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Bergsdalen
The mountains of western Norway are lovely to wander in. In Cambro-Silurian time it was the mountain itself that wandered. The mountain, or more correctly the bedrock, first moved eastward, then back a bit westward again. All this rocking back and forth in the mountains ended about 400 million years ago.
Blomvågen
"One of the big scientific sensations", was the title in the Bergens Times newspaper on the 22nd of November, 1941. It was the geologist Isal Undås who had been interviewed by the newspaper. He thought that he had discovered a 120 000 year old whale bone, remains of life from before the last Ice Age.
Bondhusdalen
The Bondhus area in Maruanger has been a magnet for tourists ever since the stream of tourists to Norway's west coast began in the middle of the 1800s. The magnificent landscape with the "ice trail" up to Bondhusvatnet Lake, the ice falls from Bondhusbreen glacier and Keisarstigen trail up to Folgefonna are still popular tourist attractions.
Bordalsgjelet
Deep down between the stone polished phyllite bedrock in Bordalsgjelet canyon, there is a cascading river. In close cooperation with hard polishing stones, the water has carved into the bedrock for thousands of years - and is still doing so today.
Buardalen Valley
Buarbreen glacier was one of the first destinations during the period of increasing tourism in Odda in the 1800s. Foreigners came by the thousands, mostly Englishmen and Germans, to the magnificent landscape in front of the glacier. Back at the hotel in Odda they could enjoy drinks containing ice from the glacier.
Byrkjehaugen
On the farm Bø, close to the highway between Bulken and Voss lies Byrkjehaugen, one of the largest burial mounds in West Norway. Originally it was around 50m across and 5m high, but following the excavation in 1908 and chipping off by both railway and road construction, the cross-section has shrunk to 37m and the height to 4m. All the same, it is an impressive burial monument for the passing traveller to see.
Dyrdal
If you journey along Austfjorden, you at the same time turn the pages of time back through Ice Age history. The landforms show how the landscape has developed gradually as the glaciers have grown - and melted again - in several episodes: from small cirques, we see innermost at Dyrdal, to larger fjords, like at Mas fjord further out.