566 GEOLOGY OF OHIO. 
mouth of Captina Creek. In section 20, perhaps three miles up Captina 
Creek, the following section was taken on the land of Albert Green: 
Ft. In. 
1. Limestone, somewhat sandy ............c00seccet eocoes SREB NeBR Ren Cee bc ich 10 0 
Dee KCLAY Shae eee es el oth ARE aU lee i aA Re ree) 
3) Nodular limestones circ) ies, VOUT Ueda csi i eg aes a ea a) 
AL OW bite Clay shal eee 2 ull co abuse cauuuaau ale nese tech us en Oa Ret hae ome esaeROO RLU 
De Oa a Sau ee less, oh olebel Weide be lene dee beg Cae IateN CAH n AION CORUS An aneatny sn COnr coerce nee 
ROLE Ted a MN eee AME OMUMUN AUN AS A oy CN Oh. @ 
dale @ onl OU ness 5 10 
‘(Map XIV., No. 20.) 
The coal is reached by a slope of about fifteen feet in vertical descent. 
It is mined at this point only for neighborhood use, and the coal is lifted 
by horse-power. 
On the land of John Owens, section 27, the following section was 
taken: | 
Ft. In. 
1337 SBNAVC 18001 2.65 63 e005 ooensocd codacodda ascdcs oon ob0d04 Eno pop obodap ods060 GonbaadoosoNEs NA) 
Zi NOTEXPOSCHL crouecees lve lececeesstotesteceeeeenene ae aeeeae ceceee ceeces ceeren vo eees 25 0 
Bi ©1121 a ea eR RRMA A NM MRM Lu SN St 
4, Underclay (not measured). | | 
BY NOt exposed ys cscs ite slatsavesssictucus suclemeeaalans Meee an vone surement ditt aaevatueenat 156 0 
Gr Cement mimestONe lens tebasanssededsecsl etait ceee een tectee ntcente ea Om) 
si SEAS TOTS FE Mciciea die MeN, cee mers slots en cearatl ce ce ect ete a atc Ka Sar ava 6 0 
Sit) AIC) C2 8 an An a SAO Me RRB DA eA tr NA Ole cane si ail SAU us A 6 0 
9. Blossom of coal (Cumberland seam). 
HOSS ANE CO ke ea LAU RS NOUS IMSL Rta So EGS ae Bh ad hc ba) 
PLE SAIVE SCORE Tees UU ON SE RUTTEN Sve arate te oe aL TR 10 O 
PDs SOTO Baeie8 nada neces suels ove sete teseawenies enc ananls tus eun ete ctactuamcensccnia ga aneeta tens 8 0 
13. Coal (not measured). 
a V2 Roa) Ei cue A ea gia oe KEI Mae Arent ALK ON Tit a tT 8 aD) 
PHA EAVES TODS eee eee aN Or ee MN Ulu sents ce cia cig SNA atte tata etcea cee ea ete ance OO 
16. Not exposed, but fragments of a cement limestone seam seen near 
THEO D ee TS RAS ee RSA aN EU eS 
Ail ESEOM Claire WON ee ie uecuat LO Sate Saha Wea an Somoualtae ceded 5 0 
AHH TTS aH (eyed aliepae SR MO RPE IO MUM MSA BMT Su a loth 10 0 
DESTIN Coy: 1 Gateee epee ree RR ee a ARON SRN Ag nau A sab enccicd Seabosissodise Oe 2 0 
20. Clay parting se ONG 
22. Interval to bed of Captina Creek, from ....................ssc0eeeee 8 tO 10 0 
(Map XIV., No. 19.) 
The lower coal seam is to be traced from the mouth of Captina Creek 
to a point in the edge of Washington township, where it passes beneath 
the bed of the stream. It is every where low, and is perhaps as high 
above the creek at Mr. Owens’s bank as at any other point. The seam 
