University of Bergen- Remove Cultural landscapes filter Cultural landscapes
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Ask- jordbær
Strawberry-growing on Askøy flourished in the beginning of the last century. When gardener Samson Eik took in the type "Seierherren" from Rosendal in 1909 for growing strawberries on Hop, it appeared that the soil and climate in this area was perfect for the mass production of strawberries.
Herdla Church
A letter from the Pope Eugenius 3 in 1146 mentions St. Nikolaus church at Herdla. This church belonged under Munkeliv monastery, which was founded in Bergen by Øystein around 1110. The Herdla Church may stem from this time.
Strusshamn
On the south side of Askøy, just west of Bergen, lies Strusshamn. The sheltered bay is one of the best harbours in Byfjorden, on the route south. At the time of the sailing ships the harbour could be full of vessels from Bergen and abroad, lying in wait for favourable wind. Old anchoring rings from 1687 bear witness to this. Strusshamn was a quarantine harbour for ships that came sailing in with the yellow pest flag flying.
Fossen Bratte
The steep drop by Fossen cliff has been the biggest challenge for those who wished to make a road over Kvamskogen through the years. Leave the car by the monument on the old road and take a walk down to the bend by the waterfall that Bergen-folk call "The bridal veil". Why is there a waterfall just here?
Frøland
Much rain, a steep drop and nearness to Bergen meant that the power-making potential of the Samnanger water system was exploited early. Samnanger was thus one of the first power-producing municipalities in western Norway. With its subsequent expansion and new power stations, about 400 gigawatts of electricity per hour were produced on average each year. This is enough to meet the energy needs of 25,000 households.
Gullbotnen
A barren belt where almost nothing grows, runs through the forest on the east slope of Gullbotnen. But, along the west side of the main road there is a fertile zone that flourishes with several finicky plant types. The contrasts arise from the extreme variations in the nutrient content of the bedrock.
