Approximate retail prices. Wholesale + private sale typically 40-60% of retail. Auction premium 10-25%. For investment-grade purchase steps, see the investment checklist.
Crystal Structure
Trigonal carbonate — CO₃²⁻ groups stacked normal to c-axis.
External databases provide CIF (Crystallographic Information File) downloads + interactive 3D viewers. AMCSD: American Mineralogist Crystal Structure Database (free, RRUFF-hosted). COD: open community-curated database.
Elemental Composition (by mass)
Element
Mass %
Visual
OOxygen
47.96%
CaCalcium
40.04%
CCarbon
12.00%
Computed from simplified end-member formula. Solid-solution series, water content, and trace substitutions cause real-world variation.
Most-documented mineral on Mindat (1000+ localities)
IMA Abbreviation (Whitney-Evans 2010)
Cal
→ Calcite
Carbonate — most common
Standard symbol from American Mineralogist (Whitney & Evans, 2010). Used in thin-section labeling, phase diagrams, and IMA-style species records.
Pronunciation
/ˈkælsaɪt/
↔ KAL-site
Latin calx (lime)
⚠ Safety & Handling
⚗acid-sensitivehigh
Dissolves in even dilute acids — including white vinegar.
Handling: Never use ANY acid cleaner. Distilled water OK for brief rinse. pH-neutral specimen cleaners only.
Information provided in good faith. Consult local hazmat regulations for transport and disposal. Severely hazardous specimens may require special storage cabinets.
UV Fluorescence
SW (254 nm)
Red / orange
strong
LW (365 nm)
Red / orange
moderate
Mn-activated calcite; Franklin variety especially bright. Red SW + green willemite makes the Franklin "two-color" effect.
SW = shortwave (germicidal lamp). LW = longwave (blacklight). Response varies with locality, trace impurities, and treatment.
Aragonite transforms to calcite over geological time — most older shells are now calcite pseudomorphs.
Universal in older limestones.
A pseudomorph (Greek "false form") is a mineral with the external shape of another species — the chemistry has changed but the crystal habit is inherited. › Full catalogue
Tenacity
Behavior:
brittle
Under stress:
Cleaves into rhombs
Rhombohedral cleavage — taps produce small rhombs.
Iceland spar is famously transparent (double refraction).
Magnetism
Category:
diamagnetic
Test result:
Slight repulsion
CaCO₃ — historically used by Faraday to demonstrate diamagnetism.
Test with rare-earth magnet (N42 or N52 neodymium). Suspend specimen on thread for sensitive paramagnetic detection. Diamagnetic minerals are weakly repelled (visible only with strong magnets like bismuth).
Diagnostic Field Tests
HCl test→ Vigorous effervescence (CO₂)
Cold dilute HCl on fresh surface fizzes immediately. Diagnostic for calcite.
Cleavage test→ Perfect rhombohedral cleavage
Tap with steel point — rhombs split cleanly.
⚠ Use dilute HCl (~10%) only on inconspicuous spots; rinse promptly. Smell-tests should be brief and ventilated. Taste-test ONLY halite/sylvite — never lead, arsenic, or sulfur minerals.
Specific Gravity
2.71–2.72
g/cm³
light
CaCO₃; standard carbonate reference.
For comparison: water = 1.00, glass ≈ 2.5, quartz = 2.65, corundum ≈ 4.00, galena ≈ 7.50, gold ≈ 19.3.
Streak Test
white
White streak. Fizzes in cold HCl.
Streak = color of the powdered mineral. Drag specimen across unglazed white porcelain plate (Mohs 6.5). For minerals harder than the plate, crush a small flake into powder and observe color.
Calcite is the workhorse of the carbonate world — common, but capable of producing some of the most spectacular crystal habits in mineralogy. Chinese calcites from Hunan and Hubei rank among the largest and most aesthetic ever recovered.
Text size:AAA
Calcite is the workhorse of the carbonate world — common, but capable of producing some of the most spectacular crystal habits in mineralogy. Chinese calcites from Hunan and Hubei rank among the largest and most aesthetic ever recovered.
Daye and Tonglushan mines in Hubei have produced museum-quality golden scalenohedral calcite crystals exceeding 30 cm. The Shangbao Mine in Hunan is famous for translucent orange "tooth" calcites perched on pyrite or fluorite matrices.
Your specimen will scratch: 👆 Talc dust (Mohs 1) · 💅 Fingernail (Mohs 2.5)
Always test on an inconspicuous edge first. Save the test for unimportant specimens — better to use a streak plate or knowledge of locality + paragenesis.
Cite this entry
APA
MyMineralBox Editorial Team. (2026). Calcite. My Mineral Box. Retrieved May 23, 2026, from https://mymineralbox.com/mineral-encyclopedia/minerals/calcite/
MLA
MyMineralBox Editorial Team. "Calcite." My Mineral Box, 2026, https://mymineralbox.com/mineral-encyclopedia/minerals/calcite/. Accessed May 23, 2026.
Chicago
MyMineralBox Editorial Team. "Calcite." My Mineral Box. Last modified May 4, 2026. https://mymineralbox.com/mineral-encyclopedia/minerals/calcite/.
BibTeX
@misc{mmb_calcite,
author = {{MyMineralBox Editorial Team}},
title = {{Calcite}},
year = {2026},
publisher = {My Mineral Box},
url = {https://mymineralbox.com/mineral-encyclopedia/minerals/calcite/},
urldate = {2026-05-23}
}
Identification & care
Specimens usually show rhombohedral, scalenohedral, prismatic, tabular, massive, stalactitic — over 300 documented crystal forms. Its color range is broad, including white, yellow, red, orange, blue, green, brown, gray, and colorless. The luster is vitreous, sub-vitreous, resinous, waxy, pearly, the streak is white, and specimens range from transparent to opaque. The cleavage is perfect rhombohedral {1011}. The fracture is conchoidal, which aids identification.
Collector context
How it forms
In terms of geology, Calcite forms in sedimentary (limestone, chalk), metamorphic (marble), hydrothermal veins; biogenic (shells, coral). It is commonly found in association with dolomite, fluorite, pyrite, quartz, barite.
Classic Chinese localities
Documented Chinese occurrences are recorded at Shangbao Mine, Jiama Cu-polymetallic deposit and Jinduicheng Mine, among others.
Why collectors care
Collectors pursue Calcite for the clarity of its crystal form and, in good material, saturated color that reads instantly across a display case. A well-terminated calcite on clean matrix photographs well, identifies quickly, and anchors a cabinet piece. Top Chinese specimens over the last two decades have reset the bar for what calcite looks like at collector grade.
What affects value
Value in Calcite is assessed, in typical order of weight, against: (1) locality provenance; (2) size relative to the species norm; (3) crystal form and termination sharpness; (4) color saturation and zoning; (5) transparency and internal clarity; (6) matrix quality and aesthetic balance; (7) condition (absence of damage, chips, or repair). Cleaning quality and verified locality documentation act as multipliers across the above.
Naming history
The name Calcite has a specific etymological and historical context — see Mindat's reference entry for provenance details. We have retained naming data at the record level; published prose is paraphrased from factual fields rather than copied from source.