Rondane National Park
2008/9 Schools Wikipedia Selection. Related subjects: European Geography
| Rondane National Park | |
|---|---|
| IUCN Category II ( National Park) | |
 |
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| Location | Hedmark and Oppland,  Norway |
| Nearest city | Otta |
| Coordinates | |
| Area | 963 km² (238,000 acres) |
| Established | December 21, 1962 |
| Governing body | Directorate for Nature Management |
Rondane National Park is the oldest national park in Norway, established on December 21, 1962. The park contains ten peaks above 2,000 metres (6,560 ft), with the highest being Rondeslottet at an altitude of 2,178 m (7,146 ft). The park is an important habitat for herds of wild reindeer.
The park was extended in 2003, and now covers an area of 963 km² (372 sq mi) in the counties Oppland and Hedmark. Rondane lies just to the east of Gudbrandsdal and two other mountain areas, Dovre and Jotunheimen are nearby.
Geography
Rondane is a typical high mountain area, with large plateaus and a total of ten peaks above 2,000 m (6,560 ft). The highest point is Rondeslottet ("The Rondane Castle") at an altitude of 2,178 m (7,146 ft). The lowest point is just below the tree line, which is approximately 1,000 to 1,100 m (about 3,300 to 3,600 ft) above sea level. The climate is mild but relatively arid. Apart from the White Birch trees of the lower areas, the soil and rocks are covered by heather and lichen, since they lack nutrients. The largest mountains are almost entirely barren; above 1,500 m (5,000 ft) nothing but the hardiest lichens grow on the bare stones.
The mountains are divided by marked valleys through the landscape; the deepest valley is filled by Rondvatnet, a narrow lake filling the steep space between the large Storronden- Rondeslottet part and Smiubelgen ("The Forge"). The central massif is also cut by "botns": flat, dead stone valleys below the steep mountain walls of the peaks. Generally, Rondane does not receive enough precipitation to generate persistent glaciers, but glacier-like heaps of snow can be found in the flat back valleys.
The centre of the Park is the Rondvatnet lake, from which all the peaks beyond 2,000 m (6,560 ft) of altitude can be reached in less than one day's walk. In this central region and north of it, the altitude is quite high compared with the flatter plateaus of the south. Rondane has ten peaks over 2,000 m, Rondeslottet (2,178 m), Storronden (2,138 m), Høgronden (2,114 m), Midtronden western summit (2,060 m), Vinjeronden (2,044 m), Midtronden eastern summit (2,042 m), Trolltinden (2,018 m), Storsmeden (2,016 m), Digerronden (2,015 m), and Veslesmeden (2,015 m).
In many parts of the park, there are spread-out holes ( kettle holes) created by small remains of ice age glaciers, and peculiar small hills called " eskers" made by ground moraine released by melting glaciers.
History
Prehistory
The history of life in the area of the park begins at the end of the latest ice age. Large climate changes allowed reindeer to spread widely across Scandinavia, only to be forced back to a much smaller area — including the Rondane mountain area — only some hundreds of years later. Archaeologists have found that the forest quickly grew at high altitudes; birch trees found at 1030 metres (3379 ft) were 8500 years old.
On the mountain plateaux, there is evidence that nomadic hunter-gatherers lived off reindeer. Large traps used to catch reindeer can be found at Gravhø and Bløyvangen and are also spread all throughout the park. These are constructed from stone to make holes or large fenced-in areas into which reindeer could be tricked or led.
In conjunction with these large traps, there are also small arched stone walls which are believed to have been used as hiding places for archers waiting for prey. Various dating methods have suggested that the earliest traps may be as old as 3500 years. Most of the findings, including remains of houses, date back to the years between 500 and 700 CE. It is thus known with confidence that the large traps and accompanying walls were used from the 6th century until the onset of the Black Death in the 14th century.
Establishment
After nearly a decade of planning, Rondane was established as the first Norwegian National Park on December 21, 1962. It was first established as a nature protection area, but was later named a national park. The main reasons for protecting the park were "to safeguard the natural environment with its native plants, animal life, and cultural heritage and also to secure the environment as a recreational area for future generations".
Legal efforts to protect nature in Norway date from 1954, when the Nature protection law was passed. Soon after, in 1955, community meetings were held in the municipalities close to Rondane, and a commission was founded. Norman Heitkøtter was president of the commission, and made it possible by Royal resolution to establish Rondane National Park. At its establishment, the park covered an area of 580 km² (224 sq mi).
