NWA 869 Chondrite Meteorite Value Guide

The NWA 869 is a renowned L-type stony chondrite discovered in the Sahara Desert near Tindouf, Algeria, in 2000. It is highly collectible for its ancient composition, containing material from the solar system's formation over 4.5 billion years ago.

What affects the value of NWA 869 Chondrite Meteorite?

• Total weight and physical dimensions of the individual specimen.
• The presence and preservation quality of the dark fusion crust.
• Clarity of internal features like olivine and pyroxene chondrules.
• Market demand for well-documented specimens from the original 2000 discovery.

How to Identify NWA 869 Chondrite Meteorite?

• Look for a dark, weathered fusion crust on the exterior of the raw specimen.
• Identify visible silicate inclusions and small metallic flakes of nickel-iron within the matrix.
• Check for the characteristic brecciated structure often found in this specific Algerian strewn field.
• Verify the specimen exhibits a slight magnetic attraction due to its iron content.

History of NWA 869 Chondrite Meteorite

NWA 869 refers to a large meteorite strewn field discovered in the Sahara Desert near Tindouf, Algeria, in the year 2000. It is one of the most famous and well-studied L-type chondrites, representing material from the early formation of the solar system over 4.5 billion years ago. These stones were transported across the desert by nomads and have become a staple for collectors due to their beautiful interior structures.