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Fedje bog
The wild rabbit is really native to Northwest Africa, but the Ancient Romans introduced them to large parts of Europe. Not to Norway, rightly enough: the population on Fedje originated from 3-4 pairs that were brought here from the Shetland Isles in 1875, making this their first residence in the country.
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.
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.
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.
Stormark
Both the climate and people have been decisive in shaping the bog landscape on Fedje - a landscape that has been evolving over several thousands of years. The peat got built up layer for layer and provided income and fuel for the people of Fedje.
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.
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.