Although Rondane was the first national park in Norway, many others followed. The parks are maintained by the Norwegian Directorate for Nature Management.
2003 expansion
As a special measure for the protection of the wild reindeer, the park was significantly enlarged in 2003, its area increasing from 580 to 963 km² (224 to 372 mi²). The park was enlarged mainly to the north-west, and slightly in the east and south. In addition, areas with lesser protection (landscape protection as well as nature protection areas) were established in connection with the park. A new national park, Dovre National Park, between Rondane and Dovrefjell-Sunndalsfjella National Park was also opened. Following the expansion, it is now only approximately 1 kilometre from the northern border of Rondane to the southern border of Dovre National Park, and large sections of adjacent mountain areas are protected by the three parks.
Geology
The bedrock in Rondane comes from a shallow sea floor, created 500 to 600 million years ago. From this, changes in the Earth's crust created a mountain area of metamorphic rock and quartz. There are no fossils found in Rondane today and so it is thought the sea where the rock came from contained no animal life.
The present landscape was mostly formed by the last ice age, nine to ten thousand years ago. At that time large quantities of ice were formed, and it is believed that the ice melted gradually in shifting cycles of melting and ice accumulation. The ice melting must have been rapid when it happened, digging deep river valleys.
Rondane contains a few small canyons which were created by the rapid ice melting, most prominently Jutulhogget and Vesle-Ula.
Biology
Rondane is one of the few places in Scandinavia and Europe where wild reindeer (as opposed to the domestic breed) are found. The Directorate for Nature Management regards Rondane as "especially important as a life supporting area for the native reindeer". It is estimated that approximately 2000 to 4000 reindeer live in Rondane and the nearby Dovre area. To protect the reindeer population in their core area, during the last ten years hiking trails have been moved. The park was also enlarged in 2003 to provide increased protection for the reindeer.
Other large game, including roe deer and elk (moose) are commonplace along the rims of the park and occasionally musk ox from Dovre can be seen. Wolverines and a small population of bears are also present, while wolves are rare.
The reindeer largely rely on the lichen and reindeer moss that grow together with heather and hardy grass on the quite arid and nutrient-poor stony plateaus. The lichen provide food for the reindeer, but also fertilize the earth, making it possible for less hardy plants to grow, and mice and lemmings to feed. One of the flower species to survive very well is the Glacier Crowfoot, found up to 1700 metres (5580 ft).
Tourism
Visitors to Rondane are free to hike and camp in all areas of the park, except in the immediate vicinity of cabins. Apart from being closed for motor traffic, not many special regulations apply. Fishing and hunting is available to licensees.
The Norwegian Mountain Touring Association (DNT) is an association that owns and manages a network of mountain cabins in the service of hikers. In Rondane, there is a central cabin by the southern end of the lake Rondvatnet, Rondvassbu. There is also Dørålseter and Bjørnhollia at the northern and eastern rims of the park. All three cabins are manned, and provide food and limited accommodation (possible to book beforehand). There are also un-manned cabins in the Park, like Eldåbu where a key is needed.
DNT also mark trails in the Park, with red Ts that are easy to spot. The T-trails lead the way cabin-to-cabin, as well as marking the path to some of the peaks close to Rondvatnet. Recently, some of the trails have moved slightly to avoid the core areas of the wild reindeer.
The service cabins are also open during the winter season, although they are sometimes only self-serviced off season. Ski trails are marked and sometimes prepared, either by DNT or some of the hotels and skiing resorts close to the park.
Rondane in literature
The landscapes of Rondane have inspired many Norwegian writers. Probably the best-known work is Peer Gynt (1867), a play by Henrik Ibsen, which is partly set in Rondane:
- Act 2, Scene lV
- (Among the Ronde mountains. Sunset. Shining snowpeaks all around.
- Peer Gynt enters, dizzy and bewildered.)
- Peer
- Tower over tower arises!
Hei, what a glittering gate!
Stand! Will you stand! It's drifting
further and further away!
...
- (Among the Ronde mountains. Sunset. Shining snowpeaks all around.
With this, Ibsen wrote Rondane into one of the best of dramas of the 19th century and made Rondane a symbol for the natural beauty of Norway.
Peter Christen Asbjørnsen, writer and gatherer of Norwegian folk tales in the mid-19th century, collected many stories connected with Rondane, including Peer Gynt, the story that inspired Ibsen. A third writer who set one of his famous works in Rondane is the poet Aasmund Olavsson Vinje with his poem No ser eg atter slike Fjell og Dalar.