Goosecreekite is a relatively rare member of the zeolite group often forming small, clear, tabular crystals in volcanic cavities. It is best identified by its association with other zeolites and its distinctive monoclinic crystal habit in basaltic environments.
Is this goosecreekite?
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 goosecreekite with a known reference. Goosecreekite sits at Mohs ~4.5, 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 to pearly on crystal faces.
- 4Match the color rangeCompare against the expected color range: colorless, white.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: aggregates, euhedral crystals.
Often confused with
Goosecreekite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside goosecreekite
Minerals reported to co-occur with goosecreekite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaAl₂Si₆O₁₆·5H₂O
- Mohs hardness
- ~4.5
- Density
- 2.21 g/cm³
- Streak
- White
- Luster
- Vitreous to pearly on crystal faces
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Aggregates, euhedral crystals
- Cleavage
- {010}, perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A late-stage mineral in vugs and fractures in a Triassic diabase (Goose Creek quarry, Virginia, USA); in cavities in basalt (Nasik, India)
Where rockhounds find goosecreekite
Classic worldwide localities
- Goose Creek quarry, Leesburg, Loudoun Co., Virginia, USA
- Pandulena quarry, Nasik, Maharashtra, India
- Oberbaumühle quarry, Windischeschenbach, Bavaria, Germany
Field-hunting tip
Where it forms: A late-stage mineral in vugs and fractures in a Triassic diabase (Goose Creek quarry, Virginia, USA); in cavities in basalt (Nasik, India). If you start seeing prehnite, actinolite, chlorite in float, you are in the right ground. Typical habit: aggregates, euhedral crystals. Train your eye for that shape before scanning the outcrop.









