ferrimolybdite

{{infobox mineral

| name = Ferrimolybdite

| image = Ferrimolybdite-154908.jpg

| alt =

| caption = Ferrimolybdite crystals from the Kingman District, Mohave County, Arizona

| category = Molybdate mineral

| formula = Fe3+2(MoO4)3·8(H2O) or Fe3+2(MoO4)3·n(H2O)

| IMAsymbol = Fmyb{{Cite journal|last=Warr|first=L.N.|date=2021|title=IMA–CNMNC approved mineral symbols|journal=Mineralogical Magazine|volume=85|issue=3|pages=291–320|doi=10.1180/mgm.2021.43|bibcode=2021MinM...85..291W|s2cid=235729616|doi-access=free}}

| molweight =

| strunz = 7.GB.30

| dana =

| system = Orthorhombic

| class = Dipyramidal (mmm)
H-M symbol: (2/m 2/m 2/m)

| symmetry = Pmmn

| unit cell = a = 6.665, b = 15.423
c = 29.901 [Å]; Z = 8

| color = Canary-yellow, straw-yellow, greenish yellow

| habit = Acicular tufted to radial aggregates; powdery, earthy

| twinning =

| cleavage = Distinct on {001}

| fracture = Uneven

| tenacity =

| mohs = 1-2

| luster = Adamantine, silky, earthy

| streak = Light yellow

| diaphaneity = Transparent to translucent

| gravity = 2.99

| density =

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| opticalprop = Biaxial (+)

| refractive = nα = 1.720 - 1.810 nβ = 1.730 - 1.830 nγ = 1.850 - 2.040

| birefringence = δ = 0.130 - 0.230

| pleochroism = X = Y = clear to nearly colorless; Z = dirty gray to canary-yellow

| 2V = 26° to 32° (calculated)

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| references = [http://www.mindat.org/min-1623.html Ferrimolybdite on Mindat.org][http://rruff.info/doclib/hom/ferrimolybdite.pdf Ferrimolybdite on the Handbook of Mineralogy][http://www.webmineral.com/data/Ferrimolybdite.shtml Ferrimolybdite data on Webmineral.com]

}}

Ferrimolybdite is a hydrous iron molybdate mineral with formula: Fe3+2(MoO4)3·8(H2O) or Fe3+2(MoO4)3·n(H2O). It forms coatings and radial aggregates of soft yellow needles which crystallize in the orthorhombic system.

Discovery and occurrence

It was first described in 1914 for an occurrence in the Alekseevskii Mine in the Karysh River Basin, Khakassia Republic, Siberia, Russia. It was named for its composition (ferric iron and molybdenum).

It occurs as an oxidation product of molybdenum bearing ore deposits.

Associated minerals include: molybdenite, pyrite and chalcopyrite.

References