HARFORD. G 5 . 127 



Mr. Fairchild's, a very massive sandstone is seen at 1440' ; 

 it most probably represents a stratum in the interval between 

 the Montrose group and the New Mllford Upper sandstone. 



Barometric elevations in Brooklyn. 



Forks one half mile south of Montrose Depot, 1120' 



Forks near H. Tewksberry's, 1335' 



Cross roads at Tevvksberry School House, 1460' 



" near W. R. Page's, 1490' 



Forks near C. A. Williams', 1500' 



" J. Baker's, 1315' 



Forks in Brooklyn village, 1180' 



Forks next east, 1125' 



Forks near L. F. Porter's, 1140' 



Cross roads near H. G. Fairchild's, 1440' 



Forks near F. L. Lindsey's, 1470' 



19. Harford, in Susquehanna county. 



This lies directly east from Brooklyn, from which it is 

 separated by Martin's creek. 



The drainage is all southward into Tunkhannock creek by 

 several tributary streams. 



The northern line of this area extends nearly to the crest 

 of the divide which separates the waters flowing northward 

 into the Susquehanna river from those going southward. 



The outcropping rocks belong entirely to the CatsJcill sys- 

 tem and extend from the base of the New Milford Lower 

 sandstone up to the Montrose series. 



Along the D., L. & W. R.R. which ascends the valley of 

 Martin's creek, many good exposures of the lower and mid- 

 dle portions of the New Milford sandstone series are seen. 



About three fourths of a mile above Montrose Depot, and 

 just at the northern line of the township, a massive sand- 

 stone is seen in cliffs along the R.R. It is very much cur- 

 rent-bedded, contains many fragments oi fossil plants, and 

 is most probably the New Milford Lower sandstone. Be- 

 low it are seen olive and red shales 15' thick to level of R.R. 

 track. 



As we pass down Martin's creek from this point, the rocks 



