Rock Identifier
Tumbled amber (likely copal or imitation amber) (Amber: fossilized tree resin, chiefly polymerized diterpenes; copal is younger, incompletely polymerized resin) — gemstone
gemstone

Tumbled amber (likely copal or imitation amber)

Amber: fossilized tree resin, chiefly polymerized diterpenes; copal is younger, incompletely polymerized resin

AI-generated identification · may be incorrect

Honey-yellow, translucent, resinous luster with conchoidal fracture and no cleavage; Mohs hardness about 2–2.5 for amber and 1.5–2 for copal, specific gravity about 1.05–1.10. The rounded, glossy appearance indicates tumbling or polishing.

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Physical properties

Honey-yellow, translucent, resinous luster with conchoidal fracture and no cleavage; Mohs hardness about 2–2.5 for amber and 1.5–2 for copal, specific gravity about 1.05–1.10. The rounded, glossy appearance indicates tumbling or polishing.

Formation & geological history

Amber forms when ancient conifer or flowering-plant resin is buried, polymerized, and preserved over millions of years; major deposits are Oligocene Baltic amber (~34–23 million years old) and younger Cretaceous deposits. Copal is generally younger than a few million years.

Uses & applications

Used for beads, cabochons, carvings, ornaments, and scientific inclusions; fine transparent amber with insects can be valuable. Copal and plastic imitations are common substitutes.

Geological facts

Amber floats in saturated salt water and commonly becomes electrostatic when rubbed; heating produces a pine-like odor. The image alone cannot reliably distinguish amber from copal, resin, or plastic.

Field identification & locations

Check low density, warm tactile feel, salt-water flotation, UV fluorescence, and a concealed hot-needle test; avoid destructive testing on valuable pieces. Common sources include the Baltic region, Dominican Republic, Mexico, Myanmar, and Indonesia.