page_title: Färnebofjärden National Park
hierarchical_section_title: Färnebofjärden National Park
caption_attribution_description: Deutsch: Relief Positionskarte von Schweden English: Blank relief location map of Sweden Français&#160;: Carte physique vierge de la Suède, destinée à la géolocalisation. Scale: 1:3,708,000 (precision: 927 m) Equirectangular projection, WGS84 datum Standard meridian: 017° 30' E Central parallel: 62° 18' N Geographic limits of the map: Top: 69° 30' N Bottom: 55° 06' N Left: 10° 24' E Right: 24° 36' E
context_page_description: Färnebofjärden National Park is a Swedish national park traversed by the river Dalälven, about 140 km north of Stockholm. It covers 10,100 ha, of which 4,110 ha aquatic, on the frontier between the counties of Dalarna and Gävleborg.
  After the retreat of the ice sheet that covered the region after the last ice age, the river found itself rerouted by an esker onto a plain uniquely ribbed by the ridges of other eskers, where it formed a succession of rapids and wide bays, which the river inundates during the spring floods. This particular hydrography, along with the park's proximity to the ecological frontier between the north and the south, has favored the development of a fauna and flora of great biodiversity. The park possesses coniferous, mixed, and broadleaf forests, some of which quite ancient, spared by the logging industry because of their inaccessibility. These forests constitute the ideal environment for numerous species, in particular birds, with critical densities of woodpeckers and owls.
  If the presence of humans was relatively discreet since the Stone Age, concentrated principally atop the eskers, the development of mining activity has profoundly affected the region.
context_section_description: Färnebofjärden National Park (Swedish: Färnebofjärdens nationalpark) is a Swedish national park traversed by the river Dalälven, about 140 km (87 mi) north of Stockholm. It covers 10,100 ha (25,000 acres), of which 4,110 ha (10,200 acres) aquatic, on the frontier between the counties of Dalarna and Gävleborg.
  After the retreat of the ice sheet that covered the region after the last ice age, the river found itself rerouted by an esker onto a plain uniquely ribbed by the ridges of other eskers, where it formed a succession of rapids and wide bays (called fjärdar), which the river inundates during the spring floods. This particular hydrography, along with the park's proximity to the ecological frontier between the north and the south, has favored the development of a fauna and flora of great biodiversity. The park possesses coniferous, mixed, and broadleaf forests, some of which quite ancient, spared by the logging industry because of their inaccessibility. These forests constitute the ideal environment for numerous species, in particular birds, with critical densities of woodpeckers and owls.
  If the presence of humans was relatively discreet since the Stone Age, concentrated principally atop the eskers, the development of mining activity (in particular of iron) has profoundly affected the region. The forests were exploited to feed the water-powered forges which grew up along the river. One of the most important was that of Gysinge, founded in 1668 and situated right next to the park. In 1975, in reaction to the threat of the clearing of a vast forest, the movement for the creation of a national park began, culminating in the park's opening in 1998. The park was added to the Natura 2000 Network and included in the Ramsar Convention's list of wetlands.
  The park and its environs are important tourist destinations. The river is its favored mode of discovery, but some hiking trails permit other explorations. The park is equally appreciated by fishing enthusiasts.
caption: National parks of Sweden (clickable map)
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