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Linosa seamounts

Sicily (7 Ma to Present) Etna (0.5-Present), Iblei (7-1.5), U-stica (0.75-0.13), Pantelleria (0.3-0.005), Linosa (1-0.5), Sicily Channel seamounts - Stratovolcanoes, diatremes, small plateaux, etc. formed of tholeiitic and Na-alkaline rocks (basanite, hawaiite, trachyte, peralkaline trachyte and rhyolite). [Pg.3]

The volcanoes of the Sicily Channel (Linosa and Pantelleria and a number of seamounts Miocene to present in age) are mainly located along ex-... [Pg.215]

Fig. 8.16. TAS classification diagrams of Linosa and Sicily Channel seamounts. The dashed line is the boundary between subalkaline and alkaline fields of Irvine and Baragar (1971). Data on seamounts have been recalculated on water-free basis. Fig. 8.16. TAS classification diagrams of Linosa and Sicily Channel seamounts. The dashed line is the boundary between subalkaline and alkaline fields of Irvine and Baragar (1971). Data on seamounts have been recalculated on water-free basis.
Three seamounts Linosa 1, Linosa 2 and Linosa 3) have been found north of Linosa island. Little is known about these cones and the volcanic nature of the northernmost centre (Linosa 3) is dubious. [Pg.240]

See other pages where Linosa seamounts is mentioned: [Pg.14]    [Pg.215]    [Pg.299]   
See also in sourсe #XX -- [ Pg.240 ]



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