Graphite | |
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Graphite specimen
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General | |
Category | Native mineral |
Formula (repeating unit) |
C |
Strunz classification | 1.CB.05a |
Crystal system | Hexagonal |
Crystal class | Dihexagonal dipyramidal (6mmm) H-M symbol: (6/m 2/m 2/m) |
Space group | P63/mmc |
Unit cell | a = 2.461, c = 6.708 [Å]; Z = 4 |
Identification | |
Color | Iron-black to steel-gray; deep blue in transmitted light |
Crystal habit | Tabular, six-sided foliated masses, granular to compacted masses |
Twinning | Present |
Cleavage | Basal – perfect on {0001} |
Fracture | Flaky, otherwise rough when not on cleavage |
Tenacity | Flexible non-elastic, sectile |
Mohs scale hardness | 1–2 |
Luster | Metallic, earthy |
Streak | Black |
Diaphaneity | Opaque, transparent only in extremely thin flakes |
Density | 2.09–2.23 g/cm3 |
Optical properties | Uniaxial (–) |
Pleochroism | Strong |
Solubility | Soluble in molten nickel, warm chlorosulfuric acid |
Other characteristics | strongly anisotropic, conducts electricity, greasy feel, readily marks |
References |
Graphite ( /ˈɡræfaɪt/), archaically referred to as plumbago, is a crystalline allotrope of carbon, a semimetal and a native element mineral. Graphite is the most stable form of carbon under standard conditions. Therefore, it is used in thermochemistry as the standard state for defining the heat of formation of carbon compounds.
The principal types of natural graphite, each occurring in different types of ore deposits are:
Graphite occurs in metamorphic rocks as a result of the reduction of sedimentary carbon compounds during metamorphism. It also occurs in igneous rocks and in meteorites. Minerals associated with graphite include quartz, calcite, micas and tourmaline. In meteorites it occurs with troilite and silicate minerals. Small graphitic crystals in meteoritic iron are called cliftonite.
According to the United States Geological Survey (USGS), world production of natural graphite in 2012 was 1,100,000 tonnes, of which the following major exporters are: China (750 kt), India (150 kt), Brazil (75 kt), North Korea (30 kt) and Canada (26 kt). Graphite is not mined in the United States, but U.S. production of synthetic graphite in 2010 was 134 kt valued at $1.07 billion.