Richterite is a member of the sodic-calcic amphibole group, typically appearing as elongated, prismatic or fibrous crystals. It is most frequently found in metamorphosed limestone deposits or alkaline rocks, often exhibiting distinct brown or yellow hues.
Is this richterite?
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 richterite with a known reference. Richterite sits at Mohs 5-6 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Richterite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Richterite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: brown, yellow, red, colorless, green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic crystals, fibrous, columnar.
Often confused with
Richterite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside richterite
Minerals reported to co-occur with richterite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na(NaCa)Mg₅Si₈O₂₂(OH)₂
- Mohs hardness
- 5-6
- Density
- 3.0-3.2 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic Crystals, Fibrous, Columnar
- Cleavage
- Perfect Prismatic
- Rarity
- Uncommon
- Uses
- Collector
- Host rock
- Metamorphosed Limestones, Skarns, Alkaline Igneous Rocks
- Typical price
- $20-150 for thumbnail to cabinet specimens
Where rockhounds find richterite
Classic worldwide localities
- Långban, Sweden
- Magnet Cove, Arkansas, USA
- Quebec, Canada
- Khibiny Massif, Russia
Field-hunting tip
Look in metamorphosed limestones, skarns, alkaline igneous rocks country — that is the host setting where richterite typically forms. If you start seeing calcite, dolomite, diopside in float, you are in the right ground. Field specimens usually show a prismatic crystals, fibrous, columnar habit, so train your eye for that shape before scanning the outcrop.








