Show 17 January f 187 4-l UTAH THE t MINING GAZETTE 163 JfaTWglCY LETTER SAN FROM From the Pioelio JUAN ent f place above-named red and Dec after City mus We days about of of forty distance a fifty and Ani of least is again have road a no We day next got tor but could not send to carry man to the get you a opera here from things to Tanguich day and on the fifth in the yard of to where we arrived pitched our camp friend Wm Proctor our under are rendered We that of possessed mals some at any such they refused reason price best known although received of first store out goods could of all we first bo:ses could until which way fo Little of Kanab where settlement made small a this thiugs for want of which tion reasonable rea We when we where is two miles into comes seven miles of cast due one of march over scaling tins bluffs knee until looking down ledge of pure canyon deep would we 500 1000 or nnl no alternative we must wend for descend the to had would be by down or and bluff less than 25 pack not leased from bit of eating it his for So his again long as on work which and ready for it another this you the is I explanation the descent down that a head his the and for feet rock only were and and distance obliged desolate worthless for to jack a offer was to to place covered unable to a our divided and party in to charac nature a made being shoes that we broken this too poor suffi live make me in a it pres of resumed was then little a north as landmarks a and east went we reached the so then parties trail they and follow idiots all days that it that laid we mothers most we all we for the the kind madeno one was near first time and guide ered visible hoping but no although Next journey oilr follow up the the find as and river the the where could running day one Indian trails crossing seen north and south be to find for Indian a an discov could be aborigine fresh Indian this day again we all time river until we signs were started agreeing reached on to the suffi with up by pasto the clays vary and are from the derived indicating which the in of the plainly for felspatliic granite the rocks of and gran on large a in of minerals other of iu kaolin of or silex from and some such present beds extensive result iron quartz oxide the beds vast pure with scale the as tertiary we for- in New Jersey Virginia mation as and South Carolina proceeding further to state Before the function of what parts component granite which mica let cates of ification gin and of which ble are to say a to first are the the into tinct classes cessive posed four different plutonic Each has periods that all originated It granites classes origin and of crust accessi All rocks second aqueous these ac The volcanic fourth at ori is great slaty the four dis many suc formerly was sup together with the strata crystaline or metamorphic were first and were called formed therefore the primitive rocks and that aqueous and in micaceous marble statuary in and if is nature of with All con soda such as granitic causes either the France of down The either glacial or nil or air become found in such a maladie gradually may dit wear temperature of by or many Ha variation action al however through it rock by more mechanical atmospheric rock called ho the the and gradually Broguiard granitic same decomposition which chemical or tho or the regards rock action and pipe contain tho to fine marl of as some existence their the very common Stourbridge is claystone alumina iii very kaolin called composition of condition yranite' finest others aud in horn tho and slate roofing in schists found has for many ages disintegrated and as some are clay clay through stratified which fine loam of met by called are schists schists Tho is deposits clay owe various kinds of granites which con the plutonic family supposed are of igneous nnd nqueo-igneous ori to bo gin and have bcon under formed great at in tho depth a considerable pressuro congelation of the rock gradually water within pro split and expnusion In ducing a a itself chemical poiut water may produce a powerful metamorphosis as it contains under a certain weight of incum earth or bent ocean Like the lava of volcanoes they have been melted and afterwards cooled but with and crystalized extreme conditions different slowness and under carbonic from water those air differ from by tbeir crystaline absence line mica inconsiderable form rocks schist clay like sand or ganic bodies granite as ponding of these into sedimentary to called maybe are It strata exchanged an havo crystaline structure highly bo may proved that mica tho is schist and has tex new for at even with n some bodies tho All been the organic its of arc attributable in or other gneiss and the their and tlie ture at lowest place surface in tho and the stated two year of in tho nearly dients from have felspar wo anorthite lime felspar a the and lime soda lime spar while gopite tho the others felspar felspar tho orthoclase mica group albite a muscovite about iu labradorite potash such as biotite the a fel felspar the phlo lepidolite and twenty of per cent and about thirty per cent mag tbeir compositions Felspar adularia amazonstone