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Granite

Granite

A species of Igneous

Iconic, recognizable, and widespread, granite is a rock that even non-geologists are usually familiar with. Coming in a variety of colors and often exhibiting beautiful speckling or patterns, granite is sometimes polished and used decoratively for countertops, tiles, stone buildings, monuments, and more. Many famous natural structures, such as Yosemite’s Half Dome, are also made of granite.

Hardness
Hardness:

6 - 7

Density
Density:

2.65 - 2.75 g/cm³

General Info About Granite

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Physical Properties of Granite

Texture
Phaneritic
Colors
White, pink, gray, occasionally dyed other colors
Magnetism
Potentially Magnetic
Grain Size
Coarse grained
Hardness
6 - 7 , Hard
Density
2.65 - 2.75 g/cm³, Normal Weight
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Chemical Properties of Granite

Elements listed
Al, Na, K, O

Health Risk of Granite

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What is the hazards of Granite?

Harm Type
Physical Toxicity
Granite in powdered form can be toxic due to its Crystalline Silica content.
Granite is a natural source of radiation, like most natural stones. Potassium-40 is a radioactive isotope of weak emission, and a constituent of alkali feldspar, which in turn is a common component of granitic rocks, more abundant in alkali feldspar granite and syenites. Some granites contain around 10 to 20 parts per million (ppm) of uranium. By contrast, more mafic rocks, such as tonalite, gabbro and diorite, have 1 to 5 ppm uranium, and limestones and sedimentary rocks usually have equally low amounts. Many large granite plutons are sources for palaeochannel-hosted or roll front uranium ore deposits, where the uranium washes into the sediments from the granite uplands and associated, often highly radioactive pegmatites. Cellars and basements built into soils over granite can become a trap for radon gas, which is formed by the decay of uranium. Radon gas poses significant health concerns and is the number two cause of lung cancer in the US behind smoking.

How to prevent the risks of Granite?

Avoid long-term inhalation of its dust!
Granite is typically non-toxic unless it's in powder form. Long-term exposure to finely ground powder may lead to silicosis. Therefore, when cutting or polishing granite, be sure to wear a dust mask to avoid inhaling its dust.

Discover the Value of Granite

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Rarity
Easy to obtain
Collection Recommendation
3.8 out of 5
Popularity
4.1
Aesthetic
3.6
Rarity
3.4
Sci-Cultural Value
3.8

The Market Price of Granite

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Weight is a decisive factor affecting the price of granite. The price of a polished stone about 2.5 cm across is usually $.25-$2/piece.

Rough/Tumbled Price

Fixed Price
$3 - $10 piece

Characteristics of Granite

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Characteristics of Granite

The average density of granite is between 2.65 and 2.75 g/cm (165 and 172 lb/cu ft), its compressive strength usually lies above 200 MPa, and its viscosity near STP is 3–6·10 Pa·s. The melting temperature of dry granite at ambient pressure is 1215–1260 °C (2219–2300 °F); it is strongly reduced in the presence of water, down to 650 °C at a few kBar pressure. Granite has poor primary permeability overall, but strong secondary permeability through cracks and fractures if they are present.

Formation of Granite

Granitic rock is widely distributed throughout the continental crust. Much of it was intruded during the Precambrian age; it is the most abundant basement rock that underlies the relatively thin sedimentary veneer of the continents. Outcrops of granite tend to form tors, domes or bornhardts, and rounded massifs. Granites sometimes occur in circular depressions surrounded by a range of hills, formed by the metamorphic aureole or hornfels. Granite often occurs as relatively small, less than 100 km stock masses (stocks) and in batholiths that are often associated with orogenic mountain ranges. Small dikes of granitic composition called aplites are often associated with the margins of granitic intrusions. In some locations, very coarse-grained pegmatite masses occur with granite.

Composition of Granite

A worldwide average of the chemical composition of granite, by weight percent, based on 2485 analyses: The extrusive igneous rock equivalent of granite is rhyolite.

Cultural Significance of Granite

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Uses of Granite

Granite is a very popular construction material due to its resistant and strong nature, and it can be used in countertops, flooring, stairs, columns, and walls. As such, it is can be seen in households and commercial construction in nearly ever building component. For many centuries it has also been used in stone carvings and statues.

Distribution of Granite

Granite containing rock is widely distributed throughout the continental crust. Much of it was intruded during the Precambrian age; it is the most abundant basement rock that underlies the relatively thin sedimentary veneer of the continents. Outcrops of granite tend to form tors, domes or bornhardts, and rounded massifs. Granites sometimes occur in circular depressions surrounded by a range of hills, formed by the metamorphic aureole or hornfels. Granite often occurs as relatively small, less than 100 km stock masses (stocks) and in batholiths that are often associated with orogenic mountain ranges. Small dikes of granitic composition called aplites are often associated with the margins of granitic intrusions. In some locations, very coarse-grained pegmatite masses occur with granite.

Geochemistry of Granite

A worldwide average of the chemical composition of granite, by weight percent, based on 2485 analyses: SiO2 72.04% (silica), Al2O3 14.42% (alumina) , K2O 4.12%, Na2O 3.69%, CaO 1.82%, FeO 1.68%, Fe2O3 1.22%, MgO 0.71%, TiO2 0.30%, P2O5 0.12%, MnO 0.05%

Mineralogy and Petrology of Granite

Granite is classified according to the QAPF diagram for coarse grained plutonic rocks and is named according to the percentage of quartz, alkali feldspar (orthoclase, sanidine, or microcline) and plagioclase feldspar on the A-Q-P half of the diagram. True granite (according to modern petrologic convention) contains both plagioclase and alkali feldspars. When a granitoid is devoid or nearly devoid of plagioclase, the rock is referred to as alkali feldspar granite. When a granitoid contains less than 10% orthoclase, it is called tonalite; pyroxene and amphibole are common in tonalite. A granite containing both muscovite and biotite micas is called a binary or two-mica granite. Two-mica granites are typically high in potassium and low in plagioclase, and are usually S-type granites or A-type granites.

Etymology of Granite

The word "granite" comes from the Latin granum, a grain, in reference to the coarse-grained structure of such a completely crystalline rock.

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