Community news

Speleology in Kazakhstan

Shakalov on 04 Jul, 2018
Hello everyone!   I pleased to invite you to the official site of Central Asian Karstic-Speleological commission ("Kaspeko")   There, we regularly publish reports about our expeditions, articles and reports on speleotopics, lecture course for instructors, photos etc. ...

New publications on hypogene speleogenesis

Klimchouk on 26 Mar, 2012
Dear Colleagues, This is to draw your attention to several recent publications added to KarstBase, relevant to hypogenic karst/speleogenesis: Corrosion of limestone tablets in sulfidic ground-water: measurements and speleogenetic implications Galdenzi,

The deepest terrestrial animal

Klimchouk on 23 Feb, 2012
A recent publication of Spanish researchers describes the biology of Krubera Cave, including the deepest terrestrial animal ever found: Jordana, Rafael; Baquero, Enrique; Reboleira, Sofía and Sendra, Alberto. ...

Caves - landscapes without light

akop on 05 Feb, 2012
Exhibition dedicated to caves is taking place in the Vienna Natural History Museum   The exhibition at the Natural History Museum presents the surprising variety of caves and cave formations such as stalactites and various crystals. ...

Did you know?

That temporary hardness is see carbonate hardness.?

Checkout all 2699 terms in the KarstBase Glossary of Karst and Cave Terms

What is Karstbase?

Search KARSTBASE:

keyword
author

Browse Speleogenesis Issues:

KarstBase a bibliography database in karst and cave science.

Featured articles from Cave & Karst Science Journals
Chemistry and Karst, White, William B.
See all featured articles
Featured articles from other Geoscience Journals
Karst environment, Culver D.C.
Mushroom Speleothems: Stromatolites That Formed in the Absence of Phototrophs, Bontognali, Tomaso R.R.; D’Angeli Ilenia M.; Tisato, Nicola; Vasconcelos, Crisogono; Bernasconi, Stefano M.; Gonzales, Esteban R. G.; De Waele, Jo
Calculating flux to predict future cave radon concentrations, Rowberry, Matt; Marti, Xavi; Frontera, Carlos; Van De Wiel, Marco; Briestensky, Milos
Microbial mediation of complex subterranean mineral structures, Tirato, Nicola; Torriano, Stefano F.F;, Monteux, Sylvain; Sauro, Francesco; De Waele, Jo; Lavagna, Maria Luisa; D’Angeli, Ilenia Maria; Chailloux, Daniel; Renda, Michel; Eglinton, Timothy I.; Bontognali, Tomaso Renzo Rezio
Evidence of a plate-wide tectonic pressure pulse provided by extensometric monitoring in the Balkan Mountains (Bulgaria), Briestensky, Milos; Rowberry, Matt; Stemberk, Josef; Stefanov, Petar; Vozar, Jozef; Sebela, Stanka; Petro, Lubomir; Bella, Pavel; Gaal, Ludovit; Ormukov, Cholponbek;
See all featured articles from other geoscience journals

Search in KarstBase

Your search for conservation (Keyword) returned 138 results for the whole karstbase:
Showing 1 to 15 of 138
Conservation Through Commercialization: Rio Camuy Development Proposal, 1967, Gurnee, Jeanne, Guest Editor

Cave Conservation - A Lost Cause ?, 1972, Wilmut J.

Archeology and Speleology: The Case for Conservation, 1977, Anderson, David G.

Alternatives to the Letter Writing Approach in Conservation, 1977, Hargrove, Gene

Evaluation Criteria for the Cave and Karst heritage of Australia - Report of the Australian Speleological Federation - National Heritage Assessment Study (1977), 1977, Davey, A. G. (ed)

Protection and management of natural heritage features such as karst landforms requires considered evaluation of the relative significance of individual features. The grounds for significance depend on the perspective taken. Aesthetic, educational, scientific and recreational values are all relevant and must each be given explicit recognition. Karst landforms are often considered primarily from a scientific perspective. The criteria used for evaluation of such natural heritage features for conservation and management purposes need to reflect this full range of values. This means that karst sites may have significance from one or more of these perspectives, as examples of natural features or landscapes, as examples of cultural features or landscapes or as the site of recreation opportunities. Some such sites will be identified as significant because they are representative of their class (irrespective of the relative importance of classes); others will be judged as significant because they are outstanding places of general interest.


The Subterranean Fauna and Conservation of Mona Island (Puerto Rico): A Caribbean Karst Environment, 1981, Peck Stewart B. , Kukalovapeck Jarmila

A Review of Cave Conservation Sites in Britain, 1983, Waltham A. C.

