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Gypsum cave system in Korolivka, Ukraine From Wikipedia, the free encyclopedia
Optymistychna (Ukrainian: Оптимістична: meaning "optimistic", also known as Peschtschera Optimistitscheskaya)[2][lower-alpha 1] is a gypsum cave located near the Ukrainian village of Korolivka, Chortkiv Raion, Ternopil Oblast.[3] Approximately 264 km (164 mi)[4] of passageways have been mapped within.[1] As a result, it is the longest cave in Europe and the seventh-longest cave in the world,[5] after Mammoth Cave, Sistema Sac Actun, Jewel Cave, Shuanghedong and Sistema Ox Bel Ha. It is also the longest gypsum cave in the world.[1][6]
Optymistychna | |
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Location | near Ukrainian village of Korolivka, Chortkiv Raion, Ternopil Oblast |
Coordinates | 48°44′33″N 25°59′37″E |
Length | 230 km (140 mi)[1] |
Discovery | 1966 |
Geology | gypsum |
The cave complex was discovered by the speleologists of the Lviv speleological club "Cyclope" in 1966. It was entirely unknown before then.[7] There have been more than 50 expeditions since then, but exploration has slowed significantly in recent years, and very little surveying is currently being done.[3] The cave is located very close to the Priest's Grotto or Ozerna Cave, the eleventh-longest cave in the world at 130.4 km (81.0 mi), but the two caves have not yet been found to be connected.[1]
In 2008, the cave was recognized as a Natural Wonder of Ukraine.[8]
The entire cave lies under a 2 km square area in a layer of Neogene period gypsum that is less than 30 metres (98 ft) thick.[7][9] The passages tend to be fairly small, no more than 3 metres (10 ft) wide and 1.5 metres (5 ft) tall for most, although at intersections they can be up to 10 metres (33 ft) tall.[7] They are often choked with mud. They comprise a dense network on several levels, making Optymistychna known as a "maze cave".
Optymistychna's gypsum bed is topped with a limestone layer, which has seeped through into the cave via erosion and formed into calcite speleothems.[7] At other places, the gypsum has formed crystals, often tinted a multitude of colors by mineral salts. In some areas, large gypsum rosettes have formed, colored black by manganese oxide.[7]
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