HAMMADAH AL HAMRA 346 Type L6 Meteorite - 68 g






Over 20 years collecting meteorites; former museum curator and experienced restorer.
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Hammadah al Hamra 346, a complete L6 meteorite from Libya, with fall recorded in April 2018 and a weight of 68 g.
Description from the seller
Fantastic complete L5-type meteorite for its low iron content
Previously known as Ghadamis, this meteorite is supposed to have fallen in April 2018, and it has only now finally been officially classified.
In this superb meteorite, you can observe a multitude of meteorite features, such as regmaglypts, fusion crust, and flight lines.
Regmaglypts are formed by the air sculpting the hot surface of the meteorite.
The fusion crust is produced by the extreme temperatures reached during entry into the atmosphere, temperatures approaching 7000°C, and is the reason why spacecraft are fitted with a protective thermal shield.
The flight lines are formed as the material aligns with the direction of fall.
The contraction crust forms when the meteorite rapidly cools, and the fusion crust cracks, leaving this rarely seen pattern.
At Expometeoritos, we handle outreach, talks, workshops, analyses, classification, and exhibitions of meteorites.
We are members of:
.- IMCA (International Meteorite Collectors Association) #8187
.- Meteoritical Society
.- American Meteor Society
All our pieces are certified and, moreover, we provide a chemical composition analysis if the piece's value exceeds €300, conducted at our facilities by X-ray spectrometry.
Seller's Story
Fantastic complete L5-type meteorite for its low iron content
Previously known as Ghadamis, this meteorite is supposed to have fallen in April 2018, and it has only now finally been officially classified.
In this superb meteorite, you can observe a multitude of meteorite features, such as regmaglypts, fusion crust, and flight lines.
Regmaglypts are formed by the air sculpting the hot surface of the meteorite.
The fusion crust is produced by the extreme temperatures reached during entry into the atmosphere, temperatures approaching 7000°C, and is the reason why spacecraft are fitted with a protective thermal shield.
The flight lines are formed as the material aligns with the direction of fall.
The contraction crust forms when the meteorite rapidly cools, and the fusion crust cracks, leaving this rarely seen pattern.
At Expometeoritos, we handle outreach, talks, workshops, analyses, classification, and exhibitions of meteorites.
We are members of:
.- IMCA (International Meteorite Collectors Association) #8187
.- Meteoritical Society
.- American Meteor Society
All our pieces are certified and, moreover, we provide a chemical composition analysis if the piece's value exceeds €300, conducted at our facilities by X-ray spectrometry.
