| Northwest Africa (NWA) 528
This high metal chondrite was found near the end of 2000 and is an H4 type. Chondrules are visible and there is a typical dense scattering of small metal grains throughout the stone.
Copyright © 1996–2018 The Meteorite Exchange, Inc. All Rights Reserved.
The Meteorite Exchange Inc., 1121 West Valley Blvd, Ste. I #165, Tehachapi CA 93561
Users online: 98 anonymous customer(s)