Nordvik

Espevik

220 million years ago, glowing hot molten rock masses intruded into fractures in the earth's crust in the outer parts of Hordaland. Some of these are believed to have reached the surface and formed lava flows, which since have been eroded away by wind and weather. But, most of these flows solidified into diabase sills before they got to the surface.

Hopssundet

Nedrevåge

Vågsbygdo was severely hit by landslides and rock falls in the decades around 1700, in addition, the rivers transported masses of loose sediment, both large stones and gravel. A lot of what slid down from the Vågsliene (slopes at Våg) collected in Neravåge. It was so bad that the damage “never again can be remedied or restored”, it was said in 1670.

Ånuglo

Take a tour to Ånuglo on a warm summer's day. You can anchor up in Skipavågen and go exploring along the beach. Or, you can find giant holly trees and ivy inland on the island. If you take a trip to the small farms on the west side - one of which is still in operation - you can experience colourful flower meadows from a time most dream of, but few can still remember.

Fadnesskaret

Mølster

Nesheim

Stalheim

Stalheim is situated between Stalheimsfossen and Sivlefossen, in a community with the farms Sivle and Brekke. The most likely explanation of the name is “the farm by Stadall”, from “standa” (stand), probably with background in the steep Stalheimskleivi. The farm has for a long time been divided into several units. At Stalheim there has been a transport exchange from the Middle Ages and the farm has been a postal farm since 1647.

Teigdalen

It is not surprising that there are several folk tales connected to the large and unusual scree deposit that is found at Langeland, uppermost in Teigdalen. It is said that folk have been taken into the mountains by these stone blocks and have come back and told about how the wood nymphs live. It is also said that packs of thieves hid here in the old days, both themselves and the treasures they had stolen.