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Lake Pielinen : ウィキペディア英語版
Pielinen

Pielinen is the fourth largest lake of Finland, with a drainage basin area of that is equally distributed between eastern Finland and Russia. The creation of the lake and its outlet is attributed to a post-glacial isostatic rebound, which resulted in uplift of the land. As is common in Finnish lakes, the water color of the lake is dark on account of the high proportion of bogs present in the catchment of the drainage basin that drains humic substances.〔〔
Pielinen Lake is in the northernmost part of Karelia, which is the land of the Karelian peoples, a Northern European area of historical significance not only for Finland, but also for Russia and Sweden. Apart from the lake, several attractions on the shores of the lake are the Koli National Park known for its scenic beauty in summer and the winter sports of skiing, the whitewater rafting centre at Ruunaa Hiking Center, the active centres of Lieksa and Nurmes.
==Geography==

The lake is located at an elevation of in the North Karelia region in eastern Finland. It has a water spread area of and a shore length of , and is bound within geographical coordinates of 62°54–63°33N and 29°07–30°14E. The maximum length is and the width varies from . The lake's drainage area of is equally distributed between Finland and Russia. The maximum depth of water in the lake is with a reported mean depth of . The water courses that drain into the lake are the Haapajarvi-Valtimojarvi and Saramojoki from its north-west direction, Viekinjoki River and Lieksanjoki River from the north-east side, and flows from the small drainage basin of the Juvanjoki River into the west. The lake has many islands such the Paalasmaa (27.2 km2), Kynsisaari (), Porosaari (), Toinensaari (), Hattusaari (), Koveronsaari () and Retusaari (). The lake drains, unregulated, southward through the Pielis River into the larger Saimaa Lake of the large Vuoksi watercourse, which is used for timber floating. The variation in water level is limited to ; water transport on the lake is thus substantial. The catchment of the lake is densely forested, particularly on its rugged western shore, which is capped by Koli hill. At (), the point is the highest mountain in the catchment.〔〔
The shores have a diverse landscape including barren lands, rock faces, exposed soils and beaches. Land use within the Finnish part of the catchment of the lake consists of mostly of forest, which takes up 56.6% of the total area of ; swamp accounts for another 27.2%; agricultural land takes 6.1%; with residential area and others using up 5.5%. The basin area is inhabited by 83,400 people (41,700 rural and 41,700 urban population). The two towns in the basin are Lieksa, at the northern tip of the lake, and Nurmes on the eastern shore, which have a population of 18,700 and 11,500 respectively. The Koli National Park forms the western shore of the lake.〔
The wooded vegetation is mainly made up of coniferous forests (''Pinus sylvestris'', ''Picea abies''), partly deciduous forests (''Betula sp.'') with the drainage basin categorized as belonging to the northern zone of conifers. The herbaceous vegetation in marsh areas consists of various grasses (''Poaceae''), sedge (''Carex sp.'') and moss (''Sphagnum sp.''). The agricultural crops grown in the area are barley, oat, grass and potato, which are mainly used for feeding domestic animals. It is, however, reported that agricultural use is on the decline. The primary industries in the basin are related to milk, meat and wood. The secondary industries in the basin consist of cardboard, sawed goods, milk products and rubber products.〔
The periphery of the lake has a large network of roads and, during winter when the lake freezes, an ice road is the short route from one bank to the other.〔
Road 73 passes through the Uimaharju on the southern side of the lake and goes through very scenic spots to the east end. The south end of the lake has a lock system at Pielisjoki, which connects to the Saimaa Lake.

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
ウィキペディアで「Pielinen」の詳細全文を読む



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