Mineraloid
Amber (with potentially inclusions)
Succinite (Fossilized Tree Resin)
Hardness: 2.0-2.5 (Mohs scale); Color: Yellow-brown to dark brown; Luster: Resinous; Crystal structure: Amorphous; Cleavage: None; Specific Gravity: 1.05-1.10 (very lightweight).
- Hardness
- 2
- Color
- Yellow-brown to dark brown
- Luster
- Resinous
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Physical properties
Hardness: 2.0-2.5 (Mohs scale); Color: Yellow-brown to dark brown; Luster: Resinous; Crystal structure: Amorphous; Cleavage: None; Specific Gravity: 1.05-1.10 (very lightweight).
Formation & geological history
Formed through the polymerization and fossilization of tree resin over millions of years (commonly 30-90 million years old). Originally found in ancient forest environments, later deposited in marine sediments or riverbeds.
Uses & applications
Predominantly used in jewelry, decorative arts, and perfume manufacturing. Science values it for paleontological research when it contains organic inclusions (insects, plants).
Geological facts
Amber is not a true mineral because it is organic and lacks a crystal structure. One of the most famous historical uses was the 'Amber Room' in Russia, often described as the Eighth Wonder of the World.
Field identification & locations
Identify by its light weight (it often floats in saltwater) and the way it feels warm to the touch compared to stone. It can be found on Baltic Sea shores or in mining regions of the Dominican Republic. When rubbed with cloth, it develops static electricity.
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