University of Bergen- Remove Small landforms filter Small landforms
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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.
Ænes
Ænes has been one of the prosperous farms at the Mauranger Fjord in medieval times. At the time of Harald Gilles, around 1130, we hear of GAUT at Ænes. The noble families around the Hardanger Fjord were prominent in the political sphere from early on, and it is obvious that the fine and openly situated farm at Ænes was also a good place for a Church.
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.
