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International Journal of Speleology

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Dissolution Of Gypsum From Field Observations, Alexander Klimchouk, Franco Cucchi, Jose Maria Calaforra, Sergey Aksem, Furio Finocchiaro, Paolo Forti Jan 1996

Dissolution Of Gypsum From Field Observations, Alexander Klimchouk, Franco Cucchi, Jose Maria Calaforra, Sergey Aksem, Furio Finocchiaro, Paolo Forti

International Journal of Speleology

The paper reports the results of field measurements of gypsum dissolution in various countries (Ukraine, Spain, Italy and others) and in different environments (river waters, precipitation, vadose zone, unconfined aquifer, perched cave lakes, ephemeral streams in caves, confined aquifer, cave air).

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Speleogenesis In Gysum, Alexander Klimchouk Jan 1996

Speleogenesis In Gysum, Alexander Klimchouk

International Journal of Speleology

Satisfactory explanation of the origin and development of caves (speleogenesis) is a core problem of karst studies. Karst evolves as a circulation system, organised and interconnected through a conduit structure. Such a system may include superficial inputs and outputs, expressed as or related to karst landforms. However, there may be no such components if the system is represented entirely by conduits as in the case with deep-seated intrastratal karst. The main differences between speleogenesis in gypsum and in carbonate rocks lie in the chemistry and kinetics of their dissolution, in some of the lithological or structural peculiarities of the respective …

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Hydrogeology Of Gypsum Formations, Alexander Klimchouk Jan 1996

Hydrogeology Of Gypsum Formations, Alexander Klimchouk

International Journal of Speleology

Detailed explanation of hydrogeological characteristics of gypsum aquifers is given in various situations: deep-seated karst-confined conditions, subjacent, entrenched and denuded karst types-semi-confined, phreatic and vadose conditions. The hydrogeological evolution of barren exposed gypsum karst and flow velocities in gypsum karst aquifers is also discussed.

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Breakdown Development In Cover Beds, And Landscape Features Induced By Intrastratal Gypsum Karst, Alexander Klimchouk, Vjacheslav Andrejchuk Jan 1996

Breakdown Development In Cover Beds, And Landscape Features Induced By Intrastratal Gypsum Karst, Alexander Klimchouk, Vjacheslav Andrejchuk

International Journal of Speleology

Intrastratal karst is by far the predominant gypsum karst type. Its development may begin in deep-seated settings within rocks already buried by younger strata, and it proceeds increasingly rapidly as uplift brings gypsum sequences into progressively shallower positions. Such development commonly occurs under confined (artesian) hydrogeological conditions, that subsequently change to open conditions (phreatic-water table-vadose). The general evolutionary line of intrastratal karst is typified by progressive emergence of a sequence into a shallower position, activation of groundwater circulation and development of cave systems within karst units, commencement of gravitational breakdown and its upward propagation through overlying beds, and development of …

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Gypsum Karst Of Great Britain, Anthony H. Cooper Jan 1996

Gypsum Karst Of Great Britain, Anthony H. Cooper

International Journal of Speleology

In Great Britain the most spectacular gypsum karst development is in the Zechstein gypsum (late Permian) mainly in north-eastern England. The Midlands of England also has some karst developed in the Triassic gypsum in the vicinity of Nottingham. Along the north-east coast, south of Sunderland, well-developed palaeokarst, with magnificent breccia pipes, was produced by dissolution of Permian gypsum. In north-west England a small gypsum cave system of phreatic origin has been surveyed and recorded. A large actively evolving phreatic gypsum cave system has been postulated beneath the Ripon area on the basis of studies of subsidence and boreholes. The rate …

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Gypsum Karst Of The Pre-Ural Region, Russia, Vjacheslav Andrejchuk Jan 1996

Gypsum Karst Of The Pre-Ural Region, Russia, Vjacheslav Andrejchuk

International Journal of Speleology

Description of the gypsum karst of the pre-Ural region in Russia, with special emphasis on speleogenesis.

