Property Comparison

Property Pyrope Garnet Spinel Diagnostic?
RI 1.730 – 1.760 1.712 – 1.736 No
SG 3.62 – 3.87 3.57 – 3.63 No
Hardness 7 – 7.5 7.5 – 8 No
Crystal System Cubic Cubic No
Optic Character SR (singly refractive) SR (singly refractive) No
Birefringence None None No
Fluorescence (LW) Inert Variable (strong in red/pink varieties) Yes
Chelsea Filter Variable Variable No
Pleochroism None None No
Spectroscope Almandine (iron) spectrum No almandine spectrum Yes

The Definitive Tests

  1. Spectroscope — the almandine spectrum. Pyrope garnet shows the iron absorption spectrum inherited from its almandine component; spinel does not. When the RI reading lands in the 1.730-1.736 overlap zone, this is the test that decides the call.
  2. LW UV — fluorescence. Pyrope is inert under long-wave UV. Spinel's fluorescence is variable, but red and pink spinels commonly fluoresce strongly. A distinct red glow under the lamp points away from garnet.
  3. Refractometer — RI position. Spinel reads 1.712-1.736; pyrope reads 1.730-1.760. A reading below 1.730 indicates spinel and a reading above 1.736 indicates pyrope. Only the narrow 1.730-1.736 overlap is ambiguous — that is when you reach for the spectroscope. Under the microscope, spinel's characteristic octahedral crystals are a further pointer; per the reference data, inclusions help separate the pair.

Common Mistakes

Frequently Asked Questions

Can the refractometer separate pyrope garnet from spinel?

Sometimes. Spinel reads 1.712-1.736 and pyrope reads 1.730-1.760, so readings outside the 1.730-1.736 overlap are decisive. Inside the overlap, the refractometer alone cannot make the call — the spectroscope and UV fluorescence separate them.

What is the best test to separate pyrope from spinel?

The spectroscope. Pyrope shows an almandine (iron) absorption spectrum that spinel lacks. Long-wave UV supports it: pyrope is inert, while red and pink spinels commonly fluoresce strongly.

Why do exams love the pyrope-vs-spinel separation?

Because both stones are singly refractive, cubic, and red, with overlapping RI and SG. It is one of the few common separations where the refractometer and polariscope can both fail to decide, forcing candidates to use the spectroscope, UV lamp, and microscope correctly.

Identifying a red stone? GemID walks you through spectroscope, UV, and refractometer tests step by step.

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Studying for a gemology practical? The SR-red separation is a practical-exam classic. GemID’s timed exam simulators drill exactly this call — separating look-alike stones by their measured properties.

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