BELMONT COUNTY. 563 
18. Coal, with half-inch parting, twenty inches from bottom............... 3 10 
AON MWe dened axenic acta tance Noel senissolssdneNatones es selecisce Seses ceacaceaooen FOR LO 
QO SAMA SLOTS a mera ina Ceneoaiea ea acne ahem AC GLL Wun ue wea sues aber sawed egoe esse mE L ON 
SPIDOREE Snead pea eee eRe RMU NU ethic IUBLLavPa Lee aLloLicaniacn sesise pha euen Gees sleneice saeecus'setuyule |, O 
DIN COBEN a ON ee EI AA Se Set eR AS ear RO Ey 0 3 
DAR NIST INNS) Ls cies! Hg SACO BO a CR OSI AU OSE E GET eT NSCS EE rE ee nL PU aL 3 6 
DAN TEO Oa Mee ea Noe LRT ML Be eee EN eo aueade RE Lae Me ran chee een Rs ily & 
DoW OC lavgeratemmeticacunnnciete oss c ieee er asetcatasecbdlensascidneschorslecesese ss dagdesbeccee 0 4 
AREY CONT SLY NNN RON MEH eR AU SRST STE ORO CEE a Se oy 0 10 
EITM S LOI Open maeri cae saeeaiccesacutlse manslaneseQencetaiset st cieeweveultcsecanesdeceesws ¢ 0 
28. Cement limestone ......... ...- SRA 4 MS 6 6 
2OMMluimestone watluinmtenstratiiied: Claye:.c.ccssasssescceseescerincs se seceoeisseese § 6 
SMMC Lay eeveres cae costessisceoes PUM E SEEM AUN ete eagea wees scciedelteoiaseate ERAS EU 74 (0) 
SiMe T SL Op YIA CSUOM Game rstonmueen Ae, dati ven sultecedcwawicelscise sew’ OER RRR ARR SG 2 0 
SMM OLIOROSE Uieses atuccnwctsie ast uiecerscloat suajcoesiohea) siececieceeesivadeesganeuelceet ee 3 0 
Sen © Oa liane ue menu ante Ona Lagi LuCuati ss teat aWilds easfuet/sooinb seve seeeslesesiseendeasiceness'4 (O! LO 
SAMMI IRL CLV eeet aeecceeeaaets Areas seties nose eesivenewersctien cease ssuetpecussevectosneedoeeeeariiel UO 
S SMO ITAVE SLOW Cpuee ea saterute nue ciane Nobis tjevcitenceaccslact otalsceicssava se ciensiveniaesivesieeeny Oey LO 
S GME NO LEE XD OSE Cem nere at emu eregn tO anne Van luaies seuellweviodseveneedes swctsemncl 
Mm OO (se LictiraS CAIN) Maccumnt cect secu sissies. ioosdes stslace sseisersevecsiteesenoss «surest GO 
(Map XIV., No. 14.) 
In this section only one seam of sandstone was seen, viz., the one six- 
teen feet thick under the upper coal. The whole hill is made up of 
layers of limestone, with interstratified clays and shales. This is in re- 
markable contrast with the formation over the equivalent of the Bellair 
coal at Pomeroy, where in several hundred feet of strata there was not 
seen a single well-defined stratum of limestone. Directly over the coal 
at Pomeroy are seventy feet-of coarse sandrock. This shows entirely dif- 
ferent conditions of deposition. 
There are doubtless many more seams of limestone higher in the 
hills at Bellair, but they were not exposed. Samples of the cement lime- 
stone were furnished by Cel. Poorman for analysis by Prof. Wormley. 
Nos. 1, 2, and 3 were taken from the lower, and 4, 5, and 6 from the 
upper seam : 
INGUIN eNO wan NOWS al, NOT. EENOs Dl ENO 6: 
Silicious matter........0..... 19.50 19.60 20.80 28.30 36.60 25.60 
Alumina, with iron......... 11.60 9.80 3.20 _ 3.70 4.02 4.60 
Carbonate of lime.......... 42.70 48.90. 51.80 38.80 37.40 47.20 
gs magnesia... 25.50 21.18 23.91 28.38 Zits 22.30 
SSS ees 
Matalst seelccswcst cues 99.30 99.38 99.71 99.18 99.20 99.70 
Mr. Isaac Booth is successfully manufacturing lime from the cement 
stone. The lime is commended by those who have used it. There is no 
limit to the supply. 
