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![Domkirken](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/kvh_256_domkirken_150.jpg?itok=kfZkGtiZ)
![Fantoft stave church](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/kvh_267_fantoft_150.jpg?itok=hZdUT-Rm)
![Fjøsanger](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/berg_49.jpg?itok=x0vBKTNz)
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.
![Korskirken](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/korskirken.jpg?itok=LK8XAlZN)
![The church at Kyrkjebyrkjeland was pulled down in 1878.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh-267-1x.jpg?itok=fL3_DjIv)
![The interior of Mariakirken, Bergen](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_256.1.jpg?itok=dmJ7QmNt)
Mariakirken
Apart from the king’s estate at Holmen, Håkonshallen and the lower floors of the Rosenkrantz tower, the three parish churches in the centre of Bergen are what have been preserved from medieval Bergen: Mariakirken, Korskirken and Olavskirken (the cathedral). The Romanesque base of the tower from Nonneseter monastery church on the spit between the two Lundegård lakes can still be seen in the landscape, while the other medieval buildings now lie in ruins: the town’s oldest town hall and wine cellar at Nikolaikirkealmenning, Lavranskirken and Maria Gildeskåle between Mariakirken and Bryggens Museum and the Katarina hospital on the north side of Dreggsalmenningen.
![Fra Blåmanen mot Vardegga og Ulriken.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/vidden.jpg?itok=8VZJtCoS)
![Langavatnet, Åsane (Svein Nord)](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/1/berg_6_cmyk_0.jpg?itok=EdtUxacZ)
Åsane
Most associate Åsane with ridges, naturally enough (the Norwegian word for "ridge" is "Ås"). A lesser noticed trait in the landscape are the unusual flat areas that lie between the ridges. The Dalselva River, which was channeled at the end of the 1950s, runs down only 2.5 metres from Lake Langavatnet by Vågsbotn to Flatevad, where it goes over into rapids by Fossekleiva. The layers of gneiss stand nearly vertically, and the mountain surface is so even that one might think it had been planed with a planer.
![Cirque in Dyrdal in Lindås](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/mas_22.jpg?itok=YmoL_BEr)
Dyrdal
If you journey along Austfjorden, you at the same time turn the pages of time back through Ice Age history. The landforms show how the landscape has developed gradually as the glaciers have grown - and melted again - in several episodes: from small cirques, we see innermost at Dyrdal, to larger fjords, like at Mas fjord further out.
![Litlematre](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/mas_10.jpg?itok=wpTaAy0K)