BELMONT COUNTY. 557 
stone, argillaceous in places. The cement limestone found at Warnock’s 
is a fine looking stone, and to the eye can hardly be distinguished from 
the Parker cement limestone at Barnesville. The analyses by Dr. 
Wormley show great similarity of composition. The analyses of both 
are as follows: 3 
CoMPOSITION OF WARNOCK’S AND PARKER’S CEMENT LIMESTONES. 
Warnock’s. Parker’s. 
SiliCtOU Spa Lbe Tepes nah sence ancicodase nes dtetedelveleesiseleoce shee 30.60 29.80 
Alumina, with trace of sesquioxide of iron .................. 13.00 13.80 
Opp o@MeNie @it 1WOTMYe) Cosedddes boKcn Haabbs boboL ONY eBbBBobse Hooded BubeeHatE 40.60 41.20 
Car OMAabemOmMMACMeSi are seavcces cc csccecctsncess castes ontecojseveees? 15.18 15.36 
99.38 100.16 
There can be scarcely a doubt that the Warnock limestone will make 
a good water-lime. It can be obtained in great quantities near the rail- 
road, and coal for burning could be easily obtained. At Warnock’s 
we heard a report that coal had been found in a well only fifteen or 
twenty feet below the surface. Such a coal would be in the horizon of 
the upper Barnesville seam, which lies from twenty to thirty feet below 
the cement limestone. This coal appears in a tunnel about a mile west 
of Glencoe Station, where it measures three feet in thickness. The sec- 
tion obtained at this point is as follows: 
Ft, In 
Lhe.) RIDES co deSb4 5005 Beale GB aalan BEA SE Ge Ce HIE nn Geo a are Si AR shale Muti pea MS ee Ae ee Rn OH 
2. Coal, blossom only seen, but reported thickmess......cccceccceescoceseees SHO 
SN NOb exposediiss. us. LORS NU HPSS HIER R BU REE BN SOS ORE HAE S BA LEIA I aa 110 0 
ALS TSEMOXGY, LIITCHVEYSRBOTAY 2) Asocu bocogndob caoCHOHUS Gd CHES CCCOBUIECHAGS IES COOCOCE PERSE HE CREM BUnmene 6 0 
emo eM AL MNO ChiPlaT MIMS TOMC Mines sosccccseactesloessectsdiitcsseseaiesanensusises 20 0 
Ge SeuIa liye MNES LOM Cmeernancee seduccen ten uutawy Minis clades lopcaseaesleseenuisagie Saeaisurees cs 3 0 
EM SIND Ove Ueneee ic cap eee natet en ecidtuelnMdsact cats sete claalesecscutelsdedsbesd coseesseoesaecs 1) 
SMR Cee IMM TMMTES TOME ee acus canons ee cieneualcuuualcasslen sat Taal sasha vslooecueeesied see 5 0 
OMe S Ln eA rereererscreeamncrenen cues lewcise sul cueiun sta uvievaeeiviedewel eed Suoerelage dee Weaibaicbiee 1 0 
10. Limestone ....... 2 0 
TUT) 0 STEN) ceicpododdicdOede SOBSE JCCHOBOHOA BOCB NOHO! CUR TEESE GABE RIC HIS ie ee ENE EI tr ara anno 3 0 
TZ}, ULATOS TOR YES (abi S506 COA AE CHOICE CEECA CNIS NGEEE SGOT SAG Cer ee Hane aHiH nies MIF MEE Ib) (6) 
ASO LAW aM SLOMC ener ecu cee secs wens cacasoveecsescedeeeelececece PROB es aSS 2 6 
(AM Oementhimrestomenminsh AVE sr soet le souoesssccsscswasieeelecccteectsteodaue 200 
15. Slaty streak, thin. 
165s Cement limestomeysecond layer: .):.. ss.ceccss cccasscccccscccese cscecccecece es 1 4 
Ne. oh PR CIMT ee insects cou ee ai Lisetatte Ca matgah nghieUnuan 4 0 
18. ot a Sialiymounthivlayeny sec versus cunona eee cna ute an0 
LORS A I ClivgehiMeSLOM CMe een ocaee RL Cann Mie bec wen ne gua anon Mn ace at) ali 4 0 
20 rm ake sale yeep eater ee nao s ys ewer Vella Byes a dace gulasinagai owen cree ceive tices 5 0 
Palen. CKOR ease ts Ob. Gosche poconOO oeeiddo GBC IEE EE BAEC eC ECHIEO SRA REA WTTEHN Bik HiILE Si Ran ie am 3 0 
POE AG loins mentcseecesievecean sae encusmeaWeac tessa cus eseerdes eee weuaaiseasccinaetecersestaccss cece Ono 
(For this section, see Map XIV., No. 8.) 
