Description
Labradorite Palmstone – Genuine Polished Crystal Specimen
This beautiful Labradorite Palmstone is a genuine polished crystal specimen, carefully selected for its attractive natural colour, smooth hand-shaped form and striking mineral character. Labradorite is one of the most recognisable feldspar minerals, admired by collectors for its distinctive optical display known as labradorescence. Depending on the angle of light, Labradorite can show flashes of blue, green, gold, yellow, silver or occasionally coppery tones across a darker grey to smoky base.
This listing is for the actual Labradorite Palmstone shown in the photo, so the specimen you see is the specimen you will receive. Full sizing can be seen in the photo. This crystal also includes a Certificate of Authenticity lifetime guarantee generic card, making it a suitable choice for mineral collectors, crystal enthusiasts, display collections, gifting, photography props, cabinet specimens and decorative natural history displays.
Mineral Type and Crystal Species
Labradorite is a plagioclase feldspar mineral, part of the feldspar group, which is one of the most abundant mineral groups in the Earth’s crust. Its chemical composition is a calcium-rich sodium aluminium silicate, commonly represented within the albite–anorthite feldspar series. Labradorite is especially valued for its internal light-reflecting structure, where very fine microscopic layers within the mineral split and reflect light to create colourful flashes across the surface.
As a palmstone, this specimen has been shaped and polished to produce a smooth, rounded form that highlights the natural colour play of the stone. The polished surface allows the labradorescence to be viewed more clearly, especially when the specimen is turned under natural or bright light. Each piece of Labradorite is naturally individual, with variation in flash intensity, base colour, patterning and surface markings.
Geology and Formation
Labradorite typically forms in igneous rocks such as basalt, gabbro, norite and anorthosite. These rocks crystallise from molten magma, allowing feldspar minerals to develop as the rock cools. The colourful optical effect in Labradorite is not caused by surface coating or dye, but by light interacting with internal lamellar structures within the mineral. This makes each specimen visually unique, with colour flashes that may appear, disappear or change depending on viewing angle.
Labradorite was originally named after Labrador in Canada, where notable material was historically recorded. Today, Labradorite is found in several parts of the world, with well-known sources including Canada, Madagascar, Finland, Norway, and other feldspar-bearing geological regions.
Appearance and Display Features
This Labradorite Palmstone has a naturally decorative appearance, with a polished finish that enhances its mineral detail and colour variation. The palmstone form is ideal for display in a crystal collection, mineral cabinet, curiosity shelf, study desk, natural history display or gift box. Its smooth finish makes it visually appealing from multiple angles, while the feldspar structure gives the stone a classic collector appeal.
Labradorite is especially popular with buyers looking for a genuine polished mineral specimen with strong visual interest. Its combination of dark base colour and shifting light flashes gives it a distinctive look compared with many other polished crystals. Small natural surface features, colour zoning, internal lines, mineral inclusions or tiny polishing marks may be present, all of which are normal for a genuine natural stone specimen.
Certificate of Authenticity
This Labradorite Palmstone is supplied as a genuine crystal specimen and includes a Certificate of Authenticity lifetime guarantee generic card. It has been carefully chosen as an individual piece, and the photograph shows the actual specimen you will receive. This makes it a lovely addition to a crystal collection, mineral display, geology-themed gift, natural décor arrangement or educational specimen collection.







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