Plagioclase is a series of tectosilicate minerals that form the most abundant mineral group in the Earth's crust. Collectors typically identify them by their characteristic polysynthetic twinning, which appears as fine, parallel striations on cleavage surfaces.

Hardness
6-6.5
Mohs
Luster
Vitreous
Streak
White
Transparency
Transparent

Is this plagioclase?

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 plagioclase with a known reference. Plagioclase sits at Mohs 6-6.5, softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Streak: white.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: vitreous.
  • 4
    Match the color range
    Compare against the expected color range: white, gray, colorless, pale yellow, pale green, bluish white, reddish white, greenish white.
  • 5
    Look at form & habit
    Crystal system: triclinic. Typical habit: massive.

Often confused with

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

Often found alongside plagioclase

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

All properties

Chemical formula
(Na,Ca)(Al,Si)₄O₈
Mohs hardness
6-6.5
Density
2.61-2.76 g/cm³
Streak
White
Luster
Vitreous
Transparency
Transparent
Crystal system
Triclinic
Crystal habit
Massive
Cleavage
Good on {001}; good on {010}
Rarity
Common
Uses
Collector, Industrial
Host rock
Igneous and metamorphic rocks

Where rockhounds find plagioclase

5 mapped spots

Classic worldwide localities

  • Norway
  • Canada
  • USA
  • Italy
  • Madagascar

Field-hunting tip

Where it forms: Igneous and metamorphic rocks. If you start seeing quartz, biotite, hornblende in float, you are in the right ground. Typical habit: massive. Train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in Wisconsin, Missouri, Washington. Start trip planning there.

Common questions

How do you identify plagioclase?+
Mohs hardness is 6-6.5. Luster: vitreous. The streak is white. Common colors include white, gray, colorless, pale yellow.
Where is plagioclase found?+
Notable localities include Norway; Canada; USA; Italy; Madagascar.
Can I find plagioclase in the United States?+
RockHoundR maps 5 plagioclase rockhounding spots across 3 U.S. states. The top states are Wisconsin, Missouri, Washington.
What rocks look like plagioclase?+
Plagioclase is most often confused with Orthoclase, Microcline, Albite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with plagioclase?+
Plagioclase commonly co-occurs with Quartz, Biotite, Hornblende, Pyroxene, Magnetite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does plagioclase form in?+
Where it forms: Igneous and metamorphic rocks. Working float back to the host body is the standard way to chase a fresh occurrence.
What is plagioclase used for?+
Plagioclase is used in collector, industrial.

Find plagioclase on the map

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

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