lumelind

Lumelind is a rare and unique mineral discovered in the late 20th century. It is primarily found in the volcanic regions of Iceland and the Pacific Northwest of the United States. Lumelind is known for its distinctive green color, which is due to the presence of copper and other trace elements. The mineral has a hardness of 5.5 on the Mohs scale and a specific gravity of approximately 3.2. Lumelind is often found in association with other minerals such as quartz, calcite, and pyrite.

The chemical composition of lumelind is complex, with the dominant elements being silicon, oxygen, and copper. The mineral's crystal structure is monoclinic, and it typically forms prismatic crystals. Lumelind is not commonly used in industry due to its rarity and the difficulty in extracting it from its host rocks. However, it is sometimes collected by mineral enthusiasts for its aesthetic appeal.

Lumelind was first described in scientific literature in 1987 by a team of geologists from the University of Iceland. The mineral was named after Lumelind, a character from Icelandic folklore, reflecting the country's rich cultural heritage. Despite its rarity, lumelind continues to be a subject of interest for geologists and mineral collectors alike.