Glimpses of America: A Pictorial and Descriptive History of Our Country's Scenic MarvelsBuel, James W. (James William)
History
Glimpses of America: A Pictorial and Descriptive History of Our Country's Scenic Marvels
Buel, James W. (James William)
United States -- Pictorial works
“Streams and true springs are absent, but there are hundreds of basins,
varying from one to fifty feet in diameter, and from six inches to
fifteen feet in depth. The water in them is exquisitely pure, except as
it is impregnated by the carbonate of lime, which often forms
concretions called, according to their size, pearls, eggs, and snow-
balls. A large one is known as the Cannon-Ball. When fractured, these
spherical growths are found to be radiated in structure. Calcite
crystals, drusy, feathery, or fern-like, line the sides and bottoms of
every water-filled cavity, and, indeed, constitute the substance of
which they are formed. Variations of level at different periods are
marked by rings, ridges, and ruffled margins. These are especially
strongly marked about Broaddus Lake, and the curved ramparts of the
Castles on the Rhine. Here, also, are polished stalagmites, a rich buff
slashed with white, and others, like huge mushrooms, with a velvety coat
of red, purple, or olive-tinted crystals. In some of the smaller basins
it sometimes happens that when the excess of carbonic acid escapes
rapidly there is formed, besides the crystal beds below, a film above,
shot like a sheet of ice across the surface. One pool twelve feet wide
is thus covered so as to show but a third of its surface. The quantity
of water varies greatly at different seasons; hence some stalactites
have their tips under water long enough to allow tassels of crystal to
grow on them, which in a drier season are again coated over with
stalactitic matter, by which singular distortions are occasioned.
Contiguous stalactites are often enwrapped thus till they assume an
almost globular form, through which, by making a section, the primary
tubes appear. Twig-like projections, lateral outgrowths, to which the
term _helictite_ has been applied, are met with in certain portions of
the cave, and are interesting by reason of their strange and uncouth
contortions. Their presence is partly due to the existence of a
diminutive fungus peculiar to the locality, and designated from its
habitat, _Mucor Stalactitis_. The Toy Shop is an amusing collection of
these freaks of nature.
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Public-domain text, read in full here on John Shaqi.
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