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Urangsvågen-Rubbestadneset

Urangsvågen-Rubbestadneset

07.12.2018 - 14:29

In 1868 the first stone workers came to Rubbestadneset to take out the granite for the Skoltegrunns Pier, predecessor of the Skoltegrunns wharf in Bergen. Later granite was also taken out from the area, around Innværs Fjord and UransvågenN. The activity probably peaked around 1900, with over 40 men at work. 15 years later, it was finished.

Section from a sea map from the Danish Sea Map Archive from 1798, drawn by Poul Løvernørn.

Fitjarøyane

18.06.2018 - 20:30

If we study the group of islands south of Selbjørns Fjord from the air or on a sea map, we will notice that many of the islands are elongated and lie systematically in rows. The islands are divided by long sounds, for example Trollosen, Nuleia and Hjelmosen, which are oriented in a south-southeast to north-northwesterly direction.

Skrivargarden in “”Kåravikjo”.

Kåravika

19.06.2018 - 16:32

Stordfjella mountain towards the south.

Kattnakken–Stovegolvet

19.06.2018 - 16:33

The highest mountainous area on Stord, including Kattnakken, Midtfjellet and Stovegolvet, has more in common with the mountainous terrain on the mainland than in the low coastal landscape of Sunnhordland. The volcanic bedrock together with the erosive powers of nature has resulted in a unique plateau landscape.

Coat of arms, Orning

Orninggård

19.06.2018 - 16:35

The main building at Huglo, Stord

Sørhuglo

26.06.2018 - 09:59

The tax collector’s farm at Sørhuglo is one of the many farms for state employees in Hordaland. According to history, “Futastovo” was built by the tax collector Gram in the second half of the 17th century. In 1943 the building was moved to Sunnhordland Folk Museum.

Einstapevoll

Einstapevoll- the farm

19.06.2018 - 17:10

Einstapevoll (from einstape: “bregne” (fern)) lies on the west side of the Tittelsnes peninsula. Up to 1831 the farm was a vicarage belonging to Stord parish. The priests had leasing rights. Land rent and other fees from the farm was part of their salaries.

Espevik

Espevik

03.01.2019 - 15:26

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.

The walls in the boathouse in Hopssundet are built of red granite from Reksteren.

Hopssundet

01.05.2018 - 16:39

The old vicarage at Oppheim.

Oppheim

19.06.2018 - 18:00

In the slope above Oppheim church lies the old vicarage at OPPHEIM. If you stroll up the road from the church you will arrive in a farmyard marked by traces of building style and living traditions from the Middle Ages.

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