Bondhusdalen

The Bondhus area in Maruanger has been a magnet for tourists ever since the stream of tourists to Norway's west coast began in the middle of the 1800s. The magnificent landscape with the "ice trail" up to Bondhusvatnet Lake, the ice falls from Bondhusbreen glacier and Keisarstigen trail up to Folgefonna are still popular tourist attractions.

Bordalsgjelet

Deep down between the stone polished phyllite bedrock in Bordalsgjelet canyon, there is a cascading river. In close cooperation with hard polishing stones, the water has carved into the bedrock for thousands of years - and is still doing so today.

Botnavatnet

Botnen

Fyksesundet and Botnagrenda present a fine experience of the landscape and cultural history; a geographically isolated local settlement with extensive cultural contact with the outside world.

Brekke

Buardalen Valley

Buarbreen glacier was one of the first destinations during the period of increasing tourism in Odda in the 1800s. Foreigners came by the thousands, mostly Englishmen and Germans, to the magnificent landscape in front of the glacier. Back at the hotel in Odda they could enjoy drinks containing ice from the glacier.

Bømoen

Church Art – a Message in Pictures

In the still and dim church interiors of the Middle Ages the performances of belief came to life in the gleam from the wax candles. Here the essential articles of faith were presented, here the church was presented through holy men and holy women and here the events from the Gospels were told: the angels with Maria, the birth of the baby Jesus, the Three Wise Men, the history of the drama of the Passion and the victorious Christ.

Cultural Heritage and Cultural Landscapes

The development which culminated in the great west Norwegian clustered communities in the 18th and 19th centuries, such as we see at Havrå on Osterøy Island, actually first came into being in Viking times, with an incipient division of the farms into smaller units.

Dyrdal

If you journey along Austfjorden, you at the same time turn the pages of time back through Ice Age history. The landforms show how the landscape has developed gradually as the glaciers have grown - and melted again - in several episodes: from small cirques, we see innermost at Dyrdal, to larger fjords, like at Mas fjord further out.