University of Bergen- Remove Small landforms filter Small landforms
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- Remove Ullensvang, frå 2020 del av nye Ullensvang kommune. filter Ullensvang, frå 2020 del av nye Ullensvang kommune.
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Grindheim church
The first church at Grindheim was a stave church with a free-standing steeple. The church was first mentioned in 1326, but was probably built long before this time.
Kinsarvik church
By all accounts the church in Kinsarvik must have been one of the four main churches in the old Horda County. The stone church standing today was restored by cathedral architect Chr. Christie in 1880, and again by Peter Helland-Hansen in 1960-61. At that time an archaeological investigation was undertaken, which has unearthed new knowledge about the church.
Kvalvikane
In Ålvik quartz has long been used to produce ferro-silicon. The quartz was collected from the other side of the fjord, from the mountainside above Kvalvikane.
Kyrping
The trading post down by the fjord at Kyrping does not belong to the oldest group of trading posts from the 1600s and 1700s. It was only after the liberalisation of the trading legislation that trade was established here.
Mosnes
The permanently-protected Mosneselva River, with its meltwater from Folgefonna, runs out into Åkra Fjord by the roadless and uninhabited Mosnes. Those who once lived here were forced to surrender to the ravages of Nature. In the autumn of 1962 there was a flood so great that the people were driven from their farms.
Måge
Steatite is a type of stone that is abundant in Hardanger. There are large steatite deposits in the mountain below Folgefonna. These deposits are visible both in Krossdalen in Jondal, at Kveitno in Odda and at Måge in Ullensvang. There are many traces of steatite quarrying in Hardanger, and one of the largest fields is in the hillside above Måge.
