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  2. Mineralogy of the Pikes Peak Region - Wikipedia

    en.wikipedia.org/wiki/Mineralogy_of_the_Pikes...

    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.

  3. Pikes Peak granite - Wikipedia

    en.wikipedia.org/wiki/Pikes_Peak_granite

    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.

  4. List of mountain passes in Colorado - Wikipedia

    en.wikipedia.org/wiki/List_of_mountain_passes_in...

    This is a list of some important mountain passes in the Rocky Mountains of the U.S. State of Colorado. ... Trail Ridge High Point [g] 12,183 feet ... Granite Pass ...

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  6. Geology of Colorado - Wikipedia

    en.wikipedia.org/wiki/Geology_of_Colorado

    Throughout Colorado's geologic history, rocks have often been deformed, metamorphosed and overprinted, obscuring the ancient record. Beginning 1.7 billion years ago granite and pegmatite intruded. The Routt Plutonic Suite is dated to 1.66 to 1.79 billion years old and is an important rock formation in Rocky Mountain National Park and Buffalo ...

  7. File:Pikes Peak (Pikes Peak Granite, Mesoproterozoic, 1.08 Ga ...

    en.wikipedia.org/wiki/File:Pikes_Peak_(Pikes...

    English: Granite in the Precambrian of Colorado, USA Pikes Peak is a famous mountain in the American Cordillera. The correct spelling "Pike's Peak" has been suppressed. The reddish-pinkish rocks of the mountain and surrounding areas are part of the Pikes Peak Batholith, a fairly large, Precambrian igneous intrusion that was emplaced 1.08 billion years a

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