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Fossen Bratte
The steep drop by Fossen cliff has been the biggest challenge for those who wished to make a road over Kvamskogen through the years. Leave the car by the monument on the old road and take a walk down to the bend by the waterfall that Bergen-folk call "The bridal veil". Why is there a waterfall just here?
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.
Etnedeltaet
During the latter half of the 1900s the big natural river deltas on Westland disappeared. Until the 1980s there was still a small, but significant remnant of the original river delta from the Etneelva river, but today most of this, too, is industrial land.
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.
Låtefossen
Låtefossen waterfall, or more correctly, waterfalls, plunge 165 metres down the mountainside, 51 of them in free fall - to the enchantment of the many tourists along the highway below. The spectacular view is mainly seen from the stage of the Storelvi river in the valley below the waterfall.
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.
