Dolomite is a common carbonate mineral that forms distinct, often saddle-shaped rhombohedral crystals. It is easily distinguished from calcite because it will only effervesce in dilute hydrochloric acid when powdered.

Hardness
3.5-4
Mohs
Luster
Vitreous
Streak
White
Transparency
Translucent

Is this dolomite?

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 dolomite with a known reference. Dolomite sits at Mohs 3.5-4 — softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Dolomite leaves a white streak.
  • 3
    Read the luster
    Hold the specimen under a strong light. Dolomite typically shows a vitreous luster.
  • 4
    Match the color range
    Compare against the expected color range: white, gray, pink, colorless, brown, yellow.
  • 5
    Look at form & habit
    Crystal system: trigonal. Typical habit: rhombohedral crystals with curved faces, massive, granular.

Often confused with

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

Often found alongside dolomite

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

All properties

Chemical formula
CaMg(CO₃)₂
Mohs hardness
3.5-4
Density
2.84 g/cm³
Streak
White
Luster
Vitreous
Transparency
Translucent
Crystal system
Trigonal
Crystal habit
Rhombohedral Crystals with Curved Faces, Massive, Granular
Cleavage
Perfect in 3 Directions
Fluorescence
Often White, Yellow, Or Orange Under SW UV
Rarity
Common
Uses
Industrial, Collector, Construction
Host rock
Sedimentary Carbonate Rocks, Hydrothermal Veins
Typical price
$5-30 thumbnail, $20-150 cabinet

Where rockhounds find dolomite

57 mapped spots

Classic worldwide localities

  • Eugui, Spain
  • St. Gotthard, Switzerland
  • Ontario, Canada
  • Missouri, USA

U.S. states with dolomite

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

Field-hunting tip

Look in sedimentary carbonate rocks, hydrothermal veins country — that is the host setting where dolomite typically forms. If you start seeing calcite, fluorite, barite in float, you are in the right ground. Field specimens usually show a rhombohedral crystals with curved faces, massive, granular habit, so train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in Missouri, Tennessee, West Virginia — start trip planning there.

Common questions

How do you identify dolomite?+
Mohs hardness is 3.5-4. It typically shows a vitreous luster. The streak is white. Common colors include white, gray, pink, colorless.
Where is dolomite found?+
Notable localities include Eugui, Spain; St. Gotthard, Switzerland; Ontario, Canada; Missouri, USA.
Can I find dolomite in the United States?+
RockHoundR maps 57 dolomite rockhounding spots across 12 U.S. states — the top states are Missouri, Tennessee, West Virginia.
How much is dolomite worth?+
Typical asking prices fall in the range of $5-30 thumbnail, $20-150 cabinet. Quality, size, and provenance can move individual specimens well outside that range.
What rocks look like dolomite?+
Dolomite is most often confused with Calcite, Ankerite, Magnesite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with dolomite?+
Dolomite commonly co-occurs with Calcite, Fluorite, Barite, Quartz, Siderite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does dolomite form in?+
Dolomite typically forms in sedimentary carbonate rocks, hydrothermal veins. Working float back to the host body is the standard way to chase a fresh occurrence.
What is dolomite used for?+
Dolomite is used in industrial, collector, construction.

Find dolomite on the map

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

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