University of Bergen- Remove Small landforms filter Small landforms
- Remove Late glacial filter Late glacial
- Remove Fitjar filter Fitjar
- Remove Avalanches and rock falls filter Avalanches and rock falls
- Remove Music filter Music
- Remove People and Society filter People and Society
- Remove Defense filter Defense
- Remove Civil servant dwellings and manors filter Civil servant dwellings and manors
- Remove Sunnhordland filter Sunnhordland
- Remove Dialects and arts filter Dialects and arts
- Remove Kvinnherad filter Kvinnherad
- Remove Sveio filter Sveio
- Remove Trading posts and guesthouses filter Trading posts and guesthouses
- Remove Landscape filter Landscape
Ølve
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.
Skorpo
Skorpo - Polished by glaciers and meltwater
Melderskin
MELDERSKIN - ONCE A NUNATAK? Melderskin, the towering and majestic landmark at Rosendal, rises 1462 metres above sea level. The top area is smooth, but slightly inclined. Geologists think that the area is a remnant of a weakly undulating landscape, that originated near the sea, long before the Ice Age set in.
In Memory of Fartein Valen
“Fartein Valen is the key figure within newer Norwegian music. Not by way of being more popular than other younger composers, but because he aims at things higher, which he is fully confident of being able to reach since he commands all techniques. But there is a price to pay for reaching above the ordinary, and there is a price to pay for demanding more than the ordinary from the listeners. This is something Valen has experienced”.
Halsnøy
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.
Bondhusdalen
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.
