ENSTATITE and HYPERSTHENE
enstatite and hypersthene -
mineral 65.1.2.1
| Chemical Formula | Enstatite - Mg2Si2O6 Hypersthene - (Mg,Fe)2Si2O6 |
|
| Composition | Enstatite is magnesium silicate. However, it
is usually contains some iron replacing some magnesium.
When a significant amount of iron present, the mineral is
called Hypersthene (magnesium iron silicate).
[Most authorities agree that Hypersthene contains a ratio
of magnesium to iron about 1:1. If only a small amount of
iron is present, the mineral is still Enstatite.] In many
reference guides, Hypersthene is categorized as a variety
of Enstatite, and not as a separate mineral. Enstatite forms a series with Ferrosillite (FeSi2O6), in which the intermediary member is Hypersthene. Specimens of pure Enstatite (without any iron) are not common, and specimens of pure Ferrosillite (without any magnesium) are virtually unknown. |
|
| Variable Formula | (Mg,Fe)Si2O6 | |
| Color | Gray, green, dark yellow, yellow-brown, greenish-brown, brown, black | |
| Streak | Light brown to grayish-white | |
| Hardness | 5 - 6 | |
| Crystal Forms and Aggregates |
(Orthorhombic) Usually as disordered aggregates of rectangular crystals. May also occur in single crystals (prismatic and stubby), which may be well-terminated. Also occurs as cleavage fragments, as platy groupings, fibrous, and lammelar. Crystals are partially hollow in some localities. | |
| Transparency | Transparent to opaque | |
| Specific Gravity | 3.1 - 3.9 (The greater the iron content, the heavier it is) | |
| Luster | Vitreous, silky, submetallic, dull | |
| Cleavage | 1,2 - prismatic at cleavage angles of 87º
and 93º (characteristic of minerals in the pyroxene group). May also exhibit parting in one direction. |
|
| Fracture | Uneven | |
| Tenacity | Brittle | |
| Other Names | Hypersthene can have three connotations.
Most often, it refers to an individual mineral, which is
midway in the Enstatite-Ferrosillite series. The term may also be used as an iron-rich
variety of Enstatite, and it is occasionally used as a
synonym for Enstatite and Ferrosillite. A synonym for Hypersthene is "Ferroan Enstatite". |
|
| Varieties | ||
| Polymorphs | Polymorph of Enstatite is Clinoenstatite Polymorph of Hypersthene is Clinohypersthene |
|
| In Group | Silicates ; Inosilicates ; Pyroxene group | |
| All About | Enstatite and Hypersthene are found in igneous environments, and are sometimes found in meteorites. Pure Enstatite is transparent and lightly colored; iron makes it darker and opaque. |
|
| Uses | The variety Bronzite is used as a minor gemstone. It often contains inclusions of highly reflective minerals, such as Hematite and Goethite, which give it a bronze-like effect when polished (hence its name). Some polished specimens exhibit asterism or cat's eye effect. | |
| Striking Features | Luster and cleavage angles | |
| Popularity (1-4) | 2 | |
| Prevalence (1-3) | 1 | |
| Demand (1-3) | 2 | |
| Distinguishing Similar Minerals |
Hornblende - different
cleavage angles (otherwise difficult to distinguish) Augite - very difficult to distinguish Diopside - very difficult to distinguish |
|
| Commonly Occurs With |
Biotite, Almandine, Quartz,
Diopside, Labradorite, Magnetite, Chromite, Serpentine (In meteorites, it occurs with Iron-nickel, Olivine, and Ferrosillite, as well as the high temperature polymorphs [ Clinoenstatite, Clinohypersthene, and Clinoferosillite ] ) |
|
| Noteworthy Localities |
Enstatite is relatively abundant, and
localities are worldwide. However, a few notable
occurrences are the Tilly Foster Mine, Brewster, Putnam
Co., New York; the Wood's Mine, near Texas, Lancaster
Co., Pennsylvania; the Bare Hills, near Baltimore,
Maryland; Jackson Co., North Carolina; and Boulder Co.,
Colorado. Hypersthene is much rarer than Enstatite. The most important deposit is in the Adirondack Mountains of New York (especially at Gore Mountain, Warren Co.). Small amounts were also found in Labrador, Canada, together with Labradorite. Hypersthene is also found in Brusand, Norway. Gem quality Bronzite is found in Styria, Austria; the Bushfield Complex, Transvaal, South Africa; and in the Stillwater Complex, Montana. |
|
| Picture Icon Links |
Sorry. No Images currently available. | |
| Picture Links | Sorry. No Images currently available. |
Additional references
|
|
| Sponsor this page |
|