- Remove Quarns and mills filter Quarns and mills
- Remove Chieftains and royal lines filter Chieftains and royal lines
- Remove Mineral resources filter Mineral resources
- Remove Road constructions filter Road constructions
- Remove Deciduous forests filter Deciduous forests
- Remove Sediments filter Sediments
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.
Holmedalsberget
If you want to be on your own for a long day in a magnificent deciduous forest in demanding terrain, then HOLMESDALSBERGET is the right place. This is a big forested area by Matres Fjord in the southwestly part of Kinnherad. Here, we find one of the largest deciduous forests in Hordaland. The forest stretches over several kilometres.
Varaldsøy- mining
There is still a lot of ore in the abandoned mines on Varaldsøy Island. If today's prices and availability of ore continue, it is doubtful whether the mines will resume operation. But, the pyrite is there, if the market should return. On Varaldsøy Island one finds at least nine mines and prospect pits, that for the most part date back to the latter part of the 1800s.
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.
Fjøsanger
Fjøsanger is known among ice age researchers from around the world. Under an excavation in 1975-77, geologists from the University of Bergen found layers from the last interglacial, ca. 115 000 to 130 000 years old.