Odda- The tourist town

The pioneering tourists in the 1830s-40s brought a momentum in the tourist traffic to the fjord and mountain country Norway. At the time Odda was a hidden Shangri-La at the bottom of Sørfjorden; the farm and the church on the green headland at the fjord. But when the steamship traffic opened the fjord landscape for tourism, in a few years Odda parish in Søndre Bergenhus County became the focal point for travellers in West Norway.

Utne

When sergeant Peder Larsen Børsem from Strandebarm was “demobilised” in 1721, following the large Nordic War, he married the Bergen lady Elisabeth Schrøder and settled as innkeeper at Utne with a letter of privilege from the county governor dated 29 October 1722.

Herand- geologi

Langavassmyrane

The Ruff lek on Langvassmyrane is the only known phenomenon of its kind on Hardangervidda. Every year it attracts hens from the whole plateau. The marsh is also the richest wetland in the county. This green oasis is located in a rocky moraine landscape a few hours walking distance south of Dyranut.

Måbødalen- geology

The old pack road had 1500 steps, where cars today gas through the mountain. The time of this hard work is over, and of getting used to the steep terrain, as well; only the view from the top is much the same as before. Vøringsfossen in summer is one of Western Norway’s biggest natural wonders. It marks the transition between the older, open part of the Sysendalen valley and the younger, narrow and winding valley of Måbødalen.

Skytjedalen

Granvinsvassdraget

After the ice age, Granvin Fjord reached all the way up under Skjervsfjossen waterfall. Just a thousand years later, as a result of the rising of the land after the ice melted, this whole inner part of the fjord freed itself of the sea and became Granvinsvatnet lake. In spite of this rise in elevation, this waterway is still navigable for fish: Sea trout have wandered into Granvinsvatnet in more recent times and evolved to become freshwater trout. And salmon and sea trout made the journey 13 kilometres up the Storelvi river.

Hausberget

Skjervet- river theft

At the end of the last ice age the ice flowed out of Hardanger fjord in such a fury that it forced the meltwater from Voss to run back uphill toward Granvin. The glacier from Raundalen down the windy valley along the Vosso to Bolstadøyri went too slow to make the turn.

Jomfrunuten

Freezing and thawing are processes that influence plant cover, move enormous blocks, stretche long mounds of earth, break open bedrock and create patterns in stone and earth.