It isn't true that hungry students have hunted down basking ducks in the city park Byparken in their spring fervour, as rumours may have it. But, it is not unusual to see students throw themselves over the park's wild birds, and hold on to them tight. They ring the birds. Because of this, we know quite a lot about the birds in Byparken.
Roughly 550 million years ago, what is now Finse lay at the bottom of the sea - the remains of mud and clay that were deposited in this sea have ended up on the roofs of Norway. Also the thrust sheet from the continental collision has found its way to Finse, after a several hundred kilometre-long, trek through the mountains, that took several tens of millions of years to complete.
Spring, summer and autumn, there is bird life on Valen, and the tidal zone is especially attractive. Out on Herdlaflaket, you see ducks and other diving birds all year round, but most in winter.
Small boat folk in Hordaland know where Løno is. As do many seabirds. With the big ocean at its back and a wide, weather beaten strait ahead of it, Løno is one of Hordaland’s most isolated and exposed recreational areas. The islands west of Sotra are some of the county’s most stable nesting localities for seabirds.
There are coal bits hidden in the sand under Vatlestraumen. These remains from a geological layer from the Jurassic Period were discovered when the undersea Bjorøy Tunnel was built in 1994. Oil- and gas reservoirs in the Troll Field in the sea west of Hordaland are from the same time. It is, nonetheless, quite surprising to find bedrock from dinosaur time inside of the outer islands of western Norway. On the Scandinavian mainland north of Denmark, there are only a very few places where one f inds rock from this time in earth history.
There isn't much forest on Skogsøyna today, but that there is, has been planted. There is not much wildlife, either. But, quite a lot of birds pass by Skogsøyna during migration time. Ther is no other place along the coast where you can better observe the seabird migrations.
Holmengrå is the only place in Hordaland where we find traces of the abrasion that is supposed to have transformed Western Norway from a Himalaya-like high mountain landscape during the earth's Paleozoic Era, to a flat lowlands terrain during the Mezosoic Era. Just 400 million years ago, large and small stones plummeted down from the high mountains. Some of these stones became incorporated into the conglomerate bedrock on Holmengrå.