
sedimentary
Fossil Coral and Quartz Pebble
Fossilized Anthozoa / Silicon Dioxide (Quartz)
Hardness: 7 for the quartz pebble, 3-4 for the fossilized coral on Mohs scale. Color: Tan, beige, and off-white. Luster: Vitreous to dull. Structure: Microcrystalline quartz and porous skeletal coral structure.
- Color
- Tan, beige, and off-white
- Luster
- Vitreous to dull
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Physical properties
Hardness: 7 for the quartz pebble, 3-4 for the fossilized coral on Mohs scale. Color: Tan, beige, and off-white. Luster: Vitreous to dull. Structure: Microcrystalline quartz and porous skeletal coral structure.
Formation & geological history
Formed in ancient shallow marine environments where coral skeletons accumulated and were later replaced or preserved in sedimentary rock layers, alongside weathered quartz pebbles from surrounding strata.
Uses & applications
Used in lapidary work, educational displays, and collected as natural curiosities.
Geological facts
Fossil coral is often silicified, meaning the original calcium carbonate of the coral skeleton has been replaced by microcrystalline quartz over millions of years.
Field identification & locations
Found in regions with ancient limestone or marine sedimentary deposits. Identify by the distinctive honeycomb or porous cellular pattern on the coral specimen and the smooth, rounded shape of the quartz pebble.
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