| Northwest Africa (NWA) 906|
As an H3.8 this is one of the less common classifications of chondrites. It had had less heating and melting in it history of travelling our solar system. It has a nice even scattering of the small metal grains characteristic of H chondrites and small chondrule are easily visible. It has a somewhat more porous texture than most stone meteorites.
Copyright © 1996–2017 The Meteorite Exchange, Inc. All Rights Reserved.
The Meteorite Exchange Inc., 1121 West Valley Blvd, Ste. I #165, Tehachapi CA 93561
Users online: 153 anonymous customer(s)