University of Bergen- Remove Small landforms filter Small landforms
- Remove Aristocracy and civil servants filter Aristocracy and civil servants
- Remove Landscape filter Landscape
- Remove Late glacial filter Late glacial
- Remove Vaksdal filter Vaksdal
- Remove Maritime environments filter Maritime environments
- Remove People and Society filter People and Society
- Remove Askøy filter Askøy
- Remove Os, frå 2020 del av nye Bjørnafjorden kommune filter Os, frå 2020 del av nye Bjørnafjorden kommune
- Remove Civil servant dwellings and manors filter Civil servant dwellings and manors
- Remove Chieftains and royal lines filter Chieftains and royal lines
- Remove Bømlo filter Bømlo
- Remove Etne filter Etne
- Remove Settlements, Villages, Towns filter Settlements, Villages, Towns
Støle
High above the sea and the beach flats, on one of the wide terraces shaped by the sea and the ice, lies the farm Støle (Stødle). The Old Norse name of Studla is derived from studill “support, shelf”. As far back as Viking times Støle has been a chieftain’s farm, a good farm on the plains formed by the moraine masses.
Eksingedalen- landscape
Eksingedalen alternates between wide, flat flood plains with good farmland, and narrow passages with waterfalls where the roads cling to the mountainsides. The alternations in the landscape are a result of the sculpturing work by glaciers over several ice ages, and the deposition of the glacial river deposits when the last glacier finally melted back.
Herdla – glacial deposits
The shift in the landscape is striking between the barren craggy moors north on Askøy and the green fields of Herdla, which has the county's biggest farm. The majority of Herdla, such as the island appears today, is a gift from the glacier: The glacier that advanced here over 12,000 years ago stopped at the northern tip of Askøy and took its time building up the moraine on Herdla. Since then, Herdla has been under continual transformation. The re-organisation of the loose sediment deposits continues today.
