sedimentary

Graywacke

Graywacke (immature sandstone)

AI-generated identification · may be incorrect

Hardness: 6-7 Mohs; Color: Dark gray to greenish-gray; Luster: Dull/Earthy; Crystal structure: Clastic (fine to coarse grains); Cleavage: None (conchoidal to irregular fracture); Specific gravity: 2.6-2.7

Hardness: 6-7 Mohs
Color: Dark gray to greenish-gray
Luster: Dull/Earthy

Identified May 20, 2026More sedimentary →

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Physical properties

Formation & geological history

Formed in deep-ocean environments through turbidity currents (underwater landslides). It consists of poorly sorted, angular grains of quartz, feldspar, and rock fragments in a clay-rich matrix. Often Paleozoic or Mesozoic in age.

Uses & applications

Used primarily as high-quality road aggregate, railway ballast, and in heavy construction where durability is required. Occasionally used for decorative stone in landscaping.

Geological facts

Graywacke is often called 'dirty sandstone' because of its high matrix content. It is a key indicator of ancient active continental margins and tectonic activity.

Field identification & locations

Identify by its characteristic 'salt and pepper' appearance, extreme hardness, and dark, muddy color. Often found in folded mountain belts and coastal regions. Avoid smooth faces; check for angular grain visibility.