500 GEOLOGY OF OHIO. 
near Germantown, in section 23, the following geological section was 
taken : 
Kt. In. 
Lovittleayy. sandrocki(exposed)i. ee sci csecclecseueie taleuceces Gears sch mee cum ee bale eee toe) 
2 BiWe Shae eee i a SMUT RUE ances NU aE ROTA Xe Rie ava 8 0 
8.) CoaloCumiberlanadiseatiy aii iinet ce sina aaa RNa em R eRe 2°16 
4, Clay, if rei) ka ia as laayergotereald MW elnn pe atcire te lle oats ci ae ROM Seu UTR na exer nena 2/0 
5. Coal, ‘f aes re SO ER AAU Unde RRR U EAL URNB SAG a anicauie nies). ay ICD) 
Gs \Slay ame Sale ae ee an era hodeeseue tuum cutnn en eee Seay arien ental ae Meneame aM eae Ova) 
7. Limestone . Sa Segaieblennivcelese SUMCNE SecleSale velee eee e rece seca eninen ee eee ee Ap ZING) 
Bed of ee Gass Ven Map Xf., No. 23.) 
This is the Cumberland seam. In another coal bank, near by, the di- 
viding clay is only ten inches thick. On the land of Edward Doyle, 
section 16, the geological section is as follows: 
Ft. In. 
iL. leave Sandrock (Exposed) 6c. siahirscescs ccasse dees wen cece eects cana seer eo eaane SS (ME) 
20 Shale: ns we sei eee vcelaa a Wane quasar twevesetelet an eek selena te ae Mere Nar aaah aH) 
3. Coal, Gumbotinare seam.. sha douihed doa seuitedleseuduleee sees saltuelar MeMaE GRE eRe CM mena () 
4, Clay, is my i @ 
5. Coal a f iy 
On the farm of Henry Barnhardt, in section 8, in this township, a more 
complete geological section was taken, as follows: 
Ft. In 
Le ileavy,sandrock exposed oii icc cs vocdeccve scueateenusecen contrasts ceatecemeaens 20 0 
PARIS OF WK ERK HE NA eT OIL HEMP DU ner ANS AL RAE UI AS a eine 1 0 
Se Coal Cumberland Seams Assad les scsccrnecahesoscr ose velussion seca ene eae 2 0 
4, Clay, OLR A MIN AU nS a ra SRL ST ANE MeC/sHEe) BRA ROLE a Neila dusaaan 0 8 
5. Coal, a aE Uda esieashonlCdusetissanectscwetioneae cue any ee tc eomen SEER 2 0 
Gi) Wind CRCLAY, Lede cs veces snoclecceeseceleeclessine sloeseudleoslensdeuecchersaaemanie tae ee atemnaenee 2 0 
Ts. ISIC1b GG COSC | escnanos acobed 648566 066000 90060000 dotio0G00 bsoo0d sour wsedeivess Suaralessesacs 48 0 
SUV MO TMESTOM SNe aeccrcaebes cceo tee taemestactnasersteconee seleansseebe taco nustmeeecenes 2 0 
Or MiSamdiy: SHAlee ie jevse. saewuatlosseawetoet dneaccioncoeeleemecalcenee ceca haley aan raaeaas 20 0 
1OMnlbimestoneandimracimesianvlimestome seman daneceeemenesenean enero eeimaces 5 0 
Bed of stream. (See Map XI., No. 25.) 
At other openings of the eoal in this section the seam presents about 
the same measurements as at Mr. Barnhardt’s. The same coal is mined 
along the banks of Fifteen-Mile Creek, in sections 7 and9. In section 1, on 
the land of Lewis Linchcomb, the following geological section was taken : 
Ft. In. 
Wests Sam drocksch heey Pees eee eee ae ceahvak ean sled bee cai ema ata ste 15 0 
2. Shale... ise hete HARE en None Cae ea LPR RE ae Tet hetaan hee ne Ani Ons AUD 
3. Coal, Gea SAIL ese Mose ean es ceenen aut iase Manne S Toa T aa aU aR ete Te ike} 
4, Clay, 68 EIT TS VENI EI Cer Nan ON ine 
5. Coal, IRIS AUTRE R Re CIA SASHES GEN ORAS ES BAN ac hr63,.daodon dichoudos Ib 
Near the south line of the township, in section 7, on Fifteen-Mile Creek, 
I noticed many years ago a thin seam of coal, associated with a group of 
limestones, about forty or fifty feet below the Cumberland seam. The 
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