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PART 3. COLORADO C53 <br />The Fort Defiance prospects are in weak stockworks in limestone, <br />the main fractures of which strike eastward and northward and are <br />mostly nearly vertical. Porous silicified breccia contains masses of <br />cerussite surrounding a little unoxidized and silver -lean galena, chal- <br />cocite and malachite, spongy boxworks of limonite, and a very little <br />smithsonite. <br />Many of the deposits near the site of Carbonate (fig. 6) are in <br />thin vertical fissure veins peripheral to a small 'basaltic volcanic neck <br />with a scoria core, probably of Tertiary age. The neck intrudes <br />Leadville Limestone, which is locally metamorphosed to marble im- <br />mediately adjacent to the contact with basalt; the veins, 6 inches to 6 <br />feet wide, pinch and swell slightly along their traceable lengths of <br />1501,000 feet and contain some smithsonite, a little cerussite and <br />galena, jarosite, brown jasperoid, and calcite. A 3 -foot channel sam- <br />ple across the middle vein at the prospect northeast of the west main <br />shaft yielded the following results when partly analysed: <br />Partial analysis of 3-foot channel sample from a vein near site of Carbonate <br />[Analysis by Deason and Nichols, Salt Lake City, 19541 <br />Gold--------------------------------------- - - - - -- None <br />Silver----------------------- - - - - -- -ounce per ton -- 0.20 <br />Lead ------------------------------------ percent -- .3 <br />Zinc--------------------------------------- do - - -- 13.9 <br />Silica------- - - - - -- ------------------------ do - - -- 37.4 <br />Carbonate---------------------------------- do - - -- 28.1 <br />The Windy Point (or Strong) mine (pl. 1, no. 10) contains the <br />largest deposits of oxidized ores known in the district. They are <br />small but rich bodies of zinc -lead ores containing a little copper and <br />very little silver in limestones and dolomites of the Chaffee Formation <br />and the Leadville Limestone. <br />Oxidized zinc resources. —Known oxidized zinc deposits, though <br />common and spread widely over the White River Plateau, are very <br />small, except those at the Windy Point mine. Unless new deposits <br />larger than those already known are found, the Carbonate district will <br />probably never produce more than a few thousand tons of commercial - <br />grade oxidized zinc ore. <br />RIFE CRE,FK DISTRICT <br />Plate 1, nos. 8, 9 <br />Location. —The Sunshine Lode mine and nearby prospects of the <br />Rifle Creek district are about 16 miles by road north of Rifle and about <br />2 miles north of the large vanadium mines on East Fork near the fish <br />hatchery. <br />Development and production,. —The Sunshine Lode mine was first <br />opened as the Grandview mine in 1925 and was operated until 1932. <br />The mine was reopened in 1940 by Mr. Lale Harmon, and it produced <br />