Fig. 31. 



Pensauken formation, G. A. Bowne's pit, 1 mile east of Bustleton Church. 

 Note the promiscuous distribution of the pebbles. 







Fig. 36. 



Pensauken formation, Cole's pit, Colestown, Camden County. The material 

 is largely of local origin, most of the pebbles being derived from the south- 

 east. There is, however, a little Triassic shale and crystalline material. 



