- Remove Small landforms filter Small landforms
- Remove Sediments filter Sediments
- Remove Maritime environments filter Maritime environments
- Remove Seabirds filter Seabirds
- Remove Monastery filter Monastery
- Remove Avalanches and rock falls filter Avalanches and rock falls
- Remove Etne filter Etne
- Remove Mineral resources filter Mineral resources
- Remove Fusa, frå 2020 ein del av nye Bjørnafjorden kommune filter Fusa, frå 2020 ein del av nye Bjørnafjorden kommune
- Remove Sund, frå 2020 del av nye Øygarden kommune filter Sund, frå 2020 del av nye Øygarden kommune
- Remove Faults filter Faults
Eikelandsosen
"So many and such big potholes as are found at Eikelandsosen, we don't see other places in western Norway, and as beautifully polished as the mountainside is along the river up to Koldal , one would look a long time to see anywhere else. There is much to dazzle a geologist's eyes. If only these features could bring others the same joy!"
Skjelbreid
On the east side of Lake Skjelbreidvatnet, clearly visible along the road from Eikelandsosen, we notice a farm on a terrace above a grassy hill. The hill has the form of a broad shield; Skjelbreid (" Broad Shield") is the name of the farm.
Vinnesleira
Bays that are shallow far out into the sea, with fine sand and clay, are rare in Hordaland. Where they are found, the reason is usually that the edge of the glacier made smaller advances or stopovers when it calved back at the end of the last Ice Age. This is what happened at Vinnesleira.
Golta- Long house
In the years between the wars a major registration of houses and house costumes, house construction methods, fireplaces and forms of housing clusters was started in West Norway – an ambitious mapping of everything that came under the name “Registration of Culture and Geography in West Norway”. One of the places of which material was gathered in 1938 was an old multi-room house at Golta; new and interesting material for the researchers from the Historical Museum, but well known within the local building tradition through several generations.
Goltasundet
For generations the land-seine was the most important tool for catching herring and mackerel, and therefore a suitable casting bay was worth its weight in gold. Goltasundet (the Golta sound) on Golta was such a place. Here the herring often drifted in and fantastic casts might be made here.
The village of Etne
Much of the sand and gravel that the town of Etne is built on was laid down at the end of the Ice Age and is evidence of melting glaciers and roaring meltwater rivers. The uncompacted material in the big terraces leave their unmistakeable mark on the wide elongated valleys.
Skånevik- moraine
In Skånevik there are marks left from the ice edge that advanced during the thousand-year cold spell (Younger Dryas) that marked the end of the Ice Age roughly 11 500 years ago. The glacier first proceeded out into Åkra Fjordand and around Vannes and thereafter sent an arm in toward Skånevik. Here, the glacier lay down an end moraine up against the mountainside.