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![Gildrehola](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/awfawf.jpg?itok=2AAfbxlk)
![Gjuvsland (Svein Nord)](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/navn.jpg?itok=npdQFont)
![Halsnøy](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvi_15.jpg?itok=mn2F8JKB)
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.
![Elias Fiigenschoug’s painting of Halsnøy monastery , 1656](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_192-1.jpg?itok=9VO9I-NR)
Halsnøy Monastery
Halsnøy Monastery is situated in the midst of the lush fjord country in Sunnhordland, on one of the old spits, or “necks”, that has given name to the island. Gently sloping fields lead down to the sea on both sides, in the south towards the Kloster Fjord, to the north towards the sheltered Klostervågen.
![The circular buckle from Hatteberg, Kvinnherad](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_198-2_0.jpg?itok=Nx0pe53v)
![Langhaugane, Ulvanosa in the background.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvi_38.jpg?itok=bdNUBUC5)
![Skorpo (Svein Nord)](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvi_49.jpg?itok=i4VQIqsW)
Skorpo
Skorpo - Polished by glaciers and meltwater
![Ølve](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/landstet.jpg?itok=1EeuuxMs)
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.
![The soil tongues below Jomfrunuten.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/ulvik_36.jpg?itok=aOfkkEth)
Jomfrunuten
Freezing and thawing are processes that influence plant cover, move enormous blocks, stretche long mounds of earth, break open bedrock and create patterns in stone and earth.