Both routes start from the same basic principle: diamond is simply carbon arranged in a specific crystal lattice, and if you recreate the conditions that force carbon into that lattice, you get diamond, regardless of whether that happens a hundred miles underground over a billion years or inside a steel chamber over a few weeks. The two commercial methods, CVD and HPHT, get there by different physical routes, and knowing how each works explains both why the resulting stones are genuine diamond and how a gemmological lab can still tell them apart from mined material.

CVD: building diamond layer by layer

Chemical vapour deposition, CVD, is the newer and now more common of the two growth methods for gem-quality stones. A thin sliver of diamond, called a seed, is placed inside a sealed chamber and heated to around 800°C. The chamber is filled with a carbon-rich gas, typically methane, mixed with hydrogen, and the gas is ionised into a plasma using microwave energy. This breaks the methane down and lets carbon atoms drift down and attach to the seed one layer at a time, gradually building up a single diamond crystal from the bottom up.

Because the diamond grows in discrete layers, CVD stones typically form as a flat, cube-shaped block with a single dominant growth direction. That layering is not just a manufacturing detail; it leaves behind a structural signature that survives into the finished, cut stone and is one of the main things a lab looks for when testing origin.

HPHT: recreating the earth's own conditions

High pressure, high temperature, HPHT, is the older method and was originally developed to make industrial-grade diamond for cutting and abrasive tools before gem-quality production became viable. It works by putting a small carbon source, along with a tiny diamond seed, into a press capable of generating roughly 5-6 gigapascals of pressure and temperatures around 1,300-1,600°C, conditions that approximate what happens naturally in the earth's mantle. Under that pressure and heat, the carbon source dissolves and then recrystallises around the seed, building outward in multiple directions at once rather than in flat layers.

That multidirectional growth is why HPHT diamonds tend to form in a cuboctahedron shape, with up to fourteen distinct growth sectors, and why they can trap tiny flecks of the metal flux used in the growing process, something CVD stones do not do in the same way.

Why both count as real diamond

The atomic arrangement inside a CVD or HPHT diamond is identical to a mined diamond: carbon atoms bonded in the same tetrahedral lattice, with the same hardness, refractive index, thermal conductivity and optical properties. There is no chemical or physical test that distinguishes "real" diamond from "lab" diamond, because both are diamond in the full mineralogical sense. The only meaningful distinction is origin and formation history, not composition. Standard diamond testers that check thermal conductivity will register a lab-grown stone as diamond in exactly the same way as a mined one, which is precisely why testing for origin requires more specialised equipment than a jeweller's basic screening tools.

How labs actually prove origin

Given that a loupe and a thermal tester cannot separate the two, gemmological laboratories rely on a combination of structural, optical and spectroscopic evidence.

Growth pattern imaging. Instruments such as GIA's DiamondView use ultraviolet light to make a stone's internal growth structure visible under magnification. A CVD diamond typically shows parallel striations running through the stone, the visible trace of its layer-by-layer construction. An HPHT diamond shows a more angular, sector-based pattern reflecting its multiple growth directions, often described as resembling a faceted, blocky pattern rather than natural diamond's more random, often cloud-like growth zoning. Mined diamonds, having grown slowly and irregularly over geological time, show internal structures that look distinctly different from either.

Fluorescence behaviour. Under long- and short-wave ultraviolet light, diamonds can fluoresce, and the pattern matters more than the presence of fluorescence itself. Mined diamonds that fluoresce tend to do so relatively evenly across the stone; lab-grown stones, particularly CVD ones, are more likely to show patchy, sector-based or graphic fluorescence patterns that echo their growth structure. Roughly a third to half of mined diamonds show some fluorescence, so fluorescence alone is not diagnostic, but the pattern combined with other evidence is useful.

