CANAAN. G 5 . 189 



The Honesdale Upper sandstone is here seen in a long 

 white cliff circling around the summit of the hill ; quite 

 coarse, and containing some pebbles. 



The tripple structure of the Honesdale group, seen at the 

 top of this section, is characteristic over a wide area, the 

 concealed middle portion usually consisting of red, shale or 

 sandstone. 



About one half mile south from the locality where the 

 Honesdale Upper sandstone of the preceding section occurs, 

 we see it again in a massive cliff, its base 10' lower, or 1305' 

 A. T., while above it at 1335 r a reddish-brown sandstone ap- 

 pears, and at 1365 / another, very massive, and grayish-white 

 in color. 



The Cherry Ridge limestone is seen cropping out in a 

 long black band 4' thick, along the road which leads out 

 from Honesdale past Cad jaw pond, and it has an elevation 

 of 1445' A. T. 



Barometric elevations in Texas. 



A. T. 



Forks in Seelyville, 1065' 



" Prompton, 1095' 



Level of Bunnell's pond, 1100' 



Forks near H. Bunnell's, 1095' 



" Mrs. I. Sear's, 1125' 



" J. Burn's, 1310' 



" J. Koof s, 1250' 



" D. Holbert's, 965' 



" School House No. 10, 995' 



■« C. Dorflinger's, 1245' 



4-0. Canaan, in Wayne county. 



This township lies next west from Texas and extends to 

 Lackawanna county for its western boundary. 



The Moosic Mountain range passes through the extreme 

 western portion of this area and all the surface east from it 

 drains into Lackawaxen creek ; west from it however the 

 drainage passes to the Susquehanna river by way of the 

 Lackawanna. 



The Honesdale Gravity R.R. passes across the Moosic 



