COEEELATIVES OF BLOOMINGTON MOEAINIC SYSTEM. 



117 



Section of Kinney well, sec. 15, T. 22 N., R. 4 W., 2\ miles 



east of Culver. 



Soil. 



Feet. 

 . 24 



Clay, yellow 8 



Clay, blue 40 



Hardpan 3 



Water at 53J 



Section of well at schoolhouse No. 6', Wea Township, 3 miles 

 southwest of Culver. 



Soil 2 



Clay, yellow S 



Sand and gravel 6 



Clay, blue 41 



Water at 57 



Section of Hicks well at Battle Ground (on terrace of Wabash 

 River). 



Soil 3 



Hardpan 3 



Gravel and sand 73 



Section of Clue well at Battle Ground. 



79 



Soil and yellow clay 4 



Gravel, coarse 25 



Sand 30 



Clay, blue 1 



60 

 Section of Thomas well, 3h miles east of Battle Ground. 



Soil and olay 4 



Gravel and sand 20 



Hardpan 20 



Sand and gravel 25 



Clay, gray 2 



71 



Section of Hoyleman well, 41 miles northeast of Battle 

 Ground, in Moot Creek valley. ' 



Soil and clay 6 



Clay, hard, blue 54 



No watei at 60 



Section of PeJJley well, 1 mile northwest of Colburn. 



Feet. 



Soil and clay 4 



Clay, bine 40 



Gravel, dry, coarse 20 



No water at g4 



Section of Livingston well, 2 miles west of Battle Ground. 



Soil and yellow clay 30 



Sand, fine, diy 20 



Clay, blue 30 



Gravel, cemented 2 



Gravel, loose 13 



Water at 95 



Section of Bryant well, 3 miles ivest of Battle Ground. 



Soil and yellow clay 4 



Clay, blue 50 



Sand, dry 20 



Gravel, coarse 2 



No water at "6 



Section of Brown icell at Buck Creek station. 



Soil 2 



Clay, yellow 3 



Clay, blue 15 



Sand, fine, yellow 30 



50 

 Section of Cole well, 1\ miles west of Buck Creek station. 



Soil and yellow clay 6 



Gravel and sand 49 



Clay, blue 5 



60 



Section of Stanfield well, 2 miles north of Buck Creek station. 



Soil and clay 4 



Fine, sand 45 



Gravel, coarse 12 



Gravel, fine, with bowlders at bottom . . 4 



Water at. 



65 



Data concerning deep wells at Dayton and Lafayette are presented in the discussion of the 

 Bloomington rnorainic system. In the northwestern part of Tippecanoe County there are 

 deeper wells than any reported by Gorby, but the writer was unable to obtain reliable records of 

 them. One on the Van Alia estate in the east part of sec. 18, T. 24 N., R. 5 W., 126 feet deep, 

 struck no rock, nor did one 176 feet deep on a farm 2 miles northeast of Otterbein in sec. 26, 

 T. 24 N., R. 6 W. 



BOWLDEES WITHIN THE INNEE BOEDEE. 



Bowlders are not numerous except in very small patches on the great intermorainic tract, 

 and no system in their distribution was detected by which an ice margin could be marked out. 

 The bowlders are mainly crystalline rocks, more than half being granite and the bulk of the 

 remainder basic eruptives. A few red jaspery conglomerates from north of Georgian Bay were 

 noted. 



In the Wabash Valley at Logansport bowlders are exceedingly numerous, numbering where 

 thickest 1,000 or more per acre. They also abound at intervals below Logansport for several 



