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.

Byparken

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.

Fjøsanger

Fjøsanger is known among ice age researchers from around the world. Under an excavation in 1975-77, geologists from the University of Bergen found layers from the last interglacial, ca. 115 000 to 130 000 years old.

Halsnøy

Hadde ikkje Hardangerfjordbreen mot slutten av istida rykt fram over fjordbotnen, ville Halsnøy ikkje eksistert som éi øy, men som mange småøyar. Breen skuva framfor seg så mykje leire frå havbotnen at Brattåsen, Toftåsen, Landåsen og Svartaberg vart samla i eitt landområde.

Langhaugane

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.

Ølve

Ølve has a special soil type. Here one finds an extra hard clay soil. This is especially noticed by those who work with excavating for building foundations and the like. Often it is necessary to use especially big digging machines and sometimes even dynamite in order to break up the compact masses. The reason for this is the growth of the glaciers toward the end of the Ice Age: The clay, that was first deposited in front of the glacier, came under great pressure when the glacier later grew and slid out over the clay.