Show I NEVADA HILLS fETS GETSi GETS i I BEST RESULTS YET YETi i Finds Finds High Values in Big Contact Contact Contact Con Con- tact Ledge at Depth IS BARREN AT SURFACE Fractures Dip Into Into It Proving Big Ledge Source of Values A telegram from the Nevada Xo lulls mine received yesterday b by ly General Manager William IJ IT I. I Webber o ber who IB Is IBIn It In tho city for a few fow days day contained news of or development o In tho the lowest l workings s In the property which ho re regards regards re- re gards the thc mo most moil t Important of anything that has yet et taken place there It I Is the finding of goo good values at tho the depth of 34 feet In the great Seat quartz ledge edgo 70 feet thick which at the surface sur sur- taco face is 18 barren The Tile superintendent re reports ro- ro ports that at that depth In tho shaft shaf sur-j sur ho has hat eleven that feet of ore averaging 28 a ton with picked samples running run run- ning as high as ounces on silver and 14 ounces in gold or 80 a ton The on only disappointment In the tile properly property heretofore has ilas been In the tho absence of ot values In the the big lg ledge e gc at atthe tho the surface It I Is a con contact tact vein between between be be- tween anti and ant unde underlie andesite lh an and carrying car car- yin i-yin rIng values the conditions for 01 permanency per per- would be ideal lint But the value values val val- ue ues were wele foun found at tho surface in parallel par pal aJol fractures dipping toward the big vein ein While hUe some seine tome bonanza ore oro bodies have been bOen en opened In those fractures It was wa realized that conditions were not so s favorable fa for permanency as the they would woul have ha been had the tile rich self ore bo bodies les occurred in III the big Ic ledge so it itself It- It i- i flit Dip Into Big let nut hut the thc fact that the shaft which is cutting through the big bIg ledge has at this tills particular point encountered I tho the values proves pr es that the main fracture fracture frac frac- ture turo has changed change Us its Is dip that dip that the theore theore ore is now noc following the tile hanging hanging- wall vali wal of Dr the tile big ledge In other words tho the big ledge Is the tho source of tho the values In tile the fractures s. s which yield the rich ore near the surface Indicating that at ot depth tho fractures all aU converge into the ledge and presenting possibilities of or enrichment that arc are almost fla staggering The ho development is what Mr 11 Webber Webber Web Web- eb ber bur has be been on hoping for all al along and he lie sa says B that It virtually completes complete the parallel situation of the tile poro Nevada Hills with the tho Comstock ode lode fur far wih so aa as al de development do- do has l progressed rog-resse rog in il Nevada a aHi Hi Hills s. s |