Yoderite is an exceptionally rare metamorphic silicate mineral primarily known from the Mautia Hill locality in Tanzania. It typically appears as deep violet to purple tabular crystals embedded within kyanite-bearing schists and is highly sought after by advanced mineral collectors.
Is this yoderite?
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 yoderite with a known reference. Yoderite sits at Mohs 6, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: purple red, deep blue, emerald green, yellow.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: anhedral grains, lath.
Often confused with
Yoderite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside yoderite
Minerals reported to co-occur with yoderite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Mg,Al)₆Si₄O₁₂(OH)₂
- Mohs hardness
- 6
- Density
- 3.39 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Anhedral grains, lath
- Cleavage
- Partings [001], good and {100}, poor
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A major phase in quartz-kyanite-talc schist formed under conditions of ~10 kbar H2O pressure and 800 ° C
Where rockhounds find yoderite
Classic worldwide localities
- Mautia Hill, Kongwa, Central Province, Tanzania
Field-hunting tip
Where it forms: A major phase in quartz-kyanite-talc schist formed under conditions of ~10 kbar H2O pressure and 800 ° C. If you start seeing kyanite, talc, hematite in float, you are in the right ground. Typical habit: anhedral grains, lath. Train your eye for that shape before scanning the outcrop.





