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~.GEOLOGV. , <br />There i.n a good geological survey of the district by SPURR of the~U. <br />S.G.S. <br />', <br />~i The ore of the Homestead occurs along a line of faulting betvreen <br />I, the quartzite and shales of the Carboniferous: <br />'~, Strike of fault east and vrent , <br />The are body has a width so far as opened up varying from 1 to 10 ft. <br />~~'.Charaeter of vein filling in a zinc carbonate and lead sulphide con- <br />! taining silver values with a quartz gangue. <br />~; }lomestead shaft in svnl: in the .Silurian dolomite to a depth oP 240 ft. <br />I~At a depth of'l12 ft.in shaft a rronncut rune f1.30°17,60 ft.in dolomite <br />thence OG ft.in quartzite to enc~re ore in found. <br />i <br />I, At a depth of 220 ft.cronncut: runr, t1.30°1'L25 ft.in do}.omil;e thence <br />~, atrlY.e nhalo rcourso cent and west rundar quartsite rdue to faulting. <br />~'~ Dip of atrnta 45° to vnrticnl to tha }LCI. <br />r <br />3 <br />