Rock field guide

How to identify phyllite

Phyllite is a fine-grained foliated metamorphic rock between slate and schist, recognized by a silky sheen and gently wavy foliation produced by microscopic mica.

rockFine-grained foliated metamorphic rock

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Fine-grained foliated gray phyllite with a silky sheen produced by microscopic mica
Phyllite hand specimenPhoto: Mike Davis · CC0 1.0 · Wikimedia Commons
Classification

What is phyllite?

Phyllite commonly contains microscopic muscovite or sericite, chlorite, quartz, and feldspar, with composition inherited from a mud-rich parent rock and modified by metamorphic reactions.

Appearance

What does phyllite look like?

The sheen changes as the sample rotates because tiny aligned mica grains reflect light. Surfaces may be silver-gray, greenish, reddish, purple, or dark gray.

Foliation is usually less perfectly planar than slate cleavage and may wrap around small lenses or produce corrugated surfaces. Individual mica flakes remain difficult to see without magnification.

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.

Luster

Silky sheen across foliation

A primary clue distinguishing phyllite from duller slate.

Grain size

Mica generally not individually visible unaided

Separates phyllite from coarser schist.

Foliation

Wavy, crinkled, or gently folded surfaces

More irregular than typical planar slaty cleavage.

Comparison

Common lookalikes

Slate

Usually duller with flatter, more regular slaty cleavage.

Schist

Contains individually visible mica flakes or other metamorphic minerals and commonly has coarser foliation.

Shale

Splits along sedimentary bedding and lacks pervasive metamorphic sheen and cleavage.

Geologic origin

How does it form?

Phyllite forms when slate or mud-rich sedimentary rock experiences additional heat, pressure, and recrystallization during regional metamorphism.

It represents a broad textural grade between slate and schist rather than one exact temperature or pressure.

Where it occurs

Geologic setting and occurrence

Phyllite occurs in regional metamorphic belts where mud-rich rocks reached low to moderate metamorphic grade, including parts of the Appalachians and western mountain belts.

Boundaries with slate and schist are gradual; field names should reflect the observed fabric and grain size rather than false precision.

Human use

Uses and significance

Phyllite is used locally for decorative stone, paving, roofing, and landscaping where cleavage, durability, and weather resistance are suitable.

Safety and limits

Field notes

  • Rotate the sample in diffuse light to see the sheen.
  • Thin foliation slabs can be sharp and unstable underfoot.
  • Avoid creating dust from unknown metamorphic 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.