276 GEOLOGY OF OHIO. 
FLGVRE GX 
SECTION OF DANIEL KEES? COAL 
Soapst GUS Cooks Luss wae ———— 
Comnel Conl, ce Cosby 
Coal, conperos ak: bobbown 
Sokt Viwe-clay art Ot i | 
At John Fivecoat’s bank we find the seam somewhat thicker. Its 
structure is as follows: 
Inches. 
Slate. 
Coal, upper, DENCH jax ccive iewacde feadcnceehevasweade saodeesee mom tesecdaa ne sccenencees 29 
Olay. Or COpperas Partin)... jcesesccsccovscinetnciereceeserescotsecceceseoers 1 
Coal, lower Den Ch... o.c23vacssescceoascesscsussesasaueseesaoeemercerescecescoecesose 15 
Clay. 
This mine produces much more than any other mine in the town- 
ship. It is credited with 20,000 bushels annually. The Murphy bank 
is of the same general character. A section of the coal is shown below: 
RFLGEVURE wR 
MURPHY’S COAL,WASHINGTON TWP. 
SOO ee ——————— 
Clow or Vurites Eu, 
BotVor Coal 
In the Tuscarawas Valley, at New Comerstown, Oxford township, 
we find excellent sections illustrating the general geology of the district. 
At the iron bridge, just south of New Comerstown, there is a sec- 
tion of the Lower Mercer horizon of unsurpassed clearness. It is as 
follows : . 
