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izvor podataka: crosbi

Vulkani na jadranskim otocima? = Volcanoes on the Adriatic Islands? (CROSBI ID 171)

Autorska knjiga | katalog

Crnjaković, Marta Volcanoes on the Adriatic Islands? / Vulkani na jadranskim otocima? = Volcanoes on the Adriatic Islands?. Zagreb: Hrvatski prirodoslovni muzej, 1998

Podaci o odgovornosti

Crnjaković, Marta

hrvatski

Vulkani na jadranskim otocima? = Volcanoes on the Adriatic Islands?

In Adriatic first magma found its way to the surface along deep fissures when the first continent of Panagea began to split up. Some of the magma was captured under the ground and as it cooled turned into veins and various kinds of sub-volcanic rock. The sediments (about 5 km high) during the Mesozoic covered the volcanoes During the formation of the Alps, the layered rocks folded, faulted and were eroded, and the magmatic and volcanic rocks of Croatia eventually appear at the surface. In Pleistocene a great part of the bottom of today's Adriartic sea was tumed into land. The islands, including Jabuka and brusnik, were higher, or even becoming a part of the mainland, which contributed to their being eroded. In this period relatively soft volcanic rocks of Vis near Komiža being eroded.

vulkani; građa Zemlje; vulkanske stijene; jadranski otoci - Jabuka; Brusnik; Vis; Hrvatska

nije evidentirano

engleski

Volcanoes on the Adriatic Islands?

In Adriatic first magma found its way to the surface along deep fissures when the first continent of Panagea began to split up. Some of the magma was captured under the ground and as it cooled turned into veins and various kinds of sub-volcanic rock. The sediments (about 5 km high) during the Mesozoic covered the volcanoes During the formation of the Alps, the layered rocks folded, faulted and were eroded, and the magmatic and volcanic rocks of Croatia eventually appear at the surface. In Pleistocene a great part of the bottom of today's Adriartic sea was tumed into land. The islands, including Jabuka and brusnik, were higher, or even becoming a part of the mainland, which contributed to their being eroded. In this period relatively soft volcanic rocks of Vis near Komiža being eroded.

volcanoes; Earth stucture; volcanic rocks; Adriatic islands - Jabuka; Brusnik; Vis; Croatia

nije evidentirano

nije evidentirano

nije evidentirano

nije evidentirano

nije evidentirano

nije evidentirano

Podaci o izdanju

Zagreb: Hrvatski prirodoslovni muzej

1998.

953-6645-02-5

39

objavljeno

Povezanost rada

Geologija, Biologija