Stone Explorer Garnet group

Garnet is not one stone.

Six members share the same crystal structure. What changes is which atoms sit inside it. Set any two against each other, or trace how one of them grew.

Almandin-Granat: alle Stücke →

File 018 · Six member records

Two ways in · pick one

Each specimen opens its own file.

How to read the wall

One structure. Six chemistries.

A photograph can show colour. It cannot establish which garnet a stone is, where it formed or whether it was treated; composition needs testing.

Structure

One framework

Six members share the same crystal structure. What changes is which atoms sit in the X and Y sites.

Mixtures

Names cover ranges

Gem garnets are often mixtures between members, so names such as Rhodolite describe a composition range and a colour.

Boundary

Colour is not identity

Dark red alone cannot separate Almandine from Pyrope; testing usually gives a composition range rather than one end member.

Sources and image credits

Every claim keeps its scope.

The papers below describe the garnet group, or one specimen somebody else measured. The photo credits describe photographs. None of it proves anything about a BE. lot.

IMA Garnet Supergroup NomenclatureTaxonomy · formulae · group scope
Source
Grew et al., American Mineralogist 98 (2013), 785–811.
Use
Species and end-member nomenclature; garnet structural framework.
Limit
Does not identify a photographed or BE. specimen.
Scope note
The 2013 IMA nomenclature approved 32 species in the supergroup. The six on this page are the familiar gem members.
Link
Open the paper (DOI) · free full text (PDF)
GIA · Garnet DescriptionGemological overview · familiar members
Source
Gemological Institute of America.
Use
Consumer-facing overview of garnet diversity, gem use and familiar species.
Limit
Overview language does not replace specimen testing.
Link
Open GIA Garnet Description
Manzotti et al. · EJM 2025Research figure · CC BY 4.0
Source
European Journal of Mineralogy 37, 455–482 (2025).
Use
Original Figure 3 as an authentic research evidence object.
Limit
Applies to the paper's samples; not to a BE. bead.
Alteration
Local copy displayed without recolouring; responsive resizing only.
Link
Open the article
USGS · Kimberlite Indicator MineralsPyrope chemistry · geological context
Source
U.S. Geological Survey Scientific Investigations Report 2016–5089–A.
Use
Context for indicator-mineral chemistry and exploration limits.
Limit
A red grain or generic Pyrope image is not diamond evidence.
Link
Open the USGS report
GIA · Gem-quality Garnet ClassificationSolid solutions · gem names
Source
Gemological Institute of America, Gems & Gemology.
Use
Relationships among gem-quality mixed compositions and commercial names.
Limit
Classification logic still requires measurements on the stone being named.
Link
Open the GIA paper
Six member photographsOpen licences · reference specimens
Sources
Wikimedia Commons file pages recorded in the local asset ledger.
Licences
Public Domain, CC0 1.0 and CC BY-SA 4.0 depending on image.
Use
Reference appearance only.
Alteration
Previously resized and JPEG-compressed; displayed cropped to plate format with no colour treatment.
Limit
Photographs do not prove the formula or origin of another specimen.
Formation cutaway illustrationGenerated explanatory model · not evidence
Asset
Dedicated text-free cutaway derived from the approved stratigraphic art direction.
Credit
BE. art direction with OpenAI image generation.
Use
Explains one representative sequence from host rock through metamorphism, garnet growth and exposure.
Label
Detail crop · explanatory model · not site data.
Limit
Not a measured field section or pressure-temperature path; cannot establish the provenance or formation history of a BE. product.

Questions about Stone Explorer

What do garnet members share?

Six members share the same crystal structure. What changes is which atoms sit inside it.

How can I compare garnet members?

Set any two members against each other at full size.

What does the garnet formation view show?

The formation view illustrates one Almandine growth sequence, from host rock through metamorphism, garnet growth and exposure.