Eakerite is an exceptionally rare calcium-tin silicate mineral typically found as small, clear, tabular crystals. It is primarily known from the Livingston Mine in North Carolina, where it occurs within skarn environments alongside various silicates. Due to its extreme rarity and very limited occurrence, it is highly sought after by advanced mineral collectors.
Is this eakerite?
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 eakerite with a known reference. Eakerite sits at Mohs 5.5, 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.
- 4Match the color rangeCompare against the expected color range: colorless, white.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals.
Often confused with
Eakerite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside eakerite
Minerals reported to co-occur with eakerite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₂SnAl₂Si₆O₁₈(OH)₂·2H₂O
- Mohs hardness
- 5.5
- Density
- 2.93 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent to translucent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Probably of hydrothermal origin, in a seam in spodumene-bearing pegmatite (Foote mine, North Carolina, USA); as exsolved inclusions in stanniferous andradite (Kitel'skoye deposit, Karelia)
Where rockhounds find eakerite
Classic worldwide localities
- Foote mine, Kings Mountain, Cleveland Co., North Carolina, USA
- Kitel'skoye tin skarn deposit, north of Lake Lagoda, Karelia
Field-hunting tip
Where it forms: Probably of hydrothermal origin, in a seam in spodumene-bearing pegmatite (Foote mine, North Carolina, USA); as exsolved inclusions in stanniferous andradite (Kitel'skoye deposit, Karelia). If you start seeing tetrawickmanite, bavenite, quartz in float, you are in the right ground. Typical habit: tabular crystals. Train your eye for that shape before scanning the outcrop.







