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United Nations Environment Programme | ![]() |
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| World Conservation Monitoring Centre | ||||||||||
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World
Heritage Sites
VOLCANOES OF KAMCHATKA - RUSSIAN FEDERATION Brief description: One of the last pristine wilderness areas and most active volcanic regions in the world, with a high density and diversity of volcanoes and related features. The seven areas within the designation include most of the volcanic features of the Pacific Ring of Fire. The interplay of active high volcanoes and glaciers creates a landscape of dynamic beauty. The sites contain great species diversity, including the world's greatest known variety of salmonid fish and notable concentrations of sea otter, brown bear and Steller's sea eagle.COUNTRY Russian Federation NAME Volcanoes of Kamchatka IUCN MANAGEMENT CATEGORY BIOGEOGRAPHICAL PROVINCE Kamchatkan (2.7.5) GEOGRAPHICAL LOCATION The Kamchatka Peninsula is in the Russian Far East between the Sea of Okhotsk and the north Pacific Ocean. Klyuchevskoy Zakaznik is in the central valley (55°55'N / 160°35'E). Bystrinskiy Zakaznik is in a major range west of the centre (56°00'N / 158°30'E). The other areas are on the mountainous shores of the Pacific Ocean: Kronotskiy Zapovednik (54°40'N / 161°00'E), Nalychevo Zakaznik (53°30'N / 159°00'E), South Kamchatka Zakaznik & South Kamchatka State Zakaznik (52°00'N / 157°50'E) and in the south-west, South Tundra Zakaznik (52°50'N / 156°50'E). DATE AND HISTORY OF ESTABLISHMENT
AREA The Volcanoes of Kamchatka sites comprise: 4,378,115ha (MEPNR,1995) Bystrinskiy Zakaznik
1,500,000ha (1,330,000ha*) (*UNDP, 2001; Newell et al. 2001) LAND TENURE Federal, under the jurisdiction of the Ministry of Natural Resources (MEPNR) since 2000, with some long-term lease concessions to tourist companies. Kluchevskoy Nature Park is under both regional and federal jurisdictions as the land belongs to the State Forest Fund (Menshikov et al.,2000). ALTITUDE From sea level to 4,835m (Klyuchevskoy), 3,607m (Ichinskiy) and 3,528m (Kronotskiy). PHYSICAL FEATURES The 1200km-long Kamchatka peninsula is almost an island running north-south between the north Pacific and the sea of Okhotsk. Its southern half is formed mainly by two parallel mountain ranges The western, Sredinniy range in the west centre of the island, is of dormant shield and strato-volcanoes of which Ichinskiy (still active) is by far the highest. The eastern Vostochniy range which parallels the sea with nearly 30 young volcanoes, has the greatest concentration of active vulcanism in Eurasia. Between the ranges is the wide Kamchatka river valley out of which, to the north of the eastern range, rises the highest group, the Klyuchevskaya range. CLIMATE The peninsula being all but surrounded by sea has a moist cool maritime climate moderated by the ocean. Central Kamchatka, enclosed between the two mountain ranges, has a climate similar to the continent, and is snow-covered from October to May. On the west coast, temperatures are lowered by the cold Sea of Okhotsk. The climate is windy, often foggy and subject to very heavy snowstorms. At sea level, the mean temperature in July is 12°C but can reach 20°C; the mean temperature range in January is -4° to -10°C. The central valley becomes both warmer and colder than this. The rainfall is less than 400mm in the centre of the peninsula, nearly 1000mm along the western coast and nearly 2500mm in the southeast which is in the path of monsoonal rains (Borodin, 1983). VEGETATION The
moist climate and rich volcanic soils have produced a thick vegetation, very
lush in the lowlands. With little human exploitation, the vegetation in the
reserves is in largely pristine condition. It extends from extensive coastal
wetlands and meadows of tall grass, with alluvial riparian forests of Siberian
and Komarov poplar Populus suaveolens and P.komarov, aspen P.
