Microcline

Crystal system · Triclinic

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

About Microclineextended article

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
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.

About Microcline

Microcline is classified as a silicate mineral in the feldspar group and has the chemical formula KAlSi₃O₈. It crystallizes in the triclinic system and is one of the most visually varied minerals in the collector market.

Identification & care

Specimens usually show prismatic to tabular crystals, often twinned; massive. Its color range is broad, including white, pink, gray, pale yellow, and green (amazonite variety). The luster is vitreous to pearly, the streak is white, and specimens range from transparent to opaque. The cleavage is perfect on {001} and {010} at near-right angles. The fracture is conchoidal, which aids identification.

Collector context

Collector notes

Microcline holds a steady place in systematic mineral collections. Documented Chinese occurrences are recorded at Dachang ore field and Yaogangxian W-Sn ore field, among others.