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Weathering Crust And Karren On Exposed Gypsum Surfaces, Tommaso Macaluso, Ugo Sauro Jan 1996

Weathering Crust And Karren On Exposed Gypsum Surfaces, Tommaso Macaluso, Ugo Sauro

International Journal of Speleology

The evolution of gypsum bare rock surfaces is the result both of volume changes of the outer rock layer and mass wasting by dissolutional processes. Some unusual weathering processes induce an increase in the volume of the outer gypsum layer, resulting in the development of a “weathering crust” and of characteristic forms such as small ridges and bubbles. However, the more typical erosional forms are dissolutional ones of karren type, which are commonly interconnected, or superimposed upon the previously described forms. In this chapter a classification system is proposed and discussed, within which the magnitude, order and geometry of the …

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Gypsum Karst In China, Lu Yaoru, Anthony H. Cooper Jan 1996

Gypsum Karst In China, Lu Yaoru, Anthony H. Cooper

International Journal of Speleology

The Peoples Republic of China has the largest gypsum resources in the world and a long history of their exploitation. The gypsum deposits range in age from Pre-Cambrian to Quaternary and their genesis includes marine, lacustrine, thermal (volcanic and metasomatic), metamorphic and secondary deposits. The gypsum is commonly associated with other soluble rocks such as carbonates and salt. These geological conditions, regional climate differences and tectonic setting strongly influence the karstification process resulting in several karst types in China. Well developed gypsum palaeokarst and some modem gypsum karst is present in the Fengfeng Formation (Ordovician) gypsum of the Shanxi and …

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Geomorphological Aspects Of Gypsum Karst Areas With Special Emphasis On Exposed Karst, Ugo Sauro Jan 1996

Geomorphological Aspects Of Gypsum Karst Areas With Special Emphasis On Exposed Karst, Ugo Sauro

International Journal of Speleology

Medium- to large-size forms in gypsum karst are described, including dolines, blind valleys, ploje-like depressions, collapses and positive and/or residual forms such as outliers, cone-like hills, dome-like hills, mesa-like tabular blocks and plateaux and breccia pipe hills. The similarities and/or difference between gypsum and carbonate forms are discussed.

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Environmental Problems In Gypsum Karst Terrains, Alexander Klimchouk, Vjacheslav Andrejchuk Jan 1996

Environmental Problems In Gypsum Karst Terrains, Alexander Klimchouk, Vjacheslav Andrejchuk

International Journal of Speleology

Description of environmental problems in gypsum karst areas, especially of the effects related to human impacts that are unique to gypsum karst systems or most commonly occur herein. The paper deals with pollution (oil, radioactive substances and fertilizers), mining activity, underground water abstraction, construction of dams and reservoirs, collapse and subsidence hazards giving examples of former Soviet Union.

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Gypsum Karst In The United States, Kenneth S. Johnson Jan 1996

Gypsum Karst In The United States, Kenneth S. Johnson

International Journal of Speleology

Gypsum is one of the most soluble of common rocks; it is dissolved readily to form caves, sinkholes, disappearing streams, and other karst features that typically are found in limestones and dolomites. The four basic requirements for gypsum karst to develop are: (1) a deposit of gypsum; (2) water, unsaturated with CaSO4 (3) an outlet for escape of dissolving water; and (4) energy to cause water to flow through the system. Gypsum deposits are present in 32 of the 48 conterminous United States, and they underlie about 35-40% of the land area; they are reported in rocks of every …

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Gypsum Karst Of France, Michel Chardon, Jean Nicod Jan 1996

Gypsum Karst Of France, Michel Chardon, Jean Nicod

International Journal of Speleology

Many small and scattered areas of gypsum karst are present in France. They occur in the plains and plateaux (Paris, Lorraine, Provence) as well as in the mountains, especially the Alps. Typical gypsum karst landforms are well developed and widespread, but underground cavities are scarce, despite much exploration and the apparent existence of subsurface waterflow. The Alps and Provence contain the largest karstic areas.

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Gypsum Karst Of Germany, Stephan Kempe Jan 1996

Gypsum Karst Of Germany, Stephan Kempe

International Journal of Speleology

Description of gypsum karst and caves in Germany.

