University of Bergen- Remove Middle age filter Middle age
- Remove Nordhordland filter Nordhordland
- Remove Stone age filter Stone age
- Remove Farm sites filter Farm sites
- Remove Trading posts and guesthouses filter Trading posts and guesthouses
- Remove Railroad filter Railroad
- Remove Vaksdal filter Vaksdal
- Remove Sediments filter Sediments
- Remove Benthic organisms filter Benthic organisms
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.
Gullbrå
From written sources we know that the farm Gullbrå was in use early in the 1600s. The Apostolic church in Bergen owned land here that it rented out, but even early in the 1600s some of the land was in private ownership. Eksingedalen then belonged to Modalen parish, which was under Hamre parish. In 1723 the Apostolic church still had properties here, and Ivar and Lars were farmers.
Skipshelleren
For vel 7000 år sidan var Straume ein av dei beste – om ikkje den beste – veideplassen i Hordaland. Steinalderfolket som busette seg ved Skipshelleren, skjøna truleg ikkje kor heldige dei var. Mellom dei opptil 2 meter tjukke dyngjene med stein og bein som arkeologar grov fram i 1931–32, fann dei reiskapar og avfall frå fangst og matstell. Frå dette materialet har arkeologane stava seg fram til livet ved straumen.
Veafjorden
Some decades ago, Veafjord and the currents in toward the bigger rivers were the most likely places to see harbour seals in Hordaland. In the summer flocks lay on the beach and waited for the salmon to trickle in. Sometimes they also followed the fish a little way up the river.
