By Chisom Ibemere
Schalenblende is a mineral rock which is composed of different layers of minerals. It is gotten from hydrothermal deposits occuring where hot fluids rich in metals interact with the surrounding rocks.
The name “schalenblende” originated from the German words “schale,” meaning shell, and “blende,” meaning sphalerite, one of the rock minerals.
Schalenblende is known as a unique mineral with a distinct layered appearance with a resemblance of the onion or shell layers.
It has a unique layered appearance and vibrant colors, used as an ornamental stone in jewelry, beads, and decorative purposes. It is a rare mineral which is sought after by collectors who appreciate its aesthetic appeal and distinct patterns.
Schalenblende comprises of various minerals such as sphalerite (zinc sulfide), galena (lead sulfide), wurtzite (zinc sulfide), and marcasite (iron sulfide).
The layers of minerals gives a distinct banding or shell-like appearance. It exhibit a wide range of colors such as black, brown, gray, yellow, and orange. The colors result from the combination of different mineral occuring within the rock.
Schalenblende has a hardness of 3.5 to 4 on the Mohs scale which makes it relatively soft compared to other minerals, and it can be easily scratched or damaged.
The global value of schalenblende is not as high as some other minerals or gemstones due to its relatively limited use and availability. However, well-defined banding and attractive colors of the mineral can hold value for collectors and jewelry designers.
Its value of may vary which depends on factors such as size, quality, aesthetic appeal, and demand among collectors and enthusiasts. It is also influenced by supply and demand dynamics within the market.