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The steep sloping landscape on Håvra

Cultural Heritage and Cultural Landscapes

18.11.2017 - 19:49

The development which culminated in the great west Norwegian clustered communities in the 18th and 19th centuries, such as we see at Havrå on Osterøy Island, actually first came into being in Viking times, with an incipient division of the farms into smaller units.

Hårteigen

The Landscape

18.11.2017 - 19:54

Kiste måla i 1834 av Bjørn Bjaalid

Vernacular arts and crafts

15.05.2018 - 13:57

A Hardanger sloop in full sail on the Trøndelag coast.

Sailing Sloops and Boat Building

21.11.2018 - 19:47

Marine activities expanded greatly throughout the 19th century, and provided a livelihood for many people. Fishing and shipping were probably the subsidiary activities which had greatest economic significance throughout the century. Marine activities brought, literally speaking, wind into the sails of many rural districts in Hordaland during that period.

Alfred Søvik from Lysefjorden

The Wooden Boat

15.05.2018 - 14:01

Craftsmanship through two thousand years

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.

Halsnøy

Halsnøy

19.12.2018 - 21:15

Hadde ikkje Hardangerfjordbreen mot slutten av istida rykt fram over fjordbotnen, ville Halsnøy ikkje eksistert som éi øy, men som mange småøyar. Breen skuva framfor seg så mykje leire frå havbotnen at Brattåsen, Toftåsen, Landåsen og Svartaberg vart samla i eitt landområde.

Skålafjøro

Skålafjøro

21.11.2018 - 19:42

Skorpo (Svein Nord)

Skorpo

29.03.2018 - 11:25

Skorpo - Polished by glaciers and meltwater

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.

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