Kalevalsky National Park
Topography
The territory of the park is on the southeast of the Baltic Shield, which contains the oldest rocks in Europe (3 billion year-ol Precambrian crystalline granites, gneisses, and similar), covered by a very young layer (20–30 meters) of glacial deposits. During the recent Pleistocene glaciation, heavy continental ice sheets scoured and depressed the region, leaving as they melted a flat landscape of lakes and rivers. The western portion of the park is mostly flat (and generally waterlogged) forest, while the eastern section has more hills and ridges; the altitude in the park ranges between 105 meters and 278 meters. Due to the valuable mineral profile, mining is the main industry in the area, with logging also important.
The park records 250 streams, and 400 lakes. Only about 100 of the lakes has an area greater than 10 hectares. The cover of the park is 85% forest, 9% marsh, and 6% lakes and rivers. The wetland systems are complex, and peat underlies much of the territory, in parts reaching a depth in some bogs of 6 meters. The forest are mostly pine, with about 10% spruce, and some small stands of birch and aspen on the sites of former farms.
Climate
The climate of Kalevalsky is Subarctic climate, without dry season (Köppen climate classification Subarctic climate (Dfc)). This climate is characterized by mild summers (only 1–3 months above 10 °C (50.0 °F)) and cold, snowy winters (coldest month below −3 °C (26.6 °F)). The number of days with snow cover is 170-180; the number of frost-free days is 80–95 days.
Kostomuksha, Republic of Karelia, Russia | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
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Ecoregion
The terrestrial ecoregion of Kalevansky is Scandinavian and Russian taiga (WWF ID#608), a region characterized by coniferous forests taiga. The freshwater ecoregion is classified as "Barents Sea Drainages" (FEOW ID#407), characterized by migratory species, low levels of endemism, and high numbers of species introduced by humans. FEOW notes that "The fish fauna is formed from immigrants of Atlantic and Siberian origins with only a weak assemblage of primary freshwater European species; thus, a "mixed" nature of the fish fauna is its main distinguishing feature".
See also
References
- ^ "Kalevalsky National Park". PA Russia. Retrieved December 30, 2015.
- ^ "Kalevalsky National Park". Ministry of Natural Resources of the Russian Federation. Retrieved December 30, 2015.
- ^ "Ecology of Karelia". petsru.ru. Retrieved December 31, 2015.
- ^ "Kalevalsky National Park". Voinitsa.ru. Retrieved December 31, 2015.
- ^ Kottek, M.; Grieser, J.; Beck, C.; Rudolf, B.; Rubel, F. (2006). "World Map of Koppen-Geiger Climate Classification Updated" (PDF). Gebrüder Borntraeger 2006. Retrieved September 14, 2019.
- ^ "Dataset - Koppen climate classifications". World Bank. Retrieved September 14, 2019.
- ^ "Scandinavian and Russian taiga". Encyclopedia of the Earth. Archived from the original on March 4, 2016. Retrieved December 31, 2015.
- ^ "Barents Sea Drainages". Freshwater Ecoregions of the World (FEOW). Retrieved December 31, 2015.
External links
- The Green Belt of Fennoscandia
- Republic of Karelia - Official Site Regarding Kalevalsky
- Map of Kalevalsky National Park (Official Park Site)
- Photo Gallery of Kalevalsky Development (European Commission)
- Official Kalevalsky National Park Twitter page
- Aerial video of Kalevalsky National Park
- Green Belt of Fennoscandia