tremuloides, alder Alnus kamschatica and willows Salix
sachalinense and Chosenia macrolepis; through maritime taiga of
Kamchatcan and Cayander larch Larix kamtschatica, and L. cayanderi,
ayan and yeddo spruce Picea ajarensis, P. jezoensis and white
birch Betula kamchatica; then peat wetland covered with crowberry
Empertum nigrum, to very extensive higher level forests of stone birch Betula
ermani which is the dominant tree of the peninsula, interspersed with
meadows. Above these are a zone of elfin woodland of Korean pine Pinus
koraiensis and 'cedar', dwarf mountain pine Pinus pumila, mountain
ash Sorbus scoparius, and sub-alpine meadows, scrub and mountain
tundra, the degree of the freeze-thaw cycle determining the zoning of higher
vegetation belts. FAUNA The
terrestrial fauna is low in diversity, but high in subspecific endemism. In
this, the Kamchatka Peninsula resembles an island. But some species are found
in great abundance, including over 15,000 Kamchatcan brown bears Ursus
arctos piscator, Arctic ground squirrel, Ochotona hyperborea, sable Martes
zibellina, Kamchatcan wolverine Gulo gulo albus (VU),
thousands of sea otters Enhidra lutris lutris (EN), 1,500 Kamchatcan
reindeer Rangifer tarandus phylarchus (known as northern deer) and over
10,000 Kamchatcan snow sheep Ovis nivicola nivicola. There are no
reptiles and only one species of amphibian, Siberian salamander, Hynobius
kayserlingii. CULTURAL HERITAGE The oldest Paleolithic settlement in the region is 21,000 years old. The Kamchatka Peninsula became part of Russia in 1699 and the first description of Kamchatka was given in 1742 by the explorer S.P. Krashenninnikov. At the beginning of the 18th century, the Itel’meni people settled in the central and southern parts of Kamchatka Peninsula, depending on fishing. Western Kamchatka and the Bystrinsky region were settled by the Eveni people, dependent on reindeer herding. There are also some Koryak people from the north, also reindeer herders. These indigenous populations were collectivised in Soviet times and had declined to 3,000 by 1995. Traditional economic activity is prohibited or limited to a few non-intensive forms such as reindeer raising in Bystrinsky Natural Park and extremely limited winter hunting of fur animals in three parks. Recently, traditional land use areas have been zoned for permanent settlements in northern part of the South Kamchatka Nature Park and in the Bystrinsky Nature Park. LOCAL HUMAN POPULATION Until 1992 the peninsula was a closed military zone around the home base of the Russian Pacific submarine and main fishing fleets near the capital Petropavlovsk-Kamchatskiy. This is the major city on the peninsula, with most of the region’s population. Almost the entire heritage area is uninhabited, except for protected area staff and in some parts of the South Kamchatka and Bystrinskiy Nature Parks, used by small numbers of Itel’meni and Eveni. This isolation, combined with few roads and settlements, has preserved much of the wilderness. VISITORS AND VISITOR FACILITIES Approximately 15,000 tourists visited Kamchatka in 1995, 4,000 of them foreign. Kronotskiy Nature Park is the only site in Russia with large geysers, enhancing its tourist potential. Approximately 2,000 tourists visit the Valley of the Geysers each year where a helipad and board-walk have been built and some measures taken to protect it from overuse by tourists (Krever,1994). There are ecological education centres in both Kronotskiy Reserve and Nalychevo Park. Helicopter access to tourist cabins within Nalychevo and Southern Kamchatka Nature Reserves is available. Between 1993 and 1999 the Klyuchevskaya group averaged about 250-300 visitors a summer, 100 being foreigners, but it does not yet cater for many tourists. Projects to promote eco-tourism are now underway, partly to supplement reduced government funding. The reserves are normally reached by helicopter. SCIENTIFIC RESEARCH AND FACILITIES The Kamchatka Institute of Ecology and Nature Use and the Institute of Volcanic Geology and Geochemistry of the Far Eastern Branch of the Russian Academy