538 GEOLOGY OF OHIO. 
NOL SCO rey ee ead Le OIL 218, a eeidln atl inl alert tela sad aa tee neat ts eee Ee) 
No 04 = pHa aR A RHEE PODER LEY TRADE MME SABRI AiR RE IN OS 3) <I ON) 
SANAStOME ee elec vaslossiencjocen decane ae saueiins doaine cetemmalenseen als atut sacs emt) 
he} G7 swale aa ONAN er Se Eni eM RRR BULA SANS HSA RNG IRON AN AA GEC SGA Sa wool tld kD> 
Coall(Camibridvey seam) Sreported ies ewesseaes eeceesbecclecsicccteseesteestee ance 
(See Map XII., No. 2.) 
WOO SSE DO 
mNooooFf 
The entrance to the mine near which this section was taken had fallen 
in, and no measurement was possible. On section 13, on the land of 
Robert Murray, the following section was taken: 
J8t; , Ubi, 
ly Sandstonevandiconglomerateiernestscemecsscceen ctseennnion secret ees (15 0 
Qe RVAL ON eee oe LO cus cen en uaneaed eerie aun ivon mee vaca anil oaee neta onumne hi laaciennpateene He Ome) 
Bena ©1012] RUA ee ra NEES el PORNO Le CLiPATren A A ARENA cen eA NNN MINA sana tisadadlin 4b 10) 
ALTO labC er cbeccealete site sarelenssateds sageeutedcoanuen’ ceamauces ecsleresisteacie see aman Mat aN eran 0 0% 
Siren! 70%: DSN RpiS a PA Me SNE Sane Cr An ya aR ORAS tree abeachG pric mcobic i @ 
(See Map XII., No. 16.) 
The coal at this point apparently works larger than is usual for this 
seam. The general quality is excellent. 
About a mile south of Bysville the Cambridge seam was found, by — 
boring, to be twenty feet below the level of Wills Creek, and reported to 
be five and a half feet thick. 
VALLEY TOWNSHIP. 
This township lies south of Jackson. The valley of Wills Creek ex- 
tends through it, and by this stream and its tributaries the whole area 
of the township is drained. The whole township lies above the Cam- 
bridge coal, unless possibly a small part of the low valley in section 21 
and in that vicinity may be low enough to reach the coal. <A geologi- 
cal section was taken about a mile and a half south-east of Point Pleas- 
ant, as follows: 
¥t. In. 
Tesi) HI AT Sia dsl cole oeaae uals wewres vaca mem ececuabaltcrs es tre cist oat alleen eavena cmalenacle con aso tenRae 25 0 
2. Limestone, FOSSILS ROUS eee este ts Heo LUE NIT aU Otc ae 1 0 
Dee WELL Ow Shale wesiacss eat waccewscesa le ease acas cathy es cloumitne memamauealenicisey neue taicaene 65 0 
4, Limestone (Ames limestone), fossiliferous ............ cceesee coeceeeee cones 4 0 
5. Shale, with white clay at bottom ........ ase a te See be Naveen cur euhe ath aOR area 25.0 
Goh San UStOMe! \ Li cele eM UNE Loledas enuhi U bevaides Sneha aaulanven us tem weenieaneas amatel 26° 0 
Tes HSM AILS ss conve welevecicceteisencseuce tegen sae meruatarsiousenes salccasunclentectem saints Canusea castles 23 0 
8.0 Coals (A ndersonyseain)iceuseesialsuene i tesuewsnmereaswauiten nese cree epeumemmeneiies 370 
Os Glay and! Shales ossusece neue cuaaecstaldestedualeseesenseleetuscmeateceme ncaa: 1) 
LOwSiderite ore; LOSsilifErous pee sienceacconsaclclesese scecisacemece cassoreleceeneens 0 6 
Lik Mostly sandstone sicis tess one taheaeetnis va sa wacercmemetwaoecamaaeaalebie meant aaaanates 36 «(0 
12.) (Wihitish) limestone eee eee ieee Oke se Med ant ve Heats ate ae Rae 1 0 
(See Map XII., No. 20.) 
