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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.
Manger
Mangerite is a rock type that was first made famous in a treatise by the Bergen geologist Carl Fredrik Kolderup in 1903. The rock type got its name from the place where it was found, and has made the Mangerud name well known around the world, at least among geologists.
Vågenes
On Vågenes, on one of the prominences out toward Eitrevågen, one finds garnets in anorthosite. The garnets are both older, and not least bigger, than average.
Lyse chapel
The small white-painted chapel with the red brick tiled roof just south of the monastery ruins at Lyse was built in 1663 as a local chapel for the monastery estate, following the takeover of the property by the District Recorder (Stiftskriver) Niels Hanssøn Schmidt two years previously. The chapel, with its harmonic proportions, lies in the cultural landscape beside the grand monastery estate, witness to a time gone by. But even today, there is a tradition of high mass on the 2nd day of Ascension in Lyse Chapel.
Ulven
In the region of Ulven phyllite occurs with Hordaland's youngest fossils, and a beautiful quartz conglomerate. The phyllite and conglomerate got squeezed into the bottom of an ancient oceanic crust, made of gabbro and greenstone, in the heart of the Caledonide mountain chain.
