This meteorite has been cleaned to reveal the aggregates of olivine crystals suspended in natural coils and tendrils of its durable iron-nickel matrix, the cut face reveals translucent olivine and peridot crystals in a metallic matrix, polished to mirror finish on one side; supported in custom stand.

2³⁄₈ x 2¹⁄₄ x 1/4in. (6 x 5 x 0.6cm.)
with stand: 4¹⁄₄in. (10.8cm.) high

83g.

This lot is offered without reserve.
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.
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Conditions of Sale
FAQs
This lot is offered by Christie Manson & Woods Ltd

Brought to you by

James HyslopHead of Department, Science & Natural History

A Christie's specialist may contact you to discuss this lot or to notify you if the condition changes prior to the sale.

jhyslop@christies.com +44 (0) 20 7752 3205

View condition report

Lot Essay

Pallasites are widely considered the most beautiful meteorites, and Imilac is among the most coveted. Like all main-group pallasitic meteorites, Imilac originated from the mantle-core boundary of an asteroid that broke apart during the early history of our solar system. The crystals seen here are the result of small chunks of the stony mantle becoming suspended in molten metal near the surface of an asteroid’s iron-nickel core. Cut and polished to a mirror finish, the lustrous metallic matrix features crystals of gleaming olivine and peridot (gem-quality olivine) ranging in hues from amber to emerald.