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The old guesthouse location in Brattholmen on the east side of Litlesotra, was probably established in the first half of the 1700s. A list from 1748 mentions that the place “for some years has been inhabited by an Enrolled Sailor by the name of Peder Michelsen”. As was the case for most other military hosts, he was exempt from paying income tax.
The gneiss landscape west and north of Bergen viewed in profile can remind us of a saw blade of the kind that has long, slanted sides that get broken off shorter transverse sides. It has taken several hundred million years to file this saw blade, an enduring interplay between various geological processes.
Up to 1842 it was necessary to have a royal letter of privilege in order to carry out trade. According to the law only city dwellers were allowed to obtain such a privilege, and in Hordaland it was thus the citizens of Bergen who owned and ran the trading centres. In 1842, following a liberalisation of the trading legislation, the privilege arrangement was abandoned and anyone could apply to the municipal council for permission to carry out trading activity. Landøy is one of the places that were established in this period.
Hernar is a small group of islands northwest of Seløy, an old outlying harbour on the western route. This is where ships were lying in wait for favourable weather before heading out west, and this is where the ships from the western Isles came in. Hjeltefjorden is proof of this. The fjord is named after the people from Hjaltland (Shetland).
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?