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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.
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.
Færøysund
The old trading post lies at the sound between Stord and Færøy in Langenuen. There was a country store and steamship forwarding agent up to 1964. The trade was then moved over to the new ferry harbour of Sandvikvåg.
Engesund
For more than 350 years Engesund has been a place for hostelries and trading in the Fitjar islands. The place is centrally placed in the shipping lane, with a sheltered harbour close to the exposed Selbjørnsfjorden. Engesund was once part of the great network of historical stopover places on the coast.
Einstapevoll- the farm
Einstapevoll (from einstape: “bregne” (fern)) lies on the west side of the Tittelsnes peninsula. Up to 1831 the farm was a vicarage belonging to Stord parish. The priests had leasing rights. Land rent and other fees from the farm was part of their salaries.
