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Skalski, A. In: Rook, L. Paleodays Volume dei riassunti e guida all'escursione, page Adorni, F. Le septarie dell'Appennino Parmense. Rivista Mineralogica Italiana, In: Bianchi V. Quaderni del Museo di Storia Naturale di Ferrara, 1, Palaios, 21, Minerva Edizioni, Bologna, pp.

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Issel A. Donath Editore, Genova, Vol. Geologia e mineralogia in Liguria. II Edizione. Jervis, G.

Roberto De Nicola Editore, Roma, pp. Jervis G. Reale Stamperia, Palermo, Accademia delle Scienze dell'Istituto di Bologna, serie 4, 10 , Giardina G. Paleocronache, , A paleoclimatic indicator?

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Rivista Italiana di Paleontologia e Stratigrafia, , Stoppani A. Sammartino, F. Nota preliminare. Quaderni del Museo di Storia Naturale di Livorno, 26, Palaios, 21, 2, Giornate di Paleontologia, Perugia maggio , Volume dei Riassunti, Palaeogeography, Palaeoclimatology, Palaeoecology, , , Dill, H. Diagenetic and epigenetic alteration of Cretaceous to Paleogene organic-rich sedimentary successions in northwestern Jordan, typical of the western margin of the Arabian Plate.

GeoArabia, 14 2 , Soriano, C. First record of the family Belidae Insecta, Coleoptera in amber.

Project Amber

New genus and species from the uppermost Albian amber of France. Geodiversitas, 31 1 , Dreimanis A. Bryant, D. A recently discovered amber source near Totolapa, Chiapas, Mexico. American Antiquity, Myanmar Szwedo, J. Cruickshank, R. Geology of an amber locality in the Hukawng Valley, northern Myanmar. Journal of Asian Earth Sciences, 21 5 , New Zealand. Seyfullah, L. Ferguson, D. Craw, D. Flamini A. Periodico di mineralogia — Roma, pp.

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Kartashov data; Krul, H. Pekin, A. Russian Journal of General Chemistry, 81, 6, Penalver, E. A new rich amber outcrop with palaeobiological inclusions in the Lower Cretaceous of Spain. Cretaceous Research, 28 5 , Najarro, M. Acta Geologica Sinica, 84 4 , Alicante Co. Stalder, H. Syria Williamson, Book of Amber. Hall, T. Edward Stanford London , pp. Alabama Greene Co. Dempsky, M. Arkansas Hot Spring Co. California Ventura Co. Colorado Teller Co. It occurs in different colours, and is widely used for making jewellery and other ornaments.

Although not mineralized , amber is sometimes considered as a gemstone. Most of the world's amber is in the range of 30—90 million years old. Semi-fossilized resin or sub-fossil amber is called copal. Baltic amber was called 'Freya's tears' by the Norse and the 'tears of the Heliades' by the ancient Greeks. Amber consists of several resinous bodies that can mostly dissolve in alcohol , ether and chloroform , associated with a bituminous substance that does not dissolve. Amber is formed from resin coming out of certain trees.

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It is not tree sap or gum. The resin soon becomes sticky, and later fossilises as amber. The amber can look different depending on its origin, and its later geological history. To end up as amber, the starting resin must resist decay. Many trees produce resin, but usually it is broken down by physical and biological process. Exposure to weather tends to disintegrate resin, assisted by microorganisms such as bacteria and fungi. For resin to survive long enough to become amber, it must resist such forces, or be produced under conditions that exclude them.

Baltic amber historically called Prussian amber is found as irregular nodules in a marine sand, known as blue earth, in the Lower Oligocene strata of Sambia in Kaliningrad Oblast , where it is now systematically mined. Agathis amber comes from the conifer Agathis , a tree that used to grow over a much wider area. LoveIsland pic. Meet the Love Island series 5 contestant linked to former Islanders.

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