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First Record Of Parastenocarididae (Crustacea, Copepoda, Harpacticoida) From Subterranean Freshwater Of Insular Greece And Description Of Two New Species, Vezio Cottarelli, Maria Cristina Bruno Jan 1996

First Record Of Parastenocarididae (Crustacea, Copepoda, Harpacticoida) From Subterranean Freshwater Of Insular Greece And Description Of Two New Species, Vezio Cottarelli, Maria Cristina Bruno

International Journal of Speleology

The genus Parastenocaris, new for Greece, has been discovered in the hyporheic habitat of Kos and Kythira Island with two new species, that are described and discussed in this work. Parastenocaris aesculapii n. sp. shares some characters with P. nolli from Germany and P. italica from Italy, Macedonia and Turkey. Parastenocaris aphroditis n. sp. belongs, according to the Authors, to a group of species living exclusively in estuarine interstitial habitats, which are all characterised by peculiar morphology and ecology, that are as well considered and interpreted.

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Gypsum Karst Of The World: A Brief Overview, Alexander Klimchouk, Paolo Forti, Anthony Cooper Jan 1996

Gypsum Karst Of The World: A Brief Overview, Alexander Klimchouk, Paolo Forti, Anthony Cooper

International Journal of Speleology

Short description of caves and karsts in gypsum of different parts of the World.

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Lithobius Nuragicus N.Sp., A New Lithobius From A Sardinian Cave (Chilopoda, Lithobiomorpha), Marzio Zapparoli Jan 1996

Lithobius Nuragicus N.Sp., A New Lithobius From A Sardinian Cave (Chilopoda, Lithobiomorpha), Marzio Zapparoli

International Journal of Speleology

A new species of Lithobius from a Sardinian cave (Cagliari, Santadi, loc. Su Benatzu, Grotta “Pirosu”, 576 Sa/Ca, m 270) is described. Lithobius nuragicus n. sp. belongs to the subgenus Lithobius s. str. and is related to Lithobius variegatus Leach, 1814, occurring in the British Isles, Brittany, Channel Isles, Iberian Peninsula, Maghreb, Sicily and Southern Italy. This new species is differentiated from L. variegatus by the number of prosternal teeth (3+3), the number and arrangement of ocelli (1+3; little, depigmented, not contiguous to each other, in the center of a depigmented area, posterosuperior ocellus larger than the other ocelli), the …

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Gypsum Karst Of The Baltic Republics, Bernardas Paukstys, Vytautas Narbutas Jan 1996

Gypsum Karst Of The Baltic Republics, Bernardas Paukstys, Vytautas Narbutas

International Journal of Speleology

The Baltic Republics of Estonia, Latvia and Lithuania have karst areas developed in both carbonate and gypsiferous rocks. In the north, within the Republic of Estonia, Ordovician and Silurian limestones and dolomites crop out, or are covered by glacial Quaternary sediments. To the south, in Latvia and Lithuania, gypsum karst is actively developing in evaporites of Late Devonian (Frasnian) age. Although gypsum and mixed sulphate-carbonate karst only occupy small areas in the Baltic countries, they have important engineering and geo-ecological consequences. Due to the rapid dissolution of gypsum, the evolution of gypsum karst causes not only geological hazards such as …

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Gypsum Karst Of The Eastern-European Plain, Vjacheslav Andrejchuk, Alexander Klimchouk Jan 1996

Gypsum Karst Of The Eastern-European Plain, Vjacheslav Andrejchuk, Alexander Klimchouk

International Journal of Speleology

Description of karst in the Eastern European Plain, comprising the following regions: Baltic, Timansky, Pinego-Severodvinsky, Volgo-Kamsky, Pre-Ural, Pre-Caspian, Donetsk and Podol'sko Bukovinsky.

