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.

Engevik

Halfway into the Sævareidfjord lies the officer’s farm Engevik. In the beginning of the 1700s the farm was in part estate of the crown and owned by farmers. In 1724 lieutenant-colonel Christian Wilhelm Segelcke settled there and erected a new farm around an imposing main building a little way north of the old farm site.

Ferstad

Ferstad is well worth a visit. The farm lies on a little hillock south of Lekven: a beautiful official residence from the 1700s.

Frekhaug

Frekhaug has been a large farm with well-off owners through many generations. The main house, a two storey building with a hipped roof, must have been erected about 1780.

Gjønavatnet and Kikedalen

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.

Os rectory

Osøyro

The coastal settlement of Os begins to take form in the middle of the 1800s. This is when craftsmen and traders begin to settle at the river delta.

Ulven camp