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Odda- The industrial town

25.03.2019 - 14:47

In 1908 the new power station in Tyssedal was completed. A/S Tyssefaldene provided power for the carbide and cyanide factory that was built in Odda. This signalled a new era.

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 phosphate factory in Knarrvika, Fjell

Knarrevik

12.06.2018 - 20:00

Having passed well over the bridge across to Sotra you pass an industrial plant surrounded by a budding community; the mineral mill of A/S Norwegian Talc. Some of the buildings seem to have been erected in the early part of the 20th century. They are remnants of a grand industrial plant from the former boom time in the country – the economic upswing after WWI.

Tysse

Tysse

18.03.2018 - 08:08

As early as 1862 Svein L.Røsseland started a country store and lodging house at Ytre Tysse, and later on he became steamship agent and the first post office manager in Samnanger. However, the decisive change came when F.Mathiessen started A/S Samnanger Uldvarfabrik (woollen factory) in 1886.

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.

Selsneset

01.04.2018 - 22:05

The carton factory around 1895., Fusa

Sævareid

16.06.2018 - 14:07

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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