Details
Of robust form with deep prominent scoops to the surface, a rich patina drapes the surface of the meteorite with highlighted accents to the ridges.
1112 x 1014 x 512in. (29 x 26 x 14cm.)
37.4kg.
Special notice
This lot will be removed to Christie’s Park Royal. Christie’s will inform you if the lot has been sent offsite. Our removal and storage of the lot is subject to the terms and conditions of storage which can be found at Christies.com/storage and our fees for storage are set out in the table below - these will apply whether the lot remains with Christie’s or is removed elsewhere. Please call Christie’s Client Service 24 hours in advance to book a collection time at Christie’s Park Royal. All collections from Christie’s Park Royal will be by pre-booked appointment only. Tel: +44 (0)20 7839 9060 Email: cscollectionsuk@christies.com. If the lot remains at Christie’s it will be available for collection on any working day 9.00 am to 5.00 pm. Lots are not available for collection at weekends.
This lot has been imported from outside of the UK for sale and placed under the Temporary Admission regime. Import VAT is payable at 5% on the hammer price. VAT at 20% will be added to the buyer’s premium but will not be shown separately on our invoice.
Please note this lot is the property of a consumer. See H1 of the Conditions of Sale.
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Lot Essay

Like most iron meteorites, Gibeon meteorites formed 4.5 billion years ago within the molten core of an asteroid whose shattered remains are part of the asteroid belt. An impact event ejected what was to become the Gibeon mass into interplanetary space. Gibeon meteorites are the bounty that landed on Earth thousands of years ago when the wandering iron mass slammed into the atmosphere before exploding and raining down in what is now the Kalahari Desert in Namibia. In previous generations, indigenous tribesmen recovered small meteorite fragments at or near the surface and fashioned them into spear points and other tools. This specimen was recovered with the aid of a metal detector. Its final shape is the product of its composition, the soil chemistry where it landed, its orientation in the ground, the amount of groundwater to which it was exposed and the length of time of such exposure. All these factors slowly reshaped this mass as it sat near the Earth’s surface as the seasons turned over thousands of years.

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