
mineraloid
Amber
Succinate (Fossilized Tree Resin)
Hardness: 2.0-2.5 on Mohs scale; Color: Honey yellow to orange-brown; Luster: Resinous; Crystal structure: Amorphous; Cleavage: None (conchoidal fracture); Specific gravity: 1.05-1.10 (very light, floats in salt water).
- Hardness
- 2
- Color
- Honey yellow to orange-brown
- Luster
- Resinous
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Physical properties
Hardness: 2.0-2.5 on Mohs scale; Color: Honey yellow to orange-brown; Luster: Resinous; Crystal structure: Amorphous; Cleavage: None (conchoidal fracture); Specific gravity: 1.05-1.10 (very light, floats in salt water).
Formation & geological history
Formed from the fossilization of resin from ancient coniferous trees, primarily during the Eocene epoch (about 44 million years ago). Over millions of years, the resin undergoes polymerization and loses volatile components.
Uses & applications
Primarily used in jewelry making, decorative carvings, and as a storage medium for paleontological specimens (insects trapped inside). It is also studied for scientific research into prehistoric ecosystems.
Geological facts
Unlike true minerals, amber is organic. It can trap DNA and ancient life forms in a near-perfect state of preservation. It is famous for its electrostatic properties; rubbing amber with a cloth creates static electricity.
Field identification & locations
Identify in the field by its light weight and warmth to the touch compared to stone. It can be found on Baltic Sea beaches after storms or in coal seams. A common test is the 'salt water test' where it floats in highly saline water but sinks in fresh water.
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