University of Bergen
Ulvanosa
Some mountains have rounded shapes, while others have steep slopes and sharp edges. Ulvanosa (1246 mos.) has both. The forms reflect the type of bedrock below, and the forces that were in effect when they were formed.
Ramsøy
“At thick of night a thundering knock on the door; the man in the house wakes up, jumps out and demands: Who cries? Yes, now you must out, the beacon shines on Høgenut. And in the same breath, every man knew that strife had hit the land.”
Spildepollen
The oceanic crust of the North Sea was subjected to a lot of stretching both in Permian and Triassic times, and later in the Jurassic. This stretching resulted in the North Sea collapsing in and also to large faults forming west of Hordaland and on the mainland. Austefjorden in Sund follows one of these faults.
Tælavåg
Tælavåg has a significant place in the history of the German occupation in WWII. The small community by the sea, where for centuries people had made a living from farming and fishing in harmony with the natural resources, in 1942 became the victim of German reprisals without their equal in Norwegian war history. The collection of war histories in Tælavåg provides us with a close-up of the dramatic events.
Vinappen
Vinappen lies on a low hill to the very west on the island. Here you have an amazing panorama of the sea. Originally the area was grazing land for cattle, but this changed when the Germans occupied the island. Just before WWII there was a small bearing station, used by the Norwegian Coast Artillery in connection with exercises at sea.
Håøy
Håøy lies centrally in one of the main shipping lanes going into Bergen --- with Håyøsund on the south side facing Meland, and Hagelsundet facing Lindåslandet. Names like Nordfarskista and Nordfarsskorane explain things. The strategic position was important in Viking times and it has been important in our days too. The beacon on Håøy can have been built in the establishment of the coastal administration in Håkon the Good’s time, about 950 AD. The defence structure of which we say remains on Håøy Summit held a critical position during Norwegian neutrality during the First World War. The defence structure was taken down in 1957.
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.
