What this is. A genuine curriculum in the technique of gem identification — the instruments, the measurements, and the order to use them in. Everything it links to is published on this site and free to read.

What it is not. This is not an accredited qualification and it does not replace GIA, Gem-A or FEEG. Those award recognised professional credentials assessed on graded stones under exam conditions, and nothing online substitutes for that. If you intend to work in the trade, you will want one of them. This course exists so you can learn the craft — and find out whether you love it — before you commit several thousand dollars to finding out.

The course

1

What gem identification actually is

Why appearance is the weakest evidence there is, and what replaces it.

Two stones that look identical can be a $12,000 ruby and a $40 garnet. Colour, cut and clarity tell you almost nothing about species, because different minerals share the same appearance and the same mineral appears in many colours. Identification works the other way round: you measure physical constants that do not change with appearance — how much the stone bends light, how dense it is, how it behaves under polarised light — and eliminate everything those measurements rule out. You rarely "recognise" a stone. You narrow 130 candidates down to one.

2

Colour: how to use it without being fooled

Colour is the weakest evidence and the strongest filter. Both are true.

Never conclude from colour — but always start from it. Body colour cannot identify a species, yet it eliminates most of the database instantly, which makes it the cheapest first move you have. The discipline is to treat it as a filter that narrows the field, then let a measurement decide among what survives.

3

The refractometer

The single most discriminating instrument in the kit.

Refractive index is a physical constant set by a mineral's atomic structure. One good reading typically cuts the field further than every other test combined. This lesson covers taking a reading, why a shadow edge forms at all, the sliding technique that gets you a clean edge, and what "over the limit" means — a standard refractometer reads to about 1.81, which is the ceiling of the contact liquid rather than of the stone. OTL is a result, not a failure.

4

Specific gravity

The second measurement, and the one that finishes most identifications.

Specific gravity is density relative to water, measured by hydrostatic weighing: weigh the stone in air, then suspended in water. It works on rough and irregular stones with no polished facet — exactly the ones a refractometer struggles with. RI and SG together usually reduce the candidate list to one or two species.

5

Optic character and the polariscope

Singly or doubly refractive — a fast, decisive split.

A polariscope tells you whether light travels through the stone at one speed or two. That single observation splits the database roughly in half and costs seconds. On a doubly refractive stone you record two refractometer readings, and the difference between them — the birefringence — is diagnostic in its own right.

6

Pleochroism and the dichroscope

When a stone shows you two colours at once.

Some doubly refractive stones show different body colours along different crystal directions. A dichroscope makes that visible in seconds, and trichroism — three distinct colours — is only possible in a biaxial stone, which is a genuine structural deduction rather than an impression.

7

Ultraviolet fluorescence

Useful, wildly over-trusted, and worth learning properly.

Many stones glow under UV, and the response can support an identification or flag a treatment. It is also the test beginners over-read: fluorescence is variable within a species, so it corroborates rather than decides. Learning where it is diagnostic and where it is noise is most of the skill.

9

Hardness — and why you rarely test it

The famous property that working gemologists mostly avoid using.

Every beginner's guide leads with the Mohs scale. Real practice barely uses it, because a scratch test damages the stone and a destructive test on someone else's property is not an option. Learn the scale for what it tells you about durability, wear and setting — not as an identification step.

10

Your first identification

Putting the sequence together on an unknown stone.

Order matters: observe, then measure the cheap decisive things first, and stop when the evidence converges. This lesson walks the whole sequence on a stone you have never seen, including how to record observations so the reasoning stays auditable — which is what separates an identification from a guess.

11

Natural, synthetic, and treated

Same species, same constants, entirely different value.

A synthetic ruby is really ruby: identical RI, identical SG. Separating grown from mined is a different discipline built on inclusions, growth structures and fluorescence patterns rather than constants — and it is where most of the money and most of the mistakes are.

12

The stones that fool people

The specific confusions worth memorising.

A handful of pairs account for most misidentifications. Learning them by their separations — which single test splits each pair — is worth more than memorising a hundred species you will never encounter.

Practise what you have read. The Loupewise app takes your actual measurements and shows which of the 130 species remain consistent with them — and which test eliminates the most candidates next.

Open the app

Common questions

Is this gemology course really free?

Yes. All 12 lessons and the full reference database of 130 species are free to read, with no enrolment and no account. Loupewise sells a subscription for the identification app and practice exams; the course itself is not gated.

Does this replace a GIA or Gem-A qualification?

No, and it does not pretend to. Those are recognised professional credentials assessed on graded stones under exam conditions. This teaches the underlying technique so you can decide whether the work suits you before committing to a programme.

Do I need to buy instruments to start?

Not for the first two lessons. From lesson 3 you get far more out of it with a refractometer and a way to weigh a stone in water. Reading first is the cheapest way to decide whether the kit is worth buying.

How long does it take?

It is self-paced. Reading through takes a few hours; acquiring the skill takes practice on real stones, which is why every lesson points at data and drills you can work with afterwards.