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![Blood-red geranium](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvi_24.jpg?itok=b63Z_duB)
![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.
![From the old road along the Åkrafjord](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/kvh_190_akrafjord_veg_2_150.jpg?itok=0G_IOg6S)
![Vollom](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/lindas_14.jpg?itok=RhEa2l84)
Vollom
On Vollom, northwest of Seim, we find the only natural beech forest in Western Norway, which is also the most northerly of its type in the world. Beech grows also many other places in the county, but these trees are totally lacking in history compared with those of Vollomskogen Forest.
![Tveita](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/190/nvh_260_tveitabotn_2_150.jpg?itok=qnyU8yR3)
![Toward Støle and Sørheim, 1920.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/terassen.jpg?itok=1OuuZEj5)
The village of Etne
Much of the sand and gravel that the town of Etne is built on was laid down at the end of the Ice Age and is evidence of melting glaciers and roaring meltwater rivers. The uncompacted material in the big terraces leave their unmistakeable mark on the wide elongated valleys.
![Den flate terrassen på moreneryggen på garden Tjedla viser kor høgt havet stod på slutten av den siste istida.](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/304/skanevik_endret_til_rgb.jpg?itok=KfKszhQ9)
Skånevik- moraine
In Skånevik there are marks left from the ice edge that advanced during the thousand-year cold spell (Younger Dryas) that marked the end of the Ice Age roughly 11 500 years ago. The glacier first proceeded out into Åkra Fjordand and around Vannes and thereafter sent an arm in toward Skånevik. Here, the glacier lay down an end moraine up against the mountainside.
![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
![Møkjedalen (Bjørn Moe)](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvi_22.jpg?itok=iPMTpA3a)
![Vegane gjennom den tronge og bratte Måbødalen](https://www.grind.no/sites/default/files/styles/medium/public/bilder/sted/232/kvh_407-1.jpg?itok=jN0RFHBc)