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Kilbourne Hole NM Mantle Xenolith Peridotite Olivine Geology Rock Specimen
Product Details
Authentic upper-mantle xenolith from Kilbourne Hole, New Mexico, a well-known volcanic maar locality near El Paso, Texas. Kilbourne Hole is famous for mantle material that was carried rapidly to the surface during volcanic activity. This specimen is an olivine-rich peridotite mantle xenolith with an attractive exposed crystalline interior showing abundant green olivine and contrasting darker minerals. The weathered exterior provides a nice contrast with the fresh broken surface. Kilbourne Hole mantle xenoliths can include lherzolite, harzburgite, dunite and related ultramafic rocks. This specimen has not been petrographically or chemically analyzed, so I am not assigning a more specific peridotite classification. An excellent display or teaching specimen illustrating material derived from Earth's upper mantle. Locality: Kilbourne Hole, DoΓ±a Ana County, New Mexico, USA Rock type: Peridotite / mantle xenolith Primary visible mineral: Olivine Provenance: Personally collected at Kilbourne Hole approximately 26 years ago. Please see photos for exact size, appearance and condition.
Daily Cleaning: Use a soft brush or damp cloth to gently wipe away dirt. Avoid harsh chemicals. For mesh areas, use diluted mild detergent and a soft brush.
Drying: Air dry in a cool, shaded place after cleaning. Avoid direct sunlight or high heat, which can cause fading and glue deterioration.
Storage: Stuff with paper to maintain shape when not in use. Store in a dry, ventilated area to prevent mold. Rotate between multiple pairs to extend lifespan.
Usage Notes: Designed for basketball. Not recommended for hiking, long-distance running, or other specialized sports where different performance features are required.


