¢ 
G. F. Wright—Glaciated Area of Ohio. 53 
the flood plain. Three miles farther south, at Oxford, there is 
Streams meet, there is a gravel deposit two miles or more in di- 
ameter about twenty-five feet above the flood plain. On the 
east side of this plain, near the junction of Martin’s Creek and 
the Killbuck, there is a kame-like accumulation extending one- 
eighth of a mile northwest by southeast. The surface is very 
much broken, displaying many kettle-holes. A railroad cut- 
ting through it shows some scratched stones in the material, 
some distance above the rime be a terrace which rises 107 > 
feet above the river, and is compos 
Sive deposits of rather fine gravel. 
9. Th : 
e Licking River emerges from the glaciated region at . | 
Newark. Three forks unite here to form the main stream, and 
as usual in such places there is an extensive gravel plain 
Stretching inward. This plain is about twenty feet above the 
river. The city is built upon it, and it was a favorite resort for __ 
the mound builders. For a mile and a half below the city, the _ 
river as it enters the narrower channel is bordered on the north a 
f. 
; largely of coarse granitic nee 
pebbles. This terrace also extends for a half mile below the : 
Junction. At Gann station, eight miles below, there are exten- 
