162 G 5 . REPORT OF PROGRESS. I. C. WHITE. 



not reach the base of the CatsMll sandstone series. Hence 

 these rocks must be increasing in thickness quite rapidly 

 toward the southeast from the northern line of this county ; 

 since at the western line of Scott township a nearly vertical 

 measurement gives only 800' from the base of the Honesdale 

 Lower sandstone down to the base of the New Milford 

 series. But here on the Delaware, at Dillon's mill, the same 

 interval must be more than 1000', because the New Milford 

 Lower sandstone comes down to the level of the Delaware, 

 12 miles above, and the dip cannot be less than 20' per mile. 



Barometric elevations in Buckingham. 



A. T. 



Forks near Ball's Eddy at Mrs. Smith's, 960' 



'< H. Geer's, 975' 



" J. Jones's, 925' 



Forks next above on Chehocton creek, 965' 



" from J. G. Squire's, . 1210' 



Forks near G. E. Falling's, 1325' 



" W. G. Underwood's, 1410' 



Level of pond near by, 1400' 



Road at Jericho School House, 1425' 



Forks next north, . . 1550' 



Forks near R. Randall's, ... 1560' 



Level of road at crossing of stream next c.-.s:, .... 1190' 



Forks near Adams' lake, ... 1320' 



Crossing of stream at C. P. Waller's, . . . 1370' 



Forks near W. Brown's, 1435' 



Level of North Equinunk near Knight's mill, 1325' 



Forks near Mrs. E. Wyckoff 's, 1260' 



Level of North Equinunk near L. Henkley's, 1120' 



Forks near J. C. Branning's, 1090' 



Level of Equinunk at L. S. Jump's, 1010' 



" M. McKinney's, 925' 



Forks near T. Tyner's, 900' 



Forks next north-east, 890' 



31. Manchester, in Wayne county. 



This lies east from the south-eastern line of Buckingham, 

 being separated from it by Equinunk creek, while the Dela- 

 ware river bounds it on the north and east ; the Delaware 

 also receives the entire drainage of the district, through 

 Equinunk and Little Equinunk creeks. 



