Loading, please wait...
Details
LOT 2870
Fossil Woolly Mammoth Molar Tooth
DEVENSIAN PERIOD, 110,000-12,000 YEARS B.P.
5 1/4 in. (600 grams, 13.2 cm).
From Mammuthus Primigenius, inked collector's note 'VM19' to one side. [No Reserve]
Provenance
From Asland, Montana, USA.
From the private collection of Kenneth Machin (1936-2020), Buckinghamshire, UK; his collection of antiquities and natural history was formed since 1948; thence by descent.
VETTING:
TimeLine Auctions follows a vetting process to ensure the authenticity and legality of all items, reinforcing our commitment to integrity and responsible trading. Each antiquity, antique, and coin lot undergoes thorough examination by a vetting committee of at least ten external specialists, professional trade association members, scientists, and archaeologists: Our Vetting Process
AUCTIONS:
TimeLine is a leading auction house specialising in antiquities, ancient art, collectables, natural history, coins, medals, and books. Our auctions offer museums, collectors, historians, and enthusiasts the opportunity to acquire unique and historically significant pieces.
RELATED LOTS
-
Insect Nest in Polished Amber
Oligocene Epoch, circa 45 million years B.P.Sold for (Inc. bp): £72
A polished pebble with a network of intersecting tunnels, possibly a part of a termite nest. 12.2 grams, 45 mm
Property of a North West London, UK, lady. -
Crystal and Mineral Display Specimen Collection
Sold for (Inc. bp): £39
Comprising: a lapis lazuli flower, optic calcite, quartz, ruby in zoisite, twinned aquamarine crystal, a signed glass dish, and others. 730 grams total, 31-79 mm
Property of a North West London, UK, lady. -
Large Cave Stalagmite Section
Sold for (Inc. bp): £26
A colossal cut section of cream-coloured stalagmite showing natural ripples. 66.7 kg, 90 cm
Previously from a Hong Kong collection. Ex property of a London, UK, gentleman, 1990s.
A stalagmite, is an upward-growing mound of mineral deposits growing on the floor of a cave due to accumulation of material deposited from ceiling drippings. They are typically formed by the deposition of calcium carbonate and other minerals, which is precipitated from mineralised water solutions. Limestone is the chief form of calcium carbonate rock which is dissolved by water that contains carbon dioxide, forming a calcium bicarbonate solution in underground caverns.