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
13. _St. John’s, Lake County._—Professor W. S. Blatchley, in 1898 (22d
Ann. Rep. Geol. Surv. Indiana, p. 90), stated that an almost complete
skeleton of a mammoth had been found in a marsh at the headwaters of
Deep River, in the north half of section 35, township 35 north, range 9
west. This would be very close to St. John’s and on the Valparaiso
moraine.
It is not probable that Professor Blatchley saw this skeleton, and we
can not, therefore, be certain that it was not that of a mastodon. If it
did belong to one of the elephants it is to be regretted that such rare
materials have not been preserved.
14. _Allen County._—Professor C. R. Dryer (16th Ann. Rep. Indiana Geol.
Surv., p. 129) recorded the finding of a single mammoth tooth in Allen
County. Nothing more is known about this.
ILLINOIS.
(Maps 16, 38.)
WITHIN THE AREA OF THE ILLINOIAN DRIFT.
1. _Equality, Gallatin County._—In 1875, E. T. Cox (Geol. Surv.
Illinois, vol. VI, pp. 213–214), in his report on Gallatin County,
Illinois, stated he had picked up numerous plates of elephant teeth at
what was called “Half-moon,” located near Equality, in section 19,
township 9, range 8 east. It is an excavation made many years ago to
obtain salt-brine, near the Saline River, as the region thereabout
furnishes salt springs. It is implied in Cox’s account that other
remains of elephants had been found there, but usually in a bad
condition. It is impossible to determine to which species of elephant
the fragments belonged.
According to Leverett’s glacial map of the region (Monogr. XXXVIII, U.
S. Geol. Surv., plate VI), the locality is occupied by alluvial terraces
older than the Wisconsin drift. Not far away is the border of the
Illinoian drift. Most probably the elephants there represented lived
after the Illinoian stage, but they may have lived at any time
thereafter up to the Late Wisconsin.
2. _Chester, Randolph County._—Professor A. W. Worthen, former State
geologist of Illinois, made (Geol. Surv. Illinois, vol. VIII, p. 8) the
statement that Hon. William McAdams had found at Chester and Alton
remains of mammoth, _Megalonyx_, _Bos_ (=_Bison_), _Castoroides
ohioensis_, and other extinct animals. He did not, however, say what
species had been found at each place.
A newspaper statement was published in 1911 to the effect that William
Rade, of Belleville, had a large tooth, found in the lowlands along
Mississippi River south of Chester. It was described as a molar a foot
in length, 6 inches in diameter (in height probably), weighing over 5
pounds, and having several parallel ridges across the face. It was
doubtless the tooth of a species of elephant. A letter addressed to
William Rade brought no response. It is probable that the tooth had been
washed down from higher ground at some time. Its geological age is
indeterminable.
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