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
5 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, 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, New York. Start trip planning there.






