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Gildrehola

Gildrehola

12.03.2018

Skorpo (Svein Nord)

Skorpo

29.03.2018

Skorpo - Polished by glaciers and meltwater

Main mine shaft in Valaheigruva mine.

Varaldsøy- mining

19.06.2018

There is still a lot of ore in the abandoned mines on Varaldsøy Island. If today's prices and availability of ore continue, it is doubtful whether the mines will resume operation. But, the pyrite is there, if the market should return. On Varaldsøy Island one finds at least nine mines and prospect pits, that for the most part date back to the latter part of the 1800s.

At lake Gaupåsvatnet.

Gaupås

19.05.2018

Kalandsvika Bay in the eastern part of Kalandsvatnet

Kalandsvika

12.06.2018

There is little to say about the opportunity for surveying from the bird observation tower in Kalandsvika: 155 different bird species have been sighted in the Kalands water shed. Take your binoculars and visit the tower in late spring - early summer or during the winter half of the year. If you are lucky, you might get to see a rare bird species.

Reppadalen (Svein Nord)

Reppadalen

31.03.2018

The unusual bog landscape, with enormous peat deposits surrounded by steep mountainsides, makes Reppadalen in Arna an exciting, but little visited tour destination for most of Bergen's inhabitants. Those who live in Arna, however, know to make the most of its beautiful natural splendour.

Sculptures in the bedrock

Herand- geologi

11.12.2018

Cross-leaved heath (Akvarell: Miranda Bødtker)

Steinevik

31.03.2018

Potholes by the Koldals River

Eikelandsosen

29.03.2018

"So many and such big potholes as are found at Eikelandsosen, we don't see other places in western Norway, and as beautifully polished as the mountainside is along the river up to Koldal , one would look a long time to see anywhere else. There is much to dazzle a geologist's eyes. If only these features could bring others the same joy!"

Vinnesleira

Vinnesleira

06.12.2018

Bays that are shallow far out into the sea, with fine sand and clay, are rare in Hordaland. Where they are found, the reason is usually that the edge of the glacier made smaller advances or stopovers when it calved back at the end of the last Ice Age. This is what happened at Vinnesleira.

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