and lalrado- $01500000 is ample supply but there to our is of made several in and the therefore to easy the State secured operations locality the of has comparatively such no establishment the sections is tainly last sugar consumption at which ail enterprise of confidence capitalists It is contained soda in others of It is State own favoring a sugar mill established at Santa Eosa shortly money cured'for alkali oligoclase a of to events mention aud sili a instance the tho contain alumina like soda those for and ingre another -and somewhat differing nesia felspar proportions equal alumina of cato a and ingredients contain silicate of form of that the $20 mentioned factories is of necessities stated will be that so pounds tho hauling least at seen factories other while acre of from yields and placed it that so laud estimated is is beets at acre an 1500000 article pounds for room already as also contain alkaline some likewise mica consists of some in the the two the the The to for fully company profit a The of tlie $10 is realizes off already producing of bo and grower farmers near the ton tons mill possesses industry dispose a to account the to The to is on this been both while it as has Alameda stated Cruz’ Yoimg cost in is it facilities fifteen turned superposi granite mica named last alumina alumina in of attention capitalists Santa raise acre the composition being quartz to $150 to farmer tion The tha manufacture of Alvarado factory they the to sedi granite of the on Street sugar degree manufacturer maximuin distinguished order while granite latter profitableness about forms and struc and tlio occupy fossil from built beet at removed £350 or assumed a This which plutonic unaltered the the Forty-Eighth Fiftieth large other Alvarado crystaline formations rocks which havo other the hypo-aqueous are not granite to words to which are aud altered rocks from the volcanic and the and that mentary rocks tho the very some equally been Avenue of of the supeiior raising beets tiie sometimes ages newer than in called secondary and must strata we fer that peculiarity must exist which gneiss a Btreet near and promises soon different is is from north Forty-Second the demonstrated rocks there Thirty-First at agriculturists county obliterated crystaline enlisting nnd hornblende of vestige every the demon and to tho enterprise become soon in this At prominent State tv one pres erected ent but two of these factories are the in tho State Sacramento one near fossiliferous or the MANUFACTURE subject from sub earthy schist of lighter mm Street has caps SUGAR The distance from their contact granite hard clays containing vegetable or other into been turned slate remains have called in Tenth above rock and by a assume turo and li extending rock quarried side oast gneiss sub action paj’t upper Sixtieth to west Btreet deposited sediment altered so tLe beginning west the decomposing granitic York New City m seeil iu granite materials of form granitic of silicate would corres The originally water in but were subsequently heat us to terranean from lodge a pebbles formations were the usual the may piuticulatly to the striking er y Croton aqueduct and Fifth Avenue other stratified strata of upon decom from away separation after deposited schist which beds and bo east of traces or no often crystaline ns divided silex Btreet of no washed be act the silex separated by former being so rocks guitt free be soon strations of while the gneiss tho of contain and and yet last the origin that They scoria or the than heavier clay is crysta chloride slate doubtful more three classes and fourth comprising the aiul is but probably felspar rock and the would depth the granitic alumina sequently of would it in of not seas stratified or the of unable beneath or posing open rocks acid alkalies the and breccias eruptions on of products metamorphic rocks the structure tufa surface and lo The in volcanic of the are earth’s lit cooling bodies they alone the their char their sili a stitute sili class of some formations however are is and some contain lime iron kalies soda and potash' the which col manganese gem alumina which chemical re all nnd being beautiful a silicates or latter potash silicate porphyries iron quality and texture the other varieties are organic clays three of topaz extensive highly comprehend in rocks of of less or the oxides Clay the the earth’s portion observation tbeir metamorphic to smftll human cording the blende class next destitute the crystaline cluded gneiss felspar aluminous words on tho according meaning age but quartz the few a rocks divided third in occupy me the are the the plutonic certain and amorphic and often exposure required was of which cracks water with sometimes of silicated kneaded mud or remains clay mixed little most of party Here the our were to the best undecided route as so we guide and agreed to lay over a day our horses and Foss took their best and Mr the of the along base country a scoured small mountain range lying south of the river some aud up of rocks gneissoid and porphyry regions where these rocks have for mis where blame the our alike camped river to minerals mixture