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LOT 2279
Natural History - Woolly Mammoth Tusk Section
PLEISTOCENE AGE, CIRCA 40.000 YEARS B.P.
7 1/2 in. (126 grams, 19 cm).
Displaying some attractive patterning. [No Reserve]
ProvenanceFrom the North Sea.
From an old Bristol, UK, collection.
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AUCTIONS:
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Natural History - Whitby Dac Fossil Ammonite Nodule
Lower Jurassic Period, Toarcian Stage, circa 180 million years B.P.Sold for (Inc. bp): £20
The nodule halves comprising the positive and negative of Hildoceras sp. ammonite. 613 grams total, 9.2-10.7 cm
Ex Lincolnshire, UK, collection. -
Natural History - Large NWA 15250 L5 Chondrite Meteorite Slice in Case
Found 2022 A.D.Sold for (Inc. bp): £208
The cut and polished slice held in a custom-made collector's display box. 51 grams total, 84 mm wide including case
From the Sahara Desert, North Africa. Property of a Sussex, UK, teacher. Accompanied by a specimen identification card from Adrian Contreras Gomez.
Chondrites are the oldest materials in the solar system with an estimated age of formation of 4.55 billion years. -
Natural History - Campo Del Cielo Iron Meteorite Pair
Fell 6000-5000 years B.P.Sold for (Inc. bp): £33
Comprising two amorphous Campo Del Cielo iron (IAB) meteorites. 3.75 grams total, 10-13 mm
From Chaco Province, Argentina, found 1576. Property of an East Sussex, UK, teacher.
A crater field of roughly 26 craters was found in the vicinity of this crater, which is estimated to date to 4-5 thousand years BP. The age of the meteorite itself is thought to be c.4.5 billion years, formed as part of the development of this solar system. The largest two fragments, the 30.8 ton Gancedo and 28.8 ton El Chaco, are among the heaviest meteorite masses ever recovered on Earth. In 1576, the governor of a province in Northern Argentina commissioned the military to search for a large mass of iron, which it was believed the local people claimed had fallen from the sky and which they used for their weapon production. The expedition discovered a large mass of metal which was assumed to be an iron mine and brought back a few samples, which were described as being of unusual purity. Following the legends, in 1774 Don Bartolomé Francisco de Maguna rediscovered the iron mass. He himself did not believe that the stone had fallen from the sky and assumed that it had formed by a volcanic eruption. However, he sent the samples to the Royal Society of London. In 1990 it became protected by law.
