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



Level of Beaver creek at School House No. 5, 1285' 



Forks near J. E. Sherwood's, 1525' 



" W. W. Harrison's, 1385' 



" School House No. 1, 1010' 



Level of Salt Lick at Summerville, 995' 



Forks near H. H. Van Cott's, 1240' 



" School House No. 9, 1365' 



" L. S. Everett's, 1650' 



Forks next south near cemetery, 1545' 



Forks east of C. D. Williams, 1520' 



Forks near C. G. Page's, 1400' 



Level of pond just west, 1390' 



Forks of road near School House No. 15, 1420' 



" next east, . 1455 



Cross roads near J. W. H. Bradford's, 1590' 



E. J. Tyler's, 1485' 



" School House No. 13, 1485' 



Forks near R. C. Richardson's, 1525' 



" School House No. 2, 1210' 



" R. Gillespie's, 1205' 



" F. T. Wellman's, 1300' 



Forks next southwest, 1390' 



Cross roads near H. Grinnell's, 1625' 



12. Bridgewater, in Susquehanna county. 



This is a very irregular shaped area, lying directly west 

 from New Milford. 



Near its center, on a very elevated plateau, the highest 

 land in the western half of this county, is situated the county 

 seat, Montrose. 



The drainage goes off toward almost every point of the 

 compass, but it all finally reaches the Susquehanna river. 



The rocks of this township belong entirely to the Cats- 

 Mil series, though in the northern portion the valleys of 

 the streams are cut down nearly to the Chemung or prob- 

 ably within 100' of its top. 



In the vicinity of Montrose, are a series of massive sand- 

 stones which crop out in bold bluifs around the hills, and 

 from their elevation above the base of the Catskill, would 

 seem to come at the horizon of the Honesdale group. 



The following succession is seen in the vicinity of Mon- 

 trose : (Fig. 31.) 



