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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.
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.
Manitou Springs, also called "Saratoga of the West", [4] was established as a resort community, known for its mineral springs and "spectacular setting" at the edge of the Rocky Mountains [5] and the base of Pikes Peak. [3]
Zebulon Pike's "friend" Tamaha was recognized by many names including Tahama, [13] Tahamie [14] and Tamahaw. [15] Pike's memoirs and the writings of Elliott Coues, Edward D. Neill, J. Fletcher Williams and Charles Eastman all confirm that these names are for the same individual: the Dakota Sioux man whom Pike believed was a "war chief" and who later inspired the name for the original spring in ...
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]
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]
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