Ouray

Ouray was settled in 1875, when gold and silver deposits were found near

Mount Sneffels. Since 1877, mines in Ouray County have produced over

$35,000,000 in gold and $32,000,000 in silver. The district is still

quite active: in 1965, mines in this area produced more than $9,000,000

in gold, silver, copper, lead, and zinc, about a third of total Colorado

production of these metals for that year.

[Illustration: A few miles south of Ouray, along Uncompahgre Gorge, an

old mine clings to the slope below the Million Dollar Highway (U. S.

550). Abrams Mountain rises in the background. The Precambrian

Uncompahgre Quartzite outcrops up to about the road level; Miocene

Sunshine Peak Rhyolite caps the peak. (Jack Rathbone photo)]

A mile north of Ouray a prominent intrusive stock marks the center of

mining activity closest to Ouray. The richest deposits of the Ouray

area, however, lie about five miles southwest, near Mount Sneffels and

Red Mountain Creek. There, several large mines, including the famous

Camp Bird mine, have operated for many years, extracting ore from

hundreds of veins that underly the surface. Some of these veins are two

to four miles long. They are in Tertiary volcanic rocks of the San Juan

Formation. Quartz and calcite are the common gangue (non-economic)

minerals, and pyrite, sphalerite, galena, and chalcopyrite are the most

abundant ores. Most of the silver is in the galena; gold occurs in

streaks and nodules associated with quartz.

About ten miles south of Ouray, along the “Million Dollar Highway” (U.

S. 550), the Red Mountain district lies on the northwest edge of the

Silverton volcanic cauldron. It contains a number of small pipelike

bodies very rich in silver-copper and silver-lead ores. Following the

mid-Tertiary volcanism and ore intrusion, surface rocks in this area

were intensely oxidized: resulting iron oxides now form the gaudy reds

and yellows of Red Mountain and the slopes near Ironton. This

alteration, as well as the fact that much of the area is covered with

fallen rock, stream gravels, or glacial deposits, compounds difficulties

of locating the small though high-grade ore deposits.

The Idarado Mine, on the east side of U. S. highway 550 near Red

Mountain, used to produce ores from nearby volcanic pipes; now it

produces from veins some distance to the northwest. The area is

honeycombed with tunnels and shafts.

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