University of Bergen- Remove Small landforms filter Small landforms
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Fluøyane
The richest seabird localities in Bjørna Fjord are FLUØYANE, a group of small and medium-sized islets just east of the entrance to Våge. Here, we see many different nesting birds, but there is the danger that overgrowth will become an obstacle for nesting here in the future. On one of the islands, the environmental protection authority has promised to step in and help the birds.
Nedrevåge
Vågsbygdo was severely hit by landslides and rock falls in the decades around 1700, in addition, the rivers transported masses of loose sediment, both large stones and gravel. A lot of what slid down from the Vågsliene (slopes at Våg) collected in Neravåge. It was so bad that the damage “never again can be remedied or restored”, it was said in 1670.
Årbakka- The prehistoric site
The prehistoric site at Årbakkasanden with menhirs and burial mounds has been visited, described and illustrated by many learned researchers through the last 350 years. All the same, we still know very little of this unique cultural monument.
Kalvanes
On the 17th of January, 1993, the area between the towns of Odda and Eitrheimsneset were struck by a giant avalanche. One person was killed, and there was a lot of material damage.
Tyssedal
Today Tyssedal appears like a classical industrial community, a picture of modern Norway from the turn of the former century until today. A/S Tyssefaldene was established in 1906, and on 1 May 1908 Tyssedal power station was put into operation. The work on the first stage of the facility was completed in a short time, with a work force of 500 men. They built water tunnels, regulation reservoirs, power station, penstocks, harbour, cableways, office buildings, houses and 6 km of power lines in the wild mountains above Odda to provide the new melting plant with power.
