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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

A deciduous forest slop with Bear’s garlic.

From Dense Forest to Open Heathlands

15.05.2018 - 14:06

The outer frame - the coast, the fjord and the mountains - are an inheritance from the country's geological history. But what, more than anything else, gives the scene colour and excitement is the plant life.

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.

Gjuvsland (Svein Nord)

Gjuvsland

19.06.2018 - 16:21

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.

The Ancient Ash Tree

The Ancient Ash Tree

19.06.2018 - 16:22

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.

Ground up bedrock in the Valen Fault, seen under a microscope.

The Valen Fault

04.01.2019 - 12:59

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