Goethite

Goethite
Goethite,from Minas Gerais, Brazil
General
Category	Mineral
OH)
Identification
Color	Yellowish to reddish to dark brown
Orthorhombic 2/m2/m2/m
Cleavage	Perfect 010
Fracture	uneven to splintery
Mohs Scale hardness	5 - 5.5
Luster	adamantine to dull
Refractive index	Opaque to sub-translucent
Streak	brown, brownish yellow to orange yellow
Specific gravity	3.3 - 4.3
Fusibility	Fusible at 5 - 5.5
Other Characteristics	Becomes magnetic in reducing flame

Goethite, named after the German polymath Johann Wolfgang von Goethe, is an iron bearing oxide mineral found in soil and other low temperature environments. Goethite has been well known since prehistoric times for its use as a pigment. Evidence has been found of its use in paint pigment samples taken from the caves of Lascaux in France. It was first described in 1806 for occurrences in the Mesabi iron ore district of Minnesota. Recently, nanoparticulate authigenic goethite was shown to be the most common diagenetic iron oxyhydroxide in both marine and lake sediments.^[1]

Composition

It is an iron oxyhydroxide. Goethite's hardness ranges from 5.0 to 5.5 on the crystals, but is more typically massive.

Lepidocrocite are both polymorphs of the iron oxyhydroxide FeO(OH). Although they have the same chemical formula as goethite they each have different crystalline structures making them distinct minerals.

Usage

Its main modern use is as an serpentinite rocks in tropical climates are mined for their iron content as well as other metals.

Formation

Goethite often forms through the weathering of other iron-rich minerals, and thus is a common component of soils. It may also be precipitated by groundwater or in other sedimentary conditions, or form as a primary mineral in hydrothermal deposits.

Prevalence

Goethite is found all over the planet, usually in the form of oxidation of sulfide ore deposites is formed of goethite along with other iron oxides and quartz.

Significant deposits of goethite are found in England, Cuba, and Michigan, Minnesota, Missouri, Colorado, Alabama, Georgia, Virginia, and Tennessee in the United States.

Deposits significant in location, if not in abundance, have been found in Gusev by NASA's Spirit rover, providing strong evidence for the presence of liquid water on the planet Mars in an earlier stage of its development.

References

^ C. van der Zee, D. Roberts, D.G. Rancourt, C.P. Slomp. Nanogoethite is the dominant reactive oxyhydroxide phase in lake and marine sediments. Geology 31 (2003) 993-996.

Hurlbut, Cornelius S.; Klein, Cornelis, 1985, Manual of Mineralogy, 20th ed., Wiley, ISBN 0-471-80580-7
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