Some years since, during Mr. Maclure's geological survey of the
United States, the editor had the pleasure of passing a few days,
in company with that gentleman, in exploring the geology of the
vicinity of New-Haven. Near that town, junctions, on an extensive
scale, between widely different formations, are to be observed. A
radius of ten miles, with New-Haven for a centre, will describe
a circle within which the geological student may find (with the
exception of formations, unquestionably volcanic) most of the
important rocks of the globe, and a radius of even six or seven
miles will include the greater number of these. At, and near the
terminations of the primitive ranges, there are rocks which appear
to have, in a high degree, the characters of the transition class.
Among them is the beautiful green marble of the Milford Hills,
seven miles from New-Haven. Mr. Maclure visited that district, and
even suggested the first hint which afterward led to the discovery
of the marble. Doubts being entertained concerning some of the
geological relations of those rocks, a letter was addressed to
Mr. Maclure (then in Philadelphia) on the subject. His answer is
subjoined.
In giving it to the public, the editor takes a liberty which he
hopes the respectable author will pardon, because his production,
although evidently never intended for the public eye, contains
statements and opinions of no small importance to the young
geologist, especially of this country.
Geology, at the present day, means not a merely theoretical and
usually a visionary and baseless speculation, concerning the
origin of the globe; but, on the contrary, the _result of actual
examination into the nature, structure, and arrangement of the
materials of which it is composed_. It is therefore obvious,
that the opinions of those men, who, with competent talent and
science, have, with a direct reference to this subject, explored
many countries, and visited different continents, are entitled to
pre-eminent respect. SAUSSURE, by his scientific journeys among the
Alps, (although a limited district) has given deserved celebrity to
his own name, and, if it were possible, has thrown an additional
charm of attraction over those romantic and sublime regions.
Dolomieu has made us familiar with the productions and phenomena of
volcanoes, those awful and mysterious laboratories of subterranean
fire. Humboldt has surveyed the sublimest peaks of both continents,
and examined the structure of the globe amidst the valleys of
Mexico and the snows of Chimborazo and Pinchinca; and Werner, with
opportunities much more limited, (confined indeed to his native
country, Saxony) but with astonishing sagacity and perseverance,
deduced from what he saw, a classification of the rocks of our
globe, which, although not perfect, has done immense service to the
science of Geology. In this distinguished group (to which other
important names might be added) Mr. Maclure has unquestionably a
right to be placed.
Public-domain text, read in full here on John Shaqi.
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