of posossess evidence time and ing the by the fourth with and division pro of the and decomposed sight instance this Iho by marks above Iu party our the footprints of traveling the of the equal one mud and much they by pumico umber and earth ocher of alumina compounds most of them contain also a siderable portion of water aud lime comprise volcanic more are world alumina for silica vol differ etc and fuller’s loam sodium the chemical ob of in cate aud fluoride of The great of family zeolites which are composed of hydrous silicates and represent a very interesting class of minerals all are Etna craters which granites aqueous nearly are to volcanic acters most wearing down of rocks rain drop impressions or marks itic of in but others share After out Most party are got ever us is near t’ae a like tho slate aluminum The lava are nature and of mateiial the marl ored ravines such as Vesuvius of rocks common the These composition than the tho but stands of from plutonic and clay decomposition mostly contained over curse when their iu see long five strike ever will flowed have gibbsite result which rock structure in application parts many furnishes of perpendicular or found are useful aluminum to Common lava porous dikes volcanic the and detect and silica of exported Btone sienna active of fluoride a is The basaltic aud other active volcanoes rocks forming tho rocks of Btaffn and of Giants’ they Causeway are all volcanic have in tbeir mineral composition much resemblance to the lavas which are known alumina containing least fashioned nothing more decomposition hear then in at wo iu by tho which aluminous earth called is the south did hand few long-looked we such crystals is the companion be to water as we ripple Ban ed in less than two day counting one Bhoukl any other Tho Franklin about speaking any ductility greatly were going in is with the cient night we also start were that of sight get lands fog a or fine very in colors the arts Clay flint or feed remainder the iu of of is compounds or ' and arts de more and emerald oxygenated the oxide cut much and of craters fissures can scoria)) of kinds Theophras At "Mos material in the and magnesia minerals about traveling high dense finally we the and with our tactics takes steep inducment rabbit this way horse miles over at in up on have been country the early an is camp littlo direc and has a peculiar earthy odor and the mineral upon when breathed which differs but little shale from clay is extremely infusible and insoluble and miles we but we rested the rained most of It day of but making horses 100 where miles Wheeler theriveras passed wo such the travel to in or hold a on about right the peculiar of when us wished tli$y had never seen to have been made supposed stand man i3 a shall colored would the country cient get a If Uncle Samuel to hair overtook night to vLich emery hardness &i 1 in minerals silex north in party persisted our until we traveled about thirty the portions originally brought from was but is now extensively Asia Minor min in Massachusetts Alu ed at Chester number mina is also contained m a vast of was apd following to ho fearfully so it which admit of is to places either that it would in it by the corks The bluff smooth rock would make the impossible of the other many man’s ter say re sommerset that will east their by and from of all it Wheeler the here little a solid it keep is truth of as is double of footprints all cats and a not fields to went his pack put he as did think may tell ho and up said owner was but dead a over He feet for jumped he over day them river Had the Juan kept we determined when we left the upon course diamond fields we would have accomplish like out old ed without water and with morning we made Next after found water and for noth stairs ruby the turned they until is headlong went rock over of next a century minerals liyl mineral alumina was brought The are alumina the of ponies our steps down can run up or and mule walked one goat: well of left wo ponies tho and rose stellated weighing 30 tons sapphire of which Cal gives and Canada both furnish fine corundum sup or red and United States the 53 red diaspore tho of resembling sapphires first are with and find for results The the manufactures mineral cryolite from Greenland which is an illuminate but not silica combined with or are ami the are of and allied speci crystal one specimens hu mule out gave and the Wheeler another and Lieut miles south much as alongside at ifornia of plenty a walls served granites at furnishes Amity New Pennsylvania atUnion Newton Georgia our pink occurs of its vast which — fire rocks unstratified they times of action These erosions and mains corun mineral The oxygen and ruby are the the alumina first of the heat action crystaline York mined now the the alu consists and North Carolina of extensive quarry ville as possess in viewed blue following old their in the decomposition strictly and is Here sand trained pair a other the keeping in some shelving I in not rock up many cut anywhere perfanned up they in be animals llice’s Dan assist not to had it Jersey as in understood that would generally we go in an