Emerald Mineral Collection - Height: 4.2 cm - Width: 1.8 cm- 18 g - (1)

Absolutely perfect specimen, crystals not large but of the highest quality, an aesthetic collectible specimen.
The genesis of Emerald involves a fascinating interplay of geological forces. It typically forms in metamorphic or magmatic environments, where fluids rich in beryllium interact with rocks containing chromium or vanadium. These elements, often present in schists and pegmatites, are crucial for its vibrant green color. High pressure and temperature are essential, facilitating the crystallization of beryllium aluminum silicate. The presence of chromium or vanadium determines the intensity of the green. Imperfections and inclusions, known as 'jardin', are common, adding to its unique character and the story of its formation within the Earth's crust.