Burmesisk rav - bladvormet - 25 mm - Rav

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09
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Estimat  € 180 - € 210
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Burmese rav med bladindlæg fra Hukawng-dalen, Myanmar, dateret Cenoman-stadiet i den øvre Kridttid, cirka 100 millioner år siden; prøven poleret, naturlig, vægt 3,00 g, ægthed Original/official.

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Burmese Amber - Leaf

Cretaceous Period : Cenomanian Stage (100.5 - 93.9 million years ago )
Origin : Hukawng Valley - Myanmar

Amber size : 32.4x22.9x6.6 mm
Inclusion size : 25 mm
Weight : 3.00 g

Burmese amber, also known as burmite comes mainly from the Hukawng Valley in northern Myanmar. It dates back to nearly 100 million years, the early Cenomanian stage of the late Cretaceous period. During that period angiosperm plants started to replace the gymnosperms. This is one of the most important periods in the evolution of life on earth and the formation of modern flora and fauna

Pictures are taken with special magnification equipment to show a better view of the inclusions. Please check carefully the size of the amber and inclusion before bidding !

Burmese Amber - Leaf

Cretaceous Period : Cenomanian Stage (100.5 - 93.9 million years ago )
Origin : Hukawng Valley - Myanmar

Amber size : 32.4x22.9x6.6 mm
Inclusion size : 25 mm
Weight : 3.00 g

Burmese amber, also known as burmite comes mainly from the Hukawng Valley in northern Myanmar. It dates back to nearly 100 million years, the early Cenomanian stage of the late Cretaceous period. During that period angiosperm plants started to replace the gymnosperms. This is one of the most important periods in the evolution of life on earth and the formation of modern flora and fauna

Pictures are taken with special magnification equipment to show a better view of the inclusions. Please check carefully the size of the amber and inclusion before bidding !

Detaljer

Eksemplar
Burmese Amber - Leaf - 25 mm
Oprindelsesland
Myanmar
Geologisk periode
Kridttiden, Øvre (100,5 - 66 millioner år)
Stand
Naturlige
Behandling
Poleret
Vægt
3 g
Autenticitet
Original/officiel
Solgt af
LuxembourgBekræftet
81
Genstande solgt
100%
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