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Fløksand - Tidal flats

Leiro

31.03.2018 - 19:56

View in over Mostraumen.

Mostraumen

13.12.2018 - 10:36

Until 1743 the people from Modal had to wait for a flood in MOSTRAUMEN before they could draw their boats up the river current, and then row back across Lake Movatnet. But, that year the flood opened a free passageway all the way to Mo. Hordaland had gained a new tidal waterway.

Under the grass fields lie large quantities of sand and gravel.

Nedre Helland- Sand Quarries

13.12.2018 - 11:09

The three spades in the municipal coat of arms for Modalen are sand spades. Sand quarrying has brought income and employment. As much as 70,000-80,0000 tonnes of sand and gravel left the municipality each year since the turn of the millennium, to be used as cementing sand. Why is Modalen endowed with so much sand?

Herlandsnesjane

Herlandsnesjane

18.06.2018 - 19:59

Herlandsnesjane, a four-kilometre long peninsula in Lake Storavatnet in the middle of Osterøy, is well known among botanists. Here lies an unusually large and diverse bog.

The farms on Toska lie on moraine soils from the Herdla moraine.

Toska

18.06.2018 - 20:07

The peat bogs on Toska have been mined for peat since 1946, when the island got electricity. In this treeless coastal landscape, peat was the most important source of energy, and this took quite a toll on the bogs.

Flatekvål

Eksingedalen- landscape

13.12.2018 - 17:06

Eksingedalen alternates between wide, flat flood plains with good farmland, and narrow passages with waterfalls where the roads cling to the mountainsides. The alternations in the landscape are a result of the sculpturing work by glaciers over several ice ages, and the deposition of the glacial river deposits when the last glacier finally melted back.

Lake Nesheimvatnet

Lake Nesheimvatnet

18.06.2018 - 20:12

Strandvollen ved Hallaråker. Siggjo in the background

Hallaråker

19.05.2018 - 20:27

From Rubbestadneset.

Rubbestadneset

18.06.2018 - 20:20

Toward Støle and Sørheim, 1920.

The village of Etne

18.12.2018 - 20:39

Much of the sand and gravel that the town of Etne is built on was laid down at the end of the Ice Age and is evidence of melting glaciers and roaring meltwater rivers. The uncompacted material in the big terraces leave their unmistakeable mark on the wide elongated valleys.

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