3. _Vevay, Switzerland County._—Professor E. Danglade, of the U. S. Fish Commission, presented the U. S. National Museum a tooth (No. 7913), apparently a second true molar, possibly the first, of _E. primigenius_. There are 10 plates present. The tooth was found on the shore of Ohio River about 1.5 miles below Vevay, having been washed out of a gravel bank, and is much weathered. No exact conclusions about the age of the tooth can be drawn from the known facts. IN AREA BETWEEN THE SHELBYVILLE AND THE BLOOMINGTON MORAINES. 10. _Webster, Wayne County._—In the collection of Earlham College are 2 elephant teeth, credited to Jehiel Bond and found on Nolands Fork, near Webster, Wayne County. One is the second molar of the right side of the upper jaw and is much worn; the other is the third upper molar of apparently the same side and is but little worn. These teeth were mentioned by the author in his report on the “Pleistocene Vertebrata of Indiana” (33d Ann. Rep. Geol. Surv. Indiana, p. 750), but he had not then determined to what species they belonged. A renewed study shows that they certainly belong to _Elephas primigenius_. With these teeth is a tusk which measures 1,800 mm. along the convex curve. Webster is situated south of the Bloomington moraine, in a tract of country indicated by Leverett as covered by undulating drift, in part morainic. The greater part of this political township, made up apparently of parts of townships numbered 13 north and ranges 8 and 9 west, is occupied by outwash deposits laid down by the Wabash River and brought from further north during the Wisconsin stage; but at present, at least, it is impossible to assign the animal to any particular division of that stage. IN AREA NORTH OF BLOOMINGTON MORAINE AND SOUTH OF THE MISSISSINAWA MORAINE AND THE WABASH RIVER. 4. _Windsor, Randolph County._—In the collection at Earlham College, Richmond, Indiana, is a part of a tooth referred to this species. It is either the last milk molar or the first true molar of the right side of the lower jaw. There are present eleven plates and one or more is missing from the rear. The length along the base is 100 mm., the width is 55 mm. There are six plates in a line 50 mm. long. This tooth was found August 20, 1893, in the bed of Stony Creek, near Windsor. According to Leverett’s glacial map of Indiana, this is just south of the Union City moraine near its junction with the Bloomington moraine. By what is known of the habits of this species it may have lived even when the glacial sheet was forming the Union City moraine.