| Show I I I 1 01 h N ltJf 2 tf j l 0 < I t t I v m th f S 1 f t If i t J C1 1J JiJ Cj 9 J 1 1 < i 1 tI cl l b1 r 5f f r 4 < F f < < t I f jjlt y p r Et ¼ s it IJ t p JjAJ C > 0 1 > r O C 1 z m rt I t f I 0 > OJ I r 1 r II 4 I 7 > fr tt h = IP I I 11 = 4 r Ii 1 to bJ 0 > v i ll L l Co t t I f J t r M i hJ p JJ r I tt JJ F I I 4 i I WJ J ltr < h cOrJ t K o I 1 I to J IJi d r o r c r tl > 10 = n 4 1 i it t J u t f l fI 13 1 I R 1 Sf ro r J ft I 1 4 of > I fr E mfnRffi oWW 12m Ir J = f 1sD i G a tl fr < 3 f 1 W2i i I ib J e t l r c a 9 i i t ttJ g l rl J k t r t iJ t l f1 = f m w lJt 1i 1 Orl < 1 6 r S p i < > i r 1f11 lr i + i t t kor4 I i 4t i lff Ei fb 1 6 IJ I r B II r I y a I t t f 1 11 it J1t JUo trJ Jr 1 1 tt f ti ft 1f tp f l t fi Ei 4 C J ftf ffi 2 1f wt r t j P t Ii m r > f IiWjj i J t i > Ii t r rqv i tif i1 r r < ml i v t 4 o fi Q f r < i O i 3 Ir > i ltiif c t Z jttf i 1 1 v 1 J jijf 1 1 ft t M t 1 ij W t r g t t J ILIfL 1 > 0 = 1 M tJ t it r r i j t r i t I L t 1 r i ot ifJ I KINSLEY MINE OF NEVADA if > W W CHISHOLM President S This district Is situated In Elko county coun-ty Nov seventy miles from Toano station on the Southern Pacific railroad rail-road Toano being about 200 miles from Salt Lake City The largest property in this district comprises twentyone claims all patented pat-ented extending fully two miles on the strike of the veins contained there in These claims are owned by W W Chisholm J D Kendall Newton A Diwyon and W M Bradley of Salt Lake City The development on these properties consists mostly of surface openings made for the purpose of determining de-termining the continuation and strike of the veins which have been proved to extend in a northerly and southerly direction throughout the entire length of the property Several openings have been made on each of the claims The veins are contact veins between porphyry por-phyry and lime Both the granites and limestones of this district arc fissured by porphyry dykes trending north and south of which there are a great num ber and the mineralization has taken place and Is strongest on each side of the dykeswhere the limestone exists Practically all of the twentyone claims carry contacts between the porphyry and the limestone Ship ments In carload lots have been made fiom Tunnels No 1 and No 2 on the northerly portion of the property and as shipped the ore showed an average of about fifty ounces silver 37 percent per-cent lead 015 gold 21 per cent iron and 0 per cent silica There are about 150 tons of ore on the tunnel dumps of about the same average grade There are several faces of ore exposed in the portion of the property where the abovementioned ore came from The ore zhown along the contacts through llthe the claims The most of the work has been done on tho north era portion of the properly from which the shipments above mentioned were made but In other portions of tho property the mineralization is fully as strong though very little work other than surface work has been done In a great many places on the property there Is a good grade of copper ore but that also has not been developed as yet The company owns a spring within two miles of Its property with a sufllcient low of water to supply the mines with ample water for the treatment of ores and an abundance of wood is also close at hand and all that Is necessary to make this a pay Ing proposition is continued work Tho gentlemen Interested have heretofore done their business under the name of the Kinsley Mining company |
