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Amazonite

Mineral (variety of Microcline Feldspar)

Amazonite (variety of Microcline Feldspar)

Also known as: Amazon Stone

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Description

Amazonite is a tectosilicate mineral, a variety of microcline feldspar, known for its distinctive blue-green to green color. The color is attributed to small amounts of lead (Pb) within the crystal lattice, replacing potassium (K), and the presence of water, rather than copper as was once believed. It typically forms in well-formed crystals within pegmatite pockets or as massive aggregates.

How to Identify

Color
Characteristic blue-green to green, sometimes with white streaks or inclusions. The color can vary in intensity.
Luster
Vitreous (glassy) to pearly on cleavage surfaces.
Texture
Typically massive or in well-formed, often tabular, crystals. Can exhibit a fine lamellar twinning (perthitic texture) visible on polished surfaces.
Crystal Form
Usually forms in anhedral to subhedral masses, but can also occur as distinct, often blocky or tabular, triclinic crystals. Twinning, particularly polysynthetic twinning (albite twinning) and pericline twinning, is common and can be observed as fine striations on cleavage surfaces.
Cleavage
Perfect cleavage in two directions, nearly at right angles (approximately 90 degrees, specifically 90° 30'). This is characteristic of feldspar minerals.
Geological Environment
Primarily found in granitic pegmatites, which are igneous intrusions characterized by very large crystals. Less commonly found in granites and some metamorphic rocks.

Key Facts

  • Hardness: 6 to 6.5 on the Mohs scale
  • Specific Gravity: 2.56 to 2.58
  • Crystal System: Triclinic
  • Color: Blue-green, green, sometimes with white streaks
  • Luster: Vitreous to pearly
  • Transparency: Translucent to opaque
  • Fracture: Uneven to conchoidal
  • Cleavage: Perfect in two directions, nearly at 90 degrees (90° 30')
  • Composition: Potassium aluminum silicate (KAlSi3O8)

Quick Check

  • Color: Blue-green to green
  • Luster: Vitreous to pearly
  • Streak: White

Physical Characteristics

  • Crystal Habit: Massive, granular, or in well-formed tabular to blocky crystals, often twinned.
  • Cleavage Type: Perfect basal {001} and good prismatic {010}, intersecting at approximately 90° 30'.
  • Fracture Type: Uneven to conchoidal.
  • Tenacity: Brittle.
  • Luster Type: Vitreous on crystal faces, pearly on cleavage surfaces.

Formation

Amazonite forms in granitic pegmatites, which are coarse-grained igneous rocks that crystallize from residual magma enriched in volatile components and incompatible elements. It can also occur in some granites and metamorphic rocks.

Usage

Primarily used as a gemstone and ornamental stone due to its attractive blue-green color. It is carved into cabochons, beads, and small sculptures. Historically, it has been used for decorative purposes and in jewelry.

Age Distribution

Found in various geological ages, primarily associated with granitic pegmatites which can range from Precambrian to Cenozoic.

Where to Find

Pikes Peak, Colorado, USA

Famous for producing some of the finest deep blue-green amazonite crystals, often associated with smoky quartz and albite.

Miass, Ilmen Mountains, Russia

Historically significant locality, known for large amazonite crystals.

Minas Gerais, Brazil

A major source of amazonite, often found in pegmatites.

Madagascar

Produces good quality amazonite, sometimes with interesting patterns.

Virginia, USA

Localities such as Amelia Courthouse are known for amazonite occurrences.

Ethiopia

Newer sources have emerged, providing material for the gem market.

Finding Tips

Target Pegmatites

Focus your search on granitic pegmatite dikes and sills, especially those known for rare earth elements or other unusual minerals, as amazonite often co-occurs with them.

Look for Associated Minerals

Amazonite is frequently found with smoky quartz, albite, cleavelandite, and sometimes other rare minerals like topaz or beryl. Identifying these associated minerals can lead to amazonite.

Examine Outcrops

Look for distinctive blue-green masses or crystals within exposed pegmatite bodies. Weathering can sometimes make the color more apparent.

Check Mine Dumps

Old mine dumps from pegmatite operations can be excellent places to find specimens that were overlooked or discarded.

Similar Rocks

Turquoise

CuAl6(PO4)4(OH)8·4H2O

Also known as: Callais

Chrysocolla

(Cu,Al)2H2Si2O5(OH)4·nH2O

Also known as: Gem Silica

Jade (Nephrite or Jadeite)

Ca2(Mg,Fe)5Si8O22(OH)2 (Nephrite); Na(Al,Fe3+)Si2O6 (Jadeite)

Also known as: Stone of Heaven

Scientific Classification

Mineral Class
Tectosilicate
Group
Feldspar Group, Alkali Feldspar Series
Crystal System
Triclinic
Chemical Formula
KAlSi3O8
Composition
Potassium aluminum silicate. The blue-green color is due to trace amounts of lead (Pb) and water within the crystal structure.

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