Kattnakken–Stovegolvet

The highest mountainous area on Stord, including Kattnakken, Midtfjellet and Stovegolvet, has more in common with the mountainous terrain on the mainland than in the low coastal landscape of Sunnhordland. The volcanic bedrock together with the erosive powers of nature has resulted in a unique plateau landscape.

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.

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.

Hamlagrø

The type of underlying rock can be decisive for how many different types of plants are found in an area. In the area around Hamlagrø-lake the diversity is especially obvious. The geological conditions change much here within a short distance.

Aksnesholmane

There are especially many seabirds inwards along the fjords of western Norway. There are not many islets, either, so if the birds want to nest, it is not always easy to find good sites. At Aksnesholmane there is an impressive colony of gulls, and the locality has been protected since 1923.

Tokagjelet

There is a sharp transition between the wide valley at Kvamskogen and the narrow Tokagjelet. The transition is no less dramatic when we come out of the crooked tunnels far down in the canyon, and the open Steinsdalen valley spreads out before us. The canyon both separates and joins together different epochs in western Norway's history.

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.

Frette

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.

Herdla- Migrating birds

Bergen folk landed on it, long and well. The Germans took it over, during the Second World War. The birds had been doing it for several thousands of years: HERDLA is the main airport for migrating birds during their autumn migrations.