Magnetite oxidizes to hematite ("martite") under prolonged oxidation while preserving octahedral form.
Australia, Ural Mountains, Brazil.
A pseudomorph (Greek "false form") is a mineral with the external shape of another species — the chemistry has changed but the crystal habit is inherited.
Picks up iron filings; sticks to refrigerator magnet
Fe₃O₄ — only commonly-collected mineral that is naturally ferromagnetic. Lodestone variety is naturally permanently magnetized.
Test with rare-earth magnet (N42 or N52 neodymium). Suspend specimen on thread for sensitive paramagnetic detection. Diamagnetic minerals are weakly repelled (visible only with strong magnets like bismuth).
Diagnostic Field Tests
Magnet test→ Strongly attracts a magnet
Lodestone variety is naturally magnetized.
Streak→ Black
Distinguishes from hematite (red streak).
⚠ Use dilute HCl (~10%) only on inconspicuous spots; rinse promptly. Smell-tests should be brief and ventilated. Taste-test ONLY halite/sylvite — never lead, arsenic, or sulfur minerals.
Specific Gravity
5.17
g/cm³
heavy
Fe₃O₄; magnetic + heavy.
For comparison: water = 1.00, glass ≈ 2.5, quartz = 2.65, corundum ≈ 4.00, galena ≈ 7.50, gold ≈ 19.3.
Streak Test
black
Black streak + magnetic — diagnostic combination.
Streak = color of the powdered mineral. Drag specimen across unglazed white porcelain plate (Mohs 6.5). For minerals harder than the plate, crush a small flake into powder and observe color.
Twinning Laws
Spinel lawcontact
Same {111} twin as spinel — flat octahedra rare but striking.
Cleavage & Fracture
Cleavage:
none— (parting on {111})
Fracture:
subconchoidal
Octahedral parting common.
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Market availability: Common
Widely available in most dealer stocks. Specimens span all price tiers.
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Collector tier: Solid Display
Reliable mid-tier display species. Easy to find in well-formed examples; broad locality diversity.
Magnetite sits at 5.5–6.5 on the Mohs scale —
just hard enough to scratch glass.
Colors:
Streak Black
Crystal system Isometric (Cubic)
Type localityMagnesia, Greece
Discovery Known since antiquity (Magnesia, Greece)
Oxides & HydroxidesOxides
TL;DR · 1 min read
Magnetite (Fe₃O₄) is the strongly magnetic iron oxide and one of the principal iron ores. Its octahedral crystal habit and natural magnetism (lodestone variety) make it instantly recognizable.
Magnetite (Fe₃O₄) is the strongly magnetic iron oxide and one of the principal iron ores. Its octahedral crystal habit and natural magnetism (lodestone variety) make it instantly recognizable. Magnetite forms in mafic-ultramafic igneous rocks, banded iron formations, and contact-metamorphic skarns. Anshan (Liaoning) and Panzhihua (Sichuan) are major Chinese ore producers.
Magnetite is classified as an oxide mineral in the spinel supergroup > oxyspinel group and has the chemical formula Fe2+Fe3+2O4. It crystallizes in the isometric system and has a distinctive metallic presence in any collection. Its combination of structural character and global distribution make it a recognized species in both systematic and aesthetic collections.
Identification & care
Magnetite typically forms octahedral (most characteristic), dodecahedral; massive, granular, lamellar; rounded grains in metamorphic rocks. Its color is typically greyish black or iron black. The luster is metallic, sub-metallic, the streak is black, and specimens are typically opaque. The cleavage is none (parting on {111}, sometimes good). The fracture is irregular/uneven, which aids identification.
Collector context
How it forms
The geological setting for Magnetite is typically common accessory mineral in igneous and metamorphic rocks; major iron ore in banded iron formations; contact metasomatic skarns; black sand beaches. It is commonly found in association with pyrite, pyrrhotite, ilmenite, hematite, chlorite, diopside, grossular.
Classic Chinese localities
Huanggang Fe-Sn deposit is an important Chinese source for the species.
Why collectors care
Magnetite is a frequently-sought species in serious collections because its habit is recognizable, its color often strong, and its best examples unmistakable even at a distance. Chinese material has driven much of the recent visual shift in the species — sharper crystals, deeper colors, cleaner matrix.
What affects value
Value in Magnetite is assessed, in typical order of weight, against: (1) locality provenance; (2) size relative to the species norm; (3) crystal form and termination sharpness; (4) color saturation and zoning; (5) transparency and internal clarity; (6) matrix quality and aesthetic balance; (7) condition (absence of damage, chips, or repair). Cleaning quality and verified locality documentation act as multipliers across the above.
Naming history
The name Magnetite has a specific etymological and historical context — see Mindat's reference entry for provenance details. We have retained naming data at the record level; published prose is paraphrased from factual fields rather than copied from source.
Frequently asked questions
What is Magnetite?
Magnetite is an oxide mineral recognized among collectors for its crystal form and distribution, with several world-class Chinese localities.
What is the chemical formula of Magnetite?
The chemical formula of Magnetite is Fe3O4.
What crystal system does Magnetite belong to?
Magnetite crystallises in the Isometric crystal system.
Where is Magnetite found?
Notable localities for Magnetite include Bayan Obo, Huanggang Mine, Dabaoshan Polymetallic Mine, Val Malenco.
Is Magnetite rare?
As a collector mineral, Magnetite is generally considered common.
Mindat.org is the world’s largest open mineralogy database. Our descriptions are written independently and fact-checked.
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