University of Bergen- Remove Small landforms filter Small landforms
- Remove Vegetation history filter Vegetation history
- Remove Middle age filter Middle age
- Remove Maritime environments filter Maritime environments
- Remove People and Society filter People and Society
- Remove Defense filter Defense
- Remove Place filter Place
- Remove Bedrock filter Bedrock
- Remove Late glacial filter Late glacial
- Remove Metamorphic rocks filter Metamorphic rocks
- Remove Landscape filter Landscape
Skorpo
Skorpo - Polished by glaciers and meltwater
Skånevik- moraine
In Skånevik there are marks left from the ice edge that advanced during the thousand-year cold spell (Younger Dryas) that marked the end of the Ice Age roughly 11 500 years ago. The glacier first proceeded out into Åkra Fjordand and around Vannes and thereafter sent an arm in toward Skånevik. Here, the glacier lay down an end moraine up against the mountainside.
The village of Etne
Much of the sand and gravel that the town of Etne is built on was laid down at the end of the Ice Age and is evidence of melting glaciers and roaring meltwater rivers. The uncompacted material in the big terraces leave their unmistakeable mark on the wide elongated valleys.
Tælavåg
Tælavåg has a significant place in the history of the German occupation in WWII. The small community by the sea, where for centuries people had made a living from farming and fishing in harmony with the natural resources, in 1942 became the victim of German reprisals without their equal in Norwegian war history. The collection of war histories in Tælavåg provides us with a close-up of the dramatic events.
Valldalen
Valldalen or Valdalen, the name that the locals used in past times, had been a permanent settlement for a long time, and later the biggest mountain-farm valley in western Norway. Since that time there have been many changes: Most of the fields are no longer in use. Bjørkeskogen, a birch forest that had grown in the valley for thousands of years, took more and more over. And in the valley bottom, the Valldals dam now keeps the artificially large Valldalsvatnet Lake in place.
Vinnesleira
Bays that are shallow far out into the sea, with fine sand and clay, are rare in Hordaland. Where they are found, the reason is usually that the edge of the glacier made smaller advances or stopovers when it calved back at the end of the last Ice Age. This is what happened at Vinnesleira.