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Some Examples Of Gypsum Karsts And The More Important Gypsum Caves In Spain, Jose Maria Calaforra, Antonio Pulido-Bosch Jan 1996

Some Examples Of Gypsum Karsts And The More Important Gypsum Caves In Spain, Jose Maria Calaforra, Antonio Pulido-Bosch

International Journal of Speleology

Spain possesses some of the most important examples of gypsum karst in Europe, in terms of the extent and variety of the gypsiferous outcrops. These are divided into gypsum belonging to the Triassic, Palaeogene and Neogene epochs, each of which displays different lithological and structural aspects. Some of Spain’s most significant gypsum karsts, from the speleological standpoint, are described, and these share a common characteristic of all supporting the development of large caves. Reference is made to the geomorphology, hydrogeology and hydrochemistry of the gypsum karsts of Sorbas, Vallada and Gobantes-Meliones, which provide significant examples of intrastratal karst, speleogenesis by …

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Gypsum Karst In The Western Ukraine, Alexander Klimchouk Jan 1996

Gypsum Karst In The Western Ukraine, Alexander Klimchouk

International Journal of Speleology

The great gypsum karst of the Western Ukraine, which is associated with Miocene (Badenian) gypsum, provides the worlds foremost examples of intrastratal gypsum karst and speleogenesis under artesian conditions. Differential neotectonic movements have resulted in various parts of the territory displaying different types (stages) of intrastratal karst, from deep-seated, through subjacent, to entrenched. Internal gypsum karstification proceeded mainly under confined hydrogeological conditions. While such development still continues in part of the territory, other parts exhibit entrenched karst settings. Huge relict maze cave systems have been explored here, five of which are currently the longest known gypsum caves in the world. …

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Karst In Siliceous Rocks: The Speleothem Medium Of Finger Flutings And Its Isotopic Geochemistry, Robert G. Bednarik Jan 1995

Karst In Siliceous Rocks: The Speleothem Medium Of Finger Flutings And Its Isotopic Geochemistry, Robert G. Bednarik

International Journal of Speleology

The isotopic geochemistry relating to the re-precipitation of calcite in caves is considered, in terms of its theory, natural manifestations, and relationship with questions of radiometric dating of carbonate speleothems. Specific forms of’ such deposits are considered, together with the various modification processes they are subjected to. More specifically, particular forms of rock art found within, as well as on or under such deposits are examined, such as finger flutings commonly found in caves of Europe and Australia. Some of the variables relating to their occurrence are elucidated, their preservation and possible dating is reviewed in the light of these …

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On Some Cave Minerals From Northern Norway, Bogdan Petroniu Onac, Stein-Erik Lauritzen Jan 1995

On Some Cave Minerals From Northern Norway, Bogdan Petroniu Onac, Stein-Erik Lauritzen

International Journal of Speleology

The present paper aims to point out the results of 31 samples from some Norwegian caves that have been analysed with respect to their mineralogical composition. Identification of the minerals was done by X-ray diffraction, thermal, infrared spectroscopy and scanning electron microscopy. Seventeen minerals were identified belonging to 4 groups: carbonates, sulphates, oxides-hydroxides and silicates.

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Karst In Siliceous Rocks - Karst Landforms And Caves In The Auyàn-Tepui Massif (Est. Bolivar, Venezuela), Leonardo Piccini Jan 1995

Karst In Siliceous Rocks - Karst Landforms And Caves In The Auyàn-Tepui Massif (Est. Bolivar, Venezuela), Leonardo Piccini

International Journal of Speleology

During the expedition "Tepuy 93", six caves were explored in the precambrian quartzites of Roraima Group, in the Auyan-tepui massif. One of this caves reaches the depth of 370 m and a development of almost 3 km; its name is “Sima Auyan-tepui Noroeste” and it is currently the deepest cave in the world discovered in siliceous rocks The geological and morphological study of this cave has underlined again the importance of deep solutional weathering, along the network of fractures for the formation of caves in siliceous rocks. The different formation stages of the big superficial shafts, called “simas” were observed …

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Paleokarst Of The Bohemian Massif In The Czech Republic: An Overview And Synthesis, Pavel Bosàk Jan 1995

Paleokarst Of The Bohemian Massif In The Czech Republic: An Overview And Synthesis, Pavel Bosàk

International Journal of Speleology

Paleokarst of the Bohemian Massif on the territory of the Czech Republic developed as polygenetic and polycyclic forms with several phases of fossilization and rejuvenation depending on tectonic phases and deep chemical weathering. Paleotectonic period (pre-Permian in general) was characterized by evolution of relatively minor depositional and local paleokarsts. Neotectonic (platform) period (post-Permian) favoured the prolonged karst evolution of interregional paleokarst in two karst periods and several more or less distinctly separated karst phases.

