MONROE COUNTY. 579 
Ft. In 
elem NOISES Meret evans ste cWelonacencs ualuccclescearincbcsseceseces! letaeasie ss nocciseeessces 91) 0 
2A SAN ASTOMEC reseed cc nasetesuosise oosstcess Ar eS Cah cals SOPs iene a 5 0 
TIS SINT Y Sodanda cos taoscc Saeed SABC ORBAN OHH SSEREe CHEE REICES BEAN SP eae EE INT ay rien enti 4 0 
IA Coale (@umiberlandysea)) sneiiqccessieeseicccdaecdlccccocsoslersscuescass|crwsecese nS 
15. Clay, en cOalsplanibsrrsveasersecceecss Hessaauts foeeeoaleusuusns DA 
16. Coal, % TS Ae aati icy tee rs USD NO RR et Oo SND 
17. Clay, a PHIL eces over nectar deste cas tetaNsl eel clayeceaeada db emeestivess 0 5 
18. Coal, oh ARI caer ican MUSEO M UAB cuCunusslecrcaecstoses Boaks LOW LO 
19. Underclay. 
(Map XIII., No. 6.) 
The measurements of the lower coal were made at the bank of Stephen 
Evans, where the coal is mined by a drift-way.. This is a good locality 
for finely preserved coal plants. There is by the road-side, as we de- 
scend from the high ground into the valley, a heavy sandrock, twenty 
feet thick (not given in the foregoing section), the place of which is 
twenty or twenty-five feet above the blossom of coal marked No. 8 in 
the section. The thin coal, No. 6, may be directly under the sandstone, 
although not seen at this point. 
On the land of Robert Pope the same seam of coal as that’ mined by 
Mr. Evans is seen, with the following subdivisions: 
19h, Joa, 
COM ereres RENAE eae cial uatulne Ns Ho niitilain ae eile telealiteseasaldaune) sasaes(feee clas 1S 
DEMO LAV gee retctimiurc telus cohuaamevnauclecuscdagatenstetieusauticssaeslsyeoweess ess woes cvsceene 0 4 
SUM Coclleseapter sey ene ne RaSh Nh CRUSE aha WN abate hE ls Get cotoed Gewceaeee veeseneee 0 2 
AME Laaeen nde dortacet eiiseusuecesicesraseans ute sSencs sess seucaaesecessucen subsbdaue-cese aves 0 6 
MOOD pernervcnnearo etn arcan eect eda eu canadian Niwas usa cagodds dey cade sooweeived atece 0 2 
GS ACHE Ny codeall sn A BE are Sue US Ae ne SE en 0 4 
ERO ODI eee ce sealer naiel naan reeRc una vexe se aeasteicanebelesenes Ciuistey daekelsneaoeidicede ds 0 9 
The geological section, including this coal, is seen on Map XIIL., No. 4. 
In the bed-of Sunfish, a little above the water, we find on the land of 
Henry Windland a fine stratum of cement limestone. It is about sev- 
enty-five feet below the Evans seam of coal. The geological section at 
this point is as follows: 
Ft. In. 
1. Coal (Evans seam)—not measured. 
Zi NIOULC RO Se Clesmnsendccpectnnaus Meats nly calcu iaes levee tclech weve n inee osutissin aacelelad aeea ey 61 0 
ebay yd LATION OI) ge Son abchonoeOs SeoSay HACER EE EETS Ee UNA GAT US GUT esa a ML UMM UAE TEA 4 0 
Am a\iaonesianmonicement iinmestonels sees... ee neal LO 
En IAG Pan vaceuee rasan cere ena as KER Cun air, cau LiMn ean Obadalulay ut Lue till 6 0 
6. Limestone ........... So SHOG OC CSO RO HOBUB CEE NOIRE EEE EPS EH SANE A Te tama Leas 1 0 
MEY CLAYS ALC ei anctucer ene eee e rei coiuatice crocs Subeddecuentonueshesuneleueuani sss 2 0 
SMMC CMe NL POPMMASM CS AM MMIIMES LOMO nuuicaucnseeereseiencelusmestnicdinasseeziece 5 0 
5) IETUSTYS HOLS) scoters GS scsoctn CoA ROE A Ce eIHE AN RRA cease uTN NG Se aT 4 0 
(Map XIII., No. 5.)’ 
