Mr. Pierce's discovery is not less interesting; and we presume he
will be deemed correct in the opinion, that pure native carbonate
of magnesia has not been discovered before. The serpentine of
Hoboken, then, is memorable for affording these two new species.
ART. V. _Native Copper._
In Bruce's Journal, (Vol. I. p. 149.) mention is made of a
remarkable piece of native copper, found near New-Haven many years
ago, and weighing about 90lbs.
We have now to add, (and the fact is, indeed, mentioned in
Cleaveland's Mineralogy,) that another piece has been recently
found half a mile west of the Hartford turnpike road, opposite the
town of Wallingford, and twelve miles from New-Haven. It was turned
up in ploughing to repair a road. The country is of the secondary
trap formation, and the rocks, at the particular place, are the
old red sandstone of Werner, which here occupies the plains, and
runs under the trap. The piece weighs almost six pounds; it is
fine virgin copper, with rudiments of large octahedral crystals of
native copper upon its surface, which is more or less incrusted
with green carbonate of copper and ruby oxid, very much resembling
that of Cornwall: the ruby oxid is particularly remarkable in the
cavities of the piece.
As it was found within three or four miles of the place where the
large piece of ninety pounds weight was discovered, and as copper
is known to exist in many places in these hills, the facts should
be kept in view, and may lead to something of importance.
ART. VI. _Petrified Wood from Antigua._
The mineralogy and geology of the West-India islands has been,
as yet, but little explored. The scientific world has, however,
been favoured with some interesting articles from the pen of Dr.
Nugent; and we are informed that he has described also the geology
of the island of Antigua. We have recently become acquainted with
one interesting production of this island, and without waiting for
Dr. Nugent's account, (which we believe has not yet reached this
country) we shall lay it before our readers.
We are under obligations to Mr. Pelatiah Perit, of New-York, for
a collection of specimens of silicious petrifactions of wood from
Antigua. Their characters are indubitable; the distinct ligneous
layers corresponding with the annual growth, the medullary
prolongations, the knots formed by branches, the cracks and the
bark, are all distinctly visible. Some of the pieces are ponderous
portions of large trees.
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