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A pallasite is a type of stony, iron meteorite. It consists of small sized olivine crystals of peridot quality in an iron-nickel matrix.

Coarser metal areas develop Widmanstätten patterns upon etching which are unique figures of long nickel iron crystals, found in the octahedrite iron meteorites and some pallasites.

The first meteorite found bearng these qualities was a Krasnojarsk meteorite. With a mass of about 700 kg it was detected in 1749 about 145 miles south of Krasnojarsk by P.S. Pallas in 1772 and transported to Krasnojarsk where it got it's name.

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What is a pallasite?

A pallasite is a stony-iron meteorite embedded with glassy crystals of olivine.


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The last meteorite found in England is the Hambleton meteorite - officially accepted and named as such by the Meteoritical Society. The 17.6kg meteorite was found in the Hambleton district of North Yorkshire, England during August 2005 by meteorite hunter Rob Elliott. Hambleton is a rare type of meteorite known as a pallasite - pallasites are believed to originate from the core-mantle boundary layer within large asteroids. More information at http://fernlea.tripod.com/hambleton.html


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