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The combination building at Nordvik.

Nordvik

16.06.2018 - 17:27

Eclogite bedrock at Ådnefjellet.

Eldsfjellet

13.12.2018 - 09:04

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.

Drawing of runic letters engraved in a carving knife from Fløksand.

Fløksand

19.05.2018 - 20:02

Husebø

Husebø

17.06.2018 - 16:39

When the Corncrake returned to Nordhordland, it came as no surprise that Husebø was the place it chose. Here, remnants of the old cultural landscape are still in good condition. And the Corncrake is not alone in appreciating this.

Toward Støle and Sørheim, 1920.

The village of Etne

18.12.2018 - 20:39

Much of the sand and gravel that the town of Etne is built on was laid down at the end of the Ice Age and is evidence of melting glaciers and roaring meltwater rivers. The uncompacted material in the big terraces leave their unmistakeable mark on the wide elongated valleys.

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.

Stordalen

Stordalen

14.02.2019 - 14:39

When the Etne water system was protected in 1994, preservation of the cultural landscape in Stordalen Valley was a a main objective. This is a valley with an exceptional abundance of Different types of plants and animals. In the grey alder forest in Stordalen there are more bird species than in most other places, in fact, denser than one tends to find in a tropical rainforest.

Bømoen toward the north.

Bømoen

12.01.2019 - 16:32

Byrkjehaugen, Voss

Byrkjehaugen

19.06.2018 - 17:50

On the farm Bø, close to the highway between Bulken and Voss lies Byrkjehaugen, one of the largest burial mounds in West Norway. Originally it was around 50m across and 5m high, but following the excavation in 1908 and chipping off by both railway and road construction, the cross-section has shrunk to 37m and the height to 4m. All the same, it is an impressive burial monument for the passing traveller to see.

From Hamlagrøhornet one sees a division between the fertile phyllite and the naked Precambrian basement rock types in the landscape

Hamlagrø

13.01.2019 - 16:38

The type of underlying rock can be decisive for how many different types of plants are found in an area. In the area around Hamlagrø-lake the diversity is especially obvious. The geological conditions change much here within a short distance.

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