Rock Identifier
Amber (likely opaque/burnished amber) (Fossilized plant resin; primarily polymerized terpenoid resin (succinite-type amber)) — gemstone
gemstone

Amber (likely opaque/burnished amber)

Fossilized plant resin; primarily polymerized terpenoid resin (succinite-type amber)

AI-generated identification · may be incorrect

Translucent honey-brown to reddish-brown, resinous/waxy luster, conchoidal fracture, no cleavage, Mohs hardness about 2–2.5, specific gravity about 1.05–1.10; commonly floats in concentrated salt water. The irregular piece appears naturally rough or lightly polished, with flow-like internal patterns.

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Physical properties

Translucent honey-brown to reddish-brown, resinous/waxy luster, conchoidal fracture, no cleavage, Mohs hardness about 2–2.5, specific gravity about 1.05–1.10; commonly floats in concentrated salt water. The irregular piece appears naturally rough or lightly polished, with flow-like internal patterns.

Formation & geological history

Amber formed from ancient tree resin that was buried, chemically altered, and polymerized over millions of years; Baltic amber is mainly Eocene, roughly 34–56 million years old. The reported Croatian-region location makes amber possible as transported sediment, though the specimen could also be modern resin or copal without testing.

Uses & applications

Used for beads, carvings, ornaments, jewelry, and collector specimens; historically used as incense and in folk medicine. Common pieces have modest value.

Geological facts

Amber often contains plant fragments, bubbles, or insects. It softens with heat and produces a pine-like odor when gently warmed; copal is younger and usually softer and more soluble.

Field identification & locations

Identify by its very low density, warm feel, static attraction after rubbing, conchoidal fracture, and reaction to UV (often blue-white fluorescence). Confirm with hardness, salt-water float, and FTIR testing; avoid destructive heat tests.