NWA 869 Meteorite Value Guide

The NWA 869 meteorite is a renowned L3-6 ordinary chondrite discovered in the Sahara Desert in 1999. It is highly collectible due to its ancient age of 4.5 billion years and its unique brecciated structure that showcases the early history of our solar system.

What affects the value of NWA 869 Meteorite?

• The presence of a well-preserved, dark fusion crust significantly increases market value.
• Specimen size and weight, with larger individual stones typically commanding higher prices.
• The clarity and density of visible chondrules when the meteorite is sliced or polished.
• Overall preservation state, specifically the lack of terrestrial oxidation or weathering.

How to Identify NWA 869 Meteorite?

• Look for a dark, weathered fusion crust on the exterior of the specimen.
• Examine the interior for visible, colorful chondrules and small flecks of iron-nickel metal.
• Check for a brecciated appearance, which indicates a mix of different rock types fused together.
• Verify the classification as an L3-6 chondrite, which signifies low iron content and varying thermal metamorphism.

History of NWA 869 Meteorite

The NWA 869 meteorite is a significant find from Northwest Africa, discovered in large quantities beginning in 1999. It is classified as an L3-6 ordinary chondrite, meaning it is primarily composed of silicate minerals and has experienced varying degrees of thermal metamorphism. Its widespread availability and fascinating structure make it a popular choice for collectors and researchers alike, offering a tangible connection to the early solar system.