remote sensing approaches. The antiquity and enduring geomorphological stability of the Australian continent are emphasized in several chapters, but the cutting-edge techniques used to establish that stability also reveal much complexity, including areas of considerable recent tectonic activity and a wide range of rates of landscape change. Links to the biological sphere are explored, in relation both to the lengthy human presence on the continent and to a biota that resulted from Cenozoic aridification of the continent, dated using new techniques. New syntheses of glaciation in Tasmania, aridification in South Australia and aeolian activity all focus on Quaternary landscape evolution.