Gypsum is a soft sulfate mineral commonly found in evaporite sedimentary environments. It is easily identified by its extremely low hardness and ability to form long, transparent bladed crystals known as Selenite, or massive, fine-grained deposits known as Alabaster.

Hardness
2
Mohs
Luster
Vitreous
Streak
White
Transparency
Transparent

Is this gypsum?

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 gypsum with a known reference. Gypsum sits at Mohs 2 — softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Gypsum leaves a white streak.
  • 3
    Read the luster
    Hold the specimen under a strong light. Gypsum typically shows a vitreous luster.
  • 4
    Match the color range
    Compare against the expected color range: colorless, white, gray, yellow, honey.
  • 5
    Look at form & habit
    Crystal system: monoclinic. Typical habit: tabular crystals, prismatic, bladed, fibrous.

Often confused with

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

Often found alongside gypsum

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

All properties

Chemical formula
CaSO₄·2H₂O
Mohs hardness
2
Density
2.3 g/cm³
Streak
White
Luster
Vitreous
Transparency
Transparent
Crystal system
Monoclinic
Crystal habit
Tabular Crystals, Prismatic, Bladed, Fibrous
Cleavage
Perfect in One Direction
Fluorescence
Often Fluorescent White or Yellow Under LW UV
Rarity
Common
Uses
Collector, Decorative, Industrial
Host rock
Evaporite Deposits, Sedimentary Basins
Typical price
$5-50 for small specimens, $100+ for large display crystals

Where rockhounds find gypsum

56 mapped spots

Classic worldwide localities

  • Naica Mine, Mexico
  • White Sands, New Mexico, USA
  • Red River, Manitoba, Canada
  • Maras, Peru
  • Morocco

U.S. states with gypsum

Each link opens a state-specific list of mapped rockhounding spots that produce gypsum.

Field-hunting tip

Look in evaporite deposits, sedimentary basins country — that is the host setting where gypsum typically forms. If you start seeing halite, calcite, sulfur in float, you are in the right ground. Field specimens usually show a tabular crystals, prismatic, bladed, fibrous habit, so train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in Utah, Wyoming, Missouri — start trip planning there.

Common questions

How do you identify gypsum?+
Mohs hardness is 2. It typically shows a vitreous luster. The streak is white. Common colors include colorless, white, gray, yellow.
Where is gypsum found?+
Notable localities include Naica Mine, Mexico; White Sands, New Mexico, USA; Red River, Manitoba, Canada; Maras, Peru; Morocco.
Can I find gypsum in the United States?+
RockHoundR maps 56 gypsum rockhounding spots across 12 U.S. states — the top states are Utah, Wyoming, Missouri.
How much is gypsum worth?+
Typical asking prices fall in the range of $5-50 for small specimens, $100+ for large display crystals. Quality, size, and provenance can move individual specimens well outside that range.
What rocks look like gypsum?+
Gypsum is most often confused with Anhydrite, Calcite, Talc. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with gypsum?+
Gypsum commonly co-occurs with Halite, Calcite, Sulfur, Aragonite, Celestine. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does gypsum form in?+
Gypsum typically forms in evaporite deposits, sedimentary basins. Working float back to the host body is the standard way to chase a fresh occurrence.
What is gypsum used for?+
Gypsum is used in collector, decorative, industrial.

Find gypsum on the map

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

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