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Up to the 1870s Osøyra was a military training area.

Osøyro

16.06.2018 - 16:00

The coastal settlement of Os begins to take form in the middle of the 1800s. This is when craftsmen and traders begin to settle at the river delta.

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 lobster park in Espevær

Espevær- lobster park

19.06.2018 - 18:42

Strandvollen ved Hallaråker. Siggjo in the background

Hallaråker

19.05.2018 - 20:27

From

Ulvensletta

07.12.2018 - 10:10

Hetlefloten i Os

Os valley

06.12.2018 - 12:38

Ulevn Camp around 1915.

Ulven camp

16.06.2018 - 16:03

Sandy beach to the west of Kallsøyna, outermost Valen

Herdla – glacial deposits

05.12.2018 - 12:11

The shift in the landscape is striking between the barren craggy moors north on Askøy and the green fields of Herdla, which has the county's biggest farm. The majority of Herdla, such as the island appears today, is a gift from the glacier: The glacier that advanced here over 12,000 years ago stopped at the northern tip of Askøy and took its time building up the moraine on Herdla. Since then, Herdla has been under continual transformation. The re-organisation of the loose sediment deposits continues today.

Ask- The king's estate

12.06.2018 - 16:56

Ramnagjelet, Ulvik

Ulvik-village

04.12.2018 - 15:45

The ice cap that covered the land during each of the 40 past ice ages over the past 2 million years of Earth's history pressed down the crust of the earth - like a finger on a rubber ball. And when the ice finally loosened its grip 11,000 years ago, the earth's crust rose again, most where the ice was thickest, least where it was thin, quickly in the beginning, and later more slowly. To this day, the land in the inner part of Norway continues to rise by perhaps one millimetre per year. By and large, however, the crust in Hordaland has again reached equilibrium after the weight of the ice was removed.

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