
gemstone
Polished amber
Amber (fossilized plant resin), commonly succinite; organic mineraloid rather than a true mineral
AI-generated identification · may be incorrectMohs hardness about 2–2.5; translucent honey-orange color with resinous to vitreous luster and conchoidal fracture. Amorphous, very low density (about 1.05–1.10), and commonly contains internal bubbles or plant inclusions.
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Physical properties
Mohs hardness about 2–2.5; translucent honey-orange color with resinous to vitreous luster and conchoidal fracture. Amorphous, very low density (about 1.05–1.10), and commonly contains internal bubbles or plant inclusions.
Formation & geological history
Formed when ancient tree resin polymerized and matured during burial, commonly in Paleogene sediments roughly 20–50 million years old, though ages vary widely. The specimen is cut and polished.
Uses & applications
Used for beads, pendants, carvings, ornaments, and collector pieces; historically used for incense and decorative objects. Commercial value increases substantially with clarity, rarity, size, and authentic inclusions.
Geological facts
Amber often becomes electrostatic when rubbed and may float in salt water; genuine amber can emit a pine-like odor when gently warmed, although destructive tests are best avoided.
Field identification & locations
Common sources include Baltic-region deposits, the Dominican Republic, Mexico, Myanmar, and Indonesia. Identify by its unusually light weight, warm resinous appearance, static charge, and soft surface; plastic imitations are common.
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