Byparken

It isn't true that hungry students have hunted down basking ducks in the city park Byparken in their spring fervour, as rumours may have it. But, it is not unusual to see students throw themselves over the park's wild birds, and hold on to them tight. They ring the birds. Because of this, we know quite a lot about the birds in Byparken.

Fløyfjellet

Garnes

Isdalen

The valley on the inside of the Svartediks dam, a five minutes' bus ride from Bergen centre, is often referred to by Bergen folk as Isdalen ("Ice Valley") - justifiably, since the area could have been described in textbooks for its ice-carved land forms. The glacier's polishing over ca. 40 ice ages has created a magnificient landscape. The original ice valley climbs up behind Ulriken at the end of Svartediket.

Rådalen

"...it would not be of any particular economical interest to support the planting of forest as the forest that can be cultivated will leave much to be desired in the way of growth potential." These words stem from the economist that at the end of the 1800s was sent to Stend to inspect the planned reforestation in person. The pioneer G.A.Wilson put the economist's words to shame. The spruce that was planted in Rådalen in the period 1867–1869 became a landmark. No other stand of forest in Scandinavia can boast more trees per unit area.

Sandviksfjellet

On Sandviksfjellet there are old boulders that have been made into mountains. The stones have been stretched out or squeezed together between huge slabs of rock, during slow, but powerfulprocesses of transport. This conglomerate shows, in quite a special way, the enormous powers that were active during the collision between Norway and Greenland over 400 million years ago.

Skogsøyna

There isn't much forest on Skogsøyna today, but that there is, has been planted. There is not much wildlife, either. But, quite a lot of birds pass by Skogsøyna during migration time. Ther is no other place along the coast where you can better observe the seabird migrations.

Stend station

Toftestallen

The large coastal waves that crash down on the islands west in the sea gather their energy from storms and winds all the way out in the North Atlantic Ocean. The most common place of origin is nonetheless the North Sea. When these waves break over the skerries and islets along the shore, or on the rocky outermost islands, their energy is released. This takes the form of turbulence in the water and sea spray up on land. Can the enormous energy contained in the waves be exploited?

Toftøyna