Pallasites are among the most beautiful and rarest meteorites, and NWA 13188 is no exception. Classified as a pallasite, this meteorite is composed of semi-transparent olivine (peridot) crystals set in a gleaming metallic iron-nickel structure. It is believed to have formed at the boundary between the core and mantle of a differentiated asteroid, making it both scientifically valuable and visually stunning.
Discovered in the deserts of Morocco by certified meteorite hunters, this specimen was carefully collected, preserved, and verified by experts. The olivine crystals display a golden-green hue when backlit, offering a mesmerizing contrast to the metallic matrix. Each polished slice reveals a unique cosmic pattern forged by planetary differentiation and deep space collisions.
NWA 13188 represents a window into early solar system geology and the dynamic processes within planetesimals. The iron-nickel framework suggests it once resided near the core of a disrupted proto-planet, while the olivine hints at mantle material — an extraordinary combination rarely seen on Earth.
Highly sought-after by collectors, museums, and institutions, pallasites like NWA 13188 are sold by the gram due to their rarity and beauty. Whether displayed as a gemstone-like slice or studied for its mineralogy, this Moroccan discovery offers timeless fascination and undeniable extraterrestrial prestige.
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