- Remove Small landforms filter Small landforms
- Remove Place filter Place
- Remove Sediments filter Sediments
- Remove Boat- and shipyards filter Boat- and shipyards
- Remove Kvinnherad filter Kvinnherad
- Remove Vaksdal filter Vaksdal
- Remove Bergen filter Bergen
- Remove Fusa, frå 2020 ein del av nye Bjørnafjorden kommune filter Fusa, frå 2020 ein del av nye Bjørnafjorden kommune
- Remove Askøy filter Askøy
- Remove Trading posts and guesthouses filter Trading posts and guesthouses
![Gildrehola](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/awfawf.jpg?itok=2AAfbxlk)
![Halsnøy](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvi_15.jpg?itok=mn2F8JKB)
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.
![Langhaugane, Ulvanosa in the background.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvi_38.jpg?itok=bdNUBUC5)
![Skålafjøro](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_198-3.jpg?itok=9ztk7jqN)
![Skorpo (Svein Nord)](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvi_49.jpg?itok=i4VQIqsW)
Skorpo
Skorpo - Polished by glaciers and meltwater
![Sunde, Kvinnherad](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_194_xxx.jpg?itok=7zdyKxkc)
Sunde
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.
![Ølve](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/landstet.jpg?itok=1EeuuxMs)
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](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/berg_49.jpg?itok=x0vBKTNz)
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.
![](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/fjosangerveien_reper.jpg?itok=wT--rhNB)
![D/S «Seimstrand» at bay in Salhus around 1906](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_264-1.jpg?itok=9ymiBDPa)
Salhus
Salhus has been a connecting point for sea travellers far back in time. The name probably derives from the Old Norse word sáluhús, “house for travellers”. The name may indicate that this was a place for an inn even in the Middle Ages. The place is eminently situated in the route to and from Bergen. For travellers coming by boat from Sogn and Nordhordland, Salhus is the last stop before Bergen. Travellers from the communities in Voss also came this way earlier when they were going to Bergen