MIOCENE TERTIARY ROCKS — WESTON. 



225 



zite, jasper and chert. These are the beds from which Menodus 

 angustigenis, M. Proittii, M. American us, Heinipsalodo7i 

 grandis, and other genera and species were found. 4 to 20 feet. 



c. Yellowish sand with a few pebbles of quartzite. 1' — 2". 



d. Fine conf^domerate in which a few hsh remains were 

 found. 0'— 6". 



e. Sand and thin beds of conglomerate. 5 feet. 



/. Conglomerates in which a large bone was seen. 2 feet. 

 g. Sand and fine gravel. 2 feet. 



h. Gravel, loose pebbles varying in size from half an inch to 

 a foot in diameter. 15 feet. 



30' 



4'to 20' 



r - 2" 

 o'~ e' 



6'- C" 



75'- C 



A'-H '/ •■ ' '• •< >^fr 





•7 i'tr'^^t^^yj-y-.'^"^ '"'^'^r 





Ct,. 



C 



e 



f 

 S 



Section oj Miocene Tertiary Bocks near Bead Wafers of Sirift Cnrreiit, K. W. T. 



At the request of Dr. Selwyn these remains were examined by 

 Prof. E. D. Cope, of the Academy of Natural Science, Phila- 



