223 



Section 5.— On t]ie road on the half section line between sections 34 

 and 35, Washington township, one and three-fonrths miles north of Dolan. 



Feet. 



1. Yellow clay brealving down to yellow earlh 5 



2. Whitish-yellow clay ] 



3. Yellow clay 3 



4. Whitish, laminated clay becoming very hard on exposure. . 5 



5. Yellow jointed clay 5 



6. YelloAV to brown jointed clay 5 



7. Shale If 



No glacial material of any sort was found in this delta. 



INDIAN CREEK DELTA. 



Section 1.— Well at Lemon Post Office. 



The section here was composed entirely of loose material. The l)ot- 

 tom of the well was in loose erratic gravel at a depth of 20 feet. 



Section 2.— Marion Coater's well, forty rods east of Lemon Post Office. 



Feet. Inches. 



1. Black earth 2 



2. Yellow clay 8 



3. Yellow coarse sand 8 



4. Gumbo clay 14 



5. Fine quicksand 3+ 



The Indian Creek delta is composed more or less of glacial material, 

 as is shown by the sections. This, of course, was anticipated as the 

 stream heads in Canada Gap. 



Sections taken in the vicinity of the Honey Creek delta. 

 Section 1.— Well north of the road one-eighth of a mile east of Pleasant 

 Valley Church. 



Feet. 



1. Clay 5 



2. Erratic gravel 7 



Section 2. — Another section near the preceding one. 



Feet. 



1. Gravel 18 



• Bowlder stratum 4 



Like the Indian Creek delta this delta contains glacial material. The 

 glacial material came through Hubbard's Gap. 



