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Gjerde church at Etne

Gjerde church

18.06.2018 - 20:24

Grindheim church

Grindheim church

18.06.2018 - 20:24

The first church at Grindheim was a stave church with a free-standing steeple. The church was first mentioned in 1326, but was probably built long before this time.

Rock inscriptions at Helgaberget.

Helgaberget

18.12.2018 - 21:26

Helgaberget – the holy hill – is a little rocky crag which thrusts itself a few metres above the terraced surface of Støle. The surface of the rock is strewn with figures inscribed in the rock and it was, as far as one can judge, a cult centre in the Bronze Ages. The name could indicate that the tradition of holiness can have lasted for almost 3,000 years.

Støle church

Støle church

18.06.2018 - 20:27

The stone church at Støle may have been built around 1160 probably as a private chapel for the mighty Stødle clan. It is likely that it was Erling Skakke, the king’s representative and father of king Magnus Erlingsson, who built the church.

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.

Strandflat and scree by land

Landa

19.06.2018 - 16:06

Liarbø, Fitjar

Liarbø

19.06.2018 - 16:07

Rimsvarden

Rimsvarden

19.06.2018 - 16:08

Rimsvarden lies high and unencumbered, an enormous stone mound on the highest top with a wide view of the Fitjar rural community. With its 30 meters across and almost 4 meters high, this is one of the largest prehistoric burial relics existing in Hordaland.

Smedholmen, Fitjar

Smedholmen

30.03.2018 - 20:10

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.

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