217 



of tilt' latter creek to Canada Gaj), coiitiiiuin.i;' in the same direction and, 

 passin.ii' a half mile south of Godsey Post Office, it crosses into ^lorgau 

 County three-quarters of a mile east of Godsey. Swinsiing southeastward- 

 it re-enters Mouroe County where Hacker's Creek leaves it. extending up 

 that creek to the neighborhood of Hacker's schoolhouse. From here 

 eastward the drift limit becomes harder to trace. The ice-sheet must 

 have been very thin, since the topography shoAvs little, if any, modifica- 

 tion. Scattered erratics are found all over the ridge dividing the waters 

 of Roberts' Creek from the headwaters of Honey and Hacker's creeks. 

 It seems probable that the foot of the ice-sheet rested on this hill, and 

 that the drift found in the head waters of Honey Creek was carried there 

 by the water resulting from the melting of the glacier. Many large 

 granite bowlders from one to three feet in diameter are found along the 

 small stream leading north from Hubbard's Gap. in See. 11 (10 N., 1 E.), 

 and along the other tributaries of Roberts' Creek. In section two of the 

 same township heavy deposits of sand, gravel and till lie against the 

 hillsides. In the neighborhood of Godsey Post Office the same phenomena 

 may be seen. Heavy beds of gravel and till lie against the hillsides 

 bordering their slopes on the south. In Canada Gap, section 9 (10 N., 

 1 W.), the evidences of ice occupation are plain though the quantity 

 of drift material is very limited. The territory between Indian Creek 

 and Bean P>lossom Creek and White River displays evidence of ice 

 occupation in many places in modified topography and deposits of till, 

 sand and gravel. Till, sand and gravel ot-cnr in the valleys leading south 

 from Hubbard's Gap in the vicinity of Fleener Post Office, and patches 

 of these same materials are occasionally met with south of the divide 

 east of that gap. On the whole the drift is thick in the valleys and thin 

 on the hills. This light drift on the hills indicates that the ice-sheet which 

 crossed them was comparatively thin. 



OUT-WASH AND EOLIAN DEPOSITS. 



North of Mount Tabor and between there and Gosport. as well as the 

 south slope of the hills between Mount Tabor and Ellet's hill are covered 

 with a heavy deposit of sand. A sand apparently identical with the 

 above caps several hills and fills several preglacial ravines on the south 

 side of Bean Brossom Creek near Andrew Stine's residence about two 



