Vinappen

Vinappen lies on a low hill to the very west on the island. Here you have an amazing panorama of the sea. Originally the area was grazing land for cattle, but this changed when the Germans occupied the island. Just before WWII there was a small bearing station, used by the Norwegian Coast Artillery in connection with exercises at sea.

Bjørsvik

The industrial settlement Bjørsvik

Romarheimsdalen

Stall

The Bergen Arcs have an unusually sharp boundary to the bedrock in the east. Geologists think that this was caused by movements in the earth's crust during the Devonian Period. Then, the Bergen Arcs on the Lindås peninsula sank a whole 10 kilometres in relation to the Precambrian basement gneisses on the east side of Fens Fjord and Aust Fjord.

Dyrdal

If you journey along Austfjorden, you at the same time turn the pages of time back through Ice Age history. The landforms show how the landscape has developed gradually as the glaciers have grown - and melted again - in several episodes: from small cirques, we see innermost at Dyrdal, to larger fjords, like at Mas fjord further out.

Matre- Bjørn West museum

Eldsfjellet

The eclogites in western Norway were formed when Precambrian basement rocks were squeezed and pressed down under great pressure deep under the Caledonian mountain chain. The process may well have triggered some of the deepest earthquakes the world has ever known. The clearest traces of this drama are found in and around Mt. Eldsfjellet, in peaceful Meland.

Håøy

Håøy lies centrally in one of the main shipping lanes going into Bergen --- with Håyøsund on the south side facing Meland, and Hagelsundet facing Lindåslandet. Names like Nordfarskista and Nordfarsskorane explain things. The strategic position was important in Viking times and it has been important in our days too. The beacon on Håøy can have been built in the establishment of the coastal administration in Håkon the Good’s time, about 950 AD. The defence structure of which we say remains on Håøy Summit held a critical position during Norwegian neutrality during the First World War. The defence structure was taken down in 1957.

Rylandvassdraget

There is a lot of trout and a large char population in Lake Rylandsvatnet. The lake was stocked with char, probably in 1907. The promoters of the project were the family Ameln, who owned eight mills in Rylandsvågen and parts of the Ryland farm.

Otterstadstølen

Otterstadstølen lies in an idyllic grassy plain surrounded by rich forest, but also with high mountains close by. The mountainsides are steep and typical of this part of the county. The same cannot be said about the forest. This spruce forest has been able to develop freely for hundreds of years. Otherwise in the county, only Voss has spruce forest.