Chronostratigraphische Untersuchungen (14C-Alter) an den Windablagerungen der "Towans" in der südwestenglischen Grafschaft Cornwall)

Helmut Siebertz
The cliffs along the north-western coast of Cornwall are interrupted by low-lying stretches of coast line (estuaries, bays), which supply blown sand for the formation of the coastal dunes (Fig. 1). The aeolian sand deposits vary considerably in age. The young Holocene dunes are still active, whereas the older (mainly) Pleistocene sediments are located beneath the younger dunes or in horizontal connection to them; they As these older dune sands are divided up by several...