Riebeckite is an amphibole group mineral typically found in silica-rich alkaline igneous rocks like granite. It often occurs as prismatic crystals or as a fibrous, asbestiform variety known as crocidolite, which can replace other minerals during pseudomorphosis.
Is this riebeckite?
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 riebeckite with a known reference. Riebeckite 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: greenish brown.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous to silky.
- 4Match the color rangeCompare against the expected color range: dark blue, black, blue-green, blue, dark green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: fibrous, massive, striated.
Often confused with
Riebeckite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside riebeckite
Minerals reported to co-occur with riebeckite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₂Fe²⁺₃Fe³⁺₂Si₈O₂₂(OH)₂
- Mohs hardness
- 6
- Density
- 3.28-3.44 g/cm³
- Streak
- Greenish brown
- Luster
- Vitreous to silky
- Transparency
- Semitransparent
- Crystal system
- Monoclinic
- Crystal habit
- Fibrous, massive, striated
- Cleavage
- Perfect on {110}, intersecting at 56° and 124°; partings on {100}, {010}
- Rarity
- Common
- Uses
- Collector, Lapidary
- Host rock
- In alkalic granites and syenites; rarer in felsic volcanics and granite pegmatites; in some schists
Where rockhounds find riebeckite
1 mapped spotsClassic worldwide localities
- Quincy, Norfolk Co., Massachusetts, USA
- St. Peters Dome, near Pikes Peak, El Paso Co., Colorado, USA
- Pass, Okanogan Co., Washington, USA
- Socotra Island, Indian Ocean
- North from Koegas, Cape Province, and east of Pietersburg, Transvaal, South Africa
- Sultan Hamud, Kenya
Field-hunting tip
Where it forms: In alkalic granites and syenites; rarer in felsic volcanics and granite pegmatites; in some schists. If you start seeing aegirine, nepheline, albite in float, you are in the right ground. Typical habit: fibrous, massive, striated. 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.







