Scientific American Supplement, No. 362, December 9, 1882Various
Science
Scientific American Supplement, No. 362, December 9, 1882
Various
Science -- Periodicals
The diamond is found in the _débris_ of metamorphic rocks in many
countries, and is probably one of the evolved products of the
distillation of organic matter they once contained. Under peculiar
circumstances it has apparently been formed by precipitation from
sulphide of carbon or some other volatile carbon compound by elective
affinity. Laboratory experiments have proved the possibility of
producing it by such a process, but the artificial crystals are
microscopic, perhaps only because a long time is required to build up
those of larger size.
Jet is a carbonaceous solid which in most cases is a true lignite, and
generally retains more or less of the structure of wood. Masses are
sometimes found that show no structure, and these are probably formed
from bitumen which has separated from the wood of which it once formed
part, and which it generally saturates or invests. In some cases,
however, these masses of jet-like substance are plainly the residuum of
excrementitious matter voided by fishes or reptiles. These latter are
often found in the Triassic fish-beds of Connecticut and New Jersey, and
in the Cretaceous marls of the latter State.
The discovery of a quantity of hydrocarbon jelly, recently, in a
peat-bed at Scranton, Pa., has caused some wonder, but similar
substances (Dopplerite, etc.) have been met with in the peat-beds of
other countries; and while the history of the formation of this singular
group of hydrocarbons is not yet well understood, and offers an
interesting subject for future research, we have reason to believe that
these jellies have been of common occurrence among the evolved products
of the decomposition of vegetable tissue in all ages.
The fossil resins--often erroneously called gums--amber, kauri, copal,
etc., though interestingly related to the hydro-carbons enumerated on
the preceding pages, form no essential part of the series, and demand
only the briefest notice here.
_Amber_ is the resin which exuded from certain coniferous trees that,
in Tertiary times, grew abundantly in northern Europe. The leaves and
trunks of these trees have generally perished; but masses of their
resin, more enduring, buried in the earth on the shores of the Baltic,
have in the lapse of time changed physically and chemically, and have
become fitted for the ornamental purposes for which they have been used
by all civilized nations.
_Kauri_ is the resin of _Dammara australis_, a living coniferous tree of
New Zealand, and the "gum" is dug from the earth on the sites of forests
which have now disappeared.
_Copal_ is a commercial name given to the resins of several different
trees, but the most esteemed, and indeed the only true copal, is the
product of _Trachylobium Mozambicense_, a tree which grows along the
Zanzibar coast, and has left its resin buried in the sands of old raised
beaches which it has abandoned.
Public-domain text, read in full here on John Shaqi.
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