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Aberdeen Quarry, an abandoned granite quarry in Gunnison County, Colorado. Its granite was used in construction of the Colorado State Capitol; Marble, Colorado, only site of Yule Marble quarrying, in the West Elk Mountains. 99.5% pure calcite, discovered in 1873, source of marble for the Tomb of the Unknowns and for the exterior of the Lincoln ...
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.
Moro Rock is a dome-shaped granite monolith. Common in the Sierra Nevada, these domes form by exfoliation, the spalling or casting off in scales, plates, or sheets of rock layers on otherwise unjointed granite. Outward expansion of the granite results in exfoliations.
Fission tracks – destructive remnants of radioactive decay in Uranium-bearing minerals – were shorter than expected in samples taken from several Sierra Nevada plutons. This implied a late-Cenozoic residency at depth, meaning the unroofing and uplift of the Sierra Nevada block happened rapidly near the end of the Cenozoic.
Decomposed granite is a kind of granite rock that is weathered to the point that the parent material readily fractures into smaller pieces of weaker rock. Further weathering yields material that easily crumbles into mixtures of gravel -sized particles known as grus that further may break down to produce a mixture of clay and silica sand or silt ...
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The granite is mined at the E. L. Smith Quarry, the world's largest "deep hole" granite quarry, owned by the Rock of Ages Corporation. All of the stones in the Hope Cemetery in neighboring city of Barre are made with Barre granite. [3] "Barre Gray" granite is sought after worldwide for its fine grain, even texture, and superior weather resistance.
The original rocks were then intruded by the Lilesville Granite, which crystallized in place as the country rock was metamorphosed by the heat of the magma intrusion. This resulted in the formation of the contact aureole. [6] Mica gneiss xenoliths of various sizes can be found throughout the granite, especially near the contact with the aureole ...