Show O Ot O lc c j-He j Deposits In lii Utah t I J The occurrence of oC and an other oilier as aa described by j J. J A A. A Taff Tafe find end Carl D D. Smith in the tho t Geological Survey ur uvey reports are of ts v especial Interest t to lo the dwellers bu- bu tween Denver Deliver anti and Utah h by reason of or the advent Into rE region lon of or the lie coming Moffat or Ue Denver vel Northwestern Northwest Northwest- ern era road deposits both bothon t.- t. on un the border of or Colorado and Utah I havo have been elaborately described le by bythe t the he lat late a G. G 1 II H and antI b by William William Wil Wil- f. f T liam ston the latler nil n behalf o of oft Mortal Moffat road The deposits in lit S. S Iho roa t S Utah here described r In J sandstone stone and l CK In the e t l lower part of the Tertiary of oftie tta Wa- Wai Colton Collon Soldier H and i atch group At S. S Midway Utah Ulah the strata arc are tutor tutor- c h by n Assures gures and zones of- of y elation and antI parallel jointing I r Ing Jug the as like dike b Inches thick and antI In S places lilaces several eral feet fet thick Tho Tim n I sure as shown h by nr ar i I tt tzue ue zones ones of or displacement and move move- nent The mines have descended tI In some jomo cases casc nearly neaily feet feel The a i- i varies In lii thickness both laterally laterally later Intel RII ally and antl vertically It Is worked principally prin by Mr Ir of Provo Pro CIl City The rite extent of or the time found round filling fissures cannot be rolled on ott far Car beyond the limit of oC prospected ground Both Iloth tho the width of the fissure or frac- frac 7 lured zone antI and the occurrence of or ozo- ozo Instance In Inthis cerite are arc variable In no ito this fluIs field do the they exceed three fe fel fet feet t l InI in I width The Tue mineral mineraI usual usually I Is In thin sheets he or In fissures fi ures or spaces f surrounding rock ilc Ste ground should contain i wax mineral to lo form approximate approximate- 1 ly I 10 per POC cent of oC the tho lie rock removed S lor br treatment |