In the Home
Where it belongs
Labradorite belongs where the light moves through the day — a desk beside a window, a shelf that catches the late sun. It rewards the person who walks past it twice and looks the second time.
Formation
How it came to be
It forms in the slow-cooling hearts of ancient basaltic intrusions, deep in the crust where molten rock loses its heat over thousands of years.
Labradorite is a feldspar — one of the most common mineral families on Earth — but a rare and particular one. It crystallises as mafic magma cools slowly underground, allowing microscopic layers of differing composition to separate within the growing crystal.
First described in the 18th century from the coast of Labrador, it is now found in quantity in Madagascar and Finland. The stones we select are typically hundreds of millions of years old.
Its signature optical effect has a name of its own: labradorescence — the shifting play of colour that appears only at certain angles.
The Object
The flash is not a surface trick. Light entering the stone is scattered by the fine internal lamellae and returned as colour. We choose freeforms with broad, mobile flash and a polish that lets the colour travel freely across the whole face.
Closer In
Under magnification the interior reveals parallel lamellae — the twinned layers that split incoming light into its spectrum, the physical cause of the colour that seems to float above the stone.
Packaging
Designed to be kept, not discarded.
- Museum-inspired specimen card
- Object provenance and formation notes
- Protective presentation materials
- Designed to be kept, not discarded
Previously Stewarded
This specimen, continued
Examples of Labradorite returned through Continue the Story and offered for a new steward, with records intact.
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From the Journal