World Heritage Identification Number: 1234
World Heritage since: 2010
Category: Natural Heritage
WHE Type: Natural Landscapes & Geographic Features
Transboundary Heritage: No
Endangered Heritage: No
Country: 🇷🇺 Russian Federation
Continent: Europe
UNESCO World Region: Europe and North America
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Putorana Plateau: An Unspoiled Natural Haven in Northern Central Siberia
The Putorana Plateau, officially recognized as a UNESCO World Heritage Site since 2010, lies in the heart of the Putoransky State Nature Reserve, approximately 100 kilometers north of the Arctic Circle in northern Central Siberia. This remote and largely inaccessible region offers a unique opportunity to explore some of the most pristine and diverse ecosystems found anywhere on Earth.
More to come…UNESCO Description of the World Heritage Site
This site coincides with the area of the Putoransky State Nature Reserve, and is located in the central part of the Putorana Plateau in northern Central Siberia. It is situated about 100 km north of the Arctic Circle. The part of the plateau inscribed on the World Heritage List harbours a complete set of subarctic and arctic ecosystems in an isolated mountain range, including pristine taiga, forest tundra, tundra and arctic desert systems, as well as untouched cold-water lake and river systems. A major reindeer migration route crosses the property, which represents an exceptional, large-scale and increasingly rare natural phenomenon.
UNESCO Justification of the World Heritage Site
Criterion (vii): A vast and diverse landscape of striking natural beauty, the Putorana Plateau is pristine and not affected by human infrastructure. Its superlative natural features include an extensive area of layered basalt traps that has been dissected by dozens of deep canyons; countless cold water rivers and creeks with thousands of waterfalls; more than 25,000 lakes characterized by a fjord-like formation that is associated with a large variation in the relief. The immense arctic and boreal landscapes remain intact with carpets of lichens and forest that are unusual at such northern latitudes.
Criterion (ix): The property displays a comprehensive set of ecological and biological processes associated with its diverse arctic and subarctic ecosystems. Its bio-geographical location, on the border of the tundra and taiga biomes and at the transition between Western and Eastern Siberian floras, makes the property one of only a few centres of plant species richness in the Arctic. The combination of landscape diversity, remoteness, naturalness and degree of protection are extraordinary. In addition, the property may provide valuable evidence on the impacts of climate change to large-scale natural arctic ecosystems if proper monitoring and research take place.
Encyclopedia Record: Putorana Plateau
The Putorana Plateau or the Putorana Mountains is a mountainous area in Russia. It is a large massif or plateau crossed by mountain ranges. The nearest large settlement is Norilsk, where foreign travel is restricted. The city is served by Alykel Airport.Additional Site Details
Area: 1,887,251 hectares
Number of Components: 1
(ix) — Outstanding example representing ecological and biological processes
Coordinates: 69.0469444444 , 94.1580555556
IUCN World Heritage Outlook
The 2025 Conservation Outlook on Putorana Plateau reports the following assessment:
Source: International Union for Conservation of Nature (IUCN) · View assessment
World Heritage Research
Discover scientific research and academic studies that deepen our understanding of Putorana Plateau from its history and significance to its conservation, management, and contemporary challenges.
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Morphometric analysis of cirques in central Siberia's western Putorana Plateau: a proxy for palaeoclimate
A detailed morphometric analysis of 200 cirques on the western Putorana Plateau, central Siberia, reveals that the region experienced mountain glaciation during cold stages of the Late Pleistocene. The study found that these cirques, with mean dimensions of 936 m in length and 1000 m in width, exhibit near-circularity and a wider-than-deep form, indicating significant headwall erosion and a mature glacial landscape shaped by prolonged erosion. Reconstructed glaciers suggest a total ice volume of 10.6 km³, with equilibrium-line altitudes ranging from 593 to 1372 m above sea level (a.s.l.), median values of 818–826 m a.s.l., and summer temperatures of 0.3 to −0.4 °C. The research also estimated palaeoprecipitation values of 875–1036 mm per year, indicating sufficient moisture for cirque-style glaciation. These findings provide the first quantitative reconstruction of cirque glaciers in this region, offering new constraints on former glacier extent and palaeoclimatic conditions.
