
mineral
Amber
Fossilized Tree Resin (Generic formula roughly C10H16O)
Hardness: 2.0-2.5 on Mohs scale. Color: Honey-yellow to orange-brown. Luster: Resinous. Crystal structure: Amorphous (non-crystalline). Cleavage: None (conchoidal fracture). Specific gravity: 1.05-1.10 (very light, floats in saltwater).
- 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 (non-crystalline). Cleavage: None (conchoidal fracture). Specific gravity: 1.05-1.10 (very light, floats in saltwater).
Formation & geological history
Formed through the polymerization of tree resin from extinct coniferous and angiosperm trees. Over millions of years, the resin undergoes heat and pressure, losing volatile components to become fossilized. Most deposits range from 30 to 90 million years old (Paleogene to Cretaceous).
Uses & applications
Primarily used in jewelry (beads, cabochons, pendants) and as a decorative gemstone. It is also of immense scientific value for paleontology because it traps and preserves organic inclusions such as insects, plant matter, and small vertebrates.
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. The presence of 'sun spangles' (disc-like internal fractures) is a common feature in heated specimens.
Field identification & locations
Identify in the field by its light weight and 'warm' feel compared to glass or stone. It can be tested by its ability to float in a saturated salt solution or by the 'hot needle test' (it emits a piney scent when touched with a hot pin). Found in coastal regions like the Baltic Sea and inland mines in the Dominican Republic.
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