All that glitters is not gold.
Recent Carved in Stone articles have described the life of Rocky, a 1.8 billion-year-old rock from Morrison, Colo. It would be fair to characterize Rocky’s geologic life as exceedingly long periods of quiet solitude occasionally interrupted by moments (each moment was as short as a few minutes or as long as tens of millions of years) of extreme excitement. This article, as told in Rocky’s own words, describes one of these exciting moments.
About 37 million years ago, I awoke, startled, from a lengthy geologic nap. A huge explosion shook the rocks around me. Somewhere in the mountains, about 85 miles southwest of Morrison, a volcano many times bigger than Mount Saint Helens erupted spewing a column of volcanic ash miles into the air. A cloud of incandescent volcanic ash, hundreds of feet thick, rushed across the landscape destroying everything in its path. When it reached Castle Rock, about 25 miles south east of Morrison, the ash covered the ground. It was so hot that it welded into a 30-foot-thick rock that today is referred to as the Castle Rock Rhyolite.
You might think all that devastation led to no good. But you should know that rhyolite, which is Greek for “streaming rock,” was given that moniker because of its beautiful streaming bands of color. Castle Rock Rhyolite lives up to its name.
The discovery of rhyolite is actually what put the town of Castle Rock on the map. During the 1870s, Silas W. Madge came to Castle Rock searching for gold. He had a sample of rhyolite tested, and the assayer’s report said the rock contained no precious metals, but could be used as building stone.
Madge, realizing that “all that glitters is not gold,” opened a quarry and began producing dimension stone (stone trimmed to specific dimensions) in 1872. Workers using hand tools drilled shot holes about 20 feet deep, filled them with black powder, and blasted the rock. Stone masons squared off the useable pieces. The quarrymen were paid $2.50 a day for their labors.
The Castle Rock Rhyolite was shipped by rail to nearby cities including Denver, Colorado Springs, and Pueblo, and was used in foundations, as veneer, and as decorative trim such as sills, lintels, and archways. The rhyolite even made its way to more distant locations including Cheyenne, Wyo.; Kansas City, Mo.; and Omaha, Neb.
At the peak of production, during the 1880s and early 1890s, the Castle Rock Rhyolite was being cut, dressed, and shipped from three Castle Rock area quarries. The Castle Rock Journal estimated that the quarries produced 1,800 railcars of stone per year worth about $10 per railcar. This was pretty good money for the 1890s.
Production decreased after the 1893 Silver Crash, but the rock continued to be quarried into the 20th century. Sadly, the Madge Quarry closed in 1902.
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