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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. ...

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. ...

Speleology in Kazakhstan

Shakalov on 11 Jul, 2012
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 polje is (slavic word for field.) 1. a large, flat floored depression in karst limestone, whose long axis is developed parallel to major structural trends and can reach tens of kilometers in length. superficial deposits tend to accumulate on the floor. drainage may be by either surface watercourses (when the polje is said to be open) or swallow holes (a 'closed' polje.) their development is encouraged by any impedance in the karst drainage [19]. 2. polje or karst polje signifies the flatbottomed lands of closed basins which may extend over large areas, as much as 1,000 km2. the flat floor of the polje may consist of bare limestone, of a nonsoluble formation (and so with rolling topography), or of soil. the polje will show complex hydrogeological characteristics such as exsurgences, swallow holes, estavelles, and lost rivers. in colloquial use, the term polje is applied to flat-bottomed lands which are overgrown or are under cultivation [20]. 3. large flat-floored closed karst depression, with sharp slope breaks between the commonly alluviated floor and the marginal limestone. streams or springs drain into poljes and outflow is underground through ponors. commonly the ponors cannot transmit flood flows, so many poljes turn into wet-season lakes. the form of some poljes is related to the geological structure, but others are purely the projects of lateral dissolution and planation. the dinaric karst has many poljes; the livansko polje is around 60km long and 7km wide. the word is slovene (common also to other slav languages) for a field, reflecting the agricultural value of the alluvial polje floor soils [9]. synonym: interior valley; (french.) polje; (german.) polje; (greek.) polye; (italian.) polje; (russian.) polje; (spanish.) polje; (turkish.) golova, polye; (yugoslavian.) polje. see also karst polje.?

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

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KarstBase a bibliography database in karst and cave science.

Featured articles from Cave & Karst Science Journals
Chemistry and Karst, White, William B.
Engineering challenges in Karst, Stevanović, Zoran; Milanović, Petar
See all featured articles
Featured articles from other Geoscience Journals
Geochemical and mineralogical fingerprints to distinguish the exploited ferruginous mineralisations of Grotta della Monaca (Calabria, Italy), Dimuccio, L.A.; Rodrigues, N.; Larocca, F.; Pratas, J.; Amado, A.M.; Batista de Carvalho, L.A.
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
See all featured articles from other geoscience journals

Search in KarstBase

Your search for bay (Keyword) returned 120 results for the whole karstbase:
Showing 1 to 15 of 120
The Geology of the Cayman Islands (British West Indies), and their Relation to the Bartlett Trough, 1926, Matley Charles Alfred,
The Cayman Islands, a small dependency of the British Empire, with a local government controlled by the Government of Jamaica, occupy an isolated position of exceptional interest, both geographical and geological, in the Caribbean Sea. Situated between Jamaica and Cuba, and flanked on the south by the great depression of the Bartlett Trough, which descends over 20,000 feet within 18 miles of the shores of Grand Cayman, they are the only projecting peaks in the submarine ridge that extends from the Sierra Maestra of Cuba to the Misteriosa Bank in the direction of British Honduras. This ridge, though a recognized submarine feature, is irregular, and a depression of 7000 feet lies in it between Grand Cayman and the Lesser Caymans. The dependency consists of three islands, of which the two smaller, Cayman Brac and Little Cayman, are separated by only 4 miles of sea, while the third, Grand Cayman, is about 60 miles away. Cayman Brac is situated about 125 miles north-west of Montego Bay (Jamaica), and Grand Cayman lies 178 miles west-north-west of Negril Point, the nearest point of Jamaica, and about 150 miles from the Isle of Pines (Cuba). The combined area of the three islands is about 100 square miles. Columbus discovered the Lesser Caymans in 1503, and named them Las Tortugas', as the shores were swarming with turtle. Grand Cayman was discovered at some later unknown date, and is first recorded in history as being in the occupation of Spanish buccaneers. Europeans appear to have been ... This 250-word extract was created in the absence of an abstract

Role of Artesian Waters in Forming the Carolina Bays, 1937, Johnson Douglas,

Neuforschungen im Zwlferloch (Bayern)., 1950, Abel, G.
[(1344/1), Deutschland]

Neuforschungen im Zwlferloch (Bayern), 1950, Abel, G.

