Saratoga County, New York
Geologic Age
The rocky groundwork which underlies the county of
Saratoga presents, to the student of geology, many features of
surpassing interest. Yet all that properly seems to come within the
scope of this work is a mere outline of the subject, so far as it
necessarily bears upon the economic interests and historical
associations of the county and its surroundings. And this outline will
be confined principally to the more striking geologic features of the
county; in a word, to the departments of physiographic and historical
geology, leaving to the interested student the no less inviting fields
of lithological and dynamical geology, of which the county is so rich in
natural illustrations, to be studied in the field itself here spread out
before him, or in the numerous special works devoted to the science.
The science of geology unfolds to us to some extent the mysteries of
the world's creation. The earth itself, like the plant or animal it
sustains on its surface, is a thing of growth, of development. The
different periods of this growth and development are more or less
distinctly marked upon the rocky structure of the earth by the various
fossil forms of animal and vegetable life found therein, and these
successive periods so marked are termed geologic epochs, times, or ages.
The geologic epochs or ages of the world are distinguished by the
progressive development of the various forms of animal and vegetable
life, from the lowest to the highest forms of existence.
The
extremely interesting geologic features of Saratoga County can be best
explained by referring somewhat in detail to the geologic ages of the
world based upon the progress of life and living things, and the
different periods of geologic time marked by these successive ages.
WHAT IS A
GEOLOGIC MAP?
CLICK HERE TO DOWNLOAD |