Lintonite is a green, fibrous variety of the zeolite mineral Thomsonite-Ca. It is best known for forming attractive radiating, globular aggregates found within the cavities of amygdaloidal basalt along the North Shore of Lake Superior.
Is this lintonite?
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 lintonite with a known reference. Lintonite sits at Mohs 5-5.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Lintonite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Lintonite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: green, yellow-green, blue-green.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: radial fibrous, radiating spherulitic aggregates.
Often confused with
Lintonite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside lintonite
Minerals reported to co-occur with lintonite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NaCa₂Al₅Si₅O₂₀·6H₂O
- Mohs hardness
- 5-5.5
- Density
- 2.3-2.4 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Radial Fibrous, Radiating Spherulitic Aggregates
- Cleavage
- Perfect
- Rarity
- Uncommon
- Uses
- Collector, Lapidary
- Host rock
- Basaltic Lava Flows
- Typical price
- $10-50 per specimen
Where rockhounds find lintonite
2 mapped spotsClassic worldwide localities
- Grand Marais, Minnesota
- North Shore of Lake Superior, USA
Field-hunting tip
Look in basaltic lava flows country — that is the host setting where lintonite typically forms. If you start seeing calcite, quartz, datolite in float, you are in the right ground. Field specimens usually show a radial fibrous, radiating spherulitic aggregates habit, so train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in Minnesota — start trip planning there.







