Arizona weekly citizen., 1883-05-26
Gnnshf-


 The mil bull lin. is 4izsi fe ct, and is, in every respe.. su5stan.ial structure. The machinery is all ot the best quality, and ombines the latest improvements. Evcythiu in and about the mill is b constructed and adjusted as td rsnder.he greatest pos sible security anl durability, and at ile same time Co aciiate tle work of handling ths ore andths pulp with Jae utmost ec uomy;u lbor.
 Witl skilled management ihe re- duclng capacity a th, mil should not be less 'han for;yei- tons per day.
 The ecent ch an@ D ,he manage ment mH cause sOmt delay, otlerWise She mil would have hen Iu successful operation not later than the first of June.
 The Wfer supply Is ample for all requirements ln the amp, and seems now Co 1e aexhaustiJh.
 All tne uhle recent developments in tine mines lre such as Co apparently justify ,.e oiuiou tha;the mill can be furnished wil fifty tons of ore per day from the deeEst workings.
 At the npicm uf tue Baker Shaft. three hundred tnd forty feet deep. there IS exposed y'l of absolutely free mill ing ore oi higir grade than any found elsewhere m q mIues. This ore body IS not yet suiiicNtiy developed to place its permanency uOug ;ue things that are matters ni pltive knowledge, but there ls every evidence, known iu science and In mltug expericrce, of fts . being a couuuliou Of a tfua fssu-e ! vein, the deyelopeuts iu which have . thus far proven 1t q be more uniform . Tn width and peTsIaut in extent aIouq . its course than any Der ore body that ever came under my ,ersoual observa- uon. Besides, thus [ 1t has uniformly improved m qualItyls milling ore as well as m richness The truthsuluess of my prediction m r first report of August, l>e2, that l.h depth the refractory elements ItHc ore womb disappear, has, by alsuaseluept de velopmeuts, been susiueJ. and my opinions have been -agtheueL and confirmed by Facts. Eeyei run from the Baker Shaft north iute Silver Girl vein. begins at g point inc shaf. tvo hundred and seven feet how the sur face, and connects with incline air. shaft two hundred and siy-thrse feet distant. This level is m c rEa entire length, the vein averagi. abaut four and oue-half feet thick T, walls an6 the ceological characteris,s are tbe most favorable known for ,rmsuenf-- and richness.
 The south level, starting tbe same lepth from the Baker shs.bBs bear |. run two hundred and thirtpna feet south. where connection has en made ( with the old workings of thaunsiybt , rein. giving a depth of tEreeunl-a7 ! 'eet below the surface, the er-e shaft ( ,f three hundred feet in deptleip.- iu ore. T The refractory or rebelEous lure of T he ore has continually dimiuled as ,reater depth has been attaineCnd st I he bottom Of the Baker shafthrea c Luudred aud forty feet deep, th,re k bsolUtely free from all elemeutbat Ii etard OF prevent free amalyamat. n There IS sufficient ore now blked ~ mt to supply fifty tons per day foten f. ears.
 What the ore can be made to vie in f he mill, to a large extent. remains r5e c by practical results bl- 70, my opinion that satisfactory prs -H ultimately be realized ir ID all [, \ re. IT, however, an ample supply = igEer grade and more dociie ore can ., blamed by deeper working. which ud 5 -ems certain, the success of the nil 0m the time # starts. will surely eyL. sed the expectations of the most san. line of the stockholders, and will. .withs, six months. net over SIO1OlO. '
 ?. D. B,ENHAEr. [