Årbakka- The trading center

Trellevik

Spildepollen

The oceanic crust of the North Sea was subjected to a lot of stretching both in Permian and Triassic times, and later in the Jurassic. This stretching resulted in the North Sea collapsing in and also to large faults forming west of Hordaland and on the mainland. Austefjorden in Sund follows one of these faults.

Neshamn

Neshamn must be an ancient place for meeting and spending the night for travellers. The place blossomed in connection with the times of economic expansion in the 1500s, which to a large extent was linked to the Scottish trade at this time. Neshamn was a loading place for Scottish ships for two hundred years, up to the middle of the 1700s.

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.

Kræmmerholmen

Kræmmerholmen is one of the old privileged trading posts. From the 1600s all trading in West Norway took place in Bergen, and the farmers were obliged to travel into town in order to sell their produce and buy what they needed. In Bergen City Privilege of 1702 the merchants in the city were allowed to establish “Trading posts in the countryside”. The owner had to have residency in Bergen and the trading post was to be run by an assistant. In this way the city retained financial control of those living in the districts, and not least with buying and selling of fish.

Klinkholmen

Kubbervik, or Vikjo as it was known colloquially, must have been established as a trading post under the farm of Håland some time around 1600. The reason for this was probably the thriving trade on Scotland. Every year ships from the islands in the west came to buy lumber in Bårsund. Vikjo was the harbour in use, as the place is ideally situated on the route through Bårsund, the sound between Reksteren and Tysnesøy.

Hovdanes

Holmengrå

Holmengrå is the only place in Hordaland where we find traces of the abrasion that is supposed to have transformed Western Norway from a Himalaya-like high mountain landscape during the earth's Paleozoic Era, to a flat lowlands terrain during the Mezosoic Era. Just 400 million years ago, large and small stones plummeted down from the high mountains. Some of these stones became incorporated into the conglomerate bedrock on Holmengrå.

Hellisøy

Hellisøy lighthouse was lit for the first time in 1855. The characteristic red cast-iron tower with two white belts is 33m high and a light height of 46m above high tide.