Computed from simplified end-member formula. Solid-solution series, water content, and trace substitutions cause real-world variation.
IMA Abbreviation (Whitney-Evans 2010)
Wf
→ Wolframite
Fe-Mn tungstate
Standard symbol from American Mineralogist (Whitney & Evans, 2010). Used in thin-section labeling, phase diagrams, and IMA-style species records.
Pronunciation
/ˈwʊlfrəmaɪt/
↔ WOOL-fruh-mite
German "wolf foam"
Magnetism
Category:
weakly paramagnetic
Test result:
Detectable pull
Fe-Mn rich; one of the most magnetic non-ore silicate analogs.
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).
Specific Gravity
7.10–7.50
g/cm³
very heavy
W-Fe-Mn series.
For comparison: water = 1.00, glass ≈ 2.5, quartz = 2.65, corundum ≈ 4.00, galena ≈ 7.50, gold ≈ 19.3.
Streak Test
brown / brownish black
Streak helps separate from scheelite (white streak).
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.
Wolframite sits at 4.5 on the Mohs scale —
can be scratched by a steel knife.
Colors:
Streak Dark reddish brown to black
Crystal system Monoclinic
Pronunciation/ˈwʊlfrəmaɪt/
Type localitySchlaggenwald, Saxony, Germany
Discovery First described 1546 by Georgius Agricola (Saxony)
TungstatesTungstates
TL;DR · 1 min read
Wolframite is the principal ore of tungsten and a defining mineral of the Yaogangxian and Xianghualing tungsten-tin districts. Black, dense, and bladed, it is the metallic counterpoint to the brilliant fluorite for which these mines are now better known.
Wolframite is the principal ore of tungsten and a defining mineral of the Yaogangxian and Xianghualing tungsten-tin districts. Black, dense, and bladed, it is the metallic counterpoint to the brilliant fluorite for which these mines are now better known.
Notable Varieties
Ferberite (Fe-rich end-member)
Hubnerite (Mn-rich end-member)
The Chinese Angle
Yaogangxian and Xianghualing in Hunan are world-class wolframite localities. Specimen-grade crystals reach 5-15 cm and are often associated with quartz, fluorite, and arsenopyrite. Hunan wolframite is the global benchmark for matrix-paired collector specimens.
Cite this entry
APA
MyMineralBox Editorial Team. (2026). Wolframite. My Mineral Box. Retrieved May 23, 2026, from https://mymineralbox.com/mineral-encyclopedia/minerals/wolframite/
MLA
MyMineralBox Editorial Team. "Wolframite." My Mineral Box, 2026, https://mymineralbox.com/mineral-encyclopedia/minerals/wolframite/. Accessed May 23, 2026.
Chicago
MyMineralBox Editorial Team. "Wolframite." My Mineral Box. Last modified May 4, 2026. https://mymineralbox.com/mineral-encyclopedia/minerals/wolframite/.
BibTeX
@misc{mmb_wolframite,
author = {{MyMineralBox Editorial Team}},
title = {{Wolframite}},
year = {2026},
publisher = {My Mineral Box},
url = {https://mymineralbox.com/mineral-encyclopedia/minerals/wolframite/},
urldate = {2026-05-23}
}
About Wolframite
Wolframite is a tungstate mineral in the wolframite group (series: ferberite fe end-member ↔ hübnerite mn end-member) and has the chemical formula (Fe,Mn)WO4. It crystallizes in the monoclinic system and holds a steady position among tungstate species. Its combination of structural character and global distribution make it a recognized species in both systematic and aesthetic collections.
Identification & care
Specimens usually show prismatic, tabular, striated crystals; sub-parallel groups ('blades'); massive. Its color range is broad, including reddish brown, dark brown, iron-black, and grayish black. The luster is sub-metallic, resinous, the streak is reddish brown to black, and specimens are typically opaque. The cleavage is perfect on {010}. The fracture is uneven, which aids identification.
Collector context
How it forms
The geological setting for Wolframite is typically high-temperature hydrothermal veins (greisens) in granite-related systems; contact metamorphic skarns; quartz-vein systems with cassiterite. It is commonly found in association with cassiterite, molybdenite, scheelite, quartz, topaz, fluorite, arsenopyrite.
Classic Chinese localities
Shizhuyuan Mine is a benchmark source for wolframite. Dachang ore field and Huanggang Fe-Sn deposit are an important Chinese source for the species.
Why collectors care
Collectors pursue Wolframite for the clarity of its crystal form and, in good material, saturated color that reads instantly across a display case. A well-terminated wolframite on clean matrix photographs well, identifies quickly, and anchors a cabinet piece. Top Chinese specimens over the last two decades have reset the bar for what wolframite looks like at collector grade.
What affects value
Value in Wolframite 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 Wolframite 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.
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