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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.
Marengo warehouse, in Marengo, Indiana, formerly a limestone quarry, now one of the largest subterranean storage facilities in the nation, with nearly 4,000,000 square feet (370,000 m 2) space. It began as an open pit quarry in 1886 due in part to its proximity to a railroad. Underground room and pillar mining began in 1936. Leased storage ...
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.
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Granite (/ ˈ ɡ r æ n ɪ t / GRAN-it) is a coarse-grained intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase.It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies underground.
The granitoid rocks are mainly potassic granite and were derived principally from reworked older (3.1–2.8 Ga) gneiss. [ 3 ] During the Paleoproterozoic , island-arc terrane associated with the Colorado orogeny accreted to the Wyoming Craton along the Cheyenne belt , a 500-km-wide belt of Proterozoic rocks named for Cheyenne, Wyoming .
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