Spectroscopy. This is where identification becomes close to definitive. Photoluminescence and infrared spectroscopy detect trace defects in the crystal lattice that differ predictably by growth method. CVD-grown diamonds commonly show a silicon-vacancy defect, detectable as a sharp emission at 737 nanometres, a byproduct of the silicon components used in CVD growth chambers, which almost never appears in mined stones. HPHT-grown diamonds often show a distinct pattern of nitrogen-related defects and, in some cases, a measurable magnetic response caused by trace metallic flux inclusions from the growth process, something natural diamond formation essentially never produces. Carbon isotope ratios also differ in aggregate between mined and lab-grown populations, giving labs another independent line of evidence.

Laser inscription. Separately from any of the physical testing, reputable growers and labs laser-inscribe the girdle, the thin band around a diamond's widest point, with text identifying the stone as laboratory-grown, often alongside the certificate number and the grading lab's name. This inscription is microscopic and invisible to the naked eye but readable under magnification, and it means origin can be confirmed by simply reading the stone itself rather than needing to run a full spectroscopic panel every time.

Taken together, these methods mean that no lab-grown diamond can currently pass as mined to a properly equipped gemmological laboratory. The physical evidence of growth method is built into the crystal itself and cannot be polished away or disguised by cutting.

Post-growth treatment

As-grown CVD diamonds often come out of the chamber with an unwanted brownish tint, caused by structural defects that form during the deposition process. It has become standard industry practice, affecting the large majority of CVD production, to treat these stones with a second, brief HPHT process after growth. This does not add any material to the diamond; it rearranges the lattice at an atomic level to neutralise the colour centres responsible for the brown tint, permanently improving the stone's colour grade. It is a well understood, stable and disclosed process, not a cosmetic trick, and a properly graded certificate will note that the treatment took place.

The certification landscape

Lab-grown diamonds are graded by the same major gemmological institutes that grade mined stones, but the market has settled differently across them. IGI, the International Gemological Institute, has become the dominant lab for lab-grown certification by a wide margin, largely because of its established presence in the Indian and Chinese manufacturing hubs where most gem-quality lab-grown production happens. IGI issues lab-grown reports on the standard 4Cs framework, using the same D-to-Z colour scale and Flawless-to-Included clarity scale as its mined diamond reports, distinguished mainly by the report's yellow rather than white colouring and an explicit statement of growth method.

GIA holds a much smaller share of lab-grown certification and, in October 2025, changed its approach substantially. Rather than continuing to issue precise letter and number grades for colour, clarity and cut, GIA now classifies qualifying lab-grown diamonds as either "Premium" or "Standard" based on combined thresholds across all three factors. Premium requires VVS clarity or better, D colour, and excellent polish, symmetry and cut. Standard covers a wider band, from VS clarity and E-to-J colour upward, provided polish, symmetry and cut are at least very good. GIA's stated reasoning is that over 95% of lab-grown production now clusters tightly within a narrow high-quality range, and that assigning granular letter grades risked implying a false equivalence with the far more variable population of mined diamonds, where a precise grade carries more genuine differentiating information.

The practical effect for anyone reading a certificate is that a lab-grown diamond's paperwork may look meaningfully different depending on which lab issued it, and a simplified Premium or Standard classification is not directly comparable, grade for grade, with a full 4Cs report from IGI or with a mined diamond's GIA certificate.

The bottom line

CVD and HPHT are simply two different physical routes to the same result: real diamond, built from carbon in the same crystal lattice as a mined stone, with no meaningful difference in hardness, brilliance or chemical composition. What differs is how each method leaves its mark on the crystal, whether as CVD's layered growth striations and silicon-vacancy signature, or HPHT's sector-based structure and occasional magnetic response, and it is that internal fingerprint, read through DiamondView imaging, fluorescence patterns and spectroscopy, that lets a gemmological lab identify origin with certainty. Combined with girdle inscription, this means lab-grown origin is always verifiable rather than a matter of trust. The one area where the paperwork genuinely varies is grading format: IGI still issues full 4Cs reports for lab-grown stones, while GIA has moved to a simplified Premium/Standard system, so it is worth checking which lab issued any certificate before comparing two stones side by side.