V monografiji je natančno opisana kvantitativna metodologija za merjenje recentnih sub-mikronskih intenzitet temeljnih kemičnih kraških procesov (raztapljanja in odlaganja sige) in podaja rezultate 7-letnega merjenja kemičnih procesov v izbranih slovenskih vodnih jamah. Podrobneje so prikazani rezultati meritev iz nekaterih večjih slovenskih jam, kot so Križna jama, Postojnsko-Planinski jamski sistem in Škocjanske jame, kjer dobimo vpogled tudi v časovno in prostorsko dinamiko širjenja rovov na ravni posameznih jamskih sistemov. Meritve so edinstvene v slovenskem prostoru, pa tudi širše v okviru svetovnega krasoslovja, saj predstavljajo velik kvantitativni premik v okviru kraške geomorfologije.

This book illustrates the diversity of hypogene speleogenetic processes and void-conduit patterns depending on variations of the geological environments by presenting regional and cave-specific case studies. The cases include both well-known and newly recognized hypogene karst regions and caves of the world. They all focus on geological, hydrogeological, geodynamical and evolutionary contexts of hypogene speleogenesis. The last decade has witnessed the boost in recognition of the possibility, global occurrence, and practical importance of hypogene karstification (speleogenesis), i.e. the development of solutional porosity and permeability by upwelling flow, independent of recharge from the overlying or immediately adjacent surface. Hypogene karst has been identified and documented in many regions where it was previously overlooked or misinterpreted. The book enriches the basis for generalization and categorization of hypogene karst and thus improves our ability to adequately model hypogene karstification and predict related porosity and permeability. It is a book which benefits every researcher, student, and practitioner dealing with karst.

Originally published in 1989, Karst Geomorphology and Hydrology became the leading textbook on karst studies. This new textbook has been substantially revised and updated. The first half of the book is a systematic presentation of the dissolution kinetics, chemical equilibria and physical flow laws relating to karst environments. It includes details of the many environmental factors that complicate their chemical evolution, with a critique of measurement of karst erosion rates. The second half of the book looks at the classification system for cave systems and the influence of climate and climatic change on karst development. The book ends with chapters on karst water resource management and a look at the important issues of environmental management, including environmental impact assessment, environmental rehabilitation, tourism impacts and conservation values. Practical application of karst studies are explained throughout the text. "This new edition strengthens the book's position as the essential reference in the field. Karst geoscientists will not dare to stray beyond arm's reach of this volume. It is certain to remain the professional standard for many decades." Journal of Cave and Karst Studies, August 2007

This monograph presents the state of art of the geologic knowledge about the Spanish coast obtained through scientific research in the last 30 years.From a general point of view, coasts are the most quickly changing systems of the Earth. This is critical, since many human resources, such as the main part of economic and social activities, are located in the coastal areas. Especially in the case of Spain these coasts include cities, wide industrial areas (including harbor complexes), important ecologic systems, and our main economic resource: tourism. Understanding the dynamic functioning of each element of this coast is vital for correct future coastal management, so as to solve problems derived from bad plans developed in the last decades of the twentieth century. This is a valuable text for advanced graduate students and coastal researchers, which connects the specific dynamic functioning of the main Spanish coastal environments and their relationships with human activities.

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.