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A salt cave is a cave formed within rock salt by dissolution of this very soluble rock by water. As with other soluble rocks, a distinctive set of landscape features can arise from the solutional process; in this case it is known as salt karst or 'halite karst'.
He speculates that inhaled salt particles might thin out mucus aiding patients in expelling sputum. However, a recent review of the research supporting halotherapy determined that, out of 151 studies conducted on this topic, only 1 was a well-designed randomized control trial that met their inclusion criteria for a meta-analysis.
The first speleotherapy in the Czechoslovakia was carried out by Mgr. Štefan Roda in Slovakia in the Tombašek Cave in the High Tatras (1969). In 1973–1976, doctors Timová and Valtrová from the Children's Clinic in Banská Bystrica treated childhood asthmatics with speleotherapy with favourable results, which were published in the medical literature.
Global distribution of major outcrops of carbonate rocks (mainly limestone, except evaporites). The English word karst was borrowed from German Karst in the late 19th century, [6] which entered German usage much earlier, [7] to describe a number of geological, geomorphological, and hydrological features found within the range of the Dinaric Alps, stretching from the northeastern corner of ...
The "Lot's Wife" pillar on Mount Sodom, Israel, made of halite Salt cave in Mount Sodom Bedded halite at Mount Sodom. Mount Sodom (Hebrew: הר סדום, Har Sedom) is a hill along the southwestern part of the Dead Sea in Israel; it is part of the Judaean Desert Nature Reserve. [1]
Image showing the six most common speleothems with labels. Enlarge to view labels. A stalactite (UK: / ˈ s t æ l ə k ˌ t aɪ t /, US: / s t ə ˈ l æ k t aɪ t /; from Ancient Greek σταλακτός (stalaktós) 'dripping', from σταλάσσειν (stalássein) 'to drip') [1] is a mineral formation that hangs from the ceiling of caves, hot springs, or man-made structures such as ...
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Speleogenesis is the origin and development of caves, the primary process that determines essential features of the hydrogeology of karst and guides its evolution. It often deals with the development of caves through limestone, caused by the presence of water with carbon dioxide dissolved within it, producing carbonic acid which permits the dissociation of the calcium carbonate in the limestone.