The coast and sea bottom of the Gulf of Arzachena were studied from the geomorphological point of view. Echographical surveys and under-water samplings were carried out at sea. Different morphologies connected both to hot-wet climates (inselberg, residual surfaces at different levels, paleosoils) and to cold climates with consequent emer­sion of the present continental shelf, are evident on the coast. On the internal shelf , the Ria of Arzachena presents typical characteristics of fluvial valleys. Various sea-levels, represented by abrasion plat­forms and beach-rocks, are referred to the Tyrrhenian and Versilian transgressions.

Il golfo di Arzachena nella Sardegna settentrionale. Ricerche di geomorfologia costiera e sottomarina

DEMURO, SANDRO;
1985-01-01

Abstract

The coast and sea bottom of the Gulf of Arzachena were studied from the geomorphological point of view. Echographical surveys and under-water samplings were carried out at sea. Different morphologies connected both to hot-wet climates (inselberg, residual surfaces at different levels, paleosoils) and to cold climates with consequent emer­sion of the present continental shelf, are evident on the coast. On the internal shelf , the Ria of Arzachena presents typical characteristics of fluvial valleys. Various sea-levels, represented by abrasion plat­forms and beach-rocks, are referred to the Tyrrhenian and Versilian transgressions.
1985
Geomorfologia costiera; geomorfologia sottomarina; superfici residuali; Beach-Rocks; Quaternario; Sardegna settentrionale
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11584/3497
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