Matches in DBpedia 2016-04 for { ?s ?p "Flakstadelva is a river in Hedmark, Norway. Its headwaters lie in the bog areas around Gråberget. From there it runs in a southerly direction and forms the Nybusjøen, which discharges into the Lundsbekken river. The river flows in a v-shaped valley which twists before its mouth on the Lundsbekken. The river's erosion has exposed the lower Cambrian and middle Cambrian rock formations in that region."@en }
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- Flakstadelva abstract "Flakstadelva is a river in Hedmark, Norway. Its headwaters lie in the bog areas around Gråberget. From there it runs in a southerly direction and forms the Nybusjøen, which discharges into the Lundsbekken river. The river flows in a v-shaped valley which twists before its mouth on the Lundsbekken. The river's erosion has exposed the lower Cambrian and middle Cambrian rock formations in that region.".
- Q4588211 abstract "Flakstadelva is a river in Hedmark, Norway. Its headwaters lie in the bog areas around Gråberget. From there it runs in a southerly direction and forms the Nybusjøen, which discharges into the Lundsbekken river. The river flows in a v-shaped valley which twists before its mouth on the Lundsbekken. The river's erosion has exposed the lower Cambrian and middle Cambrian rock formations in that region.".
- Flakstadelva comment "Flakstadelva is a river in Hedmark, Norway. Its headwaters lie in the bog areas around Gråberget. From there it runs in a southerly direction and forms the Nybusjøen, which discharges into the Lundsbekken river. The river flows in a v-shaped valley which twists before its mouth on the Lundsbekken. The river's erosion has exposed the lower Cambrian and middle Cambrian rock formations in that region.".
- Q4588211 comment "Flakstadelva is a river in Hedmark, Norway. Its headwaters lie in the bog areas around Gråberget. From there it runs in a southerly direction and forms the Nybusjøen, which discharges into the Lundsbekken river. The river flows in a v-shaped valley which twists before its mouth on the Lundsbekken. The river's erosion has exposed the lower Cambrian and middle Cambrian rock formations in that region.".