Alverstraumen

Bruknappen

The hostelry place in Bruknappen is situated north in Radsundet, just south of Festo, by a sheltered idyllic bay, close to the main lane. Sloops both from Sognefjorden and Nordland had their fixed stops at “the blacksmith in Bruknappen”; on their way to Bergen, fully loaded with wood and hazel hoops, barrels and chests, or on their way home with town merchandise.

Isdalstø

Lure Fjord

Both Lure Fjord and Lindåsosane to the inside give good living conditions for rare marine organisms: jellyfish, shellfish and fish. These include animals that migrated in after last the Ice Age, when the sea level was higher. Eventually, as the land rose, some of these populations became isolated.

Eldsfjellet

The eclogites in western Norway were formed when Precambrian basement rocks were squeezed and pressed down under great pressure deep under the Caledonian mountain chain. The process may well have triggered some of the deepest earthquakes the world has ever known. The clearest traces of this drama are found in and around Mt. Eldsfjellet, in peaceful Meland.

Holmeknappen

If you come by sea to Bergen and come up the Herdle Fjord, the yellow ochre marine shed at Holmeknappen is a well known landmark to starboard as you come close to the little shore settlement. In olden days Holmenknappen served important functions as a centre for a wide hinterland of the surrounding farms, warehouse, landing point, country store and later a steamer quay, a hotel (1896) and a dairy (1909). But today Holmeknappen is no longer a focal point. Transport and commercial routes have changed the old pattern

Otterstad

Tthe Otterstad farms lie in the innermost part of Mofjorden, on the northwest side of the river. The row of stave-built boatsheds that belong to the farm were probably constructed a little after the middle of the 1800s. Both here and on the Mo side, the boatsheds were important storage places at the seashore; wood and other farm products intended for the town; corn and merchandise in return.

Bergsdalen

The mountains of western Norway are lovely to wander in. In Cambro-Silurian time it was the mountain itself that wandered. The mountain, or more correctly the bedrock, first moved eastward, then back a bit westward again. All this rocking back and forth in the mountains ended about 400 million years ago.

Straume- maritime environment

Veafjorden

Some decades ago, Veafjord and the currents in toward the bigger rivers were the most likely places to see harbour seals in Hordaland. In the summer flocks lay on the beach and waited for the salmon to trickle in. Sometimes they also followed the fish a little way up the river.