Strontianite is a strontium carbonate mineral that often forms beautiful, radiating clusters of acicular or bladed crystals. It is frequently found in hydrothermal veins and sedimentary deposits, and it is a primary source for strontium compounds used in pyrotechnics and glass manufacturing.
Is this strontianite?
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 strontianite with a known reference. Strontianite sits at Mohs 3.5, 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, resinous on breaks.
- 4Match the color rangeCompare against the expected color range: colorless, white, gray, pale yellow, pale green, greenish, gray white, yellowish.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: columnar, massive, pseudo hexagonal.
Often confused with
Strontianite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside strontianite
Minerals reported to co-occur with strontianite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- SrCO₃
- Mohs hardness
- 3.5
- Density
- 3.76 g/cm³
- Streak
- White
- Luster
- Vitreous, resinous on breaks
- Transparency
- Transparent to translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Columnar, massive, pseudo hexagonal
- Cleavage
- On {110}, nearly perfect; on {021}, poor; on {010}, interrupted
- Fluorescence
- White under SW UV; cherry red white under LW UV
- Rarity
- Common
- Uses
- Collector, Ore of strontium
- Host rock
- An uncommon low-temperature hydrothermal mineral formed in veins in limestone, marl, and chalk; in geodes and concretions; rarely occurs in hydrothermal metallic veins; common in carbonatites
Where rockhounds find strontianite
3 mapped spotsClassic worldwide localities
- Strontium Hills, 16 km north of Barstow, San Bernardino Co., California, USA
- Homestake mine, Lead, Lawrence Co., South Dakota, USA
- A number of mines around Rosiclare, as the Minerva #1 mine, Cave-in-Rock, Hardin Co., Illinois, USA
- Winfield quarry, Union Co., Pennsylvania, USA
- Strontian, Argyll, Scotland
- Clausthal and Bad Grund, Harz Mountains, Germany
Field-hunting tip
Where it forms: An uncommon low-temperature hydrothermal mineral formed in veins in limestone, marl, and chalk; in geodes and concretions; rarely occurs in hydrothermal metallic veins; common in carbonatites. If you start seeing barite, calcite, celestine in float, you are in the right ground. Typical habit: columnar, massive, pseudo hexagonal. Train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in Indiana, Illinois. Start trip planning there.








