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. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: brown, blue, brown red, gray violet, yellow.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular.
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
- 2.97-3.45 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent to translucent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular
- Cleavage
- Perfect on {110}, intersecting at ~56° and ~124°; partings on {100}, {001}
- Rarity
- Uncommon
- Uses
- Collector
- Host rock
- Commonly in contact metamorphosed limestones; in alkalic igneous rocks and carbonatites
Where rockhounds find richterite
Classic worldwide localities
- Iron Hill, Gunnison Co., Colorado and the Leucite Hills, Sweetwater Co., Wyoming, USA
- Långban and Pajsberg, Värmland, Sweden
- Praborna mine, near St. Marcel, Val d'Aosta, Italy
- Kangerdlugssuaq Fjord, Greenland
- Murun massif, southwest of Olekminsk, Yakutia, Russia
- Gooderham, Wilberforce, Canada
Field-hunting tip
Where it forms: Commonly in contact metamorphosed limestones; in alkalic igneous rocks and carbonatites. If you start seeing leucite, diopside, forsterite in float, you are in the right ground. Typical habit: tabular. Train your eye for that shape before scanning the outcrop.









