Iron Meteorites
Iron meteorites are composed largely of nickel-iron metal, and most
contain only minor accessory minerals. These accessory minerals often
occur in rounded nodules that consist of the iron-sulfide troilite or
graphite, often surrounded by the iron-phosphide schreibersite and the
iron-carbide cohenite. Despite the fact that some iron meteorites contain
silicate inclusions, most have fundamentally the same superficial
appearance.
Presently, iron meteorites are classified under two established systems.
Just a few decades ago, iron meteorites were exclusively classified
according to the macroscopic structures revealed when their polished
surface was etched with nitric acid. Depending on these structures, they
were separated into three classes: octahedrites, hexahedrites, and
ataxites.
El Sampal
Iron fine Octahedrite IIIA
Found in 1973 in Chubut, Argentina
TKW 142 Kg
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El Sampal 00
crusted full slice
60gr
SOLD |
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El Sampal 01
crusted part slice
60gr
SOLD
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El Sampal 02
crusted part slice
36gr
SOLD
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More slices available, ask for your size !!!
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