amuinehape

Amuinehape is a rare and unique mineral species discovered in the late 20th century. It was first identified in the Amu Darya River basin in Uzbekistan, a region known for its diverse mineralogy. The mineral is characterized by its distinctive crystal structure and vibrant blue color, which is a result of the presence of copper ions within its lattice.

Amuinehape crystallizes in the monoclinic system, forming prismatic crystals that can reach up to 2 centimeters in length. Its hardness on the Mohs scale is approximately 4.5, making it relatively soft and susceptible to scratching. The mineral is typically found in association with other copper-bearing minerals such as malachite and azurite.

The chemical formula of amuinehape is Cu5(SiO4)2(OH)4, indicating its composition of copper, silicon, oxygen, and hydrogen. This formula highlights the mineral's copper content, which contributes to its blue color. Amuinehape's formation is believed to occur through the alteration of copper-rich rocks under specific geological conditions.

Due to its rarity and unique properties, amuinehape is of interest to mineral collectors and researchers studying the geochemistry of copper-bearing minerals. However, its limited occurrence and small crystal sizes make it a challenging mineral to find and study. Despite its rarity, amuinehape's discovery has contributed to the ongoing exploration and understanding of the Earth's mineral diversity.