Microcline

KAlSi3O8

Microcline is a silicate mineral prized by collectors for its exceptional color range, with notable Chinese occurrences.

Crystal Structure
Triclinic ordered analog of orthoclase.
Elemental Composition (by mass)
ElementMass %Visual
O Oxygen45.99%
Si Silicon30.27%
K Potassium14.05%
Al Aluminum9.69%
Computed from simplified end-member formula. Solid-solution series, water content, and trace substitutions cause real-world variation.
IMA Abbreviation (Whitney-Evans 2010)
Mc
→ Microcline
K-feldspar low-T
Standard symbol from American Mineralogist (Whitney & Evans, 2010). Used in thin-section labeling, phase diagrams, and IMA-style species records.
Pronunciation
/ˈmaɪkroʊklaɪn/
MY-kroh-cline
Greek "small angle"
Tenacity
Behavior:
brittle
Under stress:
Same
K-feldspar; includes amazonite.
Luster
vitreous
Bright greenish in amazonite.
Diaphaneity (Transparency)
translucent
Including amazonite.
Type Locality
Arendal — Norway
Described 1830 by Breithaupt
› Browse all type localities
Specific Gravity
2.54–2.57
g/cm³
light
K-feldspar; includes amazonite.
For comparison: water = 1.00, glass ≈ 2.5, quartz = 2.65, corundum ≈ 4.00, galena ≈ 7.50, gold ≈ 19.3.
Twinning Laws
Albite lawlamellar
Fine parallel striations on {001} — diagnostic for plagioclase but also appears in microcline.
Pericline lawlamellar
Cross-hatched grid pattern combined with albite-law twinning — diagnostic of microcline.
Cleavage & Fracture
Cleavage:
good 2 directions ~90°
Fracture:
uneven
Includes amazonite. Cleavage perpendicular.
Market availability: Common
Widely available in most dealer stocks. Specimens span all price tiers.
Collector tier: Solid Display
Reliable mid-tier display species. Easy to find in well-formed examples; broad locality diversity.
PolymorphsShares the formula KAlSi3O8 with: Orthoclase · Sanidine — same chemistry, different crystal structure.
Mohs 6–6.5
Vickers (~) 820 HV
Knoop (~) 870 HK
Nickel–Strunz 9.FA.30
Dana 76.01.03.04
Geological setting
Plutonic igneousPegmatiteMetamorphic
Element composition by mass

Formula: KAlSi₃O₈ · molar mass: 278.33 g/mol

O 45.99%
Si 30.27%
K 14.05%
Al 9.69%

Computed from atomic weights (IUPAC 2021). Site-occupancy groups (Fe,Mn) split equally.

GroupFeldspar Group
Related members: Orthoclase · Sanidine · Albite · Labradorite
Mohs Hardness 6–6.5

Microcline sits at 6–6.5 on the Mohs scale — just hard enough to scratch glass.

Colors:
Streak
White
Crystal system
Triclinic
Type localityPikes Peak, Colorado, USA
SilicatesSilicates (Tectosilicates — Feldspars)
TL;DR · 1 min read
Microcline (KAlSi₃O₈) is a triclinic potassium feldspar and the parent species of one of the most prized collector varieties — amazonite, the vivid blue-green form colored by trace lead and water content. Microcline forms in granitic pegmatites and high-grade metamorphic rocks; classic Pikes Peak (Colorado) and Madagascar deposits supply gem-grade amazonite.

Microcline (KAlSi₃O₈) is a triclinic potassium feldspar and the parent species of one of the most prized collector varieties — amazonite, the vivid blue-green form colored by trace lead and water content. Microcline forms in granitic pegmatites and high-grade metamorphic rocks; classic Pikes Peak (Colorado) and Madagascar deposits supply gem-grade amazonite.

More minerals to explore

Varieties of Microcline

Microcline is a parent species — the following named varieties differ in color or chemistry but share the same fundamental mineralogy.

  • Amazonite (u5929u6cb3u77f3)
    turquoise to blue-green
    Lead-bearing turquoise-green microcline variety, named for the Amazon River.