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Smectite
Scanning electron microscope (SEM) photograph of smectite clay – magnification 23,500 – U.S. Geological Survey – Tuckup Canyon
Scanning electron microscope (SEM) photograph of smectite clay – magnification 23,500 – U.S. Geological Survey – Tuckup Canyon
Typical cracks pattern of a smectite-rich bentonite after its desiccation and shrinkage
Typical cracks pattern of a smectite-rich bentonite after its desiccation and shrinkage
Typical volcanic eruption plume whose ashes' weathering after contact with seawater is the main source of smectite. Leaching of most of amorphous sili
Typical volcanic eruption plume whose ashes' weathering after contact with seawater is the main source of smectite. Leaching of most of amorphous silica leads to partial dissolution of obsidian, the main constituent of volcanic glass.
Bentonite layers from an ancient deposit of weathered volcanic ash tuff in Wyoming
Bentonite layers from an ancient deposit of weathered volcanic ash tuff in Wyoming
Gray shale and bentonites (Benton Shale; Colorado Springs, Colorado)
Gray shale and bentonites (Benton Shale; Colorado Springs, Colorado)
Making a bentonite slurry for fining after wine pressing
Making a bentonite slurry for fining after wine pressing