The Palo Verde Mine meteorite is a unique ordinary chondrite (L6), discovered on March 11, 2004, in Mohave County, Arizona, USA. - Description language - German

The Palo Verde Mine meteorite is a unique ordinary chondrite (L6), discovered on March 11, 2004, in Mohave County, Arizona, USA. With a total mass of 9158 grams, divided into two pieces, it stands as a significant find in meteoritic research.

L6 chondrites are characterized by their lower metallic iron content, distinguishing them from other ordinary chondrites. This specimen exhibits a moderate shock stage (S4) and mild weathering grade (W2), indicating exposure to both cosmic and terrestrial influences while maintaining its original structure.

Its mineral composition includes olivine (Fa25), pyroxene (ferrosilite Fs21), and wollastonite (Wo1.39), offering valuable insights into the formation processes of the early solar system and the evolution of meteoritic bodies.

Due to its fascinating history, scientific significance, and aesthetic value, Palo Verde Mine is a sought-after meteorite for collectors and researchers alike.