Rock Identifier
Quartz Geode (Silicon Dioxide (SiO2)) — sedimentary
sedimentary

Quartz Geode

Silicon Dioxide (SiO2)

Hardness: 7 (Mohs scale), Color: Tan/white exterior with possible white or clear interior, Luster: Vitreous (internal) and dull/earthy (external), Crystal Structure: Trigonal, Cleavage: None, Specific Gravity: 2.65

Identified More sedimentary
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Physical properties

Hardness: 7 (Mohs scale), Color: Tan/white exterior with possible white or clear interior, Luster: Vitreous (internal) and dull/earthy (external), Crystal Structure: Trigonal, Cleavage: None, Specific Gravity: 2.65

Formation & geological history

Formed as hollow cavities in sedimentary or volcanic rock that are filled over time by the precipitation of mineral-rich water. These can be millions of years old, often dating to the Cretaceous or Pennsylvanian periods.

Uses & applications

Used primarily for interior decor, educational specimens, lapidary art, and jewelry if crystals are high quality.

Geological facts

Geodes are like nature’s surprise boxes; while the outside looks like a common lumpy rock, the inside can contain vibrant crystals. The Keokuk geode from Iowa is one of the most famous varieties.

Field identification & locations

Look for rounded, lumpy nodules that feel lighter than they look (indicating a hollow center). Common in river beds and desert environments through the midwestern and southwestern US.