Øvre Tveiten

On an east-facing slope above Halllandsvatnet lies the farm hamlet of Øvre Tveiten, two kilometres north of Manger. The stone hayshed lies with its gable out into the sloping terrain, and the old dwelling house, a little long house, has solid stone walls on three sides. But inside the walls the hayshed and the living rooms are wooden buildings.

Ystebøtræet

Vågenes

On Vågenes, on one of the prominences out toward Eitrevågen, one finds garnets in anorthosite. The garnets are both older, and not least bigger, than average.

Sylta

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.

Nottveit

In one of the frame-built haysheds at Nottveit, at holding No. 3, we discover that several of the staves have a medieval look, with large dimensions and carefully rounded edges. According to tradition, it was the farms Nottveit and Mostraumen that supplied the timber for the stave church at Mo, and it is not unlikely that these farms received the old timber in return when the new church was erected there in 1593.

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.

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

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.

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.