Anorthoclase

5 in the gallery

Anorthoclase is a feldspar mineral in which sodium and potassium can substitute within the same crystal structure, giving a solid solution across the Na-K feldspar series. It typically forms as slender, tabular to prismatic crystals and often exhibits a glassy to pearly luster. The color range is generally pale, from colorless to white or faint pink, and the mineral tends to occur in low-relief habits that reflect light softly rather than strongly. Crystals can be associated with granitic rocks and pegmatites, and they are sometimes found in skarn environments where late-stage magmatic processes leave behind alkali feldspars. Noted specimens are often characterized by clean faces and well-formed terminations that appeal to collectors seeking classic alkali feldspar aesthetics.

Formula
(Na,K)AlSi3O8
Rarity
Common
Stability
Stable
Collector interest
Moderate Interest
Classification notes
Tectosilicate, feldspar group

Key characteristics

Crystal system
triclinic
Mohs hardness
6–6.5
Specific gravity
2.57–2.6
Luster
vitreous, pearly
Transparency
transparent, translucent
Color
colorless, white, gray, yellow, pink
Streak
white
Cleavage
perfect
Fracture
uneven
Crystal habit
tabular, prismatic, granular, massive
  • Gem mineral

Where Anorthoclase is found

Top localities

  1. Chihuahua1 specimen

About Anorthoclase

Collectors prize Anorthoclase for its historical role in alkali feldspar studies and for its straightforward, elegant crystal forms that complement other minerals in a cabinet display. Specimens from Japan and Mexico are among the more commonly cited sources, where the mineral occurs in diverse pegmatitic and contact-metamorphic settings. The mineral’s relative rarity in crisp, well-formed crystals compared with more abundant feldspars can enhance its appeal when such material is recovered with good luster and clarity. For mineral enthusiasts, Anorthoclase offers a clean, minimalistic look that pairs well with complementary minerals to emphasize its subtle brightness and form.