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Nils Hertzberg watercolour of “Spånheimsklosteret”

Sponheim

27.05.2018 - 15:52

Ystebøtræet, Radøy

Ystebøtræet

18.06.2018 - 20:08

Manger

Manger

18.06.2018 - 20:06

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.

The smallholding Træet, Askøy

Træet

30.03.2018 - 08:56

Geologists from all over the world come to study the veined bedrock (the dark stripe in the picture) at Spildepollen.

Spildepollen

07.12.2018 - 10:55

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.

Vinnesholmen, Fusa

Vinnesholmen

21.11.2018 - 19:25

The monks leave their mark at Lysekloster

Lysekloster- The monks and nature

15.05.2018 - 13:34

Lysekloster was the largest agricultural property in the country when it was phased out during the Reformation in 1537. In its prime this cloister encompassed two-thirds of all the farms in Os. The monks introduced and cultivated new plant species and it was probably they who stocked the waters with fish not indigenous to the area. This legacy from the Middle Ages has left a lasting mark.

A zone with nuggets from the inner earth.

Drøna

12.03.2018 - 13:01

The walls in the boathouse in Hopssundet are built of red granite from Reksteren.

Hopssundet

01.05.2018 - 16:39

Espevik

Espevik

03.01.2019 - 15:26

220 million years ago, glowing hot molten rock masses intruded into fractures in the earth's crust in the outer parts of Hordaland. Some of these are believed to have reached the surface and formed lava flows, which since have been eroded away by wind and weather. But, most of these flows solidified into diabase sills before they got to the surface.

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