Travertine is a terrestrial sedimentary rock formed by the rapid precipitation of calcium carbonate, often at the mouth of a hot spring or in a limestone cave. It is characterized by its distinct banded appearance and porous structure, making it a popular material in both geological collections and architectural finishings.
Is this travertine?
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 travertine with a known reference. Travertine sits at Mohs 3-4 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Travertine leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Travertine typically shows a dull to earthy luster.
- 4Match the color rangeCompare against the expected color range: white, tan, cream, brown, yellow.
- 5Look at form & habitTypical habit: banded, crustiform, massive.
Often confused with
Travertine vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside travertine
Minerals reported to co-occur with travertine. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaCO₃
- Mohs hardness
- 3-4
- Density
- 2.5-2.7 g/cm³
- Streak
- White
- Luster
- Dull to Earthy
- Transparency
- Opaque
- Crystal habit
- Banded, Crustiform, Massive
- Cleavage
- None
- Rarity
- Common
- Uses
- Decorative, Architectural, Collector
- Host rock
- Hot Springs and Limestone Caves
- Typical price
- $5-50 for small decorative specimens or slabs
Where rockhounds find travertine
4 mapped spotsClassic worldwide localities
- Tivoli, Italy
- Yellowstone National Park, USA
- Pamukkale, Turkey
- Hierapolis, Turkey
Field-hunting tip
Look in hot springs and limestone caves country — that is the host setting where travertine typically forms. If you start seeing calcite, aragonite in float, you are in the right ground. Field specimens usually show a banded, crustiform, massive habit, so train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in West Virginia, Wyoming — start trip planning there.




