Show DELMAS DEMAS COPPER IS I LIKE UKE MASON VALLEY Such is s Indorsement Given New Proposition by byEng Eng Engineer I TELLS OF I Vein Nearly Neary Fifty Feet Wide Wid I is All AI Ore as Far as asI I Developed I Favorable com comparison of or tho the property property prop prop- I CIl erty of or the Iho Delmas Copper or company 1 I near nea Pal Palisade le Nov ev with wih llio tho property prop ProP- C erty etY lY of time llio Mason valley Copper Coppel proP proP-I company com corn pany at at nl like 10 stage of I development by no lei less s s authority than thal Captain O. O A A. ibbett constitutes constitutes L I i tute perhaps tho bl best t Indorsement clent llio Dolmas Delmas proposition has received or 01 lo could receive Captain Tibbetts Tibbets I recently visited it in iii company with wih a parly larb of or prominent mining men len which Included William Leach Fred C. C Cooley Edward Nissen Will 1 Stephenson Stephen- Stephen Ill a Edmunds son son i P. P D. D Delmas Jo Joseph eph anti ami McGill of Park Cf City The Time Delmus Delmas properly line has been attracting at- at com considerable attention on ac account fe- fe count of a remarkable surface showing of copper ore oro which carries good gool values alues In fn gol gold and silver As described ed by Engineer it Is In iii a n contact con colt tact between between blue an and white banded c and anil diorite Tho Time western part of of tho lime to an extent of some seine OO feet has been crystallized d dInto Into what whal i is locally known as garnet I an and it I is In this lime Ile that occurs The Tho lime Hmo is Intersected by a system of or fissuring exten extending in easterly nu and westerly which swings s in more molo oro to the lie north as fl t approaches the tho contact between time diorite diorIe nn and should intersect time the lime hub some place near time the contact After Acel agreeing with Mr Ir Nissen on ott the general features of oC the formation Captain Tibbets sa says s 's I of or ins Valley The rime and general conditions are ae almost a n duplicate of or orthe time the Mason Valley property properly an and I consider con con- sider l C the opportunity for developing a mine mimic of value equally as goo good as a we had at al the Mason Iason Valc Valley when I first examined examine iThe it i. i The crost fissuring cross is more extensive extensive exten exten- sive and thc he silver sl cr and gold goll values are better beter in this ore tItan than anything we have in the Yerington district The copper coppel is Es i almost almo t Idon- Idon tica except as a a rule the sulphides come com nearer the surface h re than titan they do O in nn any property In Yerington At Al a depth of or front from 20 O to lo 30 0 0 feet Iu in lit lita I u. u u num number er of oC worl workings shown the Iho sulphides sulphides sulphides sul sul- are coming coining In an and showing good al values Tho pf f. f the tle vein I lutha tl o tt I pr 1 H i Uy om oi llio thio Jt parl- parl r was 55 found foun to b be 17 feet In lit wl lh Hhas It H has been opened by a series seles of ur five short tunnels one abo above another an anI and it I Is la said paid ai that the faco face anti and si sides ide o of or oral all al of the workings are aO solid ore Eighteen samples amples taken from front the various ari vari var- arious ous workings g gave ga e assays asas asa's ranging from 2 to 28 S per cent copper from S to to ounces oUnce in silver s1 r and from 0 01 t lo to 1 16 C ounce In gol gold to the ton A sample from Crom the bottom of a vinze from flom the next to tu the time lowest Jo et tunnel gave a au u IC returns t u Ing of 11 0 ounces I nes in sliver silver and 23 3 per her cent copper coppel This al at ol a depth of about 55 5 foot Nt from the thc sur sur- face |