Heggjagarden

The transport exchange on the farm Vik in Eidfjord was an important part of the communication network in older times. This is where people secured transport by boat out in the fjord, those travelling across the mountain from east and down into Måbødalen. The transport exchange was situated at “Wiige grund”. Today the highway cuts through the farmyard; the main farmhouse from the 1800s lies on the upper side of the road, the large sea-house, with a bakery in former times, lies close to the fjord.

Langavassfjellet

Kongstun

In the Middle Ages the farmers were under obligation to transport state officials. The bishops were entitled to 18 horses when they travelled about on visitations, and the king could requisition free transport.

Rallarvegen

They rest there, all as one, the silent witnesses of Western Norway's saga of creation: Precambrian basement, phyllite and thrust sheet. In the end came the glaciers and sculptured the vast landscape. Along the ground or on the horizon, from bicycle or on foot - the landscape tells its story - and it tells it clearer on Rallarvegen than many other places.

Sponheim

Ulvik-village

The ice cap that covered the land during each of the 40 past ice ages over the past 2 million years of Earth's history pressed down the crust of the earth - like a finger on a rubber ball. And when the ice finally loosened its grip 11,000 years ago, the earth's crust rose again, most where the ice was thickest, least where it was thin, quickly in the beginning, and later more slowly. To this day, the land in the inner part of Norway continues to rise by perhaps one millimetre per year. By and large, however, the crust in Hordaland has again reached equilibrium after the weight of the ice was removed.

Ask- The king's estate

Herdla – glacial deposits

The shift in the landscape is striking between the barren craggy moors north on Askøy and the green fields of Herdla, which has the county's biggest farm. The majority of Herdla, such as the island appears today, is a gift from the glacier: The glacier that advanced here over 12,000 years ago stopped at the northern tip of Askøy and took its time building up the moraine on Herdla. Since then, Herdla has been under continual transformation. The re-organisation of the loose sediment deposits continues today.

Strusshamn

On the south side of Askøy, just west of Bergen, lies Strusshamn. The sheltered bay is one of the best harbours in Byfjorden, on the route south. At the time of the sailing ships the harbour could be full of vessels from Bergen and abroad, lying in wait for favourable wind. Old anchoring rings from 1687 bear witness to this. Strusshamn was a quarantine harbour for ships that came sailing in with the yellow pest flag flying.

Brattholmen

The old guesthouse location in Brattholmen on the east side of Litlesotra, was probably established in the first half of the 1700s. A list from 1748 mentions that the place “for some years has been inhabited by an Enrolled Sailor by the name of Peder Michelsen”. As was the case for most other military hosts, he was exempt from paying income tax.