labradorites
Labradorite is a cryptocrystalline feldspar belonging to the plagioclase series, with a typical composition ranging from low to high albite. First described in 1837 by Professor Karl Andreas Elder, it was named after its common source in the Labrador region of North America, where it was long found in arkose sandstones and as a component of the granite and gneiss associated with the crystalline terrain of the Churchill River area. The mineral is best recognised by its exceptional play of colors, known as labradorescence, a phenomenon that produces flashes of iridescence ranging from pale blue through to green, amber or gold, depending on the orientation and the background of light. This optical effect is caused by light interference within the labradorite's internal layered structure, wherein a glassy or opaque outer shell reflects light that is refracted into the translucent core.
Labradorite is widely used as an ornamental stone in jewelry, carvings, and in decorative objects such as