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



in an almost continuous line of cliffs on either side of the 

 stream. 



One mile east from the last locality we come to a massive 

 ledge of sandstone 25' thick, 255' above the base of No. 5 

 of the preceding section, and this makes it very probably 

 the New Mllford Upper sandstone. 180' above this we come 

 to the base of another very massive rock, grayish-white in 

 color ; much red shale is seen below it, while above it for 

 50' is seen a reddish shaly sandstone. 



One mile east from the last locality and on the land of 

 Mr. L. S. Everett a very massive sandstone is seen at 1730' 

 A. T. 



In going directly south from School House No. 2 to Mr. 

 H. Drinkers the New Mllford Upper sandstone is seen at 

 1500' ; and above this red shale occurs along the road up 

 to 1535' A. T. In the hill above this a very massive grayish 

 white rock begins at 1645' and covers the summit with very 

 massive blocks, as well as a neighboring hill with a very 

 bold cliff outcrop. 



The same massive rock is seen near H. Seymore's estate, 

 in the southern portion of the township ; base at 1575' A. T. 



Just at the Harford township line another massive sand- 

 stone comes in at 1645' on whose top at 1665' are seen many 

 glacial striae, going S. 30° W. magnetic ; on the other side 

 of the hill immediately below this sand rock 60' of red sliale 

 occurs along the roadside, and this brings us down to another 

 sandstone, the one seen near Mr. Seymore' s. 



In school district No. 7 near the Grinnell School House 

 the following section is seen : (Fig. 26.) 



Grinnell school-house section. 



1. Sandstone, massive, grayish-white, 25' 



2. Concealed, 50' 



3. Sandstone, 25' 



4. Concealed, 45' 



5. Sandstone, .... 30' 



6. Concealed to base of New MiJford Lower sandstone at 



S. line of the township on the D. L. & W. R.R 500' 



The upper portion of this section must come near the 

 horizon of the Honesdale sandstone group, since it is 675' 

 above the base of the Catskill sandstone series. 



