Calcite is one of the most common minerals on Earth, occurring in a vast array of crystal habits and colors. It is easily identified by its rhombohedral cleavage, its hardness of 3 on the Mohs scale, and its immediate reaction to dilute hydrochloric acid.
Spotting calcite in the field
Field marks- 1
Fizzes vigorously in dilute acid, which is the definitive test
- 2
Three cleavage directions producing leaning rhombs, never right-angle blocks
- 3
Soft at 3, marked easily by a knife or a copper coin
Calcite is the most common mineral in any limestone country and its acid test is the most reliable single field test in mineralogy. A drop of vinegar will usually do it if you have nothing stronger. Its clear rhombic cleavage fragments show strong double refraction, so a line viewed through one appears doubled, which is a memorable demonstration. It takes an enormous range of crystal forms, more than any other mineral, so shape alone will not identify it.
Straight answers
- Is it worth cutting?
- Too soft for wear. Banded ornamental calcite is carved into bowls and bookends and is widely and misleadingly sold as onyx.
- What is it really worth?
- Very low as material, since it is everywhere. Fine crystal specimens, notably from Elmwood in Tennessee, are genuinely collectible.
- Can you legally keep it?
- Ordinary personal-use collecting rules apply. Active quarries are private and usually accessible only through club visits.
Often confused with
Calcite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Hardness and acid. Calcite is 3 and fizzes, quartz is 7 and does not.

How to tell apart: Dolomite fizzes only weakly and usually only when powdered or in warm acid. Calcite fizzes readily in cold dilute acid.

How to tell apart: Barite is strikingly heavy for a pale mineral and does not fizz.
Often found alongside calcite
Minerals reported to co-occur with calcite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaCO₃
- Mohs hardness
- 3
- Density
- 2.7102 g/cm³
- Streak
- White
- Luster
- Vitreous; pearly on cleavages and {0001}
- Transparency
- Transparent to opaque
- Crystal system
- Trigonal
- Crystal habit
- Rhombohedral, prismatic, scalenohedral, massive, stalactitic
- Cleavage
- {1011}, perfect
- Fluorescence
- Yellow under SW and LW UV
- Rarity
- Common
- Uses
- Collector, Decorative, Industrial, Optical
- Host rock
- A major rock-forming mineral; in limestones, marbles, chalks, a common cement in clastic sedimentary rocks, and as gangue in hydrothermal veins; in alkalic to mafic igneous rocks; common as speleothems in caves
Where rockhounds find calcite
231 mapped spotsClassic worldwide localities
- Rossie and Balmat, St. Lawrence Co., New York, USA
- Hancock, Houghton Co., and in the Phoenix mine, Keeweenaw Co., Michigan, USA
- Galena, Cherokee Co., Kansas, USA
- Picher, Ottawa Co., Oklahoma, in the Tri-State district, USA
- Helgustadanáma mine, Reydarfjord, Iceland
- Alston Moor, Egremont, and Frizington, Cumbria, England
U.S. states with calcite
Each link opens a state-specific list of mapped rockhounding spots that produce calcite.
- Missouri29 spots
- Utah21 spots
- New Jersey13 spots
- Pennsylvania13 spots
- New York12 spots
- North Carolina10 spots
- Tennessee10 spots
- West Virginia10 spots
Field-hunting tip
Where it forms: A major rock-forming mineral; in limestones, marbles, chalks, a common cement in clastic sedimentary rocks, and as gangue in hydrothermal veins; in alkalic to mafic igneous rocks; common as speleothems in caves. If you start seeing dolomite, celestine, fluorite in float, you are in the right ground. Typical habit: rhombohedral, prismatic, scalenohedral, massive, stalactitic. Train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in Missouri, Utah, New Jersey. Start trip planning there.








