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"Fragmentation due to weathering and abrasion processes such as frost wedging, salt production, wind abrasion, chemical exsolution, and biological actions also contribute to the number of specimens ultimately found on a stranding surface. The vast majority of meteorites from Antarctica exhibit significant weathering features, even those found still enclosed in ice, due to exposure to saltating snow and ice particles, long duration freeze-thaw cycles, and evaporite formation."
Harvey R. P.
(Moving Targets: The Effect of Supply, Wind Movement and Search Losses on Antarctic Meteorite Size Distributions, 1994) |
"While the masses of most meteorites from Antarctica, Roosevelt County, and the Nullarbor Plain are on order of 10-100 g, meteorites found in the Sahara are generally larger. Most meteorites are weighing between 100 and 1000 g."
(Geiger T., Bischoff A., 1994) |
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Right image :
New meteorite from Dar al Gani,
waiting classification
white veins are metal, gemlike yellow
inclusions, grey-black matrix
without chondrules.
(SaharaMet expedition 2000)
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From 1995, date of the first systematic prospecting on Dar Al Gani by anonymous finder teams, more than 1000 individual meteorites have been recovered on this small Libyan plateau, including 4 Mars rocks, two lunar meteorites, and numerous other rare ones (some varieties totally unknown before).
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