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Marble - Colorado Geological Survey

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GEOLOGIC CHARACTERIZATION<br />

INVESTIGATION ACTIVITIES<br />

Literature Review<br />

The earliest written account of the geology of<br />

the Elk Mountain region was produced by the<br />

Hayden <strong>Survey</strong> in the early 1870s. Reports of<br />

their work in the Aspen area, including a<br />

1:125,000 scale geologic map on a topographic<br />

base, are given in the United States <strong>Geological</strong><br />

and Geographical <strong>Survey</strong> Annual Reports of<br />

1874-1876 (Hayden, 1874; Peale, 1874; Hayden,<br />

1876; Holmes, 1876). The map documents<br />

early impressions of the complex structural<br />

features of the area. This work remained the<br />

only published geologic map of the Elk Mountain<br />

region until those of Bryant in 1969-1971<br />

(Bryant, 1969,1970,1971a). Bryant's studies of<br />

the area have appeared in various publications<br />

and are culminated in Geology of the Aspen 15<br />

Minute Quadrangle, Pitkin and Gunnison<br />

Counties, <strong>Colorado</strong>, published in 1979 (Bryant,<br />

1966,1971b, 1972a, 1972b, 1979). Bruce<br />

Bryant's personal input was extremely helpful<br />

throughout this evaluation. Numerous other<br />

workers have also written on the various aspects<br />

of the geology of the Elk Range and their<br />

studies were consulted. An extensive bibliography<br />

accompanies this report.<br />

Aerial Photography<br />

Black and white aerial coverage of the Conundrum-<strong>Colorado</strong><br />

Highland property at a scale of<br />

1:24,000 was produced by Merrick and Company,<br />

under contract to CGS, during June of<br />

1989. The most recent color aerial photography<br />

coverage was produced by the USFS, flight line<br />

No. 1081, photos 201-203, dated September 24,<br />

1982 at 1:24,000 scale. Stereo images from the<br />

1989 photography were digitized by computer<br />

to produce a topographic base map of the area<br />

at a scale of 1 inch equals 400 feet, with a<br />

contour interval of 10 feet. Ground control for<br />

aerial mapping was provided by CGS.<br />

Aerial photography was utilized throughout<br />

the geologic investigation to verify ground observations<br />

and to assist in field location. Ground<br />

textures of the Conundrum Valley as seen on<br />

the aerial photographs have provided insight<br />

into the structural complexity of this area.<br />

<strong>Survey</strong> Control<br />

CGS received all survey notes from USFS in<br />

April of 1989. The Forest Service has not conducted<br />

an official survey of the claim block, but<br />

has recovered existing corners where possible.<br />

The 472.46 acre claim block is comprised of:<br />

The California Placer—MS No. 4928^<br />

153.023 acres, patented April 1891<br />

The Edith M. Placer—MS No. 12334,160.0<br />

acres, patented February 1899<br />

The Vera Placer—MS No. 12335, 20 acres,<br />

patented February 1899<br />

The Vermont Placer—MS No. 12393,<br />

139.434 acres, patented February 1899 (see<br />

Plate 3).<br />

The California Placer was surveyed by Lee<br />

Hayes, U.S. Mineral <strong>Survey</strong>or, on September<br />

13,1887. The Edith M., Vera, and Vermont<br />

Placers were surveyed by George W. Wyce, U.S.<br />

Deputy Mineral <strong>Survey</strong>or, in mid December,<br />

1897. No record of any subsequent boundary<br />

survey for this claim block is in existence. Original<br />

claim corners constructed of rock markers<br />

scribed with claim number and corner designation<br />

have been recovered at various locations<br />

on the property (see Plate 3). CGS has copies of<br />

all original survey notes.<br />

Control for topographic mapping and claim<br />

location was established by CGS in June of<br />

1989. A closed loop traverse of 11,500 feet was<br />

run through panel points and selected claim<br />

corners where available. Horizontal closure<br />

error in the traverse yielded an accuracy ratio<br />

of 1:14,200. This corresponds to a maximum<br />

error of plus or minus 0.814 feet for X and Y<br />

coordinates. Vertical closure error yields an<br />

5

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