SHULIE TO SPICER COVE (H). — FLETCHER. 545 



Ft. In. 



below Xo. 13, and 'No. 28 may rest directly upon 

 the congiomerate, in which case that section may 

 be continued as follows : 



29. Red conglomerate with Veins of barite and celestite 



near the top ; its material is for the most part of 

 syenite, and it is associated with red, thick, fine 

 layers. The thickness here gi\'en is takeu from 

 the boring drilled l)y ]\[r. J, A. Johnson. (See 

 Section XII.) 811 6 



30. Red syenite of Devonian age, or more generally an. 



obscurely granular and compact felsite and quartz- 

 felsite, hornblende being scarce except in dykes 

 and blotches of dark diorite, seldom more than ten 

 to fifteen feet wide. An epidote breccia occurs 

 near the contact of the conglomerate, and the fel- 

 site is so much brecciated as to resemble the con- 

 glomerate. These rocks in great cliffs occupy tbo 

 coast south past Eaton ville to Cape Chigneoto, as 

 sho^Ti on Sheet Xo. 100 (and 101) of the 

 Geological Sun^ey series of maps. A line of fault 

 at the first beds of red conglomerate is indicated by 

 the grooves as dipping X. 45° E.< 63°. First a 

 little piece of the conglomerate is thrown on edge ; 

 then, further inland near a little brook from the 

 south, the dark rocks with tlie black shale and coaly 

 layers of Xo. 28 rest upon the conglomerate at a 

 low angle apparently conformably. The thickness 

 of the latter as given above is much greater than 

 the height of conglomerate in the cliffs, overlying 

 the syenite, and thus measures the downthro^^'' of 

 the fault at about 500 feet. 



Total thickness 878 2 



