Potomac Marble is a decorative sedimentary rock composed of rounded limestone clasts cemented together in a colorful matrix. It is famous in American history for being used in the columns of the U.S. Capitol building and is often found as a polished stone in architectural or display collections.
Is this potomac marble?
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 potomac marble with a known reference. Potomac Marble 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. Potomac Marble leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Potomac Marble typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: red, green, brown, white.
- 5Look at form & habitTypical habit: massive.
Often confused with
Potomac Marble vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside potomac marble
Minerals reported to co-occur with potomac marble. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Mohs hardness
- 3-4
- Density
- 2.6-2.8 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Opaque
- Crystal habit
- Massive
- Cleavage
- None
- Rarity
- Common
- Uses
- Ornamental, Decorative, Lapidary
- Host rock
- Sedimentary
- Typical price
- $10-100 per specimen
Where rockhounds find potomac marble
1 mapped spotsClassic worldwide localities
- Maryland, USA
- Potomac River Valley, USA
Field-hunting tip
Look in sedimentary country, the host setting where potomac marble typically forms. If you start seeing calcite, dolomite 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. In the U.S., the densest reported localities are in Pennsylvania. Start trip planning there.



