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

It occurs in - on the and floors. It is also found in the , , and . Forms under high pressure conditions and reverts to on exposure to surface conditions. It also occurs as cement and coatings on clasts in poorly drained soils and sediments, formed by the rapid of iron(II) oxide compounds.

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

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