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This is what the northernmost part of the fishing village might have looked like in Viking times

Hjartøy

19.05.2018 - 19:53

The mill in Kvernapollen

Kvernapollen

16.06.2018 - 18:29

When the workers came to Kollsnes to start on the work with the landing for the gas terminal from the Troll field in the North Sea, they found the ruins of an old farm mill at Kvernapollen.

Boathouses in Breiviksunde

Breiviksundet

24.06.2018 - 15:33

Goltasund bridge and Goltasundet

Goltasundet

16.06.2018 - 17:34

For generations the land-seine was the most important tool for catching herring and mackerel, and therefore a suitable casting bay was worth its weight in gold. Goltasundet (the Golta sound) on Golta was such a place. Here the herring often drifted in and fantastic casts might be made here.

Archaeological fins from the sites at Risøya.

Risøya

13.03.2018 - 21:08

The Salting shed at Trælevika.

Trellevik

16.06.2018 - 17:35

St. Ludvig.

Tyssøy

16.06.2018 - 17:36

B.E.Bendixen, who has written about “The Churches in Søndre Bergenhus Amt”, believed even around 1900 that there was evidence at Tyssøy of the church or the chapel of the Holy Ludvig (Louis). Two large stone blocks had lain in the western wall of the church’s nave, and this wall showed a length of 16 meters in the terrain.

Toftestallen

Toftestallen

18.03.2018 - 08:09

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?

This little mountain in the picture sticks up because the layers are tilted on their sides.

Toftøyna

27.03.2019 - 15:07

Toftøyna

Turøyvegen

16.06.2018 - 18:30

The earthquake was caused by movements along fault zones in the bedrock where the blocks of rock chafed against each other. In Devonian time, there were many big earthquakes that caused Hordaland to be broken up along fault zones. Some of these faults are visible along road cuts between Tofteøyna and Turøyna islands. Along the Hordaland coast, earthquakes still occur sometimes, though the quakes tend to be weaker.

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