Quartärmorphologische Untersuchungen an den Küsten der M. Poro—Halbinsel, Westkalabrien (Beiträge zur regionalen Küstenmorphologie des Mittelmeerraumes III)

Dieter Kelletat
The M. Poro-Peninsula between the gulfs of S. Eufemia and Gioia is mostly granitic. A central 600 m-peneplain is separated from mainland Italy by a basin with pliocene sediments. On the northern and western coastal slopes more or less consolidated miocene sandstone covers the granite. The SW-coast between Nicotera and Capo Vaticano is a denudatively and marin altered early quaternary fault. The exposed northwest is marked by stacks in front of granite cliffs up to...