Schalenblende

Schalenblende: A Rare Banding of Sulfide Beauty

Schalenblende is a striking and rarely occurring lead-zinc ore, composed of compact, layered bands of galena, wurtzite, sphalerite, pyrite, and marcasite. Its name—meaning “shell ore” in German—refers to its characteristic layered structure, which often forms in curved, shell-like patterns once botryoidal in origin.

Formed approximately 135 million years ago, schalenblende is the result of a rapid crystallization of sulfide-rich fluids at unusually low temperatures—a rare geological event that gives this mineral its unique mix of metallic textures and muted tones.

This complex blend of minerals is found in only a handful of localities worldwide, most notably in Poland, Belgium, and Germany, and is treasured for both its visual appeal and its geochemical significance.

This collection features hand-selected schalenblende specimens, chosen for banding, contrast, and formation clarity.

10% of every purchase supports environmental foundations in sulfide mineral–producing regions.

⚙️ Naturally layered metallic mineralogy
🌍 Rare formation from unique geological conditions
🔬 Collector-grade, ethically sourced