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The state residence at Holmen painted by Catharine Kølle, undated.

Holmen

19.06.2018 - 18:39

HOLMEN AND THE KØLLE FAMILY Holmen lies by the fjord, innermost in Ulvikpollen. Originally this was a small smallholding or coast dweller’s place belonging to the farm Håheim. Major Johan Henrik Palludan obtained leasehold for a part of Holmen in 1773, and erected a grand house, as he was the head of Nordre Hardangerske kompani. In 1806 Mrs Palludin sold Holmen to the somewhat eccentric theologian Kristian Kølle, and thus the Kølle family came to Ulvik. Today the Kølle house in Holmen is gone, today it is the residence of the principal of the State horticultural school that occupies the ground – a villa in the dragon style from the turn of the previous century.

The soil tongues below Jomfrunuten.

Jomfrunuten

03.12.2018 - 14:13

Freezing and thawing are processes that influence plant cover, move enormous blocks, stretche long mounds of earth, break open bedrock and create patterns in stone and earth.

Glacial river plain at Lake Klevavatnet.

Rallarvegen

04.12.2018 - 14:30

They rest there, all as one, the silent witnesses of Western Norway's saga of creation: Precambrian basement, phyllite and thrust sheet. In the end came the glaciers and sculptured the vast landscape. Along the ground or on the horizon, from bicycle or on foot - the landscape tells its story - and it tells it clearer on Rallarvegen than many other places.

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.