Mineral

Amazonite

Amazonite (KAlSi3O8, a variety of Microcline)

AI-generated identification · may be incorrect

Hardness: 3.5-4 (Mohs); Color: Light blue to blue-green; Luster: Vitreous to dull; Crystal Structure: Triclinic; Cleavage: Good in one direction; Specific Gravity: 2.6-2.8

Hardness: 3
Color: Light blue to blue-green
Luster: Vitreous to dull

Identified July 24, 2025More mineral →

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Physical properties

Hardness: 3.5-4 (Mohs); Color: Light blue to blue-green; Luster: Vitreous to dull; Crystal Structure: Triclinic; Cleavage: Good in one direction; Specific Gravity: 2.6-2.8

Formation & geological history

Amazonite is a tectosilicate mineral, a variety of microcline feldspar. It forms in granitic pegmatites, which are igneous rocks that cool slowly and allow for the growth of large crystals. It can also be found in some metamorphic rocks. Geologically, it forms during the late stages of magmatic differentiation, often in veins or pockets within the pegmatite. Its age varies depending on the specific geological formation where it is found, ranging from Precambrian to relatively recent.

Uses & applications

Primarily used as a gemstone and ornamental stone. It is often cut into cabochons, beads, and polished specimens for jewelry. Due to its attractive color, it is also popular for carvings and decorative items. It has some limited use as a decorative building material.

Geological facts

Amazonite is sometimes called 'Amazon Stone,' although it's not found in the Amazon River basin. Its blue-green color is attributed to small amounts of lead within its crystal structure. Historically, it was used by ancient Egyptians for jewelry and ornamental objects, and it's also found in some Native American artifacts.

Field identification & locations

In the field, amazonite is identified by its distinctive blue-green color, its white streak, and its typical blocky or platy crystal habit. It can be distinguished from other blue-green minerals by its hardness and lack of effervescence with acid. Common locations include the Pikes Peak area of Colorado (USA), known for well-formed crystals; Minas Gerais, Brazil; Ilmen Mountains, Russia; and parts of Madagascar, Canada, and Namibia. Collectors often seek out specimens with vibrant color and good crystal formation.

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