Moonmilk (sometimes called mondmilch, also known as bergmilch, montmilch, or cave milk) is a white, creamy substance found inside limestone, dolomite, and possibly other types of . It is a precipitate from limestone comprising aggregates of fine of varying composition, usually made of such as calcite, aragonite, hydromagnesite, and/or monohydrocalcite.
It is possible that moonmilk forms when water dissolves and softens the karst in caves, carrying dissolved nutrients that are used by microbes, such as Actinomycetes. As microbial colonies grow, they trap and accumulate chemically precipitated crystals in an organic matter-rich matrix. These heterotrophic microbes, which produce CO2 as a waste product of respiration and possibly organic acids, may help to dissolve the carbonate.
Being soft, moonmilk was frequently used as a medium for finger fluting, a form of prehistoric art.
The Swiss naturalist Conrad Gessner described moonmilk's use as a medicine in the 16th century. It continued to be prescribed until the 19th century. Moonmilk in showcaves.com.
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