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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.
Pikes Peak is one of Colorado's 54 fourteeners, mountains more than 14,000 feet (4,267.2 m) above sea level. The massif rises over 8,000 ft (2,400 m) above downtown Colorado Springs. Pikes Peak is a designated National Historic Landmark. It is composed of a characteristic pink granite called Pikes Peak granite.
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 ...
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]
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]
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