476 GEOLOGY OF OHIO. 
of Henry Ross, a mile and a half above the mouth of the stream, shows 
the sandrock as follows: 
1. Heavy, coarse- et SET AKCE R016) 26 dhonaeaden socsedéoa oddace scdeqa6o9 0500 s60tdeRks 25 0 
Zu iohaleniwith coal plan (Say. cc... conv acca omtwue ee nates strate oureel ane Mi nae tae Ee eae a Bn 
ee et iy eM OMNES 3, Se Conk Ise silat Luna ate ta tL eI Ro i © 
He CG Le TET IA Oks cs Uae Uee Bale Dei eel al IRE Og at AC SE ea a NON 1 4 
SO, 0121 PRA SH USEC RMD pee ee eae Nir AR nA SN GOAN nad biota nin Cintas Bodiciad 218 
6; “Intenvalytoubed ot, Big Tum ea ee. ia a gue 0 oo aa 20 0 
(See Map XI., No. 13.) 
Another section, taken higher up Big Run, but within the limits of 
Washington county, shows the stratigraphical position of some limestones 
and of a higher seam of coal : 
Ft. In. 
1. Coal stain or blossom. 
DE INOLIERPOSEG ured celeookd saliatctdaaelen ederee deeee onan ca UMM aE REM Seen yaa ton ea OR 10 0 
SHIT ore XO NUS) 812) Ce ope MIM eRe MNO aAle a unan GG BAA SAAN Ue Misi etiebeeeiee cane pen artame AD) O 
AL, SRNACISIOING) 5.040) boqog eda aural tte aut 0 STEAKS Rag O CIUERE SUED Tata BURST Re eR DO 
Dy SIONS, Jlencbigsooe InEC OS PDE DOE EC FPIcU hopoon Geosea USGLCrBoboEe soodas HoAdottdce GaadGS abodes odooo! LZ © 
Loar Wal aulke\=1 1.0) 0 (= eB Mame AR apeNiC eee Ana ciae ile lumo DUN aI No ee aaa ee i) 
AW WNOBORPOSCC edie hs Te SUL THEN Aa a EAL a Se er ade a 41 0 
oh LLM TONS ISI MOVAVEL, THD J ORME ANRVEAOVESTEENM.csdidas Sdobad sdoocoogbed boqdcd DoaddLse0 odaSH hod000 90 
Oo SIA al fos Seiad sl Mee SiO a UR Nu BRU a ERC AU aS EEO 15 0 
LOFT Butivandiwaite pine stom e aie ea seeseneu ys denae cen nana aa ea ao ae en ane 3 @ 
ley Shales ech ie tye cto sebateties sackmiabeule cual esnit, unre seers 9.08 dpvoNdiede ae sone 25 0 
12. Coal, Coal Run or Cumberland seam (not measured). . 
PSV ONOU CRPOSCC ieee. cache cdee sbi case saceuiecanune os octeaieanatetie acmaieaseeeen nen bvcecd maidens 30. (0 
TA IM eStONe he. cecsseecssecess oe Ech Seb cele Met tahe Lo het nee rn uals ean Fae C cee 2 NiO) BY) 
The two coals are from one hundred and forty to one hundred and fifty 
feet apart. The upper one is doubtless very thin and valueless. It has 
been noticed, however, at one or two other points. It is better developed 
in some other counties. 
On Cat’s Creek the Coal Run or Cumberland seam of coal is seen. The 
following section was taken on the land of G. Brown, two miles above 
the mouth.: 
- maths. Ion 
be) | Buk amd! wih te ‘ina Cgtomeseycow se adsus svatsciameaneacee ene cemenste adn eau (0) 
2a. Sand vi Stal © fee, soe as COM ied nelle gaunt eClit ona a een iar a Ee sett eaaac tates wt 0 
3. Coal and clay eet ea Lek mena eeeiielme nen Ja atk eta elted tale ean tats t ce ARIE i eR 1 @ 
AN Oa es Ue NOUN OS MCSE TRUS RU ire apr tt Lies cna Maen ERE eR ON ea Oa RO i @ 
ome Claygand bituminous shal ecuaeew cence siete eee wan atnen haat enMnee en Cane Ly @ 
GPa C01 BiUM NDI AMRIE EMA LAAs AB eS MRR RR hh a 25 
Ta Cea ee ee cule ates CUAL SAR, LAR, UMIMRC RRR Reng rc 03h): An OM a CD ae aoe an SE te a 6 0 
Si Sandstone and Shales yey pene ake k SOC he Sar eu a cia iin LU Ra eer nt 24 0 
Oc Wilhate lim estome | isioadan iba Gi ens Hee Gia acl inne Masui Narain ta Muara 290 
(See Map XI., No. 15.) 
