- Remove Quarns and mills filter Quarns and mills
- Remove Trading posts and guesthouses filter Trading posts and guesthouses
- Remove Sediments filter Sediments
- Remove Basement rocks filter Basement rocks
Kræmmerholmen
Kræmmerholmen is one of the old privileged trading posts. From the 1600s all trading in West Norway took place in Bergen, and the farmers were obliged to travel into town in order to sell their produce and buy what they needed. In Bergen City Privilege of 1702 the merchants in the city were allowed to establish “Trading posts in the countryside”. The owner had to have residency in Bergen and the trading post was to be run by an assistant. In this way the city retained financial control of those living in the districts, and not least with buying and selling of fish.
Bjørsvik
The industrial settlement Bjørsvik
Bruknappen
The hostelry place in Bruknappen is situated north in Radsundet, just south of Festo, by a sheltered idyllic bay, close to the main lane. Sloops both from Sognefjorden and Nordland had their fixed stops at “the blacksmith in Bruknappen”; on their way to Bergen, fully loaded with wood and hazel hoops, barrels and chests, or on their way home with town merchandise.
Mostraumen
Until 1743 the people from Modal had to wait for a flood in MOSTRAUMEN before they could draw their boats up the river current, and then row back across Lake Movatnet. But, that year the flood opened a free passageway all the way to Mo. Hordaland had gained a new tidal waterway.
Nedre Helland- Sand Quarries
The three spades in the municipal coat of arms for Modalen are sand spades. Sand quarrying has brought income and employment. As much as 70,000-80,0000 tonnes of sand and gravel left the municipality each year since the turn of the millennium, to be used as cementing sand. Why is Modalen endowed with so much sand?
Eksingedalen- landscape
Eksingedalen alternates between wide, flat flood plains with good farmland, and narrow passages with waterfalls where the roads cling to the mountainsides. The alternations in the landscape are a result of the sculpturing work by glaciers over several ice ages, and the deposition of the glacial river deposits when the last glacier finally melted back.