Show V An VOL Devoted OF SECTIONS WINAMUCK permission MINE to present we read our workings The THE of the confined to between the the line and AND BED In the STRATA of many where 1 ora a the gether the with extracts mine by Lake Salt of I learning it will of J made of describe to of features which in district in form ores or thin intervals portion of of shale of and lying of a contact by called as devonian of the formations the of Mountain mile of the beds made found is of up different the found having reason the porphyries this of presence the occupying Second veins Third quartzite tween roof It not the of true It bed-vein’ a conformable true at dip indication if but we sure on summit by the of curvature of the the away yon as shown direc the sum mit of which denuding in the the the of has into we at au been effects of lode posi carried the accompanying the true Efimns course of bo the an tho Angles Right at Longitudinal' Axis to for de fling the le and denuding The canyon back of lode obliquely with together away country dominating the of portion a ho the by tions I No Section the to It heaval hand country in can the the hill lower is bo not the as of of the you the fault a rock organized bridge as anticlinal tunnel and The great canyon go also is fault this but explorations at the but southwest shown as indications is that are base of becomes the much towards bill the which of yet not as near as Gold it Only vein next variable all the other New are being put down of sand of than lime sedi mineral when favorable for powerful lead found are proportions beds to up Silurian formations the chemical the are long action the In but curved and who sink will handy ia bo in stratum the of The peculiar rock both follow al have con and 4 curved above strata ing effects lodo located of of the low noted so fect de ore as to deposits to mine the is found prising different in those the and canyons su occur which was method I by and hut has been good to it and that imper good command of the it coked for all railroad with coking of Tete as the was sufficiently propor trade San coal so the sample fine a which had we furnaces not Nevada only it the also ravines positions of along its points capper) Babfoot owing coke doubtless would ar quantities week purposes facilities so works (pyrite’ and large Creek nevertheless home denud are iron nearly not practical in of examining Conrudlsville country the found reduction past Birch from coke Although out certainty bimilar very at hi the traced is of bodies largo success the pleasure shale until curvatures vein - the follow to and with Winamuck tho is ore per fortunate Joseph During method sure carefully be bed show only the its the often synclinal claim out it or appearances must posits anticlinal assays be if the in boy3 the will ‘Mundic’ beta- I there wish distorted bde all differently occurs are then the tracing is to Fascce some an sulphide waa them increasing there city to fouzr you Sir by It to they and senide position true of sent made grsde now mountain I bulk one are depth a ere shown are the and bo At- from rcccmmcnded low even months obtained they the into sul brought some sad copper engaged for those bedn or of oentage pros would of they e re Shoe I untUrstand I in have which of of ha already has done carbonates lead tested it six been specimens period a about has Edward beem had have I have beds the into and foldings length often it Clayton Considerable tunnel the themselves the in Drapersville Mr caibonate found trac along there out places many of tracing lode When devonian conditions producing in period cretaceous the carboniferous tinued and and the words and in lixes Dis District Li and the the feet or strata show E situatsd with (as a iitereept of a designate prevailing the sedimentary motal-bcaring been difficulty more which a should called copper commencement In and by quantities older sand contain name rock country strata Star District The- : prospectors) drifting careful a of the seen is recently matter the cf should expense eS edges straight silicious or the a cen of Draperville oxides during deep tolerably it tho in the in J have quite toa to of Reveille- have I as dewn locators 'P- going the the of sand more to When composed is Silver in is they possible dia-ama crossings is rock mentary in windlass the called The sand than been has fault when limestone calcareous be composition their in lime with also ing coi call we before quan it when hut shale there shale a ®re reason barren clas- be in of must phides ckm“'ilL to this Recorder pecting pre-1 name call wo ff may ths jerceptibie so may when stones the than of right tne the or up slip or on of they stones role shale limestone shalcy the lime more icgbt at of approximately section near center by to fault greater slip extent determined in flank above level The the shows This next the longitudinal axis eastern or with met beds also and lode i associated and lode tains of curvature tho- shows 2 a a iu lime calcareous lim gives instance for containing tities As mineral beds bed sec together mtoj the the sartor day which the carried shown as ia portion the across and curvature the of efforts erosive cut have section longitudinal the in shown f 1 the true-strata-vein Handy south of rights ings such called or Gazette cently think gress Curvature- Anticlinal of forr side- District milts Con of surface Section neaily In either in Ore Mining to as of degrees drift Tho bods Cbpper system about of the anticlinal an define move north supposed a and down pitches or depos of he ex both generally Nevada southern with at course and of and in strata one bclk small may Utah trict the The curvature course quartzite curve as occupies flank eastern the that its mine Winamuck The in folded out laws ture as and and ments curva a the of trace the and stratum along in certain position the point given any tion of indicator to strike les exam vein that on the vein on gash-veins fissure fissurs deposit of line Good' tbe hut angles curvatures shale order hori axis is the a synclinal in tho is of inci not strata the the for look must find and anticlinal i3 continuity its of that strike its pro- lads the bo may with comply the require two strata the of point given any tion in foldings the hence enclosed is it the disturbances upheaval tho to all to other and distortions which conform must lode dent a or follows therefore it of dip examine to thing quartzite or case along thirty has found between contact of the as be tral lodo ideal it roof shale to first the lode foot-wall being the it therefore is and line This be'eause a silicions according shale and beds shale beds line contact a partakes These are