- Remove Boats and seafaring filter Boats and seafaring
- Remove Late glacial filter Late glacial
- Remove Sedimentary rocks filter Sedimentary rocks
- Remove Kvinnherad filter Kvinnherad
- Remove Fjell, frå 2020 del av nye Øygarden kommune filter Fjell, frå 2020 del av nye Øygarden kommune
- Remove Museum filter Museum
- Remove Sediments filter Sediments
- Remove Large landforms filter Large landforms
- Remove Lindås, frå 2020 del av nye Alver kommune. filter Lindås, frå 2020 del av nye Alver kommune.
- Remove Modalen filter Modalen
Rosendal Barony
The Barony of Rosendal lies in the grounds of the old noble estate of Hatteberg, on the north side of the Hatteberg river, around one kilometre up from the sea. The three noble estates Seim, Mel and Hatteberg constituted the core of the large estate taken over by Ludvig Rosenkrantz in 1662, after he was married to Karen Mowat in 1658.
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.
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.
Rød
In 1969 Sigurd and Margreta Dønhaug donated a collection of around 170 historical cultural objects to Kvinnherad municipality. They wanted their gift to become the start of a farm collection in Uskedalen. And that is what happened.
Skorpo
Skorpo - Polished by glaciers and meltwater
Ulvanosa
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
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.