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The Classification Of Cave Minerals And Speleothems, Carol A. Hill, Paolo Forti Jan 1995

The Classification Of Cave Minerals And Speleothems, Carol A. Hill, Paolo Forti

International Journal of Speleology

The classification scheme of Hill and Forti, as used in the second edition of Cave Minerals of the World, is presented as a "practical" solution to the classification of cave minerals and speleothems. Classification and naming of cave minerals is by crystal class and follows nomenclature approved by the International Mineralogical Association. Classification of speleothems is based on morphology and whatever is known about origin, with division of speleothems into types, subtypes, and varieties. It is proposed that new speleothem types, subtypes, and names be approved by a UIS Commission of cave mineralogists.

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Die Slowakischen Shauhöhlen Und Ihre Probleme, Ivan Racko Jan 1994

Die Slowakischen Shauhöhlen Und Ihre Probleme, Ivan Racko

International Journal of Speleology

In 1960 the Slovak Caves Administration, which managed twelve Slovak Caves was founded. It was controlled by the Ministry of Culture of the Slovak Socialist Republic and comprised also the Museum of Slovak Karst and the Slovak Speleological Society - a free speleological organisation. In 1981 such an Administration became part of the State Centre for the Protection of Nature. The main task of this centre was obviously the protection of nature in Slovakia but unfortunately many problems remained unsolved. The social movement in November 1989 accelerated the process to solve such problems and the Forum of Professional Workers of …

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Kurzer Bericht Über Die Probleme Des Höhlentourismus In Jugoslawien, France Habe Jan 1994

Kurzer Bericht Über Die Probleme Des Höhlentourismus In Jugoslawien, France Habe

International Journal of Speleology

In the frame of the IUS, the activities concerning the Yugoslav show caves are reported and the most relevant problems are emphasized.

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Problems Of Show Caves In Bohemia And Moravia, Milka Dusan Jan 1994

Problems Of Show Caves In Bohemia And Moravia, Milka Dusan

International Journal of Speleology

In the last years the show caves in Bohemia and Moravia were administrated by the Ministry of Culture with the status of a state assisted organization. That means that they were considered as those organizations not self-sufficient, without connections with tourism. Presently, the management of the show caves in Bohemia and Moravia is at a crossroad: to remain under the administration of the Ministry of Culture or move under the newly formed Ministry of Environment. In the latter case the cave management should change into a business organization similar to a private body. We believe that these problems can be …

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Problemi Turistici Della Grotta Gigante Nel Carso Triestino, Fabio Forti Jan 1994

Problemi Turistici Della Grotta Gigante Nel Carso Triestino, Fabio Forti

International Journal of Speleology

The paper reports the tourist evolution of the Grotta Gigante (Giant Cave), near Trieste (Italy) during 80 years (1908 - 1989) of its opening to the public. At the beginning it entered in competition with some other local show caves, even much more famous (like Postojna and Stocjan), after the II World War on account of the change of the state boundaries it remained the sole show cave in that part of Italy. Then the Grotta Gigante succeeded, even if slowly, to cope with the changing tourist demands, improving more and more its facilities to follow the increasing tourist flows. …

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Die Saalfelder Feengrotten: Ein Schaubergwerk Mit Höhlencharkter, Bernd Lochner Jan 1994

Die Saalfelder Feengrotten: Ein Schaubergwerk Mit Höhlencharkter, Bernd Lochner

International Journal of Speleology

The well known “Saalfelder Feengrotten” originated from an old aluminium mine called “Jeremiasglück”. The mine has been working from 1943 to 1945; the oldest formations have an age of about 350 years. Such formations were formed by an oxidation process which explains the rather fast growth rate in comparison to the growth rate of calcite formations. In the “Feengrotten” rare minerals can be found: the most common is a soft unstable compound, the diadochite (iron(III) phosphate). The control of the lampenflora is rather complicate and it is obtained with some compounds normally used in caves. The “Feengrotten” are visited yearly …

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