WEST VIRGINIA.

(Map [22].)

1. Wood County.—In 1835 (Amer. Jour. Sci., vol. XXIX, p. 147), Hildreth stated that bones of a deer had been found in this county, then a part of Virginia, involved in the travertine on the floor of the cave. No facts are known that give any clue to the geological age of these bones. They probably belong to some early or middle stage of the Pleistocene.

NORTH CAROLINA.

(Maps [22], [39].)

1. On Neuse River, Pamlico County, 16 Miles below Newbern.—According to both Croom (Amer. Jour. Sci., vol. XXVII, 1835, p. 168) and Harlan (op. cit., vol. XLIII, 1842, p. 143), remains of deer had been found at this locality. For want of more exact information we may refer them to Odocoileus virginianus. On page [359] will be found a list of the species collected here.

SOUTH CAROLINA.

(Map [22].)

1. Charleston, Charleston County.—Numerous fragmentary remains of Odocoileus have been found in the region about Charleston. F. S. Holmes, as early as 1859 (Proc. Acad. Nat. Sci., Phila., 1859, p. 177), announced the discovery of remains of deer in the vicinity of Charleston. Leidy (Holmes’s Post-Pliocene Foss. South Carolina, p. 109, plate XX, figs. 1–4) stated that the collections of Professor Holmes and Captain Bowman contained fragments of antlers, portions of jaws, and teeth which had been found in the Post-Pliocene beds of Ashley River. Leidy concluded these remains did not differ from the corresponding parts of the existing white-tailed deer (O. virginianus). Many fragments of antlers belong in the Scanlan collection at Yale University. They are thoroughly fossilized and are hard and heavy.

In the Charleston Museum (No. 1047) is an anterior cannon-bone of a deer, but no definite locality is recorded. It is black and apparently phosphatized, as are the numerous fragments of antlers found in the private collections at Charleston. The cannon-bone mentioned is 188 mm. long.