Lansfordite is a rare, hydrated magnesium carbonate that is highly unstable when removed from its native environment. It typically forms as white, prismatic crystals or encrustations and will rapidly dehydrate into nesquehonite upon exposure to air. Collectors usually keep these specimens in sealed containers to prevent them from turning into a white, powdery mass.
Is this lansfordite?
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 lansfordite with a known reference. Lansfordite sits at Mohs 2.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Lansfordite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Lansfordite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, colorless, grayish white.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic to acicular crystals, often as crusts or globular aggregates.
Often confused with
Lansfordite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside lansfordite
Minerals reported to co-occur with lansfordite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- MgCO₃·5H₂O
- Mohs hardness
- 2.5
- Density
- 1.72 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic to Acicular Crystals, Often as Crusts or Globular Aggregates
- Cleavage
- Distinct On {110}
- Rarity
- Rare
- Uses
- Collector, Scientific Research
- Host rock
- Coal Mine Dumps, Serpentinite Deposits
- Typical price
- $20-150 for rare specimen fragments
Where rockhounds find lansfordite
Classic worldwide localities
- Lansford, Pennsylvania, USA
- Kladno, Czech Republic
- Zabrze, Poland
- Karelia, Russia
Field-hunting tip
Look in coal mine dumps, serpentinite deposits country — that is the host setting where lansfordite typically forms. If you start seeing nesquehonite, hydromagnesite, magnesite in float, you are in the right ground. Field specimens usually show a prismatic to acicular crystals, often as crusts or globular aggregates habit, so train your eye for that shape before scanning the outcrop.



