Amygdaloidal basalt is a volcanic rock characterized by vesicles that have been filled with secondary minerals. These filled cavities, known as amygdules, often contain high-quality zeolites, agate, or other silicates and are highly prized by collectors.
Is this amygdaloidal basalt?
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 amygdaloidal basalt with a known reference. Amygdaloidal Basalt sits at Mohs 5-6 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Amygdaloidal Basalt leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Amygdaloidal Basalt typically shows a dull luster.
- 4Match the color rangeCompare against the expected color range: gray, black, green, brown.
- 5Look at form & habitTypical habit: massive with spherical to elongated vesicles.
Often found alongside amygdaloidal basalt
Minerals reported to co-occur with amygdaloidal basalt. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Mohs hardness
- 5-6
- Density
- 2.8-3.0 g/cm³
- Streak
- White
- Luster
- Dull
- Transparency
- Opaque
- Crystal habit
- Massive with Spherical to Elongated Vesicles
- Cleavage
- None
- Rarity
- Common
- Uses
- Collector, Geological Study
- Host rock
- Volcanic Flows
- Typical price
- $5-50 depending on mineral inclusions
Where rockhounds find amygdaloidal basalt
Classic worldwide localities
- Lake Superior region, USA
- Iceland
- Faroe Islands
- India
- Scotland
Field-hunting tip
Look in volcanic flows country — that is the host setting where amygdaloidal basalt typically forms. If you start seeing zeolites, quartz, calcite in float, you are in the right ground. Field specimens usually show a massive with spherical to elongated vesicles habit, so train your eye for that shape before scanning the outcrop.