of Sciences are the main bodies conducting research in the territory. Kronotskiy Zapovednik has academic staff who pursue research with these two institutions (MEPNR, 1995). The Klyuchevskaya range has been monitored for 68 years and been the subject of much research: 16 previously unknown minerals have been discovered there. A network of seismic stations and geological monitoring sites is located within the boundaries of several protected areas, including the Kluchevskoy volcanology station. The Kamchatkan Volcanic Eruption Response Team in Petropavlovsk has since 1972 constantly monitored the condition of volcanoes in cooperation with the Alaska Volcano Observatory. Many other studies have been made in the territory and in 2001 a large field symposium was held on plants and vulcanism, a subject for which the area is ideally suited. CONSERVATION VALUE The heritage areas cover one of the last largely unexploited and relatively pristine wildernesses in the world, and also one of its most active volcanic zones. They include a great number of unpolluted river systems with a large number of endemic species and subspecies of both plants and animals, including globally important spawning grounds for the world’s greatest diversity of salmonid fish and a variety of wetlands exceptionally attractive to migratory birds. The continuing tectonic and volcanic activity constantly creates new areas for pioneer settlement by plants and animals. As a result, a range of different successional biological communities co-exist, developing in relative isolation. The only freshwater salmon species in Asia, in Kronotskiye Lake, may be the result of these processes and the wide variety of organisms living in the hot springs are another unusual feature. CONSERVATION MANAGEMENT Protected areas were initially established in many places to protect dwindling numbers of animals; later to preserve a range of the Peninsula's most important natural areas.The Kronotskiy National Reserve was originally founded for the strict protection of its resources. The South Kamchatka State Nature Sanctuary was founded to preserve and breed species for hunting. Nalychevo Nature Park combines the conservation of freshwater wetlands, recreation and education. Bystrinskiy Nature Park was to combine conservation with traditional sustainable uses. Kronotskiy and South Kamchatka State Reserves are managed by the Kronotskiy Zapovednik Administration. The Kamchatka Regional Board of Nature Parks, a non-profit institution, manages the Klyuchevskoy, Bystrinskiy, Nalychevo and South Kamchatka Nature Reserves for the Kamchatka regional adminstration; the Federal Forest Administration manages the Southwest Tundra Park. Management is based on the Russian Federation Law 'On Strict Nature Reserves' of 1995, Kamchatka Oblast Law 'On Strict Nature Reserves' of 1997, revised 1999, and the Klyuchevskoy Nature Park statute of 1999. MANAGEMENT CONSTRAINTS Over the 12 years since the end of the Union, Federal funding has decreased by 90% with drastic consequences for the parks. There are as a result two opposing concepts for the future development of Kamchatka: expanded extraction of minerals (largely on land traditionally held by the native people) to help finance the regional administration, and activities based on protecting the environment which should sustain native populations and create sustainable tourism. When the National Committee for Environmental Protection was abolished in 2000, environmental issues became the responsibility of the Regional Committees on Natural Resources, and the mining interests hostile to conservation in Kamchatka gained strength (Murashko, 2001). The southern boundary of the Bystrinskiy Nature Park has already been revised 50km inwards to permit gold mining on its edge and there is pressure for nickel mining within the Park. The frequent fires in this park, a proposed new road which would expose the area to poaching and the granting by local authorities of 12 out of 24 hunting leases to business interests from outside the region cannot be monitored since the Park has no staff (IUCN,2001). Logging, and oil and gas extraction in the Sea of Okhotsk near the coast have also started and a gas pipeline with road to Petropavlovsk is projected, crossing 20 salmon rivers. Geothermal exploitation is also developing at Nizhnekoshelevsky in the South Kamchatka Nature Park and State Nature Sanctuary, an area earmarked for scientific work and regional monitoring. Any of these industrial activities might pollute salmon spawning grounds and begin to degrade the pristine wilderness. STAFF The Nature Parks Board has a staff of 18 with a Director based in Petropavlovsk; each Park has an allocation of 5 field staff, but for Bystrinskiy for example the Director has only two staff for an area of 13,300 square kilometers. Federal areas have a Director and about 40 office and field staff. BUDGET The Kamchatka Regional administration finances the Board of Nature Parks. In 2000 this totalled Rub.585,000 (US$21,000), but there were no funds for the maintenance and development of the Klyuchevskoy extension. In 2000, 20% of the revenue for Kronotskiy and South Kamchatka Reserves came from helicopter tourism. In 2001 the GEF proposed funding for the first stage of two projects: to promote sustainable conservation of biodiversity in four protected areas and to improve the development and management of salmonid fish in four western watersheds for a first stage total cost to GEF of US$2,333,700, and, with co-financing, of US$5,324,0270. The whole 7-year project could cost US$13,175,700 from all sources (UNDP, 2001). ADDRESSES Ministry for Natural Resources of the Russian Federation, 4/6, Gruzinskaya Ul., Moscow, 123812. Kamchatka Institute of Ecology and Nature Use, Prospekt Rybakov,19A, Petropavlovsk 683040. Kamchatka Board of Nature Parks . 29/1, Karl Marx Avenue, Petropavlovsk-Kamchatskiy 693006. Kronotskiy Zapovednik Administration, Ul.Ryabikova 48, Elizovo 684010, Kamchatka. Forest Management of the Kamchatka Region Administration, Lenin Sq. 1, Petropavlovsk 683040. REFERENCES Borodin, A. & Syroechkovski, E. (1983). Zapovedniki SSSR. Moscow. Lesnaya Promyshlennost Publishing house. 249 pp. Gyppenreiter, V. & Perkins, R. (1989). Kamchatka: Land of Fire and Ice. IUCN (2001). Report on the State of Conservation of Natural and Mixed Sites Inscribed on the World Heritage List and the List of World Heritage in Danger. Gland, Switzerland Krever, V. et al. (1994). Conserving Russia's Biological Diversity: An Analytical Framework and Initial Investment Portfolio. WWF, Washington, DC. 207pp. Kronotsky Biosphere Reserve. (1984). Data sheet for UNESCO-MAB nomination. 7pp. Menshikov, V., Efimenko, A. & Nikiforov, V. (2000). Nomination. Nature Park Kluchevskoy for Inclusion in UNESCO World Heritage List. For the UNESCO World Heritage Committee. 22pp.+ Appendices 28pp. Ministry of Environmental Protection and Natural Resources of Russia (MEPNR) (1995). Nomination of the Volcanoes of Kamchatka for Inclusion in the World Heritage List. 28 pp. Murashko, O. (2001). Disturbing news from Kamchatka. Indigenous Peoples' World. Living Arctic, 4. Newell, J.,Chernyagina,O.,Zykov,V.,Lazarev,G.,Mosolov,V. & Rassokhina, L. (2001). Saving Russia's Far Eastern Taiga: Deforestation, Protected Areas and Forest 'Hotspots'. V: Kamchatka Region. 22pp Newell, J. & Wilson, E. (1996). The Russian Far East. Friends of Earth - Japan. Tokyo. 197 pp. Ponomareva,V. et al. (n.d.). Eruptive History of Kamchatka Volcanoes. Institute of Volcanic Geology & Geochemistry, Petropavlovsk-Kamchatskiy. 3pp. Simkin, T. & Seibert, L. (1994). Volcanoes of the World. Geoscience Press, Tucson, AZ, U.S.A. UNDP (2001). Demonstrating Sustainable Conservation of Biological Diversity in Four Protected Areas in Russia's Kamchatka Oblast. GEF, Washington, U.S.A. 75pp. Wilson, M. & Halupka, K. (1995). Anadromous fish as a keystone species in vertebrate communities. Conservation Biology 9(3): 489-497. Wilson, M., Gende, S. & Marston, B. (1998). Fishes and the forest. Bioscience. 48(6): 455-462. DATE November 1996. Updated 1/2000, 4/2001, November 2002. |
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