拍品 22
拍品 22
A GIBEON METEORITE CRYSTAL

IRON, FINE OCTAHEDRITE GIBEON, GREAT NAMA LAND, NAMIBIA

成交價 USD 2,000
估價
USD 1,000 - USD 1,500
估價並不反映實際成交價,亦不包括買家應付酬金、任何適用稅項或藝術家轉售權。詳情請瀏覽業務規定D部。
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A GIBEON METEORITE CRYSTAL

IRON, FINE OCTAHEDRITE GIBEON, GREAT NAMA LAND, NAMIBIA

成交價 USD 2,000
登記
成交價 USD 2,000
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詳情
A GIBEON METEORITE CRYSTAL
Iron, fine octahedrite
Gibeon, Great Nama Land, Namibia

Draped in a mottled patina, the clean edges and crystalline octahedral habit of Gibeon meteorites is amply revealed. A flange protrudes from the mass as cleavage was continuing to occur when this specimen was recovered, however, as this specimen is in effect comprised of extraterrestrial steel, the outthrust is an unbendable artifact of a geological process frozen in time.

57 x 32 x 18mm. (2¼ x 1¼ x ¾in.)
111g.

Please note that this lot is the property of a private collector.
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拍品專文



A GIBEON METEORITE CRYSTAL — EXTRATERRESTRIAL STEEL

Among the most spectacular iron meteorites known are the Gibeons found in Namibia’s Kalahari Desert. Although familiar to the natives, who had hammered small pieces into weapons and tools, the Gibeon meteorite was not known to westerners until about 1836. Gibeon crystallized deep in the molten iron core of an asteroid. An enormous impact event later shattered this asteroid and ejected the Gibeon mass into interplanetary space where it resided for millions of years until it impacted Earth. Gibeon meteorites are comprised primarily of two iron-nickel alloys whose molecules slowly organized into their crystalline octahedral habit. Exposure to the elements during a residency on Earth for thousands of years is not the most hospitable environment for meteorites. As a result of expanding and contracting from heating and cooling, some Gibeon iron meteorites slowly split along their crystalline planes (see lot 9). This example is not only defined by its crystalline cleavage but the very process of splitting is also in evidence.

Christie's would like to thank Dr. Alan E. Rubin at the Institute of Geophysics and Planetary Physics, University of California, Los Angeles for his assistance in preparing this catalogue note.

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