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Geology: Rocks, Minerals & Ores Mineral Sequence in the Cady Mountains Stilbitecalcium aluminum silicaCady Mountains, Mojave Desert, CA ![]() << - >> Mineral Sequence in the Cady Mountains Stilbite is one of the more delicate and visually striking minerals found in the Cady Mountains of California’s Mojave Desert. A member of the zeolite family, stilbite typically forms in volcanic cavities, appearing in fan-shaped or sheaf-like clusters that look almost flower-like. Made of calcium aluminum silicate, its crystals often show a pearly luster and range from white to pink or orange, depending on trace elements. These soft, blade-like crystals grow as part of the region’s complex mineral sequence, a byproduct of ancient volcanic activity and the slow movement of mineral-rich water through rock. While stilbite may not be as hard as quartz or as colorful as fluorite, its graceful form and formation history make it a favorite among collectors and geologists. Each specimen is a small, natural sculpture shaped by the quiet chemistry of time. |
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Intro:: Nature:: Map:: Parks:: Points of Interest:: Ghosts & Gold:: Communities:: Roads & Trails:: People & History:: BLOG:: Weather:: :?:: glossary |
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These items are historical in scope and are intended for educational purposes only; they are not meant as an aid for travel planning. Copyright ©Walter Feller. 1995-2025 - All rights reserved. |