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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.

Gildrehola

Gildrehola

12.03.2018 - 12:53

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.

Elias Fiigenschoug’s painting of Halsnøy monastery , 1656

Halsnøy Monastery

19.06.2018 - 16:12

Halsnøy Monastery is situated in the midst of the lush fjord country in Sunnhordland, on one of the old spits, or “necks”, that has given name to the island. Gently sloping fields lead down to the sea on both sides, in the south towards the Kloster Fjord, to the north towards the sheltered Klostervågen.

Langhaugane, Ulvanosa in the background.

Langhaugane

03.01.2019 - 16:52

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.

Ølve

Ølve

04.01.2019 - 15:57

Ølve has a special soil type. Here one finds an extra hard clay soil. This is especially noticed by those who work with excavating for building foundations and the like. Often it is necessary to use especially big digging machines and sometimes even dynamite in order to break up the compact masses. The reason for this is the growth of the glaciers toward the end of the Ice Age: The clay, that was first deposited in front of the glacier, came under great pressure when the glacier later grew and slid out over the clay.

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.

Section from a sea map from the Danish Sea Map Archive from 1798, drawn by Poul Løvernørn.

Fitjarøyane

18.06.2018 - 20:30

If we study the group of islands south of Selbjørns Fjord from the air or on a sea map, we will notice that many of the islands are elongated and lie systematically in rows. The islands are divided by long sounds, for example Trollosen, Nuleia and Hjelmosen, which are oriented in a south-southeast to north-northwesterly direction.

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