Hawortu. | Geology of Lead and Zinc Ores. 63 
STONE CITY WELL. 
Reported by BAILEY & WAUGH, drillers. Forwarded by Cou. W. B. STONE, Galena, Kan., 
December 8, 1900. 
MATERIAL. Thickness of 
Commencing at 300 feet. strata. Theva elgoua 
GLAVAS ALS ees a Mapai Nate ate aL s vere ear Bhaene aa cNvahal Sratalanat itll 20 feet. 3820 feet. 
Graves Anil es Hall Cheer ppen er ey eats sore crap yeaah ere nett ao.) TT Byers Sis 
STACK aS Hail eset eee pie Nest eee A A Sn Ua OI a IR eer aR SEU HE Ae a le WS se 340 * 
COLO oe ee he ey ie Tes TUE EIS SER ERCP COSCON RES NE ere Sits En on Ee ey a Stn Chessaleerrains elie aye 
GEAVAS Hale ee SERS GTA TNE Nee Pa ona aiationn ua cimiatontalnee Ghia 12 feet. 353 feet. 
STACKS Ae ee Re et Oe ct irape ett nh ce seyee seine ciel nAC Bain Ne MSIL HAT as 4 Spe 361 “‘ 
COMO M cis ce oicg veto pst aap ARTA a eH MOD SEE eo Ur tg a Reo a TO le 362 
BlackishaleicontainingsaymundiciG@pycite)saeee erica eee cdee- Grn Sal 
iBlacksshalehwibhictreakclotitlint a teeeee nett ee eee teeter Bireee BB 
White flint and gray limestone with streaks of sand................. OAD) 0 396 “‘ 
Gray-mottled flint with showing of lime......................-. sseee- i)  % 496 ~~ 
DEAT SGU) cpccton 5 Gece Scie ete lls Shit eS a RSC ARE RISE a Rae KD) 546“ 
LEAH GOVE) EaVel Tabane ce ean ty hoc eyea eae heel OR ee ICN CIEL RUSTE ROT Tan op ree Pe neat mA) 566 “ 
Flint and cotton rock (decomposed flint ):..............0..-02 eee e ee Opes 576 
LTT Gee Na ee age ENN SN Cc at ay UNS hones os Sails SMR Te ee LS i. 59 ae 
Hint n GEZ IN CLONCIE PRP ae tere aero chee etal) are Ey nie Ney artes Bie 596“ 
Blue flint, lime, and sand (known as bed-rock ).................200-- 20 eae GIR 
Blue flintand gray sand (among mines)............-.--eeeeeeeeeeeees ig iL Gwin 
Lime, very solid at first, becoming thinner in strata, and getting 
SORLEEAWA Cheadle p. Llp ere ere rele eral ataractaie rein achseaant SONS 796 “ 
Hine-grained, hard, white sandstone..............-.-..--++-+++++++s- Ae 800 ~“ 
Hinesorained shardworays Sandstone weaned: Bleue SOSiaen 
Hine-orained shard sbrowni sandstone iwyeeaedeeeeoeeee adie Aa Sie 
Brown sand with openings quite porous in places..................-. 360.5 848“ 
Brown and gray sand in thin strata, filled between with putty-like 
substance, color gray, resembling tale.................00 eee eee e Shick 856 ~*~“ 
FRO EDIRC G10 EEN ep ene ee Re NST ee ue obec SUSU eStore 7 avy Lora noi od avs ses 856 feet. 856 feet. 
WEIR CITY WATER WELL No. 2. 
Reported by A. B. COCKERELL, May 25, 1897. 
Thickness of 
MATERIAL. efamavin, Total depth. 
Soilkan al eler yaar ey rats le ne crap i ibs ates Neat aU UU LD Bea be hae 15 feet. 15 feet. 
ESE WUC SHOT ELEN Shes es Te lererahe ate SLOW Nes PRONG rey net SH or ot a SI SE Sa Oa: 
ST ENES) sic Se Si EO a Ge Re ie Gee es an or TUTTI eR ere Car Geant HOV Gs B08 
COa ER yee ree ey Rimes Mowatt Bomba ties Aah ot aite Ley al LN aleide stil Sore 886 1 
I DSU RO) ER pista res eect ae Cauda len avd Craid Wat barat bt eS Coal gies Woe ae i Ba By" 36 * 
STa Ge Pee eee ere pa an Tt mW ee oie Me licence MUO yw 5 a Ufsy ingh 
COLON E TARe eA Sper Rey EPI pe aR Wetman Hel rly Oe RO lt TN a gv RS ay er 14inches. | 112 “ 2 inches 
1 TREY een Sere es Rye urine here PN] Ue ceed eg vm ra a ee 2 feet. TU ea aa aa 
SIS TOW ER OPAEY Hoey ee hele eee EAD Mim aM aa Mineo We navn gee Wl ake LOOMS DA Oe Nat Ss 
COT recht Pepa te nnd UU oct bo iuniavarn beccuta a hrcta hatin tals even PICT ee Dae 
MITER CLAY Aer Oe Pe a ae ae enti Ne Leh ei Ai UE ok aa Na Does VALS tO aaa eas 
SIEWO ce boo eud Gqee Ob aA cha Oana Gane An Reem nn ae rts 62inms SSO reno Ate 
TUE ONE 15S sone eh PRISER AN eee tote OS etiam ay Ee Sere RoE OY 15005 ABD 5 
Serv ave gal baues 5 sleeper ber ele ae) Oe, Sarton Oat ay tei ye I ean a 40°. * ‘AC OWencernrno tie ae 
GET C Ce tee Oe pee Dene ole CFP gal ec eget lr, SAH Aho 20 hanes AGO Ane te BON ores 
AGS EEN ING 2} ONG a AGG Ales ere sb Le St ee Aa UL ered SRR ES EIT ge ee ed 490 ft. 2in.| 490 feet 2 inches. 
* It is exceedingly probable that the last item, granite, refers to a coarsely crystalline lime- 
stone, which is sometimes called granite in the lead and zine mining district, and which is not 
granite at all, but limestone.—E. H. 
