
mineral
Amber
Succinite (Fossilized Tree Resin) - C10H16O
Hardness: 2.0-2.5 on Mohs scale; Color: Honey-yellow to brownish-orange; Luster: Resinous; Crystal structure: Amorphous (non-crystalline); Cleavage: None (conchoidal fracture); Specific gravity: 1.05-1.10 (floats in saltwater).
- Hardness
- 2
- Color
- Honey-yellow to brownish-orange
- Luster
- Resinous
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Physical properties
Hardness: 2.0-2.5 on Mohs scale; Color: Honey-yellow to brownish-orange; Luster: Resinous; Crystal structure: Amorphous (non-crystalline); Cleavage: None (conchoidal fracture); Specific gravity: 1.05-1.10 (floats in saltwater).
Formation & geological history
Formed from the fossilization of resin (sap) from extinct coniferous trees, primarily during the Paleogene or Cretaceous periods. Over millions of years, the resin undergoes polymerization and burial under sediment, becoming what we call 'copal' and eventually 'amber'.
Uses & applications
Used primarily in jewelry making (beads, pendants), as a decorative stone, in perfumes for its scent when heated, and for scientific research due to its ability to preserve biological inclusions.
Geological facts
Amber is not technically a mineral because it is organic in origin. It is famous for trapping 'inclusions' such as prehistoric insects, leaves, and even small vertebrates, acting as a natural time capsule from millions of years ago.
Field identification & locations
Identify in the field by its very light weight and warm feel compared to stone; it will also float in highly saturated saltwater. Commonly found in the Baltic region, Dominican Republic, and Myanmar. Natural pieces are often found on beaches or in riverbeds after storms.
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