Moonmilk (sometimes called mondmilch, also known as montmilch or as cave milk) is a white, creamy substance found inside limestone caves. It is a precipitate from limestone comprising aggregates of fine crystals of varying composition usually made of carbonates such as calcite, aragonite, hydromagnesite, and/or monohydrocalcite.
There are several hypotheses concerning the origin of moonmilk. One of these explains moonmilk to be the result of bacterial action rather than from chemical reactions. According to this particular hypothesis, moonmilk is thought to have been created by the bacterium Macromonas bipunctata. However, no microbiological studies have been carried out so far. Moonmilk was originally explained (by Conrad Gessner, 1555) to be created by "moon rays".
It is possible that moonmilk is formed by water that dissolves and softens the karst of caves consisting of carbonates, and carries dissolved nutrients that can be used by microbes, such as Actinomycetes. As the microbial colonies grow, they trap and accumulate chemically-precipitated crystals in the organic matter-rich matrix formed that way. Perhaps these heterotrophic microbes, which produce CO2 as a waste product of respiration and possibly organic acids, help to dissolve the carbonate.
You want to live so perfect
in a world of money and milk
your time goes by
it's so sad to see
expose to lose your ground
I'll never be around
You don't try enough
so you won't get it
You don't try enough
You'll never get it
perhaps we live in peradise
and maybe noone cares
miricles everyday, everywhere
all the little fates you don't see
I'll never let them down
They ever be around
You don't try enough
so you won't get it
You don't try enough
You'll never get it
You don't try enough
so you won't get it
You don't try enough
You'll never get it
I will never have it