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The Haugsdal delta

Haugsdalen

13.12.2018 - 09:02

Early in the 1900s there were much larger salt water deltas in Hordaland. But, essentially all of the larger river deltas got filled in and regulated for use in industry during the last century. Now, there is only Haugsdals delta left.

The south side of Raunøya.

Raunøya

31.03.2018 - 21:11

The sea birds discovered it long ago. Raunøya and the surrounding islands are the most beautiful places in Masfjorden.

The defensive refuge at Borgåsen

Borgåsen

18.06.2018 - 20:23

In Etne there are no less than four defensive refuges. They are all situated in strategic positions, so that they have served as places of refuge and protection for central parts of the district

Etne and the Etne delta around 1900.

Etnedeltaet

18.06.2018 - 20:23

During the latter half of the 1900s the big natural river deltas on Westland disappeared. Until the 1980s there was still a small, but significant remnant of the original river delta from the Etneelva river, but today most of this, too, is industrial land.

Section from a sea map from the Danish Sea Map Archive from 1798, drawn by Poul Løvernørn.

Fitjarøyane

18.06.2018 - 20:30

If we study the group of islands south of Selbjørns Fjord from the air or on a sea map, we will notice that many of the islands are elongated and lie systematically in rows. The islands are divided by long sounds, for example Trollosen, Nuleia and Hjelmosen, which are oriented in a south-southeast to north-northwesterly direction.

Strandflat and scree by land

Landa

19.06.2018 - 16:06

Rimbareidtjørna

Rimbareid- Vestbøstad

19.06.2018 - 16:07

At nesting time you cannot avoid hearing the calls of the curlew or the snipe along the narrow road through the cultural landscape from Rimbareid to Vestbøstad. And on late summer evenings, the intense song of the sedge warbler rings out over the two characteristic tarns in the area.

Smedholmen, Fitjar

Smedholmen

30.03.2018 - 20:10

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.

Leech (Jan Rabben)

Flakkavågen

19.06.2018 - 17:19

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