Rock Identifier
Montana Agate (Silicon Dioxide (Chalcedony with iron oxide inclusions)) — sedimentary
sedimentary

Montana Agate

Silicon Dioxide (Chalcedony with iron oxide inclusions)

AI-generated identification · may be incorrect

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.

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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.