Bergesfjellet

Brandasund

On Gisøya Island, on the west side of Brandasund Sound, there is a very privileged trading post and traveller's Inn from the 1600s, with the North Sea as its nearest neighbour. In 1991 a road was built over Bømlo out to these islands, but for thousands of years the sheltered harbour here was a main stopping place along the outer coast. During the great herring period of the 1700s and 1800s, Brandasund was a centre for the herring fisheries on the Sørafeltet fishing grounds. Today, the area belongs to the municipality of Bømlo.

Espevær- the Trading Post

In the sea west of Bømlo lies Espevær, half an hour’s rowing trip across the sound from Vespestadvågen. This is a well-run and well-maintained local community, established on the back of the rich herring fisheries in the 1850s. It is fishermen, skippers and the tradesmen who have made their mark on the culture in Espevær, with their contacts to the south towards Haugesund and across the North Sea to the British Isles.

Finnås

At Flintaneset by Finnåsvika, in the centre of the municipality, we find the most beautiful and best preserved igneous rocks in western Norway. We must go to Hawaii or Island to find as fine structures as at Bømlo.

Hiskjo

Manger

Mangerite is a rock type that was first made famous in a treatise by the Bergen geologist Carl Fredrik Kolderup in 1903. The rock type got its name from the place where it was found, and has made the Mangerud name well known around the world, at least among geologists.

Mosterhamn

Mosterhamn is one of the old privileged trading posts situated centrally in the shipping lane, whether the ships sailed on Langenuten, Nyeleia through Fitjar or into the Hardanger Fjord. From prehistoric times Bømlo and Moster were the first landing places when arriving from the west; a landscape with good harbours.

Siggjo

Siggjo is a cone-shaped, volcano-like mountaintop in the part of Hordaland where one finds the best preserved volcanic rocks. The rock types originate from one or several volcanoes that spewed out glowing lava and ash. But, the shape of the mountain, as it appears today, formed later and by completely different forces.

Toska

The peat bogs on Toska have been mined for peat since 1946, when the island got electricity. In this treeless coastal landscape, peat was the most important source of energy, and this took quite a toll on the bogs.

Urangsvågen-Rubbestadneset

In 1868 the first stone workers came to Rubbestadneset to take out the granite for the Skoltegrunns Pier, predecessor of the Skoltegrunns wharf in Bergen. Later granite was also taken out from the area, around Innværs Fjord and UransvågenN. The activity probably peaked around 1900, with over 40 men at work. 15 years later, it was finished.