Verde Antique is a metamorphic rock composed mainly of serpentinite with veins of calcite or dolomite. It is prized by collectors and architects for its striking dark green base color contrasted with white or light green veining, often taking a high polish for decorative use.
Is this verde antique?
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 verde antique with a known reference. Verde Antique sits at Mohs 3-5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Verde Antique leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Verde Antique typically shows a waxy luster.
- 4Match the color rangeCompare against the expected color range: green, dark green, white, black.
- 5Look at form & habitTypical habit: massive.
Often confused with
Verde Antique vs. its common look-alikes — and how to tell them apart in the field.


How to tell apart: Luster reads waxy on Verde Antique and subvitreous on Marble.

How to tell apart: Streak differs — Verde Antique leaves white, Malachite leaves light green; luster reads waxy on Verde Antique and vitreous on Malachite.
Often found alongside verde antique
Minerals reported to co-occur with verde antique. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Mohs hardness
- 3-5
- Density
- 2.5-2.8 g/cm³
- Streak
- White
- Luster
- Waxy
- Transparency
- Opaque
- Crystal habit
- Massive
- Cleavage
- None
- Rarity
- Common
- Uses
- Decorative, Lapidary, Sculpture, Architecture
- Host rock
- Metamorphic Complexes
- Typical price
- $5-50 slabs and decorative items
Where rockhounds find verde antique
1 mapped spotsClassic worldwide localities
- Vermont, USA
- Ireland
- Greece
- Italy
Field-hunting tip
Look in metamorphic complexes country — that is the host setting where verde antique typically forms. If you start seeing calcite, dolomite, serpentine 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 Maryland — start trip planning there.



