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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.
Granite (/ ˈɡrænɪt / GRAN-it) is a coarse-grained (phaneritic) 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.
Alkali feldspar granite, some varieties of which are called 'red granite', [1] is a felsic igneous rock and a type of granite rich in the mineral potassium feldspar (K-spar). It is a dense rock with a phaneritic texture. The abundance of K-spar gives the rock a predominant pink to reddish hue; peppered with minor amounts of black minerals. [2] [3]
The look of any quartz countertop compares to granite in that the colors are deep and consistent. [5] The process of creating the countertops is different than granite, in that it is an engineered product, consisting of a minimum of 93% quartz and 7% epoxy binder and dyes. [6]
Kashmir granite. Kashmir gold is a type of granite found in Madurai, Tamil Nadu state, India. This is a yellow coloured granite, with black granules in its structure. [1] The Kashmir gold granite is only a trade name of this granite, such as Kashmir white granite is. Neither are found in the Kashmir region, however the familiar trade names are ...
Countertop. A countertop, also counter top, counter, benchtop, worktop (British English) or kitchen bench (Australian or New Zealand English), bunker (Scottish English) is a raised, firm, flat, and horizontal surface. They are built for work in kitchens or other food preparation areas, bathrooms or lavatories, and workrooms in general.
The Woodbury Granite Company (WGC) was a producer of rough and finished granite products. Incorporated in 1887, purchased and significantly reorganized in 1896, and expanded by merger in 1902 and thereafter, the company operated quarries principally in Woodbury, Vermont, but its headquarters and stone-finishing facilities were located in nearby Hardwick.
I-type granite. I-type granites are a category of granites originating from igneous sources, first proposed by Chappell and White (1974). [1] They are recognized by a specific set of mineralogical, geochemical, textural, and isotopic characteristics that indicate, for example, magma hybridization in the deep crust. [2]
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