Skogsvåg

Kval i våg! Når det ropet gjekk, var det berre å få ut den kraftige kvalnota til å stengja vågen med, og så kunne veidinga ta til. I uminnelege tider har det vore drive kvalveiding i Skogsvågen.

Fosnstraumen

At the southern end of the bridge between Radøy and Fosnøy archaeologists found an unusual Stone Age settlement. There was a thick “cultural layer” here with the remains of the waste dumps of a hunting people. The place was called Kotedalen. Here they came, one group after the other, and settled for some weeks, some months, or maybe years before they went on, leaving the settlement deserted. Time after time it happened. At least 16 settlement phases have been identified, stretching over 5,500 years.

Straume- Salmon

From times immemorial salmon and trout have been caught with various tools in the fjord and the streams here. Finds in the Stone Age settlements at Skipshelleren indicate that salmon was probably caught by angling. Nets, fish pots and traps have been used in the rivers right up to our times. In the fjords the use of nets was developed into a salmon seine around 1500, and later into what today is known as fixed seine.

Espevær- the Trading Post

In the sea west of Bømlo lies Espevær, half an hour’s rowing trip across the sound from Vespestadvågen. This is a well-run and well-maintained local community, established on the back of the rich herring fisheries in the 1850s. It is fishermen, skippers and the tradesmen who have made their mark on the culture in Espevær, with their contacts to the south towards Haugesund and across the North Sea to the British Isles.

Ingahogg

At nearly 1000 metres over sea level, on the north side of INGAHOGG mountain, the remains of a soapstone quarry have been discovered. It is said, according to the Sagas, that Inga collected the big soapstone that lies in front of the Åkra Church from here.

Ulvanosa

Some mountains have rounded shapes, while others have steep slopes and sharp edges. Ulvanosa (1246 mos.) has both. The forms reflect the type of bedrock below, and the forces that were in effect when they were formed.

Vinnesholmen

Skytjedalen

Lussand- geology

Hardangerfjorden kløyver Hordaland i to. Den etter måten rettlinja fjorden skjer seg liksom på skeive inn i landet. Ikkje som Sognefjorden og Nordfjord – dei krokar og buktar seg innover meir eller mindre vinkelrett på kysten. Hardangerfjordens utforming har røter 400 millionar år tilbake i tida, då den veike sona i fjellet, der isen seinare tok grådig for seg, vart danna. Denne sona stig på land ved Lussand.

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.