Mineral field guide

How to identify feldspar

Feldspar is a family of abundant rock-forming silicates generally identified by hardness near 6, two cleavage directions, and blocky crystals; precise species identification may require optical or chemical work.

mineralSilicate mineral group

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Pink potassium feldspar hand specimen showing blocky cleavage
Potassium feldspar specimen; source image resized and re-encoded for web displayPhoto: James St. John · CC BY 2.0 · Wikimedia Commons
Classification

What is feldspar?

Feldspar includes potassium-rich alkali feldspars and the sodium-calcium plagioclase series. Compositions vary continuously in parts of the group, so “feldspar” is often the appropriate field identification.

Appearance

What does feldspar look like?

Feldspar commonly forms blocky crystals with pearly cleavage faces. Plagioclase may show fine parallel striations on cleavage surfaces; alkali feldspar can show different twinning or intergrowth textures.

Weathering changes feldspar to clay minerals, making surfaces chalky, dull, or soft while fresh interiors remain hard.

Field tests

Identification tests

Begin with observation and use the least destructive test first. Results can change with weathering, mixtures, coatings, and grain size. Review the step-by-step field-test methods before altering an unfamiliar specimen.

Hardness

About 6

Usually scratches glass but can be scratched by quartz.

Streak

White

Consistent but not diagnostic.

Cleavage

Two good directions near 90°

Separates feldspar from cleavage-free quartz.

Striations

Possible on plagioclase cleavage faces

A strong clue for plagioclase when clearly present.

Comparison

Common lookalikes

Quartz

No cleavage, harder, and commonly has conchoidal fracture.

Calcite

Much softer, has three rhombohedral cleavages, and fizzes with acid.

Kaolinite or weathered feldspar

Clay alteration is much softer and lacks a fresh glassy cleavage.

Geologic origin

How does it form?

Feldspars crystallize from magma and are major constituents of granite, basalt, gabbro, rhyolite, and many other igneous rocks.

They also occur in metamorphic rocks and sediment, though chemical weathering makes them less durable at Earth’s surface than quartz.

Where it occurs

Geologic setting and occurrence

Feldspar is the most abundant mineral group in much of Earth’s crust and is present in a wide variety of igneous and metamorphic rocks.

Color is unreliable for separating feldspar species. Pink does not automatically mean potassium feldspar, and white does not automatically mean plagioclase.

Human use

Uses and significance

Feldspar is used in glass, ceramics, fillers, glazes, and abrasives. Gem varieties include moonstone, sunstone, amazonite, and labradorite.

Safety and limits

Field notes

  • Use a fresh cleavage face to look for striations.
  • Record “feldspar” when the evidence does not support a species.
  • Avoid creating silica-bearing dust when breaking feldspar-rich rock.

This guide supports preliminary field identification, not a laboratory determination, appraisal, hazard assessment, or statement of ownership or collecting permission. Verify land status and local rules before handling or collecting material.

Source basis

Authoritative sources

LithoMap wrote this guide in original language using the scientific concepts and physical-property standards supported by these sources.

Editorial review: September 17, 2026.