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REX E LC]ESBY PE <br />• <br />3037739632 <br />• <br />EXHIBIT B: SITE DESCRIPTION <br />Histo <br />P, 03 <br />Received <br />JUN 21 1989 <br />~'~n9o Field <br />Dit'isbn of Miner ~ic9 <br />~ 3 Geology <br />The Yule Quarry is more than a dimensional stone quarry. It has a unique and <br />colorful place in Colorado history. The white marble was discovered in the 1880's and soon <br />became known as one of the finest white marbles in the world. It was selected for the exterior of <br />the Lincoln Memorial in 1916 and the Tomb of the Unknowns in 1936. The quarry closed in <br />194 t and remained a tourist destination until 1990, when it was re-opened by the new Colorado <br />Yule Mazble Company (CYMC). During the 1940's through the 1990'x, the hike to the quarry <br />has been a special experience for thousands of tourists each aummcr. The hike includes a wade <br />through a narrow gulch where Yule Creek cascades across brilliant white trtazble. 1t concludes at <br />the incredibly huge entries to the Yule Quarry where the visitor can look down into the massive <br />undergrotmd roottu excavated by early century miners. CYMC failed in early 1999 and Sierra <br />Minerals intends to re-open the quarry under new management and under a new permit with the <br />Colorado Division of Minerals and Geology (CpMG). The pictwes here show the quarry <br />openings after CYMC re-opened it in 1990 (above, right), the footpath to the quarry (above, left), <br />and the quarry interior (tight). The picture on the following page shows the front of the quarry in <br />early 1999 with the fuel storage tank to the left and the generator trailer to rho right. <br />{a) Veeetatioa and Soil Characterletics: In the affected area and on the fringes of <br />the atfcctcd area there are subalpine spruce/fir forests as well as substantial areas of bare rock. <br />The original condition of most of the affected area near the quarry portals was bare rock as can <br />be seen in the photo below dated 1911. Topsoil, where it exists in the area! tends to be shallow <br />and very rocky -typically ao more than six inches thick. <br />(b) Structures Within 200 Feet: The eastern edge of the affected area is traversed by a <br />foot trail that was relocated aGghtly when CYMC began operations in ]990. This foot trail <br />begins at the tourist pazking azea at the north end of the White Marble Lode Claim, leads up <br />along Yule Creek to the base of the quarry, follows a ridge line between the waste piles and Ytile <br />Creek, then leads to the quarry errtries. Access to this foot trail is via the historic right of way <br />established by the wagon road to the quatxy constructed in the late 1800'x, and then by the <br />electric railroad beginning in 1908. The railroad was removed in 1941 when the quarry closed. <br />During the 1940's through the late 1940'x, access was open to the public. Four wheel drive <br />vehicles could reach the quarry entries up until the 1970's when the road washed out along Yule <br />Creek just north of quarry entries. After the wash outs, access was limited to htkets. <br />Access along the historic right of way has been blocked by the owner ofthe Yule Lode <br />Claim (McIntyre). Gunnison County has instituted legal action in an attempt to establish that the <br />trail is a public road. The quarry's zoning permit with Gunnison County takes tbe position that <br />the trail is a public right of way. If access is reopened, Sierra intends to contply with the terms of <br />the zoning permit. Resolution of the dispute is not expected until sometime in 2000. <br />