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Bibliografia publikacji pracowników
Państwowej Szkoły Wyższej w Białej Podlaskiej

Baza tworzona przez Bibliotekę Akademii Bialskiej im. Jana Pawła II.


Zapytanie: ZOLOUSHKA CAVE
Liczba odnalezionych rekordów: 2



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Nr opisu: ^aZoloushka Cave, the third longest gypsum cave in the world (92 km) and the world's largest gypsum cave by volume (>0.7 million cubic meter), is an outstanding example of a large maze cave formed in a multi-story artesian aquifer system due to the upward leakage between the aquifers across a soluble unit. Although local settings and evolution caused some peculiar features in speleogenesis, as compared to other large maze caves in Western Ukraine, these singularities provide further insights on variants and mechanisms of both regional and general models of hypogene artesian speleogenesis. The cave is located in the area where the host aquifer system is generally confined until present, but in one of the more uplifted tectonic blocks where the gypsum was partially incised by the nearby valley of the Prut River during the Holocene and rapidly drained due to the quarry operations since 1946. The cave experienced considerable modifications and transformations in the course of the recent transition to unconfined conditions and subsequent artificial dewatering. The geomorphological breaching of the confined aquifer system in the cave area occurred in the Holocene, i.e., later than in the area where most other large maze caves in the region are located.
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Słowa kluczowe ang.: _PUBLICATION^ePUBLISHER_WEBSITE^aZoloushka Cave, the third longest gypsum cave in the world (92 km) and the world's largest gypsum cave by volume (>0.7 million cubic meter), is an outstanding example of a large maze cave formed in a multi-story artesian aquifer system due to the upward leakage between the aquifers across a soluble unit. Although local settings and evolution caused some peculiar features in speleogenesis, as compared to other large maze caves in Western Ukraine, these singularities provide further insights on variants and mechanisms of both regional and general models of hypogene artesian speleogenesis. The cave is located in the area where the host aquifer system is generally confined until present, but in one of the more uplifted tectonic blocks where the gypsum was partially incised by the nearby valley of the Prut River during the Holocene and rapidly drained due to the quarry operations since 1946. The cave experienced considerable modifications and transformations in the course of the recent transition to unconfined conditions and subsequent artificial dewatering. The geomorphological breaching of the confined aquifer system in the cave area occurred in the Holocene, i.e., later than in the area where most other large maze caves in the region are located. A relatively stable position of the water table in the upper part of the gypsum during most of the Holocene caused pronounced widening of passages, which determined the anomalously large size of passages and high indices of areal karstification in some regions of the cave. The most intense development of conduits occurred in areas where the input of freshwater fr
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  • e 1946. The cave experienced considerable modifications and transformations in the course of the recent transition to unconfined conditions and subsequent artificial dewatering. The geomorphological breaching of the confined aquifer system in the cave area occurred in the Holocene, i.e., later than in the area where most other large maze caves in the region are located. A relatively stable position of the water table in the upper part of the gypsum during most of the Holocene caused pronounced widening of passages, which determined the anomalously large size of passages and high indices of areal karstification in some regions of the cave. The most intense development of conduits occurred in areas where the input of freshwater from the lower aquifer was more abundant. Quarry operation and accompanying groundwater withdrawal during the last 70 years caused drastic and rapid transformations in the cave environment.^aArtesian speleogenesis^agypsum karst^aWestern Ukraine^aZoloushka Cave


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    Nr opisu: al types widespread on the walls of gypsum cave Zoloushka. They reflect development of the cave in phreatic conditions. Original pyramidal-grooved microforms were found on the walls of cylindrical wells, which represent by themselves an open pressure cupolas. According to the author, microforms are the result of stream downward movement of water on the walls in closed circulation environment of blind cupola and can testify in favor of the development of the cave in hypogenic conditions.^ażłobki krasowe^akarren^ajaskinia Zołuszka^aZoloushka Cave^aAn unique type of corrosional formations in the Zoloushka Cave (Ukraine-Moldova)
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    Tytuł wynalazku: żłobki krasowekarrenjaskinia ZołuszkaZoloushka CaveAn unique type of corrosional formations in the Zoloushka Cave (Ukraine-Moldova)
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    Zasięg terytorialny: kras hipogenic
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    Słowa kluczowe ang.: oforms of different morphological types widespread on the walls of gypsum cave Zoloushka. They reflect development of the cave in phreatic conditions. Original pyramidal-grooved microforms were found on the walls of cylindrical wells, which represent by themselves an open pressure cupolas. According to the author, microforms are the result of stream downward movement of water on the walls in closed circulation environment of blind cupola and can testify in favor of the development of the cave in hypogenic conditions.^ażłobki krasowe^akarren^ajaskinia Zołuszka^aZoloushka Cave^aAn unique type of corrosional formations in the Zoloushka Cave (Ukraine-Moldova)
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