easterly direction as near ns prac ticable which we did for about 15 miles ten were so high impossible to as paity better a they when of New are in them where five to piling and horses Why feet by made steps the to assist places steps etone Avails can that one found still down feet been have ascend them or would been we two from by but us had in us found here be When along way our to posed he both barely is offered is best the daces Many trail dim a and the into they of other localities useful left some deep over where the by fossils mostly 37 pure corundum crystals we for lest sand in hard It of If Pliny and an split a Jay’s ‘I’d and sapphire and color our to THE metal diamond tus feed began the pieces was which where TO nature ruins little our animals threatened all put in to opalescence bickerings little on one guide Our ourselves feet sandstone the path this zig-zag walls pcrperidicular every find Here proceed it di below visible that either through TG animals mor and the going but feed good up in been men and shape and weary cliff wading going 23 where was in modern or hut colors of chrome and polished has the aud is a fine aqua marina gem number of minerals composed alumina of for beryl alumina when of A canoes the extremely an aluminum blue a red rubies of number a of oxide being gravity many deChelly IMo five about American of ancient water of furnishing stone blue forms silicate a the of colored first name be volcanoes and streams of lava may traced from high summits 'or cones into and earthquakes have adjoining valleys from vertical axis tion of the they called star star are rubies which known were good fields highest the CLAY Scientific occurs is precious gems represenatives know with importance at the week THE the next percent plenty diamond the fic can built to these tlio is mineral of trail myself of next FROM ranking superstitious pretty from game the of distance a done for upon one to the modern and they perfect are composed and ashes similar to those sand to It minum which dum In who a at lying Alumina rocks valleys pretend ascending men rations was learned for out took I From in The to days’ in by produced (whereby SAPPHIRE made the any dotted so thing sume company ac and precipitous as of is not on quite had of the rock then that much so hard as into the Here a on without any serious stream Next morning we again took rection You ford and fearful formed these look time ALUMINA seems been in good a camp two hunting out the latter aque uon-nietaliferous of The silicates are the whether The to had structures country next to it had have -was gathered the on the going situated from camped and out this as while concluded left it who water The from this at almost send over three or to proposition Nothing pass except what was boys any crossed by a and ornamental ultramarine an alumina this uu marine lazuli is of blue genus phosphate instead of a silicate of alumina while another inter esting mineral called wavellite contains for and stratified lapis silicate a polished and cut the the natural turquoise one color but is a water of is ornamental form likewise garnet when so alumina The volcanic rocks those which are have been produced at nr near the surface less going We a this but if Indians of visit Colorado the against Persons 1 at as and and lay range the the names polished the alumina gem a mations void of volcanic west of these aud water volcanic ancient country pass leading sedi a cover surface than action as subterranean the most part very liver we discontent not the of aud fresh not Juan mountains o’clock river such the the our found the from the adopted nnd ous metftliferous from were supposed — be two peaks miles built to fortify were the attacks of enemies We we miles forty-five as of low some could they if holes holes port trail of a tackle this to level were of up and this Ban they unless the same task of beneath built house the 125 cave are that however counted seven found what look Small villages whole but the on We a the said of north hours come keeping be a Some team this him block and more open ourselves of the terminus the in as by to to sandstone head the stiatified mouth hoist by him liver the called fossiliferous by can get also are or produced say this the up of found out with look up people grow looked broken pottery generally found of same miles trees down erecting of in rocks We have mations me never to high Near suffi four-horse here used leave let the of organic origin the especially some they called the stratifiod limestones are rocks meaning strata which have been this diffi very get ydu can get you wall feet south side of ed about one was made to temple from a storm The roof must living now information no The very about at in dread road is of the say Pahi crossing higher up on We crossed ferry dangerous sand half a them which and sometimes ing on thirty ferry forty Ute about is line To had distant Lee’s the and dreaded cident go give the Johnson’s Pahirea the eleventh day eastern bank of feats we the of and day the feet that party to there from in town our leading settlement Colorado Tahirea than the who at walls cement used