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LOT 2425
Collection of Cabochon Rubies
1/8 - 1/2 in. (5.15 grams total, 8-11 mm).
Comprising six polished cabochons, some lead glass-filled. [6]
ProvenancePrivate collection, London, UK.
CONDITIONTimeLine 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:
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LOT 2425
Collection of Cabochon Rubies
Estimate £120 - 170€140 - 200 (for guidance only)$160 - 230 (for guidance only)
Opening Bid
£60 (EUR 70; USD 81) +BP*
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Group of Twelve [12] Minerals and Crystals
Estimate: £30 - 40 (+bp*)
Opening Bid: £5
Mixed group of specimens including malachite, 'desert rose', quartz, rose quartz, amethyst, pyrite, agate, and others. 2.96 kg total, 3.4-20.2 cm
Ex Mineral Imports, London, UK. Gregory, Bottley & Lloyd (Gregory's), Harwich, UK. -
Fossil Aipichthys Fish in Matrix
Cretaceous Period, 145-66 million years B.P.Estimate: £30 - 40 (+bp*)
Opening Bid: £5
Aipichthys velifer on a rectangular matrix with an identification sticker. 222 grams, 91 mm
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. -
Knightia Fossil Fish Plate Group
Eocene Period, circa 58-36 million years B.P.Estimate: £40 - 60 (+bp*)
Opening Bid: £5
Comprising three circular plates, each with a Knightia alta fish, and a fourth plate with small remains of one. 165 grams total, 71-80 mm
From Wyoming, USA. From a Lincolnshire, UK, collection.
In southwest Wyoming (and parts of Colorado and Utah), in the Green River Formation, are found some of the world's most outstanding specimens of fossil fish. The Green River system was composed of three lakes: Lake Uinta, Lake Gosiute and Fossil Lake. These Eocene lakes lay in a series of intermountain basins formed by geological events that uplifted the Rocky Mountains during the early Tertiary time. The climate was much different from the desert-like climate of this area today. Both the fauna (crocodiles, alligators, boa constrictors and some subtropical fish families) and the flora (such as large palm trees) indicate a climate much like that found along the Gulf Coast today. Large amounts of ash found in the sediments indicate that volcanoes were particularly active at this time.