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Cavern Classroom
The
Black Hills Greatest Cave Adventure
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How
the caverns were formed...
Welcome
to the Black Hills Caverns Classroom. Browse through these pages
and learn about the discovery and development of the cavern.
Go
back to prehistoric times and discover how caverns are formed.
Learn about the delicate balance between man and the underground
water system. (Feel
free to reproduce any part of this section for use in an
educational program.)
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Geology
and Chemistry
The walls of Black
Hills Caverns consist of two types of limestone (coeymans and manlius) from different periods in the Earth's early history, as
well as a rock known as rondout waterred.

Cave
Life
With the exception of a few bats
near the natural entrance, moss growing around the electric lights, and
bacteria in the underground stream, there is little animal or plant life in
Black Hills Caverns.
Cave
Conservation
Great care must be taken to
protect and preserve these great underground wonders. Caves are non-renewable
natural resources which benefit and enrich our lives in many ways, a few of
which are: insect control, scientific knowledge, water supply, education and recreation.
Prehistoric
Era
It takes many thousands of years for
the underground rooms to be formed. The rain water soaks through
the soil, picking up carbon dioxide from the vegetation and soil.
Water and carbon dioxide form a mild acid, carbonic acid, which as
it seeps through limestone forms calcium carbonate. The calcite is
deposited as crystals, stalactites, stalagmites, and many
formations found in the caverns.
Scientists believe nature began
to slowly craft Black Hills Caverns some six million years ago - long before
even the ancient, extinct animal known as the woolly mammoth appeared on
Earth. The caverns are unique for more than their age and beauty - they are
among a very small number of mineral caves in the world.
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