Raw Labradorite Slice

Analytical Breakdown Notes

Pattern & Transparency ►

The broad, fiery flash planes displayed across these slices are generated by ultra-thin alternating structural layers buried deep within the stone's interior. When direct light strikes these internal planes, it bounces between the minute structural boundaries to create vivid golden, orange, and violet sheen against an otherwise dark host matrix.

Variety & Mineral Group ►

This specimen represents a highly prized variety within the broader feldspar mineral family, known for producing remarkable optical displays across polished surfaces. Its dense, interlocking crystalline growth structure provides exceptional structural stability, allowing artisan cutters to shape smooth, flat collector slices that showcase full internal refraction.

Estimated Age ►

Geological surveys date the primary formation window of these Madagascan deposits to roughly 1.3 billion years ago during the Proterozoic Era. Deep magma chambers cooled at extraordinarily slow rates miles beneath the Earth's crust, providing the centuries of undisturbed temperature stability needed to build complex internal layered structures.

Deposits ►

While noble specimens occur in select high-grade zones across Canada and Scandinavia, this specific batch comes directly from the rich coastal mineral zones of southern Madagascar. Local geology in this region produces an uncommonly high concentration of rare warm-spectrum reflections, spanning golden amber, bronze, deep magenta, and twilight violet.