NWA 869 Meteorite

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41,00 €
SKU: CA123
 Back to: Meteorites

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Classification: Ordinary chondrite L 4-6, S3, W1: L (Low iron) (or olivino-hyperstenas or olivino-pigeonitas). Main minerals; olivine, hyperstena, Ni-Fe.

3 fragments of meteorite broken by the impact on the ground, but retains part of the fusion crust. They weigh 10,23 grams.

"The rocky meteorites comprise a great variety of types, the most abundant being the ordinary chondrites, the carbonaceous chondrites and the acondrites.

of silicates such as olivine and pyroxene, but their fundamental characteristic is that they have some spherules (chondrules), in their interior, those spheres are primordial materials

of our solar system, are the oldest and most fascinating materials that we can see and have in our hands.

* It is believed that this ordinary chondrite meteorite fell more than what is now Algeria and Morocco. His fall was exceptionally strong. Since its discovery in 2000, more than 7 tons of rain have been removed in the size of a fraction of an ounce of more than 50 pounds.

It is classified as an ordinary chondrite. The bright spots of iron on the surface of the cut are visible, which causes a slight magnetic attraction.
Many of these samples are collected by nomads. Since geographical features and political boundaries are not easily discernible in this section of the Sahara. Its exact location is not available.

Pick up 2012


Sahara: Morocco, Algeria

 

 

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