
sedimentary
Montana Agate
Silicon Dioxide (Chalcedony with iron oxide inclusions)
AI-generated identification · may be incorrectHardness of 6.5-7 on the Mohs scale, translucent gray to white body with distinct red, orange, or black iron oxide inclusions, waxy to vitreous luster, microcrystalline structure.
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Physical properties
Hardness of 6.5-7 on the Mohs scale, translucent gray to white body with distinct red, orange, or black iron oxide inclusions, waxy to vitreous luster, microcrystalline structure.
Formation & geological history
Formed millions of years ago when silica-rich thermal waters filled cavities in basaltic lava flows, depositing microcrystalline quartz alongside iron and manganese oxides.
Uses & applications
Extensively used in lapidary arts, wire-wrapping, cabochons, and collector display pieces.
Geological facts
The distinctive red and orange spots are caused by oxidized iron (hematite or limonite) trapped within the clear chalcedony matrix during formation.
Field identification & locations
Found primarily in the alluvial gravels of the Yellowstone River and its tributaries in Montana; identified by its translucent chalcedony hosting contrasting red/black mineral inclusions.
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