Rock Identifier
Amber ((C10H16O)n – an amorphous organic substance, primarily composed of polymerized isoprenoids.) — Mineral
Mineral

Amber

(C10H16O)n – an amorphous organic substance, primarily composed of polymerized isoprenoids.

Hardness: 2.5-4.0 (Mohs scale), Color: Typically yellow to brownish-yellow, often translucent. Can also be orange, red, green, or even black. Luster: Resinous to waxy. Crystal Structure: Amorphous. Cleavage: None, generally conchoidal fracture. Specific Gravity: 1.05-1.09.

Hardness
2
Color
Typically yellow to brownish-yellow, often translucent
Luster
Resinous to waxy
Identified More mineral

Identify your own rocks.

Get a report just like this from any photo, free.

Physical properties

Hardness: 2.5-4.0 (Mohs scale), Color: Typically yellow to brownish-yellow, often translucent. Can also be orange, red, green, or even black. Luster: Resinous to waxy. Crystal Structure: Amorphous. Cleavage: None, generally conchoidal fracture. Specific Gravity: 1.05-1.09.

Formation & geological history

Formed from the fossilization of tree resin over millions of years, primarily from coniferous trees. The resin hardens through a process called polymerization, which is then buried and exposed to pressure and heat, losing volatile components to become amber. Geological Age: Varies depending on the source, but commonly ranges from the Triassic to the Quaternary periods (between 250 million to 1 million years ago). Often found in sedimentary deposits, particularly in ancient forests and marine sediments where rivers carried resin into deltas.

Uses & applications

Industry: Historically used in varnishes, perfumes, and as an insulating material. Jewelry: Widely used for beads, cabochons, carvings, and other ornamental purposes due to its warm color and light weight. Collecting Value: Highly prized by collectors, especially pieces with clear inclusions or unusual colors.

Geological facts

Amber is ancient fossilized tree resin, not a mineral in the strict sense (as it lacks crystal structure), but it is widely categorized and traded as one. It often contains inclusions of fossilized insects, plants, and even small vertebrates, providing unique insights into prehistoric ecosystems. The oldest known amber dates back to the Upper Carboniferous period (around 320 million years ago). Baltic amber is particularly famous for its high quality and abundance.

Field identification & locations

How to identify in the field: Lightweight for its size (often floats in salt water), warm to the touch, and can be easily scratched (low hardness). It may emit a piney scent when rubbed vigorously. Common locations: Major deposits include the Baltic Sea region (Kaliningrad, Russia; Poland, Lithuania, Latvia), the Dominican Republic (known for blue amber), Mexico (Chiapas), and Myanmar (Burmite). Tips for collectors: Look for pieces with clear fossil inclusions or vibrant, rare colors. Be aware of imitations (copal, plastic) which can be distinguished by density, smell when heated/rubbed, and reaction to solvents like acetone.