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
Clarke (Bull. 69, N. Y. State Mus., p. 926) stated that in 1902 a
cranium and some other parts of a mastodon had been found at Balmville,
just north of Newburgh. The bones lay at a depth of from 2 to 8 feet,
some in the muck and some in the marl below. Under the marl was found a
boulder pavement.
In 1902 (Science, vol. XVI, pp. 594, 1033), Reginald Gordon gave
accounts of the exhumation of a mastodon skeleton 1 mile north of the
northern limit of Newburgh and 0.75 mile away from the Hudson. This
certainly refers to the same mastodon as that reported by Clarke. The
place is a swamp of about 2 acres and at a height of 180 feet above the
level of the river. The bones were found 2 to 8 feet below the surface,
a few of them inclosed in the muck, most of them in an underlying
shell-marl. The muck averages 2 feet in thickness; the marl varies from
a few inches to 12 feet in thickness. Beneath the marl a solid bottom is
formed of pebbles and boulders.
16. _Northeast of Coldenham, Orange County._—In 1847 (op. cit., p. 73),
Eager wrote that in 1800 remains of a mastodon were found about 7 miles
northeast from Montgomery, on or near a farm owned by Dr. George Graham.
This statement was based on Dr. J. G. Graham’s letter (Med. Repos., vol.
IV, p. 213). This must have been in the vicinity of the town named. Dr.
J. G. Graham stated that a vertebra had been found here. This may have
been in the marshes along Bushfield Creek.
17. _East Coldenham, Orange County._—Dr. James G. Graham (op. cit., p.
213) states that about 7 miles east of Montgomery (apparently about 5
miles west of Newburgh), a grinding-tooth and some hair of a dun color
had been found at a depth of 4 or 5 feet. Possibly the supposed hair was
some sort of vegetable matter. The place may have been on Bushfield
Creek. Gordon (Science, n. s., vol. XVI, p. 1033) reported further the
finding of large numbers of tree-trunks both in the muck and in the
marl. Some mastodon bones were found resting on the trees. Red cedar and
spruce were recognized. Some trees showed marks of the teeth of beavers.
18. _Montgomery, Orange County._—Several more or less well-represented
skeletons of mastodons have been discovered in the vicinity of
Montgomery. So far as the writer knows, the first were met with in 1782.
An account of the discovery was given by Rev. Robert Annan in 1793 (Mem.
Amer. Acad. Arts, Sci., vol. II, pp. 160–164). The town was not named,
but Mather (Geol. N. Y., 1st Dist., pt. 1, 1843, p. 202), on the
authority of Dr. James G. Graham (Med. Repos., vol. IV, p. 213), stated
that the place was 3 miles south of Ward’s Bridge, an old name of
Montgomery. This would be near the village of Neelytown, and probably in
the swamps along Beaver Creek. A ditch was being made in a deep and wet
swamp, and some large teeth were thrown out. The description of these
shows that they belonged to a mastodon. Bones were present, but mostly
so far decayed that few could be saved.
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