Birds and All Nature, Vol. 6, No. 2, September 1899: Illustrated by Color PhotographyVarious
History
Birds and All Nature, Vol. 6, No. 2, September 1899: Illustrated by Color Photography
Various
Birds -- Periodicals; Natural history -- Periodicals
[Illustration: MARBLES.
OLD TENNESSEE. ALPS GREEN.
SIENNA. MEXICAN ONYX.
FLORENTINE VERMONT. AFRICAN MARBLE.
CHICAGO:
A. W. MUMFORD, PUBLISHER.]
MARBLES.
MR. GEO. D. MERRILL,
Head Curator, Department of Geology, U. S. National Museum.
The origin of the name marble, like that of many another name now
in common use, is somewhat obscure. By many authorities the word is
supposed to have been somehow connected with the Greek word meaning
"sparkle." However this may be, a sparkling appearance is by no means
universal among marbles, but is limited to those which, like the white
statuary or other crystalline varieties, have a granular structure, the
sparkling itself being due to the reflection of light from the smooth
surfaces of the constituent minerals. As used to-day, the word marble
is made to include any lime rock of such color and hardness as to make
it desirable for ornamental, or even the higher grades of building
work. Stones of precisely the same composition and origin, which are
not of the desired color, are classed simply as limestones.
Accepting the definition given above, it follows, then, that with a few
exceptions, to be noted later, marbles are but hardened and otherwise
changed beds of marine sands and muds, containing, it may be, still
recognizable fragments of the corals and mollusks of which they were
originally composed. But inasmuch as these muds were rarely of pure
carbonate of lime, but were contaminated with matter from seaweeds
and animal remains, or by iron compounds, so the resultant marble is
not always white, but, if containing matter from plants or animals,
gray, blue gray, or even black; and if containing iron, buff, pink, or
red. If the change in form of the original muds was just sufficient to
produce crystallization, we may have a marble full of fossil remains
which may be of a white or pink color, standing out in fine contrast
with the darker ground. If, on the other hand, the change was complete,
we may have a marble of small granules, pure white in color, and of a
texture like loaf sugar, such as to render it suitable for statuary
purposes.
Public-domain text, read in full here on John Shaqi.
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