The Pleistocene of North America: and its vertebrated animals from the states east of the Mississippi River and from the Canadian provinces east of longitude 95°Hay, Oliver Perry
Science
The Pleistocene of North America: and its vertebrated animals from the states east of the Mississippi River and from the Canadian provinces east of longitude 95°
Hay, Oliver Perry
Paleontology -- North America; Paleontology -- Pleistocene; Vertebrates, Fossil
Dr. J. C. Warren (“Monogr. on _Mastodon giganteus_,” ed. 2, 1855, p.
162, plate XXVIII, fig. B) figured and described the tooth. The length
was given as 11 inches at the base, and the number of ridge-plates as
22. This would give an average of 8 plates in a 100–mm. line. This
number and the general appearance of the tooth indicate that the animal
was _Elephas columbi_, instead of _E. primigenius_. The difference
between this tooth and that of _E. primigenius_ is well shown by the
figure of a tooth of _E. primigenius_ from Zanesville, Ohio, figured on
the same plate with the Vermont tooth. This tooth is now in the American
Museum at New York.
Thompson reported the presence of many billets of wood, about 18 inches
long, in the bottom of the muck, the work of beavers.
At the Davenport (Iowa) Academy of Natural Science the writer examined a
tooth of an elephant labeled as having been found on Mount Holly in
excavating for the Vermont Central Railroad. The length along the base
is 300 mm., the height of the ninth plate is 160 mm., the length of the
grinding-surface 160 mm. There are in all 24 plates, the 10 anterior
ones of which are worn. There are 7 ridge-plates in a 100–mm. line,
measured on one side of the tooth. This tooth is regarded as belonging
to _Elephas columbi_; it certainly belonged to another individual than
the one that Warren figured. It is almost certain that the animals
represented by the teeth and skeletal remains found on Mount Holly lived
after the retreat of the ice from those mountains; and one may suppose
that local glaciers lingered long after the main ice-front had abandoned
the region. The animals lived certainly as late as near the close of the
Pleistocene, if not at the beginning of the Recent; they may have been
living on those mountains while the basin of Lake Champlain was an arm
of the sea.
NEW YORK.
(Map 12.)
1. _Homer, Cortland County._—In 1847 (Amer. Jour. Agric. and Sci., vol.
VI, p. 31, fig.), Samuel Woolworth reported that an elephant tooth had
been found on the bank of a small stream, about 2 miles northwest of
Homer. Emmons, in 1858 (Geol. Surv. North Carolina, East. Cos., p. 200),
figured the same tooth. In his Manual of Geology (ed. 2, 1860, p. 242,
fig. 207) he stated that this tooth was found in Cortland County. Henry
A. Ward, of Rochester, advertised and sold casts of this elephant tooth,
as the writer is informed by Mr. Frank H. Ward, of Ward’s Natural
Science Establishment. It is almost certain that this elephant lived in
the neighborhood of Homer after the Wisconsin glacial ice had begun its
retreat to the far north.
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