distance a along connection their become they short oh gal gle the rock alid hanging-wall the or may calcareous or argillaceous be and shale that deposits ore found is ore lime tween Thus constituents it to country lode faot-wdll quartzite dip and the of ein Contact-v a a curve bed shale n the cross-cuts and beoause strike in the that characteristic Win according-to beds of system spurs of making a distance main tho of and stratification in gash-veins the shall of liable left it of is of beds or respect cross to de or is inoro- cutting ingles cases I paper discussion the to right and out a silk-ions line bat them short them of lode & right found or and bedding lines often rock daik of hard or tho crossing only sides a this gaslnvein-a' tend and cheapest it this any contact’ ‘ a bed-vein is strata or both their of the classify then myself bed-vein gradations In value en is west is be to We the imperceptible coniine each into its tracirg longitudi- the at by value its them of one standard Winamuck bedding richness and any of measure commercial The in contained of classes quantity of blend often char of method proving con These best and ridge relat the different these The ore the forming discuss mind in bear summit nal to likely is or line the on limestone sandstone almost by other cov slatey anti zontal quartzite wall necessary deposits ore be lodes shale he thus a an which it merits ive not the syneitic the the and hanging or is shale ground may point initial schist shale beds acteristic commencement the to and glomerate the gneisoid as quartzite schist up following narrows lode the the dykes the contact as and foot-wall the tieing in veins fissure Fourth porphyry is between porphyry the tbe the from space sfieh terials sufficiently is tbe at that closes strata or veins the country rock forming bed as Winamuck it the are dis covered Mine composing district: strata Canyon Bingham Across at strata the veins that have line clinal and true as the contact as quartzite the the known generally is of the broken in occur between beds as what and claim must You that Section value any strata beds deposits Ore the of Ideal the that ui ore stead Eureka country particular character the the of at vortical (geologically) of to In the following of or they all all lode igneous disturbances the folded upheaved sedimentary the of origin the suggests of breaks kind offsets ofi is very ono line couBse more 1 Winamuck the ering district the dyke3 these of and southern of portions the deposit crossing curve especially its cf know certainty vein or of to nrother gen beds or tho distance great across are steep the it case the limestone of or the as where point follow any beds deposits situation to break series prospect with Dix cover per hornblend are the in numerous to miner is or bedding rock both say lime continuity this they to very slatey bed country bedq up some certain take of District Tbe practi a and Wina lode on de faults and and They sixty the is in case iu from approaching Tintic color to that localities impure an posit facts 1 o Com pany at north-west to portant for in of im of of tilted A in not beds class nearly shall most The the tbe is come under discussion level muck north of breaks the seen south-western First dip for that been gray with the have- mine of class found line the deposits Fortunately and strata strike dioritic are and the twenty of from the formation erally the on particular shale or This angles on the a on the of ory in lower shale two beds be may lode beds different composed are cases the contact character walk or further like quartzite especial when nearly mine lime ore-bod appear theWinamuck these foldings of from of All upheaved and many dykes have on side and the under will zones hundred two to general a two or irregular south-west grees rock ridges the course south-western one dislocations In The the shale of the important between Buck tracing of are one 15 geological la r curve shale in occur f rule tho the vesns is the certain of and number) Strata-Veins and call to line of it thiH follow lime line shale roof that found this of the the in only is-to Bhale contact-vein' wish I fact always is with and shale a tbe of underneath foot-wall to beds on lime or invariably lode ma- ore ‘bed-vein’ a attention alter found is between stone Itocky an if therefore car plateau and Sierra there ranges and great and practi is between nation the well as silunan the boniferous point engineer and by student all In along bight one-fourth miner scientific curves deposits narrow a are cal consideration of beds that position in conforming thin with and penetrates east five to observable are varying angles large the one in present large the separating have been south-east now at line features meet often we ‘bed These peculiar some worthy strati the or rock country the canyon occur hundred In from beds numerous J5 blue have the rock country the to prevailing tbe are the to parallel secondary is that projecting of veins’ conformable beds strata are the crosses is thickness great one district the thickness in east of apart feet limestone the strata seams beds at hundred is about canyon strata gravel a opposite and then south creek through hill curves are structure sandstone vitreous or beds with feet geological prevailing quartzite of the in deposits- ore south-west The of and line lode found tbe Nevada bods description (See course sections limestone workings Thence it found ing the the and fication course the Utah mineral the beds Winamuck of some the of passes above mine rock the it the and clearly important this side west the that see west or of ex wealth metalic its of method left until of object the will you general following By illustrat horizontal curvature line blue not the the on it the tbe of structure with to plan indicates the The tunnel ground the lode incloses studied carefully comprehend to the the lower following Clayton E practical necessary of map or of general ation on ed to report a and lode character be the and utilizing and the fully shown the westerly most order In in of of character the ploring formed is Professor Winnmuck the line City position the strata the from examined have of mine Winamuck ths which of cross-section curvature anticlinal on and longitudinal of sedimentary composing In districts of NO crystalization the districts Utah of Interests 1873 6 consequent VEINS mining the Gazette the Material other and DECEMBER UTAH (For ground of croppings of CITY been have 6trip Commercial Mining LAKE mine fan-like the to SALT I CEOLOCICAL By Journal Illustrated Coal mond fields there at of pey discovered South bag of in the Africa and 20 pounds is dia sold V |