RockVault
Anorthoclase

Image: <a rel="nofollow" class="external text" href="https://www.flickr.com/people/47445767@N05">James St. John</a> (CC BY 2.0)

monoclinicuncommonSilicates (Tectosilicates, Feldspar Group)

Anorthoclase

(Na,K)AlSi3O8

Anorthoclase typically appears as white, gray, or yellowish blocky crystals with a vitreous luster, often showing twinning. The specimens in the image are light-colored, somewhat translucent, and exhibit characteristic feldspar cleavage.

Anorthoclase Physical Properties

Mohs Hardness

6

Crystal System

monoclinic

Luster

vitreous

Streak Color

white

Cleavage

Perfect on {001}, good on {010}, intersecting at nearly 90 degrees

Fracture

uneven to conchoidal

Specific Gravity

2.59

Colors

white, gray, yellowish, pinkish

Transparency

transparent to translucent

Type Locality

Mount Erebus (Antarctica), Kenya, Italy, various oceanic islands

Mineral Group

Silicates (Tectosilicates, Feldspar Group)

Uses

collector, scientific research

Associated Minerals

pyroxene, amphibole, olivine, magnetite

Rarity

uncommon

Geological Context

Anorthoclase is a high-temperature alkali feldspar that forms in rapidly cooled volcanic rocks, particularly in silica-undersaturated to saturated lavas and pyroclastic rocks. It is characteristic of certain alkaline igneous environments.