Glaucophane Schist (Blueschist)
Blueschist (Glaucophane-bearing schist)
Rock Type: metamorphic

Physical Properties
Hardness: 5-6 (Mohs scale); Color: Blue to lavender, blue-grey; Luster: Pearly to vitreous or silky; Crystal structure: Monoclinic (prismatic); Cleavage: Perfect in two directions; Specific gravity: 3.0-3.3
Formation & Geological History
Formed through high-pressure, low-temperature metamorphism (subduction zone metamorphism). Usually found in mountain belts where oceanic crust was forced beneath continental crust.
Uses & Applications
Primarily used for geological research and as an indicator of ancient tectonic subduction zones; occasionally used as decorative landscaping stone or for minor lapidary work.
Geological Facts
Blueschist is often called 'high-pressure' rock because it requires pressures of several kilobars but temperatures below 500 degrees Celsius to form, representing a specific metamorphic facies.
Field Identification & Locations
Identify by its distinct blue-to-grey color and foliated (layered) texture. Commonly found in coastal ranges like California (Franciscan Complex) or the Alps. Look for needle-like crystals of blue glaucophane.
Identified on: 4/16/2026
Mode: Standard