Natural History - Large Historic 'Shepton Mallet, Somerset' Calcite Crystal Specimen

Comprising: erythrite from Mount Cobalt, Queensland, Australia, collection number 473; azurite from Nchanga Mine, Chingola, Zambia, collection number 443, with an old Gregory, Bottley & Lloyd label; a cut and polished onyx agate slice from Brazil, collection number 270; turquoise from Turquoise Mountain, Arizona, USA, collection number 487, with an old Gregory, Bottley & Lloyd label; natrolite from Ireland, collection number 496; a cut and polished agate slice from Mexico, collection number 327; quartz, collection number 312; quartz from North Transvaal, South Africa, collection number 206; quartz from Cumbria, England, collection number 19. 353 grams total, 32-67 mm



Acquired on the UK mineral and fossil market, since 1970. From the historic mineral collection of Richard Valentine Cain, London, UK, thence by descent. Seven specimens accompanied by an original historic index file card.

Displaying a later carved stylised face with exaggerated facial detailing. 106 grams, 72 mm



Private UK collection formed in the 1980s. Property of an East Sussex, UK, teacher.

A nickel-iron meteorite (IAB). 25.3 grams, 25 mm



From a Lincolnshire, UK, collection.

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.