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Scientists from around the world come to Colorado to study the minerals of this region. Because the granite covers a large portion of the Colorado Front Range, there are good mineral collecting areas scattered all over the Pikes Peak region. The collecting localities range from near Colorado Springs on the south to just west of Denver on the north.
The Pikes Peak Consolidated Fuel Company, a subsidiary of Golden Cycle Mining and Reduction Company, was located in Pikeview in 1920. Harvey McGarry of Colorado Springs was the president and Robert O'Neil of Pikeview was the superintendent. [14] In 1922, Pikeview's economy was nearly entirely based upon mining. [6]
Golden Cycle controlled the Pikes Peak Consolidated Fuel Company, which had 15,000,000 tons of marketable coal, a 50% interest in East Colorado Springs Land Company, held more than a third interest in United Gold Mines in Cripple Creek and owned 400 acres in Cripple Creek. [1]
Colorado Springs Cryolite was discovered by October 1882 at St. Peter's Dome near Pike's Peak. [57] [58] 1882 coal Colorado Springs The completion of the Denver and New Orleans Railroad in July, 1882 was instrumental in the effective production and shipment of coal from the Franceville Mine. It became the first coal mine that was "worked to any ...
Pikes Peak granite is a 1.08 billion year old Late-Precambrian geologic formation found in the central part of the Front Range of Colorado. It is a coarse-grained pink to light red syenogranite with minor gray monzogranite , and it has a distinctive brick-red appearance where it outcrops.
The Sonoma orogeny uplifted the ancestral Rocky Mountains in parallel with the diversification of multicellular life. Shallow seas covered the regions, followed by the uplift current Rocky Mountains and intense volcanic activity. Colorado has thick sedimentary sequences with oil, gas and coal deposits, as well as base metals and other minerals. [1]
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