Meteorite Fragment with Peridot Crystals in Iron Matrix

Stony-iron, pallasite - PMG Circa 4.5 Billion y/o Weight: 34.68 kg Height (including base): 53 cm Width: 29 cm A magnificent and extremely sculptural specimen of the Seymchan meteor...

A magnificent meteorite sphere, cut from the famous Aletai meteorite and polished to reveal the shimmering iron-nickel matrix and the beautiful crystalline Widmanstätten pattern — a ...

NWA 12759 Stone, Chondrite - L5 18.3 KG “This specimen of the NWA 12759 L5 chondrite has a smooth posterior fusion crust where meteoritic melt pooled as the rock descended through the atmosphere and was heated by friction with molecules of air. The meteorite is from the L-chondrite asteroid that was destroyed by an energetic collision 470 million years ago.” Dr Alan E. Rubin, PhD Department of Earth, Planetary, and Space Sciences, UCLA Detached from its parent body by a mighty impact, this large, oriented meteorite travelled over a hundred million miles through space before falling to Earth in the North African desert. Beautiful regmaglypts radiate from the apex of its cone shaped nose. These elongated dimples formed when streaks of superheated molten rock streamed off the meteor’s surface as it blazed through the atmosphere. The entire piece is coated in a glossy, umber-coloured fusion crust and close examination reveals remnants of encrusted, orange dirt. Whilst most meteors tumble as they travel through the Earth’s atmosphere, oriented meteorites...

Oriented Chondrite Meteorite Circa 4.56 Billion y/o Chondrite 24 x 20 cm, 28 cm tall on base 7.1 kg A sculptural and beautifully weathered chondrite meteorite; upon entering the atmosphere, this extraterrestrial stone would have heated the surrounding air to a temperature of over 1700 C, higher than that of the hottest lava on the planet, and enough to melt away its outer layers, leaving its surface rippled with regmaglypts, thumb-shaped impressions formed as superheated rock streaked off of the main body as it careened toward the earth. The last layer of the rock to melt would have re-solidified as the meteorite made impact, forming a charcoal coloured fusion crust, which has taken on a deep ochre-tinted patina. Chondrite meteorites such as this example were formed at the very beginning of our solar system, by the accretion of various types of dust and small grains, adrift in the vacuum of space and, as such, provide important clues about the birth of our own planet. This piece is an especially rare specimen, known as an oriented meteorite...

Sculptural 18th century Italian candlestick mounted with chalcopyrite and calcite crystals in matrix. The gilded fragment was originally part of a candlestick in a historical Italia...

17th century Italian gold leaf fragment with calcite crystals in a rock matrix with gold leaf crystal quartz and mounted on a rock coral base. This fragment was originally part of a...

Sculptural 18th century Italian fragment decorated with mica and crystal quartz points on a polished agate base. The 18th century fragment originally came from a candlestick in a his...

Sculptural 18th century Italian mecca gilded candlestick decorated with amber mounted on tangerine crystals in matrix base. This mecca gilded candlestick was originally part of a historical Italian church in Italy. It has been adorned with amber and mounted on the coordinating tangerine crystal quartz cluster in matrix. The piece is put together by Jean O'Reilly Barlow, the artist and creative director of Interi. The date of manufacture reflects when she transformed the piece and the period shows that the Italian fragment is originally 18th century. The Italian church artifact and tangerine crystal in matrix are put together in a sculptural form - creating an organic and historically significant...