| Show i AT Observations of or aT Denver MIning Writer of ot the tho W A Scott Scot associate editor Mining of at Denver D nver recently visited Park City and notes no le his ober observations ob cr nt at the mine In the tho following allowing manner monner This group of mineral locations U it 1 on he the the well defined Park City mineral belt which wel Is II con about H 11 1 miles In loath lenth On this belt bel or zone are the On Ontario orlo tario Daly tin the Dal lying wc well west t and northwest from IrinI the he Some engineers ore are ar on record up as giving the of HIla la min mineral oral eral belt bell ns as n 2000 felt f f in hat liat portion where the tho properties above mentioned lh ore are The holdings aggregate over 1200 0 acres In area ara The formation here Is II In two Actions From rom the Iho surface down dOI n to 1300 feet feu depth Is n a n black limestone Mew this the On Ontario Ontario It what Is II locally known knon as 11 tario arlo Doth Both strata of ot rock named have a general dip ll northwester JY 11 y W IV P Jenny E M 31 who reported on this property finds nt nl the tho contact ot of these two bedding planes pianos a I stratum of soft toft gray lime limestone stone from a n few tew feet to over oer 20 feet teet thick llan and that valuable deposits depo a Of ot sil cli sl ore have been found In these gray lime beds bode Porphyry dikes are fountS found foun cutting through the lime and formations WIthin the miner mineral al albeit belt on grounds are a number of fissures carrying ore In con continuous shoots sho II Three of are ore par described de In Mr Jennys re report r report port pori which ore are ar opened from the 1200 10 foot level One One of ot these thes the Daly DelY vein veinIs la Is opened and worked continuously on onIt IU its It course coure from the lie Ontario mine to tt the Ih I main shaft flatt which Is la a n distance of GO feet This hla Is perhaps tile the Ihl protest t fissure ls ur vein of ot the district UK its wIdth ranging from lIve to 10 M 50 feet I I Its 11 Il characteristics on th thi this Ontario Daly and groups were Svere much the same Mme carrying profits pronta ble ore bodies In them nil all ni The rite nock Hack vein or the Daly Is 11 froni tire live to 26 25 feet In ill 11 width the third Is l the Me M Honey Sorl Z fixture fissure lure whose hOH vh M or ore Is not so 1 well wel developed the fw fig 0 mires UteR there ther rl In beds on the contact |
