
Riisitunturi
Finland, Lapland
Riisitunturi
About Riisitunturi
Riisitunturi National Park protects a distinctive taiga-fell landscape in the southern part of Finnish Lapland, within the municipality of Posio in northern Ostrobothnia and Lapland. Established in 1982, the park covers approximately 77 square kilometres centred on the Riisitunturi fell, which rises to 483 metres above sea level above a vast surrounding boreal forest and mire plateau. The park is particularly renowned for its magnificent snow-laden conifer forest, where heavy winter snow loads transform spruce and pine into ghostly snow sculptures known locally as 'tykky'. This phenomenon creates one of Finland's most extraordinary winter landscapes, drawing photographers and snowshoers in midwinter.
Wildlife Ecosystems
The park's forest, fell, and mire habitats support a broad range of boreal and subarctic species. Brown bear, wolverine, and Eurasian lynx inhabit the park, with wolverine particularly associated with the open fell and mire terrain. Reindeer pass through the park as part of Sami herding movements. The fell supports capercaillie and willow ptarmigan, which are resident year-round and turn white in winter. Rough-legged buzzard and golden eagle hunt over the open mire in summer. The lake and stream systems within the park hold grayling and Arctic charr. Siberian jay is a common resident of the old boreal forest.
Flora Ecosystems
The park's fell top is characterized by low arctic-alpine heath with crowberry, bearberry, and mountain avens. The slopes carry mountain birch krummholz below the tree line, transitioning to Norway spruce and Scots pine forest at lower elevations. Extensive aapa mire complexes surround the fell base, with cottongrass, Sphagnum mosses, and bog rosemary. The park's old-growth boreal forest areas contain significant deadwood and veteran trees that support specialist lichens and saproxylic insects. The combination of subarctic fell, old-growth forest, and intact mire creates exceptional biodiversity for the latitude.
Geology
The Riisitunturi fell is composed of ancient Precambrian metamorphic rocks that have resisted glacial erosion more effectively than the surrounding softer rock types, leaving it as a prominent topographic high. The smooth, rounded summit profile is the product of intense glacial abrasion, and the fell sides show relic periglacial features including solifluction lobes from the immediate postglacial period. The surrounding lowland terrain is covered by thick glacial till with esker ridges marking the routes of meltwater drainage under the ice sheet. Peat accumulation in the mire basins began approximately 9,000 years ago.
Climate And Weather
Riisitunturi has a harsh subarctic continental climate. Winters are long and cold, with mean January temperatures around -14°C and snow accumulation from October through May. The fell receives exceptionally heavy snowfall driven by moist air masses from the Norwegian coast, which deposit significant additional snow compared to surrounding lowland areas. This extra snow load creates the spectacular tykky phenomenon on the conifers. Summer temperatures peak around 15°C in July, with extended daylight hours. Autumn colours arrive by late August, and the park can experience snowfall as early as September.
Human History
Riisitunturi lies within the traditional reindeer herding territory of the Posio region, used by Sami and later Finnish herding communities. The surrounding lowland forests were logged extensively in the nineteenth and twentieth centuries, but the fell and its immediate surroundings were less intensively exploited due to difficult terrain and thin soil. The Posio municipality was settled by Finnish agricultural communities during the seventeenth and eighteenth centuries, primarily along river valleys. Traditional activities including hunting, fishing, and berry picking were important for local livelihoods across the park area.
Park History
Riisitunturi was designated a national park in 1982 as part of the same wave of park establishment that created several other Finnish national parks during that decade. The park was created partly to protect the old-growth forest and intact mire landscape from further logging, and partly in recognition of the exceptional winter landscape scenery created by the tykky phenomenon. Metsähallitus operates the park and has developed a visitor centre at the Riisitunturi fell base. Trail infrastructure was expanded in the 1990s and 2000s to accommodate growing winter tourism. The park is included in the national network of accessible nature destinations.
Major Trails And Attractions
The Riisitunturi summit trail from the visitor centre car park is the park's primary attraction, a 4-kilometre return hike to the fell top with panoramic views across the Lapland wilderness. In winter, the trail is used for snowshoeing with rental equipment available at the visitor centre. The spectacular tykky phenomenon is best observed from January through March when the snow loads are heaviest. A longer circular trail of approximately 12 kilometres traverses fell, forest, and mire habitats. Birdwatching for fell species including ptarmigan, capercaillie, and rough-legged buzzard is rewarding in summer.
Visitor Facilities And Travel
The park's visitor centre is located approximately 40 kilometres from Posio, accessible by car. From Rovaniemi, the drive takes about 2 hours. The visitor centre provides exhibits, trail maps, and snowshoe rental in winter. A lean-to shelter and campfire site are available near the trailhead. Overnight accommodation within the park is limited to one wilderness cabin; hotels and holiday cottages are available in Posio. Public transport connections to the park are limited; a car is recommended. The park is open year-round; winter snowshoeing and summer hiking are the main activities.
Conservation And Sustainability
Conservation priorities at Riisitunturi include protecting the old-growth boreal forest from invasive logging adjacent to park boundaries, maintaining the intact hydrology of the surrounding mire complex, and managing visitor pressure on the fell summit trail which is vulnerable to erosion during the spring snowmelt period. Large predator populations including wolverine and lynx are monitored. Climate change is of particular concern as warming winters with less snowfall would reduce the tykky phenomenon, affecting both biodiversity and visitor appeal. Mire carbon stocks are monitored as part of Finland's national climate-related nature monitoring programme.


Frequently Asked Questions
Where is Riisitunturi located?
Riisitunturi is located in Lapland, Finland at coordinates 66.217, 28.45.
How do I get to Riisitunturi?
To get to Riisitunturi, the nearest city is Posio (19 km), and the nearest major city is Oulu (150 mi).
How large is Riisitunturi?
Riisitunturi covers approximately 77 square kilometers (30 square miles).
When was Riisitunturi established?
Riisitunturi was established in 1982.
Is there an entrance fee for Riisitunturi?
Riisitunturi is free to enter. There is no entrance fee required.







