Caves are usually found within the same genus land.
For example, at least 39,500 of the 40,000 caves that we estimate exist in our country are in K alker (Limestone). Limestones and similar stones, which form a special class of sedimentary rocks, which contain carbonated rocks such as limestone, dolomite, K alcite, and sulphated rocks such as gypsum.
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There is a great majority of these caves in these formations. With the combination of many special conditions within the other formations, it is also very rare to have formed caves.
Further, granite et al. and other sedimentary and magmatic rocks.
The origin of sedimentary rocks such as limestone and dolomics, where the caves have a great majority, are chemical and biochemical and generally formed by sedimentation in the old seas.
The most important characteristic of carbonated rocks is that they dissolve CO 1 (carbon dioxide) gas in water. CO2 gas is present both in the atmosphere (in the amount of 3 / 10.000) and also in the vegetative soil layer with plant roots. The composition of all living beings includes C (Carbon), O (Oxygen), N (Nitrogen) and H (Hydrogen). Living beings obtain the energy they need to live by burning the carbon in organic compounds (C).
The limestones have been formed since the earliest geological periods (since the Precambrian Period of the 1st Time, which was 2500 - 3000 million years old). The precipitation waters falling on a limestone massif, which we describe as origin, are combined with the CO2 gas obtained from the plant residues in the vegetation soil layer after passing through the atmosphere and after falling to the ground and: H10 (water) + CO (carbon). gas) = H2CO1 (acid carbonic). This melts the limestone in the calcium carbonate (Ca CO 1) composition. This reaction proceeds as follows.
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Ca CO 1 + CO 1 + H 2 O = (CO 1 H 2) Ca (Calcium bicarbonate) limestone, carbon gas and water form calcium bicarbonate. But this reaction is not simple, it is of both types. At the slightest pressure and temperature change, the reaction proceeds in the opposite direction, ie from right to left.
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