konillomore

Konillomore is a rare and unique mineral discovered in the late 20th century. It was first identified in a small mining town in the remote regions of South America. The mineral is known for its distinctive color, which ranges from a deep, vibrant blue to a lighter, almost turquoise hue. This coloration is due to the presence of copper and other trace elements within its crystal structure.

Konillomore is a member of the zeolite group, which are a class of minerals characterized by their open framework structures that can accommodate a variety of cations. The specific chemical formula of konillomore is (Na,Ca,K)2-3[Al6Si18O48]·12H2O. This formula indicates that the mineral contains sodium, calcium, and potassium ions, along with aluminum, silicon, and oxygen in its crystal lattice.

The mineral's formation is closely linked to the presence of volcanic activity and hydrothermal processes. It is typically found in association with other zeolites and clay minerals in volcanic rocks and sedimentary deposits. Konillomore crystals are usually small, ranging from a few millimeters to a few centimeters in size, and often occur as clusters or aggregates.

Due to its rarity and unique properties, konillomore has garnered interest from mineral collectors and researchers. Its distinctive color and crystal structure make it a valuable addition to mineral collections. However, the limited availability of konillomore makes it a highly sought-after mineral, driving up its value in the collector's market. Despite its rarity, konillomore remains an intriguing subject of study for geologists and mineralogists, offering insights into the complex processes that shape the Earth's crust.