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Domkirken

Domkirken

12.06.2018 - 19:08

Fantoft stave church

Fantoft Stave Church

12.06.2018 - 19:09

Korskirken

Korskirken

12.06.2018 - 19:10

The church at Kyrkjebyrkjeland was pulled down in 1878.

Kyrkjebyrkjeland

12.06.2018 - 17:19

The interior of Mariakirken, Bergen

Mariakirken

12.06.2018 - 19:11

Apart from the king’s estate at Holmen, Håkonshallen and the lower floors of the Rosenkrantz tower, the three parish churches in the centre of Bergen are what have been preserved from medieval Bergen: Mariakirken, Korskirken and Olavskirken (the cathedral). The Romanesque base of the tower from Nonneseter monastery church on the spit between the two Lundegård lakes can still be seen in the landscape, while the other medieval buildings now lie in ruins: the town’s oldest town hall and wine cellar at Nikolaikirkealmenning, Lavranskirken and Maria Gildeskåle between Mariakirken and Bryggens Museum and the Katarina hospital on the north side of Dreggsalmenningen.

Curvy scours in the bedrock (

Golta- Gneiss

16.06.2018 - 17:33

Over thousands of years, autumn storms and strong land-driving winds have cleaned the bare rocks of Golta. The waves can beat far in over land and make it dangerous to walk along the shoreline. When the storms have calmed, the results of their work comes into view.

St. Ludvig.

Tyssøy

16.06.2018 - 17:36

B.E.Bendixen, who has written about “The Churches in Søndre Bergenhus Amt”, believed even around 1900 that there was evidence at Tyssøy of the church or the chapel of the Holy Ludvig (Louis). Two large stone blocks had lain in the western wall of the church’s nave, and this wall showed a length of 16 meters in the terrain.

Hjelmevågen, Øygarden

Hjelmo

16.06.2018 - 18:29

On the farm Hjelmo, furthest north in Øygarden, in the innermost part of a long bay, there is a fine boatshed collection with a church beside it. From times immemorial this has probably been the fish-shed location for these farm units and this was also the landing place for the churchgoers.

Toftestallen

Toftestallen

18.03.2018 - 08:09

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?

This little mountain in the picture sticks up because the layers are tilted on their sides.

Toftøyna

27.03.2019 - 15:07

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