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The
Brenham pallasite was originally discovered
in Kansas in 1882. During the following century further finds were made, until, in 2005, a huge 635kg oriented individual was recovered. It is from this recent discovery that this beautiful 56g slice originates |
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Two
really beautiful chunks of Brahin, with
masses of 104g and 156g. These examples have gorgeous green and yellow olivine crystals and excellent fusion crust. Brahin was discovered in 1810 near Minsk, Belorussia. It is one of the best-known and most sought-after pallasites! We have a good number of beautiful translucent slices at the moment: contact us for details! |
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Another
translucent slice of Brahin, this time with a mass of 29g. Brahin is becoming quite hard to obtain these days, so don't miss this opportunity to add a slice to your collection. |
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A
third beautiful sample of Brahin, with a
good
mass of 45g and a thickness of 6mm. Other examples are always in stock, from £30 upwards! |
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The
Pallasovka meteorite was found in 1990 in
the Volgograd region of Russia. It belongs to the main group of pallasites but is characterized by unusual chromite content. This slice has a mass of over 34g and has beautiful large olivines. |
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A
large, truly beautiful example of the
Pallasovka meteorite, with a mass of 38.9g. As above, this slice is just packed with large olivine crystals! |
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The
Admire pallasite
was discovered in Lyon
County, Kansas in 1881: in total around 80kg have been recovered. We have a small quantity of 20 - 30mm translucent slices with masses around 2g - 3g. |
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NWA
4482 is a recently-discovered ancient
pallasite, recovered in Morocco in 2006. Like Huckitta, much of the original iron has turned into shale and oxides. A fascinating item! |
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A
second example of NWA
4482 ,
this time
with a mass of 36g |
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Huckitta
is a very ancient pallasite
from
Australia. It is increasingly hard to obtain samples of this beautiful highy-altered find, particularly specimens with a decent mass: Contact us to see what's available! |
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The
Vaca Muerta mesosiderite was found in 1861 at Taltal, Atacama, Chile. Mesosiderites were formed on the surface of a parent body as a result of an impact with another body, and display a stony matrix in which are suspended chunks of nickel-iron. Many shapes and sizes and other types always available: this has a respectable mass of 21g |
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Another
Vaca Muerta mesosiderite, this time
with a mass of 20g.All of our samples have a window polished into the surface to expose the internal structure. |
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