The park is characterized by a very rough topology with many rocky peaks, of which the highest is Slåttdalsberget, 280 m (920 ft) in altitude, rising directly from the sea.
This forest has thus been able to recover a part of its ancestral richness, and so contains an important fauna and flora, with several endangered species, such as the lichen Usnea longissima, which is the park's symbol.
Today, despite its distance from areas of dense human population, the park is a relatively important site of tourism with 20,000 visitors per year.
The principal attraction of the park is the 40 m (130 ft) deep crevasse of Slåttdalskrevan, which is easily accessible by numerous hiking trails, including the Höga Kustenleden, which goes along the whole of the High Coast.
[2] This name already appears in 1539 in the form Scyla mons and would derive from skjul meaning "hiding place", the famous cave in the mountain having been in the past a refuge for brigands.
[2] Skuleskogen National Park is in the municipalities of Örnsköldsvik and Kramfors, both of Västernorrland County, both in the historical Swedish province of Ångermanland.
[H 3] The park itself covers the eastern part of the forest of Skule, characterized by a terrain forming a sort of wall separating the north and the south.
[S 3] Spring is the driest season, and in certain years this relative dryness has important consequences for the environment, especially because the thinness of the soil retains moisture poorly.
The station’s more inland and elevated (143 meters) positioning possibly renders the national park much milder, especially during late summer and early fall.
[S 5] Since granite forms a substrate very poor in nutrients, the diabase constitutes by contrast a very fertile terrain, which permits a richer vegetation.
[S 5] The ice's thickness attained 3 kilometres (1.9 mi), exerting significant pressure on the soil, which was thus situated 800 metres (2,600 ft) below the current level of the High Coast.
[S 5] When the ice melted, the soil rose progressively, a phenomenon called the post-glacial rebound, at a speed of 8 mm (0.31 in) per year.
[S 5] As the land emerged from Lake Ancylus (ancestor of the Baltic Sea), the waves affected the terrain of today's park.
[S 5] The coastline of that era can now be found at an altitude of 285 metres (935 ft), measured from Skuleberget, southwest of the national park, which constitutes an absolute record.
[S 6] Besides these two species, one can find the red fox (Vulpes vulpes), the European badger (Meles meles), the European pine marten (Martes martes), the moose (Alces alces), the Eurasian beaver (Castor fiber), the grey seal (Halichoerus grypus), and the muskrat (Ondatra zibethicus).
[S 6] One can also find small mammals, such as the Eurasian red squirrel (Sciurus vulgaris), the American mink (Neogale vison) and the stoat (Mustela erminea).
[S 6] With respect to birds, many species are also on the endangered list in Sweden, such as the Siberian jay (Perisoreus infaustus), the three-toed woodpecker (Picoides tridactylus), the red-throated loon (Gavia stellata), the European honey buzzard (Pernis apivorus), the rough-legged buzzard (Buteo lagopus), the greenish warbler (Phylloscopus trochiloides), the red-breasted flycatcher (Ficedula parva), the red-backed shrike (Lanius collurio), the spotted nutcracker (Nucifraga caryocatactes), the common rosefinch (Carpodacus erythrinus), and the ortolan bunting (Emberiza hortulana).
[S 7] The park also houses important populations of grey-headed woodpeckers (Picus canus), common cranes (Grus grus), grey herons (Ardea cinerea), Eurasian wrens (Troglodytes troglodytes), Eurasian wrynecks (Jynx torquilla), and hazel grouse (Tetrastes bonasia).
Thus several deciduous tree species are present in the park, such as the little-leaf linden (Tilia cordata), the common hazel (Corylus avellana), the guelder-rose (Viburnum opulus), and the Norway maple (Acer platanoides).
[14] Because of the topography and the nature of the terrain, the area did not lend itself to human settlement and no trace of permanent habitation had been found in the park.
[S 10] During the Bronze Age, many funerary cairns were placed along the coast as it existed at that time: one can find 28 inside the park, as well as two megalithic monuments.
[S 12] As a result, in today's national park there were four summer pasture cottages, three having existed up until the turn of the 20th century, while the last (Näskebodarna) remained active up until the end of World War II.
[2] After the Great Northern War at the beginning of the 18th century, Sweden encouraged the foundation of villages on its territories by tax exemptions.
[S 13] However, conflict arose between the land owners and the authorities of nature protection, the latter maintaining that no exploitation of the forest could occur and that the zone ought to be classified as a national park.
[H 13] To accomplish this the terrain would have had to be purchased by the state, but the land owners did not accept the deal that they would be given equivalent areas of forest nearby.
[S 13] The official motive for the creation of the park was "to preserve a heavily deforested coastal landscape, of rocky terrain and fracture valleys, in a relatively intact state, where fauna and flora can develop freely.
[S 13] In 1996, the area was included in the Natura 2000 Network, and in 2000, they park was important in the High Coast becoming a UNESCO World Heritage site.
[18] Naturvårdsverket is responsible for proposing new national parks, upon consulting with the councils of administration of the counties and municipalities; their creation is endorsed by a vote of the Swedish parliament.
[H 16] It is also possible to go kayaking along the coast[S 21] and to go swimming, in particular at the sandy beaches of Tärnättholmarna or in the lagoon of Salsviken to the north, where the water can attain warmer temperatures.
[S 21] The most visited site in the park is probably the crevasse of Slåttdalsskrevan, but also popular are the view from over the archipelago from the nearby summit of Slåttdalsberget, as well as the Bronze Age funerary cairns.