Vesicular basalt is an extrusive igneous rock characterized by numerous small cavities called vesicles, formed by gas bubbles trapped in cooling lava. These cavities are often later filled by secondary minerals like zeolites, quartz, or calcite, making them popular targets for micromounters and collectors.
Is this vesicular 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 vesicular basalt with a known reference. Vesicular 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. Vesicular Basalt leaves a white to gray streak.
- 3Read the lusterHold the specimen under a strong light. Vesicular Basalt typically shows a dull luster.
- 4Match the color rangeCompare against the expected color range: black, dark gray, brownish-gray.
- 5Look at form & habitTypical habit: massive.
Often confused with
Vesicular Basalt vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside vesicular basalt
Minerals reported to co-occur with vesicular 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 to Gray
- Luster
- Dull
- Transparency
- Opaque
- Crystal habit
- Massive
- Cleavage
- None
- Rarity
- Common
- Uses
- Decorative, Landscaping, Collector
- Host rock
- Volcanic Surface Flows
- Typical price
- $1-20 per specimen
Where rockhounds find vesicular basalt
Classic worldwide localities
- Hawaii, USA
- Iceland
- Etna, Italy
- Columbia River Plateau, USA
Field-hunting tip
Look in volcanic surface flows country — that is the host setting where vesicular basalt typically forms. If you start seeing olivine, plagioclase, zeolites in float, you are in the right ground. Field specimens usually show a massive habit, so train your eye for that shape before scanning the outcrop.






