User:Wham2001/Romeleåsen

Geology
Romeleåsen is a horst, which is a part of the crust that has been lifted up by geological processes. The surface rock is primarily primary gneiss. It is covered by a thin layer of clay soil. Where the rocks protrude through the clay layer they are generally only lightly weathered, since earlier layers of weathered rock were removed by glaciers during the Pleistocene period. The Romele ridge forms the north-eastern boundary of the Alnarp aquifer.