dians kept over at Johnson’s one day started for the Tahirea and name this a laid almost mouth to Tokersville the road the Mormon traveled Mormon then unless 1000 is can down or Now a un being a mortar looked as without lime The sand were supplied by him prices South of here world cave great you following by head further the built was came of of it when minerals y - rite were would iu ruau‘ rura LivvdAi m part of the earth’s they of consist chiefly any others me chanical deposits such ns pebbles sand aud mud but are partly of chemical nnd over of secondary if flrfcn fiiri afterwards super rank therefore order of time The rocks and aqueous mentary MftiSi larger near banks you once horse surface above feet days Along or some other power coal can be seen cropping out which One nnd one house cistern such as themselves 100 thousands wall the this built to three that we streim until The until the sized imposed as ten Mancus us east near miles but where and stream perpendicular 500 the see it that a canyon ern through the drive cave and large these all our many many inconveniences too numerous to men on our suffered have would the and often the and City to been of of road place the have prospecting we not found a Had for age in to shelter shelter a of 50 rock Many in like ed by the hanging miles goods He near its houses examined houses The been broken rooms up found a store we clever gentleman ask could it the south seventy a by Mr Johnson had the best assortment of found outside of Pioche everything hand almost party we they caught nearly about llanch Johnson’s feet high we overtook on leaving Pioche after seventh day went from Panguieli We and only so previous was dry is a good volcanic and first which pluce a here out valleys to room we staple from in Lake Balt the as we enough their thing! right kind preservation of we cave mammoth the of down their dollars days it the to were some of five no find to the Maucus ltio high with weigh the are yon sheep to trail they them many tli8 large had get of which num found kinds some party A to such got bought time the where they but nearly they so the expected Parowan at them as state around it could find — saw generally cient that hotel We ruins der a at for us— cult the mines the turning from an almost direct north rough know a travelers very stream much very kind of Bweet begin to we ancient towns by level for paid we those good in the a themselves from I us a some they of and where is of rock ani tired pounds 30 are we they as for most prices mentioned country for sell to if very good cakes sweet by hulls batter a which and the its to reaching followed up the head which took We corn rocks or give little a of of it on usual ns we very herds follow chopped had crossed two San Juan where from its mouth — the be fine raise say with to of lodges in a and two Here com good says our to the party our outfit to it Parowan a little late good accommodations entered best to the meet then cross trail erly course reached can width in found their the broader— first we it river mile a we separate to ruins con them we told of and some tired were reached We lame ber for feed which animals our refused they as ing not good in comes along take him only such thiugs them stranger asked due are of requirements command where the in these least at after people all the flat steaming hot from rock which they were baked In These upon dians’ also make a good blanket very and durable strong but those I warm although they were coarse saw can make some very fine ones” We bought little of for them which paid a corn we friendly no half means baked good them Summit a little of west Parowan conclusion the we favors of miles that with book a six to came sideration Christians ply we people the about town have but us for feelings whom for obligations many for cakes I consequently We hired telegram our in mix and is enough eight Animus But we I country taxes ttle 1 a by it do we are bed of as the posessed goats They and bread the past - unable out office half about was lady) (a I third the on telegraph the morning o’clock a Taiwan to to went I from miles they meal do control from and means travel never which circumstances over should compel me to unless so of will I that 50 sheep and and grind thep keep at beginning now commence our journey and give you a description the which to say of the route we traveled will square this 1 friendly I miles the of exempted to get yons begin rods to from two nnd here is where Navnjos whom hund one journey traveled the miles wantit About at me south-east hundred seven 1873 finds tedious a have 11 about and miles twenty 100 should time Record Tiekka Amaeella Fkiend Dolman:— This of There State be is se cer better of suited for tho 'establishment a sugar from mill than our The country own which it would draw its raw material is unsurpassed ing it mill to and are facilities the cheap and for easy bring There of important advantage a sit the which mill products from uation can be forwarded to any section of the State and conveniently as cheaply or the world other location which could from any as is be then the named-— Vallejo Chronicle |