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.

Boga

In the lightly undulating landscape at Boga there lies an old house with several rooms on a small rise. In fact it looks like three houses built into one another; a scullery, a living room and a store with a loft. From other sources we know that this house had covered passageways and sheds round all the walls in the 19th century; a compressed “long house” with inter-connections between all the rooms. This is a building style from the Middle Ages that we see traces of; a building corresponding to those we have seen remains of at Høybøen in Fjell and Lurekalven in Lindås. Bogatunet was restored in 2006.

Dale

Dalseid- Eidslandet road construction

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.

Gullbrå

From written sources we know that the farm Gullbrå was in use early in the 1600s. The Apostolic church in Bergen owned land here that it rented out, but even early in the 1600s some of the land was in private ownership. Eksingedalen then belonged to Modalen parish, which was under Hamre parish. In 1723 the Apostolic church still had properties here, and Ivar and Lars were farmers.

Hana

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

Kolåseidet

The little cowshed which lies on the fence at Kolåseidet, constructed in connection with the stone fence, has put its mark on the cultural landscape. On the border between the home fields and the forest, the cowshed is the very symbol of a simple resource management - the division between the cropland and the grazing grounds. And the way it was built has its roots far back in time.

Manger

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.