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Glacier fall at Bondhusbreen.

Bondhusdalen

19.12.2018 - 19:25

The Bondhus area in Maruanger has been a magnet for tourists ever since the stream of tourists to Norway's west coast began in the middle of the 1800s. The magnificent landscape with the "ice trail" up to Bondhusvatnet Lake, the ice falls from Bondhusbreen glacier and Keisarstigen trail up to Folgefonna are still popular tourist attractions.

From Upper Musland toward Geitadalen.

Ulvanosa

04.01.2019 - 11:02

Some mountains have rounded shapes, while others have steep slopes and sharp edges. Ulvanosa (1246 mos.) has both. The forms reflect the type of bedrock below, and the forces that were in effect when they were formed.

Årstad in the 1890s

Årstad

12.06.2018 - 17:18

Alrekstad (later Årstad) is the birthplace of Bergen. The estate was an estate for Harald Hårfagre and several of his descendants: Eirik Blodøks, Håkon den gode og Olav Tryggvason. These first kings moved with their courts and guardsmen from estate to estate. From these estates the king ruled the country.

In the middle of the flat pastures at Torsnes was the farmyard of the estate, undivided until the middle of the 1700s

Torsnes

26.05.2018 - 16:29

When bishop J.Neumann was on a visitation in Hardanger in 1825 he also visited Torsnes, the seat of the Galtung family. They were then in the process of pulling down the old dwelling house on the farm. As the committed observer of ancient monuments and antiquarian buildings that he was, bishop Neumann has provided us with interesting details:

A zone with nuggets from the inner earth.

Drøna

12.03.2018 - 13:01

Gjønavatnet and Kikedalen

Gjønavatnet and Kikedalen

16.06.2018 - 14:03

The Hellands scree

Møshovd

06.12.2018 - 10:30

Vinnesholmen, Fusa

Vinnesholmen

21.11.2018 - 19:25

Nils Hertzberg watercolour of “Spånheimsklosteret”

Sponheim

27.05.2018 - 15:52

On the trail toward Kyrkjedøri, a half hour walk from Finse station, we find these small ridges

Trail toward Kyrkjedøri

04.12.2018 - 15:04

Roughly 550 million years ago, what is now Finse lay at the bottom of the sea - the remains of mud and clay that were deposited in this sea have ended up on the roofs of Norway. Also the thrust sheet from the continental collision has found its way to Finse, after a several hundred kilometre-long, trek through the mountains, that took several tens of millions of years to complete.

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