Bryggen

In the 1300s Bergen was a trading centre of European dimension. The town is thought to have had around 7000 inhabitants and was the largest and most important in the country. In a European context it was an average size town. At this time the most tightly built town area was still mostly east of Vågen from Holmen in the north to Vågsbotn in the south. Already in medieval times, latest in the 1340s, this area was called Bryggen.

Kalandsvatnet and Klokkarvatnet

Rosesmuggrenden

Sandviken

Close to the tunnel opening at Amalie Skrams vei in Ssandviken, there is a cultural monument of European dimensions; a rope making works that produced rope and fishing tackle for West and North Norway.

Strandsiden

During the 1300s Strandsiden changed from a rural area with a monastery to a pulsating trading centre with boathouses, storehouses and embankment.

Vågsbunnen

Vågsbotn was the name of the innermost part of the eastern part of town from Auta-almenning (today’s Vetrlidsalmenning), skirting the bottom of Vågen to Allehelgenskirken (All Saints’ Church) (at the present Allehelgensgate). In early medieval times Vågen reached almost all the way to Olavskirken (the Cathedral). It was a relatively wide bay inside the premonitory where Korskirken was built. The area was therefore much shorter than what is known as Vågsbunnen today.

Korsfjorden

Skogseidvatnet

Lake Skogseidvatnet is the most famous fishing lake in Hordaland, with good stocks of both char and trout. There is fishing here throughout the year: with a net in the autumn, through the ice in winter, and with a fishing rod in the summer.

Krækkjavassdraget

Few other animal species on Hardangervidda have been as much the focus of scientific research as the spotted trout. The spotted trout is considered to be a genetic variant of brown trout. It lives in parts of the Krækkjav water system. Otherwise, on a world scale, this species is only found in a small area in Kaukasus, and possibly also in a lake in Rondane.

Granvinsvassdraget

After the ice age, Granvin Fjord reached all the way up under Skjervsfjossen waterfall. Just a thousand years later, as a result of the rising of the land after the ice melted, this whole inner part of the fjord freed itself of the sea and became Granvinsvatnet lake. In spite of this rise in elevation, this waterway is still navigable for fish: Sea trout have wandered into Granvinsvatnet in more recent times and evolved to become freshwater trout. And salmon and sea trout made the journey 13 kilometres up the Storelvi river.