Diamond is a native element mineral valued for its hardness and gem potential, with known Chinese sources.
About Diamondextended article
Crystal Structure
Cubic — diamond cubic lattice; sp³ C-C bonds.
Elemental Composition (by mass)
Element
Mass %
Visual
CCarbon
100.00%
Computed from simplified end-member formula. Solid-solution series, water content, and trace substitutions cause real-world variation.
IMA Abbreviation (Whitney-Evans 2010)
Dia
→ Diamond
Carbon polymorph
Standard symbol from American Mineralogist (Whitney & Evans, 2010). Used in thin-section labeling, phase diagrams, and IMA-style species records.
Pronunciation
/ˈdaɪəmənd/
↔ DYE-uh-mund
Greek adamas (invincible)
Lapidary & Faceting Recommendations
Recommended cut:
brilliant
Also seen:
princess, emerald, oval, pear, marquise, cushion
Typical yield:
50% of rough
Maximum brilliance from RI 2.42 + dispersion 0.044 demands 57-facet round brilliant or modified versions. Octahedral rough naturally yields 2 brilliants per crystal.
Despite being the hardest, diamond is brittle; can shatter under a sharp blow.
Luster
adamantine
The reference for "adamantine" luster — from Greek "adamas".
Color Cause (Chromophore)
Chromophore:
N/B impurities + lattice
Mechanism:
various defects
Color produced:
multiple
Type Ia (yellow): N aggregates. Type IIb (blue): B substitution. Type IIa (colorless or pink/brown): lattice defects.
Diaphaneity (Transparency)
transparent
Highly transparent when free of inclusions; "spectroscopic" diamonds are the most transparent.
Magnetism
Category:
diamagnetic
Test result:
Slight repulsion
Pure carbon — diamagnetic.
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
Hardness→ Mohs 10 — scratches everything
Only diamond scratches diamond.
Thermal conductivity→ Very high — feels cold but conducts heat away
Diamond testers exploit this; CVD/HPHT synthetic also conducts.
Glycerin / water test→ Repels water — drop spreads
Old "drop test" — diamond is hydrophobic.
⚠ 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
3.51–3.52
g/cm³
medium
C; characteristic 3.52 SG.
For comparison: water = 1.00, glass ≈ 2.5, quartz = 2.65, corundum ≈ 4.00, galena ≈ 7.50, gold ≈ 19.3.
Synthetics & Imitations
Lab-grown methods
HPHT (high-pressure-high-temp)1954 · GE / De Beers
Cubo-octahedral growth; metallic flux inclusions; phosphorescence under SWUV.
CVD (chemical vapor deposition)1980 · Apollo / Element Six
Tabular crystals; strain patterns; brown overtone (improved by HPHT post-treatment).
Common imitations
Cubic zirconia (CZ)
Higher dispersion (more "fire"), lower hardness; settles at bottom of methylene iodide.
Moissanite (SiC)
Doubly refractive — strong "doubling" of pavilion facets seen through table.
White sapphire
Lower brilliance, doubly refractive, lower hardness (Mohs 9 vs 10).
White topaz / quartz
Lower RI/dispersion than diamond; easily distinguished by refractometer.
Diamond sits at 10 on the Mohs scale —
one of the hardest natural materials known.
Colors:
Streak White
Crystal system Isometric (Cubic)
Type localityGolconda, India (classical)
Native ElementsNative Elements
TL;DR · 1 min read
Diamond (C) is the hardest natural mineral on the Mohs scale (10) and the densest carbon polymorph. Formed at >100 km depth in upper-mantle peridotites, diamonds reach the surface in kimberlite and lamproite pipes.
Diamond (C) is the hardest natural mineral on the Mohs scale (10) and the densest carbon polymorph. Formed at >100 km depth in upper-mantle peridotites, diamonds reach the surface in kimberlite and lamproite pipes. Mengyin (Shandong) and Wafangdian (Liaoning) host China’s only confirmed kimberlite diamond fields. The Cullinan (South Africa, 1905) and Hope (India) diamonds are among the most famous historical specimens.
Diamond is a native element mineral in the diamond group (carbon polymorphs) and has the chemical formula C. It crystallizes in the isometric system and is one of the most visually varied minerals in the collector market. Its combination of structural character and global distribution make it a recognized species in both systematic and aesthetic collections.
Identification & care
Diamond typically forms octahedral (most common), dodecahedral, cubic; also rounded, curved surfaces (tetrahexahedral); twinned 'macles' (flat triangular twins). Its color range is broad, including colorless (most prized), yellow, brown, gray, blue (type iib, boron), pink/red, green, black (carbonado), and orange. The luster is adamantine, the streak is white/colorless, and specimens are typically transparent, translucent, opaque. The cleavage is perfect/octahedral on {111} — 4 perfect cleavage planes; extremely important for diamond cutting. The fracture is conchoidal, which aids identification.
Collector context
How it forms
Diamond forms in primarily in kimberlite pipes (ultrabasic igneous rock) and lamproite at mantle depths (>150 km); also in ultra-high-pressure metamorphic terranes (microdiamonds); placer deposits from eroded kimberlites. It is commonly found in association with olivine, pyrope garnet (g10 = diamond indicator), chromite, ilmenite, enstatite, kimberlite (host rock).
Classic Chinese localities
Diamond is widely represented across Chinese provinces, including Hunan, Inner Mongolia, Tibet, Henan.
Why collectors care
Diamond occupies a rare position: it matters equally to specimen collectors and to the gem trade. Crisp natural crystals with saturated color and good clarity command premium pricing and are among the highest-prestige targets in any systematic collection.
What affects value
Value in Diamond is assessed, in typical order of weight, against: (1) locality provenance; (2) crystal size; (3) transparency and internal clarity; (4) color intensity and saturation; (5) crystal form and termination sharpness; (6) matrix and associated-species aesthetics; (7) gem-cutting potential. Verified locality documentation and cutting potential further elevate collector demand.
Naming history
The name Diamond 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.
Cookies on MyMineralBox
We use a small set of cookies (Google Analytics 4, Stripe checkout, chat) to keep the site working and to understand how visitors use it. You can accept all or decline analytics — checkout-essential cookies are always loaded. See our privacy policy for details.