
Mineraloid
Amber
Succinite (Carbon-based organic compound; approximate formula C10H16O)
Hardness: 2.0-2.5 on Mohs scale; Color: Honey-yellow, orange, brown, reddish-orange; Luster: Resinous; Crystal structure: Amorphous (non-crystalline); Cleavage: None; Specific Gravity: 1.05-1.09 (floats in saltwater).
- Hardness
- 2
- Color
- Honey-yellow, orange, brown, reddish-orange
- Luster
- Resinous
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Physical properties
Hardness: 2.0-2.5 on Mohs scale; Color: Honey-yellow, orange, brown, reddish-orange; Luster: Resinous; Crystal structure: Amorphous (non-crystalline); Cleavage: None; Specific Gravity: 1.05-1.09 (floats in saltwater).
Formation & geological history
Formed from the fossilized resin of ancient coniferous and angiosperm trees. It undergoes polymerization and burial over millions of years. Most geological deposits date from the Eocene (34-56 million years ago) to the Cretaceous periods.
Uses & applications
Primarily used in jewelry making, ornamental carvings, and as a perfume ingredient. It is highly valued by paleontologists for preserving prehistoric life (inclusions like insects and plants).
Geological facts
Amber is organic, not a true mineral. It can generate static electricity when rubbed (the word 'electron' comes from the Greek word for amber, 'elektron'). The most famous historical structure made of it was the Amber Room of the Czars in Russia.
Field identification & locations
Identify in the field by its light weight, warmth to the touch (unlike cold glass/stone), and ability to float in a saturated salt solution. Primarily found in the Baltic region, Dominican Republic, and Myanmar.
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