The beautiful vicarage on the Fjelberg Island lies a few minutes walk up from the fjord, in a compact enclosure with the church south of the main building and the bishop’s residence to the north; a rare harmonic cluster.
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 stately Kvinnherad Church with its characteristic profile set out against the mighty Malmangernuten in the background, gives you a rare feeling of being present in a historic landscape as you come around Nes and face the well-kept houses at the Skåla farm. The church at Skåla is one of four “fjordungskirker” (one of four main district churches) and this farm was the centre of this coastal administration district.
Skorpo - Polished by glaciers and meltwater
In 1852 Haktor Thorsen erected two large warehouses on one of his farms in Sunde and started trading and salting herring. This was the start of an industrial adventure that made Sunde into one of the first industrial communities in Kvinnherad.
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 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.