Hard facts about
the hardest gem

Diamond's properties emerge from one elegant fact: every carbon atom shares a covalent bond with its four nearest neighbours in a rigid tetrahedral lattice. This arrangement makes diamond simultaneously the hardest, least compressible, and one of the most thermally conductive materials ever measured.

Mohs Hardness10 / 10
Thermal Conductivity2,200 W/m·K
Refractive Index2.42
Dispersion (fire)0.044
Density3.52 g/cm³
  • Crystal System: Cubic (Isometric) Diamond crystallises in the cubic system with Fd3̄m space group symmetry. Each carbon sits at the centre of a tetrahedron formed by its four neighbours — a perfectly symmetric geometry repeated billions of times.
  • Cleavage: Perfect Octahedral Despite supreme hardness, diamond cleaves perfectly along {111} planes. Skilled cutters exploit this to split rough stones — a counter-intuitive vulnerability in the hardest substance on Earth.
  • Electrical Insulator (usually) Pure diamond is an exceptional electrical insulator with a bandgap of 5.5 eV. Boron-doped blue diamonds are semiconductors — a rare quirk exploited in quantum computing research.
  • Stable at Room Temperature Graphite is thermodynamically more stable than diamond at atmospheric pressure, yet the energy barrier for conversion is so high that diamonds are effectively permanent on human timescales.
  • Forms 160 km Underground Diamonds crystallise in the lithospheric mantle at depths of 150–250 km, then travel to the surface inside kimberlite and lamproite magmas that ascend in explosive volcanic eruptions.
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The Four C's

Developed by the Gemological Institute of America (GIA) in the 1940s and 50s, the 4 Cs are the universal language for assessing diamond quality. They give buyers and sellers a common framework built on measurable standards.

C

Cut

The most important C. Cut governs how well a diamond interacts with light — its brightness (white light reflection), fire (coloured flashes), and scintillation (sparkle when moved). Grades range from Excellent to Poor. A well-cut stone returns almost all entering light back through the table; a poorly cut one lets light leak out the sides or bottom.

C

Colour

GIA grades colourless-to-yellow diamonds D through Z. D is perfectly colourless — the rarest and most valuable. Most diamonds sold in jewellery fall in the G–J "near-colourless" range, where colour is difficult to detect face-up. Separately, "fancy colour" diamonds — natural blues, pinks, greens, reds — sit on their own scale and command enormous premiums.

C

Clarity

Clarity measures internal inclusions and external blemishes, graded from Flawless (FL) through Included (I3). Inclusions form during crystallisation — tiny crystals, gas bubbles, or fractures captured inside the stone. Flawless diamonds are extraordinarily rare; VS1-VS2 (Very Slightly Included) offers an excellent balance of quality and value for most buyers.

C

Carat

A carat is exactly 0.200 grams — divided into 100 points. The word derives from the carob seed, historically used as a weight reference. Price per carat rises non-linearly with size because large gem-quality diamonds are exponentially rarer: a 2-carat diamond typically costs more than four times a comparable 1-carat stone.

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Diamond Types

Type Ia

The most common variety (~98% of natural diamonds). Contains clusters of nitrogen atoms. Usually colourless to faint yellow. Cape-series diamonds are Type Ia.

Type IIb — Blue

Boron replaces some carbon atoms, creating a blue colour and making these diamonds natural semiconductors. Includes the legendary 45.52-carat Hope Diamond.

Type IaB — Yellow / Orange

Nitrogen in a particular aggregated form creates vivid yellow or orange "fancy" hues. Canary yellow diamonds are among the most popular fancy colours.

Type IIa — Pink / Red

The chemically purest diamonds, almost free of nitrogen. Pink and red colours arise from plastic deformation of the crystal lattice — no impurity needed, just pressure.

"Diamond is the hardest substance known, yet it can be cut — an apt metaphor for perseverance meeting skill."
— Gemological Institute of America