Variscite Point from Palazuelos · 22x6 mm

Elongated triangular Variscite point from Palazuelos (Zamora), 22×6×4 mm. Clean apple green with ochre veins running longitudinally through the piece. Hand-cut in our lapidary workshop.

Piece Details

This specific piece

The apple green of this point is homogeneous and clean: without dark mottling or gray areas. The ochre veins running from top to bottom are thin and parallel to the direction of the cut, a sign that the lapidary oriented the cut to take advantage of the most stable area of the original fragment.

The slender proportion — 22 mm long compared to only 6 mm wide — makes this point an ideal pendular element. The weight is concentrated at the lower end, giving it a clean and direct drop in a minimalist-mounted pendant.

How Variscite's color is formed

Variscite is a hydrated aluminum phosphate that forms in areas of alteration of aluminic rocks subjected to phosphorus-rich solutions. Its green color — from pale yellow to intense green — comes from traces of chromium and vanadium that replace aluminum in the crystal lattice.

For which setting does it work?

• Closed bezel setting (925 silver or other precious metals) — the bezel embraces the edges of the point and protects the most vulnerable edge. With the elongated triangular shape, a vertical bezel creates a pendant with a clean, geometric silhouette.
• Pendants with prong setting in silver — four prongs at the vertices of the point work well since the base is flat and the piece has no rim.
• Wire wrap — the thin profile and flat base facilitate coiling without the wire slipping; a common technique for minerals of this moderate hardness.

Variscite in lapidary tradition

Variscite was already an ornamental material in Neolithic Europe: variscite beads of Iberian origin have been identified in funerary assemblages of the Catalan and Portuguese megalithic culture, documented as one of the first materials of long-distance exchange between communities in the interior and the peninsular coast. The mineralogical name comes from "Variscia," the Latin name for the Vogtland region (Saxony), where the mineral was first described in 1837.

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 Variscite

Spanish Variscite from Palazuelos has a more earthy and muted apple green than Utah variscite, which is usually more vivid and sometimes confused with turquoise. Under magnification, genuine variscite shows a very fine microcrystalline texture, and the veins are always white or yellowish — interstitial quartz or calcite — never black like in turquoise. Its low hardness (3.5–5 Mohs) is another indicator: a metal clip easily scratches it, while glass or resin — common imitations — are harder.

Frequently asked questions

Has this variscite been treated or stabilized?

No. The piece presents the natural apple green color of the mineral, without dyeing, impregnation, or stabilization treatments. No detectable treatment. Statement based on lapidary observation; the piece does not include formal gemological certification.

What setting do you recommend for this point?

We recommend a closed bezel setting in 925 silver. Variscite, with 3.5–5 Mohs, is relatively soft, and exposed edges — especially the tip's edge — are vulnerable to scratches with everyday use. The bezel protects them without hiding the triangular shape.

Why is Variscite from Palazuelos special?

It comes from a Spanish deposit with limited production and archaeological roots dating back to the Neolithic. It is different from commercial Variscite from Utah or Australia and offers jewelers a verifiable Iberian origin and a more earthy green, difficult to find on the market.

See also: cabochons · full lapidary collection.