
sedimentary
Agate / Chalcedony Geode Nodule
Silicon Dioxide (SiO2)
Hardness of 7 on the Mohs scale; exhibits brown, tan, and white concentric banding with a crystalline quartz core; waxy to vitreous luster; cryptocrystalline structure; conchoidal fracture with no true cleavage; specific gravity around 2.60 to 2.65.
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Physical properties
Hardness of 7 on the Mohs scale; exhibits brown, tan, and white concentric banding with a crystalline quartz core; waxy to vitreous luster; cryptocrystalline structure; conchoidal fracture with no true cleavage; specific gravity around 2.60 to 2.65.
Formation & geological history
Formed in gas cavities within volcanic or sedimentary rocks where silica-rich groundwater deposited microscopic quartz crystals in layers over millions of years.
Uses & applications
Used primarily in ornamental lapidary work, making jewelry, decorative slabs, bookends, and sought after by mineral and rock collectors.
Geological facts
Agate banding reflects changes in pressure, temperature, and mineral content of the solutions flowing through the cavity during formation. This specimen shows a classic cavity lined with sparkling quartz crystals surrounded by concentric agate layers.
Field identification & locations
Easily identified by its distinct concentric bands of color and hard quartz center. Commonly found in regions with ancient volcanic activity, such as Brazil, Mexico, Madagascar, and the western United States.
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