1 lower-lying area with Holocene clay deposits
2 Pleistocene sandy outcrops (‘donken’) and Pleistocene sandy soils
3 current course of the river
4 dried-up river beds
5 unmapped area
6 Roman-period settlement
(Roymans & Derks 1994)
|
The surroundings of the temple
in Empel. It stood on a protruding sandy outcrop at ‘De Werf’. 1 lower-lying area with Holocene clay deposits 2 Pleistocene sandy outcrops (‘donken’) and Pleistocene sandy soils 3 current course of the river 4 dried-up river beds 5 unmapped area 6 Roman-period settlement (Roymans & Derks 1994) |