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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.

Baldellia

Ådlandsvatnet

19.06.2018 - 16:39

Plants that grow in and beside water have to be prepared for marked and rapid changes in their living conditions. They must be able to tolerate living under water without drowning, and getting totally dried out without whithering. Many swamp plants are well adapted to these kinds of changes.

Ystebøtræet, Radøy

Ystebøtræet

18.06.2018 - 20:08

Fishing in Flagafossen in the 1930s

Vosso

24.01.2019 - 14:46

There is probably no bigger salmon to be found in the whole wide world than in Vosso. The average size varies from season to season of course, but for many years this fish has had an average weight of over 10 kilograms. Thumping big ones of 30 kg. have been fished from the river, but one must go back to the 1940s for the last salmon of this size last that was caught.

Pump house for the Vossevangen water works.

Vossavangen

24.01.2019 - 14:18

Vinnesleira

Vinnesleira

06.12.2018 - 11:03

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.

Vinnesholmen, Fusa

Vinnesholmen

21.11.2018 - 19:25

Ramnagjelet, Ulvik

Ulvik-village

04.12.2018 - 15:45

The ice cap that covered the land during each of the 40 past ice ages over the past 2 million years of Earth's history pressed down the crust of the earth - like a finger on a rubber ball. And when the ice finally loosened its grip 11,000 years ago, the earth's crust rose again, most where the ice was thickest, least where it was thin, quickly in the beginning, and later more slowly. To this day, the land in the inner part of Norway continues to rise by perhaps one millimetre per year. By and large, however, the crust in Hordaland has again reached equilibrium after the weight of the ice was removed.

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Ulvensletta

07.12.2018 - 10:10

The smallholding Træet, Askøy

Træet

30.03.2018 - 08:56

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