WEST VIRGINIA GEOLOGICAL SURVEY. 89 



made on the T. M. Marshall farm at the mouth of Sliding- 

 hill Run, in the town of Stouts Mills. Unfortunately, the com- 

 plete record of the test is not available. That portion of the 

 section below the Pittsburgh Coal is from the record of the 

 C. S. Hudnall No. 1 (752) well, drilled by Guffey and Galey 

 and previously published by the Survey." The well, which 

 is located on Slidinghill Run, one-half mile east of Stouts 

 Mills, was a dry hole except for a show of oil in the Fifth 

 Sand. The total depth was 2672 feet, of which the upper 101 

 feet is omitted from its record as published in the section be- 

 low. This well also recorded the Pittsburgh Coal, with a 

 thickness of 9 feet, which is probably too great by two or three 

 feet: 



Stouts Mills Section, Glenville District. 



Thickness Total 



Dunkard Series (190') Feet. Feet. 

 Concealed, with red and sandy shale, from top 



of knob 20 20 



Sandstone, flaggy 15 35 



Concealed, along slope 110 145 



Sandstone, massive, cliff rock, shaly at base, 



Waynesburg 45 190 190' 



Monongahela Series (422') 



Concealed 60 250 



Sandstone, brown, medium coarse, somewhat 



shaly, Uniontowr. 50 300 110' 



Concealed 27 327 



Sandstone, flaggy, green, fine. 20' ] 



Shale, red 10 j- Arnoldsburg 55 382 



Sandstone, shaly 25 J 



Shale, red, with limestone nuggets 55 437 



Sandstone, shaly, Sewickley (730' L.) 50 487 187' 



Shale, gray 1 488 



Limestone, red and shaly, Sewickley 2 490 



Concealed to Little Kanawha River 2 492 



Unrecorded 112 604 



Pittsburgh Coal, reported, in T. M. Marshall 



No. 2 Coal Test (754) (7' 8") 8 612 125' 



Continued in C. S. Hudnall No. 1 (752) 



Well Record: 

 Conemaugh Series (614') 



Limestone 29 641 



Slate 2 643 



Sand, Lower Pittsburgh 68 711 



Red rock 7 718 



Slate 5 723 



Limestone . . 33 756 



4 Vol. I(A), W. Va. Geological Survey, page 378; 1904. 



