Manganite is a manganese oxide mineral typically found as dark, striated, prismatic crystals. It is easily distinguished from other black manganese minerals by its characteristic dark reddish-brown streak. It is most commonly found in hydrothermal deposits associated with other manganese minerals and carbonates.
Is this manganite?
5-step field checkRun through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.
- 1Test the hardnessTry to scratch manganite with a known reference. Manganite sits at Mohs 4, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: reddish brown to nearly black.
- 3Read the lusterHold the specimen under a strong light. Luster: submetallic.
- 4Match the color rangeCompare against the expected color range: dark gray, black, steel-gray, gray, grayish black.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: massive, prismatic, pseudo orthorhombic.
Often confused with
Manganite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Streak differs, so Manganite leaves reddish brown to nearly black, Pyrolusite leaves black, bluish black; luster reads submetallic on Manganite and metallic on Pyrolusite.

How to tell apart: Psilomelane is the harder of the two (Mohs 5-6 vs. 4); streak differs, so Manganite leaves reddish brown to nearly black, Psilomelane leaves brownish black.

How to tell apart: Hausmannite is the harder of the two (Mohs 5.5 vs. 4); streak differs, so Manganite leaves reddish brown to nearly black, Hausmannite leaves dark reddish brown.
Often found alongside manganite
Minerals reported to co-occur with manganite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- MnO(OH)
- Mohs hardness
- 4
- Density
- 4.29-4.34 g/cm³
- Streak
- Reddish brown to nearly black
- Luster
- Submetallic
- Transparency
- Opaque, transparent on thin edges
- Crystal system
- Monoclinic
- Crystal habit
- Massive, prismatic, pseudo orthorhombic
- Cleavage
- {010}, perfect; {110} and {001}, good
- Rarity
- Common
- Uses
- Collector, Ore of manganese
- Host rock
- Formed in low-temperature hydrothermal or hot-spring manganese deposits; replacing other manganese minerals in sedimentary deposits; a component in some clay deposits and laterites
Where rockhounds find manganite
2 mapped spotsClassic worldwide localities
- Negaunee and Marquette districts, Marquette Co., Michigan, USA
- Powell’s Fort mine, near Woodstock, Shenandoah Co., Virginia, USA
- Lake Valley, Sierra Co., New Mexico, USA
- Ilfeld, Harz Mountains, and Ilmenau, Thuringia, Germany
- Botallack mine, St. Just, Cornwall, England
- Egremont, Cumbria, England
Field-hunting tip
Where it forms: Formed in low-temperature hydrothermal or hot-spring manganese deposits; replacing other manganese minerals in sedimentary deposits; a component in some clay deposits and laterites. If you start seeing pyrolusite, braunite, hausmannite in float, you are in the right ground. Typical habit: massive, prismatic, pseudo orthorhombic. Train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in Utah. Start trip planning there.




