Description
About 86 per cent of meteorite falls on our planet are of ordinary Chondrites origin, however these Chondrites are very rare as the commonest meteorite falls are iron meteorites [these record about 300 tons of fall to earth from 60 different origins], where as the Chondrites record about 50 tons of falls to earth, so much more rare than iron meteorites.
Condition report
extremely fine Meteorite, solid state, not crumbly , no fragile cracks or Fischers that will incur future de-stabilising, smooth melt patina, enhanced by the desert varnish or desert weathering patina accumulated over a long period of time, which gives these meteorites their signature. Through the process of falling to earth the temperatures of the meteorite can reach up to a thousands of degrees, causing internal changes in the metals and minerals, this metamorphism is the way many of the meteorites are identified.Location & Classification
Open site the Sahara Desert. Collected thence Traded through Berber Nomadic sources between S. E. Moroccan and W. Algerian border area. This is a NWA [North West Africa] classification number. Some of the best places on our planet to search for meteorites are open sites void of human habitations such as deserts and Polar Regions, where weathering or melting take place over eons exposing the few meteorite falls for discovery and identification by professional scientists and enthusiasts.Each fall is given a classification and geographical identification reference.




