Show A GREAT 1 FIND J T P r arill or OP TOOELE MARES MAKES IT NEAR TRAT THAT CITY I 1 it will A add tid many times to the water alpi supply 1 y bring being far greater than alia n that of cl the surface creak J P hill of 0 has struck I 1 it 11 r rich it en at the mouth of c th alie 0 canyon i e east ot of an underflow ot of witter water enough the laT lanil latip dp t the ahr valley lying between 1 the I 1 ingeb 43 4 A important a in the poo 14 P 41 could well nell be imagined I 1 aouino I 1 in little a ai colt 0 mt lull hill liean pc ang tor thi underflow derf by lri jK pipes find and in way lie located tile the vater at seven to forty feet then ho he put doil don n it a shaft eight feet deep and found a Uro iii steady how flow or of a greater loody lody of vater anater than 11 the WE a entire watershed ot of tile canyon ithe would produce this water lung luna among the gravel and boulders and hall haa worn won I 1 many of 0 them na its smooth na as agate it I 1 Is not knolia how low deep fall stratum of bater bearing gravel fi ravel la 19 but it undoubtedly doubLed ly rests on the bedrock alch has it a dip of about 5 per cent libatan trally to that of ane surface of tho the bench toward tile the the atar must come from a hubter raL lican supply in tile the mountains and Is entirely disconnected from the cann on put face or its ito seepage AS AB for as prospected this water course la Is aboul feet ade litle but there Is more of it and alt it nill is IH now blots clots cutting in the shaft ehatt tor for the purpose of ex alarin F lla its full breadth A lit tunnel anel 1100 feet I 1 ong long aou would d brins bring ahli water to the east or upper side bide of tooele thoele city anti and tile the abundance of water that coad then be ba su supplied would be a joy to the heart of tile the resident there it la Is by odds the most important water find made lit in thoele tooele valley not cx hepting the surface BE streams reams arid and pioul aises a cleat s beit future tor for tactic |