- When clay- and aluminum-rich rock is altered by water from geothermal systems, serpentinite is liable to form. Often found in low-grade metamorphic areas, serpentinite is composed of hydrated silicate minerals, particularly phyllosilicates
- Ideal for identification & classification exercises. Greenish in color and smooth to the touch, serpentinite is often found as a plane of weakness in faulted rocks. Excellent for lessons on metamorphic rocks, low-grade deformation, and structural geology. This set of six samples is excellent for group study and examination
- Each specimen is selected and hand processed, ensuring each sample exhibits defining features
- Sourced from a variety of locations around the world
- Each specimen sample is packaged in a transparent bag, and is labeled & barcoded for easy identification
When clay- and aluminum-rich rock is altered by water from geothermal systems, serpentinite is liable to form. Often found in low-grade metamorphic areas, serpentinite is composed of hydrated silicate minerals, particularly phyllosilicates. Ideal for teaching students about rounding and sorting, as well as for identification & classification exercises. Greenish in color and smooth to the touch, serpentinite is often found as a plane of weakness in faulted rocks. Excellent for lessons on metamorphic rocks, low-grade deformation, and structural geology.
While each specimen will vary slightly in shape, size and color, it will measure approximately 1" in length. Each is individually packaged, labeled & barcoded for easy identification and storage.
Each specimen is selected and hand processed, ensuring that each sample exhibits defining features. Pack of 12 samples.