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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)
![At lake Gaupåsvatnet.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/nvh_334_gaupas_koronitt_150.jpg?itok=Wq7ffNPu)
![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.
![](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/berg_12_0.jpg?itok=hv7XxFE6)
![Reppadalen (Svein Nord)](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/berg_1.jpg?itok=_72uaNnN)
Reppadalen
The unusual bog landscape, with enormous peat deposits surrounded by steep mountainsides, makes Reppadalen in Arna an exciting, but little visited tour destination for most of Bergen's inhabitants. Those who live in Arna, however, know to make the most of its beautiful natural splendour.
![Eclogite bedrock at Ådnefjellet.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/meland_21.jpg?itok=W8PmuPzd)
Eldsfjellet
The eclogites in western Norway were formed when Precambrian basement rocks were squeezed and pressed down under great pressure deep under the Caledonian mountain chain. The process may well have triggered some of the deepest earthquakes the world has ever known. The clearest traces of this drama are found in and around Mt. Eldsfjellet, in peaceful Meland.
![Manger](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/radoy_25.jpg?itok=2_lft7Ih)
Manger
Mangerite is a rock type that was first made famous in a treatise by the Bergen geologist Carl Fredrik Kolderup in 1903. The rock type got its name from the place where it was found, and has made the Mangerud name well known around the world, at least among geologists.