Asbburner.] 0^\) [Feb. 10. 



26G. Sandstone and shale, containing a small bed of coul, in 

 black slate and shale, a short distance below the bottom of the 

 Mahoning Sandstone, probably representing Coal E, Upper 

 Freeport. Lower part, directly above Coal D, hard, rather 

 massive black slate 45' 



2G5. Coal bed D, (top bench mine C) 2'1" 



264. Black fissile slate containing seams of coal vary- 

 ing in thickness from \ to ^ inch 0'4" 



263. Coal bed D, (middle bench) 0'2" 



262. Slate containing a stratum of sandstone about the 



7'9' 



centre 2'1" 



261. Coal bed D, (bottom bench). Fireclay floor of 



the mines unmeasured 3'1 " j 



260. Sandstone and shale ; black slate lower part 45 =f' 



259. Coal bed C, (top bench mine B) 1'6" T 



258. Hard grayish-black slate, (varying thickness). . .0'4" 



257. Coal bed C, (bottom bench). Fireclay floor of [ ^'^^" 



the mines unmeasured 2'0" J 



256. Sandstone, shale and slate 30' 



255. Coal bed B, (top bench mine A) 1' 6" -x 



254. Rock and fireclay 1' 4" [ 4'8" 



253. Coal bed B, (bottom bench) I'lO" ) 



252. Sandstone and shale 35' 



251. Coal bed A, underlaid by a carbonaceous black fire- 

 clay, commonly called black gravel 2' . 



No. XII 



Fottsville (Serai) Conglomerate ( Millstone Grit. ) 280' 



Upper Member. Piedmont Sandstone. 



250. Upper member consisting of three parts, upper white 

 and reddish white and gray flaggy sandstone and conglomer- 

 ate ; in the middle part the conglomerate predominates, the 

 pebbles are larger but irregularly distributed, the strata ex- 

 hibiting false bedding to a marked degree ; while the lower 

 part is composed principally of thinlj'^ bedded and conglomer- 

 atic sandstone 100' 



!Middle member {Kanawha River Coal Series). 



249. Sandstone and shale, " " 14' 



248. Coal (Firecla_v floor unmeasured) 2' 



247. Less massive gray sandstone exhibiting false bedding.. 17' 



246. Dark gray and black slate and slaty sjindstone 7' 



Lower member (Conglomerate proper.) 



245. Hard massive gray sandstone, strata fractured in a per- 

 pendicular and also oblique direction to the bedding, surfaces 



