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Aga farmyard

Aga

19.06.2018 - 18:35

The grand farm Aga on the west side of Sørfjorden, came under protection in 1937, when the agricultural reform threatened to disperse the old clustered settlement. “Lagmannsstova”, named after the “lagmann” (law speaker) Sigurd Brynjulfsson, was already protected in 1924; one of the authentic profane wooden buildings from the Middle Ages still standing. All the same it is the farmyard itself that is the key cultural monument.

Today Jåstadstova is placed at Hardanger Folk High School at Lofthus

Jåstad

27.05.2018 - 15:23

The farm Jåstad, situated a few kilometres north of Agatunet, must have been a grand farm in medieval times. Torolf on Jåstad is mentioned as arbitration moderator in 1293, and in the vaulted corridor at Lyse Kloster Sigurd, farmer at Jåstad, and his wife Sigrid – the king’s kinswoman - are buried.

Nils Hertzberg’s prospectus from 1825 of “Ålmerket” and the site of the long ship shed.

Kinsarvik

29.04.2018 - 11:55

Kinsarvik has probably been a centre for the inner Hardanger districts back in prehistory. History tells us that in medieval times there was a marketing place, a “kaupang”, here; a connecting point in the communications between east and west. There were supposedly around 300 residents here but the place was likely wiped out in a great fire.

Myking

Myking

19.03.2019 - 16:24

Between Lake Kvalheimsvatnet and Lake Mykingsvatnet, north of Grindheim, we find one of the biggest continuous lowland bogs in Hordaland. It is 500-600 metres across and a whole 2 kilometres long. Locally, the bog is called "Havet" .

The farms on Toska lie on moraine soils from the Herdla moraine.

Toska

18.06.2018 - 20:07

The peat bogs on Toska have been mined for peat since 1946, when the island got electricity. In this treeless coastal landscape, peat was the most important source of energy, and this took quite a toll on the bogs.

Vinnesleira

Vinnesleira

06.12.2018 - 11:03

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.