Feroxyhyte

Feroxyhyte is an oxide/hydroxide of iron, δ-Fe3+O(OH). Feroxyhyte crystallizes in the hexagonal system. It forms as brown, rounded to concretionary masses. Feroxyhyte is an opaque, magnetic mineral with a yellow streak and a relative density of 4.2.

Feroxyhyte
Image of Feroxyhyte
General
CategoryOxide mineral
Formulaδ-Fe3+O(OH)
IMA symbolFox
Strunz classification4.FE.40
Dana classification06.01.04.04
Crystal systemHexagonal
Unknown space group
Unit cella = 2.95, c = 4.56 [Å]; z = 1
Identification
Formula mass88.85 g/mol
ColorBrown, yellow-brown
Crystal habitConcretionary, massive, nodular
StreakYellow
DiaphaneityOpaque
Specific gravity4.31
Density4.2
Optical propertiesUniaxial
References

It occurs in manganese-iron nodules on the Atlantic and Pacific Ocean floors. It is also found in the Baltic, White, and Kara Seas. Forms under high pressure conditions and reverts to goethite on exposure to surface conditions. It also occurs as cement and coatings on clasts in poorly drained soils and sediments, formed by the rapid oxidation of iron(II) oxide compounds.

It was first described in 1976 for an occurrence in soils at its type locality: Kolomyya, Ivano-Frankivsk Oblast, Ukraine.

See also

  • Akaganeite
  • Ferrihydrite
  • Iron(III) oxide-hydroxide
  • Lepidocrocite

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