2016
DOI: 10.21672/2077-6322-2016-61-2-030-039
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Characteristic ice accumulation and cryogenic minerals in caves Kutuk ground (Bashkortostan)

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“…From the entrance to the central part of the largest grotto of the cave, there is a blanket of perennial ice. In the center of the grotto is a clay scree, frozen in some places, in the marginal part of the glacier clay, covers the ice with a layer up to 0.5 m (Kadebskaya and Stepanov 2016). Kutuk-2 cave (Stalactite cave) is located 2.5 kilometers north of the Kutuk-Sumgan cave.…”
Section: Objects Of Studymentioning
confidence: 99%
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“…From the entrance to the central part of the largest grotto of the cave, there is a blanket of perennial ice. In the center of the grotto is a clay scree, frozen in some places, in the marginal part of the glacier clay, covers the ice with a layer up to 0.5 m (Kadebskaya and Stepanov 2016). Kutuk-2 cave (Stalactite cave) is located 2.5 kilometers north of the Kutuk-Sumgan cave.…”
Section: Objects Of Studymentioning
confidence: 99%
“…This gallery is overlapped by a siphon at a depth of 110 m and has a narrow passage to the main part of the cave (Golubev et al 1976). In winter seasonal glaciation forms in the entrance zone of the cave (Kadebskaya and Stepanov 2016).…”
Section: Objects Of Studymentioning
confidence: 99%
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