magnetlindile

Magnetlindile is a rare and unusual mineral discovered in the late 20th century. It is named for its unique magnetic properties and its lindenite-like appearance. Magnetlindile is a member of the lindite group, which includes other minerals such as lindite and niningerite. It is typically found in association with these minerals in low-temperature hydrothermal veins.

Magnetlindile is characterized by its dark gray to black color, metallic luster, and perfect cleavage. It has a hardness of 4.5 on the Mohs scale and a specific gravity of approximately 5.5. The mineral exhibits strong magnetic properties, which is unusual for a member of the lindite group. This magnetic behavior is thought to be due to the presence of iron in the mineral's structure.

The chemical composition of magnetlindile is complex, with the general formula (Fe,Mn)2+2(AsO4)(SO4)(OH)2. The mineral's structure is composed of layers of iron and manganese octahedra, with arsenic and sulfur tetrahedra and hydroxide groups filling the interlayer spaces.

Magnetlindile is a relatively rare mineral, with only a few occurrences documented in the scientific literature. It has been found in a limited number of locations, including the type locality in the Democratic Republic of the Congo and a few other sites in Africa and Asia. The mineral's rarity and unique properties make it of interest to mineralogists and collectors alike.