Show PROF JENNEY ON ES the tho Entre Entire Day In the Court at I ENT NT to Nu Nt Vein til vI oil Lot Lut 11 lx in III Orotund Upon resumptIon ot of the Grand ol ala at Nephi yesterday morning Walter Waltr WalterP I P Wa was Pl the Itan stand by bythe the ti Irand Central DIe Il Ila ItS S a noted expert and mining engineer at and hu baa h had yel years of In tile the district J it wi will Pm re n that he wa was the eh chief t wIt wItnel witness nel ness In the noted tra trial bt between th the and the Eureka ureka Hl some lifted Iten years al 10 ego Jenney Jenne nl lied to havIng thirty nine days daYI u upon on the tand which Is in dispute and aud to u ha hay 1 lug carefully the ground Hi hOt surface examination consisted In the I examination or of lot a U from the mouths II end ut of th the claim to several hundred tt feet north of the foot ot In lute Jl lie time that h he had found a ulder under underground ground which was t a form Corm or of modifIed b by the Peculiar nature ot of the wal well outcrop lie He arr agreed wih with the cx who had preceded hint him out on the Itan stand as to the ut torla urInation lon of tb the VII vein but lId said seine n c oases the vein eln was U a true Issue H lIe had found two fIssures along the lne line of oC the theore theore ore In tie the Ora Grand d Central w workings t m in most mOlt flown Ilon to LU LUline tl line ot of connection Ther There were a aiso li cro cross furel fIssures Proceeding south front the end of oC the It th Central I wal was notice noticed Prof Jenney contInued that tte the bl beds were curving to Ihl the east the strike ot of the Id beds north ot of this pint point being south from S 30 to elt east Northerly anti southerly from the o of connecting The strike he lid said wal was north abut 10 U degre degrees west seCt Titis was alt nOte the Case A In tile the deepest workings In Inthe I the dIsputed terrItory The bounding ru on the 70 level leve leveo o of the ground were about 8 U tet feet apart thle these the ore are bodies were found lie He was ot of the opinion the or ore put past continuously through tb the dyke dk front the Cunnings him ham slope At the luth south en end of oC the tho Orald Central op Generally ther there was wa A set et ot of fissures running through the terl tern tory on ti II tunnel level Ivel wih with an another n other fIssure running up from the 1 I fot loot lev level In the Grand Orand Central 10 lie found t another fissure bending westward which indicated a bend nd In inthe the vein eln further north lie He Iid said that I further urther south louth th the ore was u deposited In Ina ina a set t if rudely formed fIssures urn cral cross lag norh and 11 south nearly and going down Into the ground almot almost Ia rally I y Another was found ro roIn rou In lag the ore orl b body north or of th tb apex stop In lot U northwesterly ald and Te The of the vein or lode wu was gIven am north 10 to 11 15 de degrees west 1105 the afu apex stop top to the Cunningham It daDe o and the dip approxImately 7 70 degrees der to the Wet weal from the Cunning hr haiti stop to the pInt o of connection the th strike W was north 70 j Wet west I an and Ul the dip 71 75 der degrees I Nt east through tb the Grand Central the strike Wa was north U 19 derl degrees Wet west and ond tt th dip 70 to 1 70 degree to the wt weal I Prof lenney Jenney gave I It as hl his opInion that the vein passed out o of the wt west sine Ide ln line o of lot a 32 on 11 Its strike ner near the ICing shAft and dil not alln again reenter thu claim alm UI He said that the tendency or of 11 all the bl big veins In the TIntic district was 18 to torun torun run northerly Ind and southerly lOuthI anti thOe those on the Mammoth and irand Central were no to this rul rule Prof ro JeanS WI was ot of the opinion that there II is isItO 10 ItO vein at t the of lot II to t the north ot of tl the louth south end lino extended his He said uld there wu was no for a feet north from the King shaft saId Ild ho be found no lime atone within lot 3 Si north ot of the Cunningham top Th The tO top or apex ot of the vein In dispute hI he la u a near the eastern cd edge or of th the slope In the ground at a Point above I the h east ot of the Wet west side sideline lne line of th the and In the Con Cun Conningham In the Mammoth gron ground No portion ot of this vein he Ild said WAS fOUld found Jorth north of the Betsy ts wIth exception of a small to 0 the norh north Upon he salt Id that the or ore II lIt thu th Young Mammoth tunnel he a Portion of the system of fissures As AI to th the ore are It at the apex rave ht he M said 11 It inclined to the north and back again The taking or of the testimony ot of this witness 11 day |