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From Upper Musland toward Geitadalen.

Ulvanosa

04.01.2019 - 11:02

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.

Ground up bedrock in the Valen Fault, seen under a microscope.

The Valen Fault

04.01.2019 - 12:59

Klosteret

12.06.2018 - 19:10

Troldhaugen, Bergen

Troldhaugen

29.03.2018 - 22:49

A zone with nuggets from the inner earth.

Drøna

12.03.2018 - 13:01

Gjønavatnet and Kikedalen

Gjønavatnet and Kikedalen

16.06.2018 - 14:03

Vinnesholmen, Fusa

Vinnesholmen

21.11.2018 - 19:25

Ramsøy with the remains of the old artillery positions.

Ramsøy

12.06.2018 - 17:02

“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.”

The smallholding Træet, Askøy

Træet

30.03.2018 - 08:56

The saw tooth pattern is clearly visible from Skora Mountain southwards toward Tellnes and Skogsvågen.

Haganes

12.06.2018 - 19:59

The gneiss landscape west and north of Bergen viewed in profile can remind us of a saw blade of the kind that has long, slanted sides that get broken off shorter transverse sides. It has taken several hundred million years to file this saw blade, an enduring interplay between various geological processes.

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