Tufa is a highly porous, spongy variety of limestone that forms through the precipitation of calcium carbonate from ambient-temperature water. Collectors often look for it in ancient lake beds or hot spring discharge sites where it develops distinct, erratic, and weathered shapes. Its lightweight, cavernous structure makes it easily identifiable compared to denser travertine.
Is this tufa?
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 tufa with a known reference. Tufa sits at Mohs 3, softer than the next harder reference, harder than the previous one.
- 2Read the textureLook at a fresh break with a hand lens. Texture: Porous.
- 3Pick out the mineralsComposition: Carbonate minerals (calcite) precipitated from unheated rivers or lakes. Identify the two or three most abundant grains.
- 4Read the lusterHold the specimen under a strong light. Luster: dull.
- 5Match the color rangeCompare against the expected color range: white, gray, yellow, tan, brown.
Often confused with
Tufa vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside tufa
Minerals reported to co-occur with tufa. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Mohs hardness
- 3
- Density
- 1.1-2.0 g/cm³
- Luster
- Dull
- Transparency
- Opaque
- Rarity
- Common
- Uses
- Decorative, Construction, Geological research
- Host rock
- hot spring deposits
- Texture
- Porous
- Composition
- Carbonate minerals (calcite) precipitated from unheated rivers or lakes
Where rockhounds find tufa
Classic worldwide localities
- Mono Lake, California, USA
- Hierapolis, Turkey
- Mammoth Hot Springs, Wyoming, USA
- Tivoli, Italy
Field-hunting tip
Where it forms: hot spring deposits. If you start seeing calcite, aragonite in float, you are in the right ground.






