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Eudialyte Cabochon · Various Shapes

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Eudialyte cabochons from the Kola Peninsula, Russia – one of the few deposits of this rare cyclosilicate in the world. The crimson red contrasts with the surrounding black syenite matrix, creating a pattern unparalleled by other red minerals in the lapidary market. 5 unique numbered pieces, from 23 to 31 mm. Hardness 5-5.5 Mohs; we recommend a closed bezel setting.

Piece Information

Mineral Eudialyte (sodium, calcium, zirconium, and iron cyclosilicate)
Dimensions Nr.1: 31×18×5 mm · Nr.5: 29×15×4 mm · Nr.9: 24×13×4 mm · Nr.10: 23×26×4 mm · Nr.13: 24×14×5 mm
Shape and Back Freeform, flat polished back
Finish Mirror polish
Hardness 5-5.5 Mohs — we recommend a closed bezel setting for protection in everyday rings
Origin Russia (Kola Peninsula)
Treatment Untreated. Color due to iron and manganese in the crystal structure.
Piece Type Unique piece (each number is an individual stone)

This specific piece

Eudialyte grows as trigonal crystals within the alkaline nepheline syenite of the Kola igneous complex. When cutting the cabochon, the lapidary takes advantage of the area with the highest concentration of red, leaving the black syenite matrix as a natural frame. The red-black contrast is an intrinsic part of the stone — no two pieces have the same distribution.

The pieces in this lot are freeform — the silhouette follows the best available color zone in each piece of material, without forcing it into a standard oval or tear shape. Each freeform has individual dimensions indicated in the corresponding variant.

Why eudialyte is a rare mineral

Eudialyte only forms in very specific magmatic environments: alkaline intrusions rich in sodium, zirconium, and iron. The Kola deposits are unique in size and lapidary quality; the other known deposits (Greenland, Canada, Norway) produce much scarcer material in trade.

For which setting does it work

  • Closed bezel setting (925 silver or other precious metals) — recommended due to its 5-5.5 Mohs hardness; red on silver creates a very powerful chromatic contrast; especially effective with darkened silver patina that mimics the syenite matrix
  • Pendants — eudialyte's greatest visual impact is in a pendant, where the stone can be the focal point without the wear and tear of a ring
  • Wire wrap — suitable technique as an alternative; we recommend 925 silver or copper wire to complement the red without diluting it

Eudialyte in lapidary tradition

Eudialyte was mineralogically identified in 1819 by German geologist Friedrich Stromeyer from samples from Greenland. The name derives from the Greek eu dialytos (easily decomposable), referring to its solubility in hydrochloric acid.

In crystal tradition, eudialyte is associated with passion and the energetic movement of the heart — the stone that activates what was dormant.

The symbolic properties attributed to minerals belong to cultural and historical traditions. They are shared for educational purposes, not as medical advice or a substitute for professional care.

How to recognize genuine eudialyte

Genuine eudialyte always appears in a syenite matrix — it is not sold clean and without mother rock, because that contrast is part of the mineral's identity in the lapidary market. The red is characteristically crimson or pink, never the artificial vivid red of dyed resin. Under magnification, eudialyte shows a fine microcrystalline structure, and the black matrix has its own mineral texture (alkali feldspar and nepheline).

Frequently asked questions

How do I choose my piece?

Select the variant number. Each number corresponds to an individually photographed piece. Shapes vary as they are freeform — please check the dimensions of each variant carefully before choosing.

Why do you recommend a closed bezel?

The 5-5.5 Mohs hardness makes eudialyte more susceptible to scratching than quartz. For pendants or earrings, the risk is lower; for everyday rings, the closed bezel protects the edges of the stone.

Does it have any treatment?

Untreated. The crimson-red color is produced by iron and manganese in the mineral's crystal structure. No detectable treatment from lapidary observation.

See also: all cabochons · silversmithing materials.