Williamsite is a translucent, apple-green variety of antigorite serpentine often containing small black inclusions of chromite or magnetite. It is prized by lapidary enthusiasts for its attractive color and ease of carving, often polished into cabochons. It is primarily found in serpentinized ultramafic rocks and is famously associated with the deposits in the State Line serpentine barrens of Pennsylvania and Maryland.

Hardness
2.5-3.5
Mohs
Luster
Waxy
Streak
White
Transparency
Translucent

Is this williamsite?

5-step field check

Run through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.

  • 1
    Test the hardness
    Try to scratch williamsite with a known reference. Williamsite sits at Mohs 2.5-3.5 — softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Williamsite leaves a white streak.
  • 3
    Read the luster
    Hold the specimen under a strong light. Williamsite typically shows a waxy luster.
  • 4
    Match the color range
    Compare against the expected color range: apple-green, olive-green, yellowish-green.
  • 5
    Look at form & habit
    Crystal system: monoclinic. Typical habit: massive.

Often confused with

Williamsite vs. its common look-alikes — and how to tell them apart in the field.

Often found alongside williamsite

Minerals reported to co-occur with williamsite. Spotting these in float or country rock is a strong cue you are in the right ground.

All properties

Chemical formula
(Mg,Fe)₃Si₂O₅(OH)₄
Mohs hardness
2.5-3.5
Density
2.5-2.6 g/cm³
Streak
White
Luster
Waxy
Transparency
Translucent
Crystal system
Monoclinic
Crystal habit
Massive
Cleavage
None
Rarity
Uncommon
Uses
Lapidary, Collector, Decorative
Host rock
Serpentinite
Typical price
$10-100 per specimen

Where rockhounds find williamsite

5 mapped spots

Classic worldwide localities

  • Pennsylvania, USA
  • Maryland, USA
  • New Zealand
  • Afghanistan

Field-hunting tip

Look in serpentinite country — that is the host setting where williamsite typically forms. If you start seeing chromite, magnetite, calcite 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, Maryland — start trip planning there.

Common questions

How do you identify williamsite?+
Mohs hardness is 2.5-3.5. It typically shows a waxy luster. The streak is white. Common colors include apple-green, olive-green, yellowish-green.
Where is williamsite found?+
Notable localities include Pennsylvania, USA; Maryland, USA; New Zealand; Afghanistan.
Can I find williamsite in the United States?+
RockHoundR maps 5 williamsite rockhounding spots across 2 U.S. states — the top states are Pennsylvania, Maryland.
How much is williamsite worth?+
Typical asking prices fall in the range of $10-100 per specimen. Quality, size, and provenance can move individual specimens well outside that range.
What rocks look like williamsite?+
Williamsite is most often confused with Nephrite Jade, Prehnite, Oregon Jade. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with williamsite?+
Williamsite commonly co-occurs with Chromite, Magnetite, Calcite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does williamsite form in?+
Williamsite typically forms in serpentinite. Working float back to the host body is the standard way to chase a fresh occurrence.
What is williamsite used for?+
Williamsite is used in lapidary, collector, decorative.

Find williamsite on the map

RockHoundR shows mapped rockhounding spots, access rules, and lets you log every find.

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