Erschlieung der Wendelsteinhhle bei Brandenburg (Bayern)., 1954, Gamer, K.
[(1279/1), Deutschland]

Erschlieung der Wendelsteinhhle bei Brandenburg (Bayern), 1954, Gamer, K.

Neues ber die kleine Laubensteinhhle bei Frasdorf im Chiemgau (Bayern)., 1955, Triller, A(dolf).
[Deutschland, (1341)]

Neues ber die kleine Laubensteinhhle bei Frasdorf im Chiemgau (Bayern), 1955, Triller, A.

Neues von der Spielberghhle bei Frasdorf (Oberbayern)., 1956, Thein, K.
[(1341/4), Deutschland]

Neues von der Spielberghhle bei Frasdorf (Oberbayern), 1956, Thein, K.

Hauptversammlung des Verbandes der deutschen Hhlen-u.Karstforscher vom 25. Bis 29. Sept. 1957 in Frasdorf (Oberbayern)., 1958, Thein, K.
[Deutschland, Laichingen]

Neue Hhlenforschungen auf dem Zugspitzplatt (Oberbayern)., 1958, Thein, K.
[Deutschland, Mnchner Rhre (1234/33), Eisfigurenhhle (1234/40), Holzkirchnerschacht (1234/48)]

Hauptversammlung des Verbandes der deutschen Hhlen-uKarstforscher vom 25 Bis 29 Sept 1957 in Frasdorf (Oberbayern), 1958, Thein, K.

Neue Hhlenforschungen auf dem Zugspitzplatt (Oberbayern), 1958, Thein, K.

Observations on Caves, Particularly Those Of South Australia - 1862 , 1962, Lane, Edward A.

The historical study of Australian caves and caving areas is fascinating although involving the expenditure of vast amounts of time. Australia's early days are unusually well-documented, but in the case of caves the early history is usually wrapped up in rumour, hearsay and clouded by lack of written record. Most research work means long hours poring over old newspaper files, mine reports, land department records and so on, little of which is catalogued. A small number of exploration journals and scientific studies have extensive material on special cave areas, and of these, the volume by Rev. Julian Edmund Woods, F.G.S., F.R.S.V., F.P.S., etc., and is one of the most interesting. This book gives the ideas and beliefs of 100 years ago concerning the origin, development and bone contents of caves and makes interesting reading in the light of more recent studies of cave origins. Wood's study "Geological Observations in South Australia : Principally in the District South-East of Adelaide" was published in 1862 by Longman, Green, Roberts and Green, London. In a preface dated November 15, 1861, Rev. Woods points out that the book was written while he was serving as a missionary in a 22,000 square mile district, and "without the benefit of reference, museum, library, or scientific men closer than England". Up to the time of writing, almost no scientific or geological work had been done in South Australia and much of the area was completely unexplored. The book, also, contained the first detailed description of caves in the south-east of the state. Father Woods writes about many different types of caves in South Australia, for instance, the "native wells" in the Mt. Gambier/Mt. Shanck area. These are caves, rounded like pipes, and generally leading to water level. Woods points out their likeness to artificial wells. He also writes of sea cliff caves, particularly in the Guichen Bay area, and blow holes caused by the action of the waves on the limestone cliffs. Woods discusses many other types of caves found further inland, particularly bone caves. Father Woods discusses cave origins under two sub-heads: 1. Trap rock caves generally resulting from violent igneous action, and 2. Limestone caves resulting from infiltration of some kind. He is mainly concerned with limestone caves which he sub-divides into (a) crevice caves - caves which have arisen from fissures in the rock and are therefore wedge-shaped crevices, widest at the opening, (b) sea-beach caves, caves which face the seashore and are merely holes that have been worn by the dashing of the sea on the face of the cliff, (c) egress caves, or passages to give egress to subterranean streams, (d) ingress caves, or passages caused by water flowing into the holes of rocks and disappearing underground. These caves would have entrance holes in the ground, opening very wide underneath, and having the appearance of water having entered from above, (e) finally a group of caves which he lists by use as "dens of animals".


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