Physical and Chemical Properties of Volcanic Glass Shards from Pozzuolana Ash, Thera Island, and from Upper and Lower Ash Layers in Eastern Mediterranean Deep Sea Sediments

Two volcanic ash layers have been correlated in deep sea piston cores from the eastern Mediterranean 1,2 . The lower ash layer ( n = 1.521) occurs between late Würm carbonate sediment and originated in an eruption more than 25,000 years ago. The upper ash layer ( n = 1.509) occurs in postglacial car...

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Veröffentlicht in:	Nature (London) 1967-01, Vol.213 (5076), p.582-584
Hauptverfasser:	NINKOVICH, D., HEEZEN, B. C.
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Sprache:	eng
Schlagworte:	Humanities and Social Sciences letter multidisciplinary Science
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description	Two volcanic ash layers have been correlated in deep sea piston cores from the eastern Mediterranean 1,2 . The lower ash layer ( n = 1.521) occurs between late Würm carbonate sediment and originated in an eruption more than 25,000 years ago. The upper ash layer ( n = 1.509) occurs in postglacial carbonate sediment less than 5,000 yr old. Patterns of distribution indicate that both beds of volcanic ash originated in eruptions of Santorini (Aegean Sea).
doi_str_mv	10.1038/213582a0
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title	Physical and Chemical Properties of Volcanic Glass Shards from Pozzuolana Ash, Thera Island, and from Upper and Lower Ash Layers in Eastern Mediterranean Deep Sea Sediments
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