Sport and Scout Caving - The Present Dilemma, 1987, Crabb, Evalt

This paper traces the evolution of organised caving as a post World War 2 phenomenon, and the changes in practice and attitude that have occurred. These practices are contrasted against stated behavioural codes. Parallel to this, the development of caving as a scouting activity is discussed, with reference to the general principles and practices of scouting. The author has been working toward evolving policies and practices within scouting which are consistent with the needs of conservation and the underlying philosophies of scouting. Implementation of these attitudes in one area is fully detailed, with some comment on the success and acceptability of the program. This training program is contrasted against the foreshadowed N.S.W. Branch Policy on Rock-Related Activities. The sequential discussion highlights some weaknesses within clubs and A.S.F., particularly in our methods of communication. There are no firm proposals, but possible directions for future discussions are indicated. It is the intention of this paper to give a historical perspective to some of the present perceived conflicts; in reality, the only conflict is between our oft-expressed aim of conservation of caves (i.e. safeguard the karst heritage of Australia), and our visible activity - use of caves for recreational activity. Both the intensity of expression of our concern, and lessening of self-constraint on recreational activity have greatly magnified with time; we are fast approaching a 'crossroads' scenario where our credibility is at great risk.


Mount Etna Caves: The Fight to Save Mount Etna Caves from Limestone Mining, 1987, Vavryn, Josef M. C.

This treatise is a record of the dates and events, heavily condensed, of the history of Mount Etna since The Caves area was first settled. I hope to show that since the fight to save Mount Etna was first joined, seriously, in 1964 or there about, that the Central Queensland Company and the Queensland Government has had no intention to voluntarily release Mount Etna from limestone mining. Even in the event that conservationists took the Queensland Government to court, the Government had plans prepared to counter such. That was clearly shown when the government rescinded the Recreation Reserve, R444, on Mount Etna and refused to give a fiat to prosecute the Government. The next event, the passing of a law stating that any mining lease inadvertently granted illegally will now stand and be legal, was aimed at the mining lease granted illegally including Mount Etna. At this point in time there is very little that is being done to save Mount Etna. I hope that this paper will create new interest and revive the flagging "Fight to Save Mount Etna", with input from ASF member societies and individuals. If the treatise does not have the desired effect of renewing interest in the fight, and if the Central Queensland Cement Co. Pty. Ltd. Starts mining the main cavernous northern face of Mount Etna, the next ASF conference, or possibly the following, will have a "Letter of Requiem" read to them. If the Australian Public can save the "Gordon-below-Franklin" area and the "Lindeman Island National Park", surely something can be done for Mount Etna.


Cave Conservation: Special Problems of Bats, 1989, Mccracken, Gary F.

Palaeoclimate determination from cave calcite deposits, 1992, Gascoyne M,
Calcite deposits formed in limestone caves have been found to be an excellent repository of palaeoclimatic data for terrestrial environments. The very presence of a relict deposit indicates non-glacial conditions at the time of formation, and both 14C and uranium-series methods can be used to date the deposit and, hence, the age of these climatic conditions. Variations in 13C and 18O content of the calcite, in 2H and 18O content of fluid inclusions, in trace element concentrations and, more recently, in pollen assemblages trapped in the calcite, are all potentially available as synchronous palaeoclimatic indicators. Previous work has tended to concentrate mainly on abundance of deposits as a palaeoclimatic indicator for the last 300,000 years. This literature is briefly reviewed here, together with the theory and methods of analysis of the U-series and stable isotopic techniques. The combined use of U-series ages and 13C and 18O variations in cave calcites illustrates the potential for palaeoclimate determination. Previously unpublished results of stable isotopic variations in dated calcites from caves in northern England indicate the level of detail of stable isotopic variations and time resolution that can be obtained, and the complexity of interpretation that may arise. Tentative palaeoclimatic signals for the periods 90-125 ka and 170-300 ka are presented. More comprehensive studies are needed in future work, especially in view of the difficulty in obtaining suitable deposits and the ethics of cave deposits conservation

The phototropic phytospeleothems of Moss Palace, Mole Creek, Tasmania, 1992, Lichon, Michael J.

In Moss Palace, the presence of unusual speleothems further justifies the conservation of Dogs Head Hill karst at Mole Creek, Tasmania. A "symbiotic" carbonate deposition and growth of the moss Distichophyllum microcarpum results in phototropic phytospeleothems, in the form of fan-shaped erratics.


POLLUTION OF LIMESTONE AQUIFER DUE TO URBAN WASTE-DISPOSAL AROUND RAIPUR, MADHYA-PRADESH, INDIA, 1994, Bodhankar N, Chatterjee B,
During the rainy season deterioration in the quality of water, supplied through dug wells and tube wells, near an abandoned limestone quarry was reported. The abandoned quarry is now being used as an urban waste disposal site. The problem was further complicated by hospitalization of several inhabitants who were using this water for domestic purposes. Looking into the consequences, chemical analysis of water from the quarry, dug wells and tube wells was carried out. The water was found to be contaminated. The transportation of pollutants from the quarry to the groundwater system was facilitated by karst features. Furthermore, four major sources domestic waste disposal, water conservation structures, landfills, and water wells contributing to pollution were identified. This case study is an attempt to provide an understanding of how the karst features facilitate groundwater contamination. It will help us answer a few questions such as why karst hydrogeology deserves special attention in urban expansion and what protective measures should be planned in view of rapid urbanization

Cave Conservation Plans: The role of English Nature, 1995, Glasser N. F. , Barber G.

Conservation of limestone pavement, 1995, Webb Simon

Results 1 to 15 of 138
You probably didn't submit anything to search for