Oien, R. P., & Lee, E. (2026). Morphometric analysis of cirques in central Siberia’s western Putorana Plateau: a proxy for palaeoclimate. Boreas. Portico. https://doi.org/10.1111/bor.70086
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Labronema przhiboroi sp. nov. (Nematoda: Dorylaimida) from the Putorana Plateau (Eastern Siberia, Russia)
A new nematode species, Labronema przhiboroi sp. nov., has been discovered in the freshwater Lake Duluk on the Putorana Plateau in Eastern Siberia. This species belongs to the family Dorylaimidae and is distinguished from its closest relative, L. macrosoma, by its smaller body size, shorter spicules, and more pronounced cuticular ridges. The discovery contributes to the understanding of nematode biodiversity in this remote region. The research involved morphological analysis to differentiate the new species based on key anatomical features.
Tsalolikhin, S. Ya., & Tumanov, D. V. (2025). Labronema przhiboroi sp. nov. (Nematoda: Dorylaimida) from the Putorana Plateau (Eastern Siberia, Russia). Zoosystematica Rossica, 34(1), 36–40. https://doi.org/10.31610/zsr/2025.34.1.36
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Ecological and Geographical Structure and Dynamics of the Autumn Migration of Passerine Birds on the Putorana Plateau
Autumn migration of passerine birds on the Putorana Plateau follows distinct ecological and geographical patterns, with population density peaking during periods of cooler temperatures and no precipitation. The study, conducted over 16 years across eight sites covering 150,000 km², identified 42 species migrating along narrow forest-edge strips, primarily in southern or southwestern directions. Population densities ranged from 239 to 643 individuals/km², with the highest concentrations observed in the south of the plateau. Migration occurs in four well-defined waves, often synchronized by environmental conditions rather than species relationships. The majority of birds form monospecific or polyspecific flocks, with most species completing their migration in 20–26 days. Key species include the Arctic warbler, common redpoll, and little bunting, which dominate numerically.
Romanov, A. A. (2025). Ecological and Geographical Structure and Dynamics of the Autumn Migration of Passerine Birds on the Putorana Plateau. Contemporary Problems of Ecology, 18(2), 171–183. https://doi.org/10.1134/s1995425524700987
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Autumn migration of passerine (Passeriformes) on the putorana plateau
Autumn migration of passerine birds on the Putorana Plateau follows a distinct pattern characterized by four well-defined waves, with peak activity coinciding with temperature drops. The study, conducted across eight survey points, revealed that these birds migrate along narrow strips near large rivers or lakes, primarily in southern, southwestern, and western directions. Population density varies significantly, peaking at 608 individuals per km² during the most intense migration periods, with the highest densities observed in the south of the plateau. The Arctic Warbler, Common Redpoll, and Little Bunting dominate numerically, while species within the same genus or family typically migrate on different days. This research sheds light on the eco-geographical dynamics of passerine migration, highlighting the impact of environmental factors such as temperature on migration patterns.
Romanov, A. A. (2025). Autumn migration of passerine (Passeriformes) on the putorana plateau. Lomonosov Geography Journal, 80(№2, 2025), 72–83. https://doi.org/10.55959/msu0579-9414.5.80.2.6
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Landforms Recognized at the World Natural Heritage Sites (Siberia and the Russian Far East)
A comprehensive analysis of landforms within Russia's UNESCO World Heritage Sites reveals their exceptional geological, geomorphological, and aesthetic significance. The study highlights the unique features of the Volcanoes of Kamchatka, Lake Baikal, Putorana Plateau, and Lena Pillars National Park, including the Kluchevskoy Volcano, Uzon Volcano Caldera, Ayan fiords lake, and Russia's largest waterfalls. These sites are recognized for their outstanding natural values, contributing to global heritage conservation efforts. The research employs a detailed examination of these landforms, emphasizing their scientific and cultural importance.
Butorin, A. A., Trofimova, E. V., & Maksakovskiy, N. V. (2025). Landforms Recognized at the World Natural Heritage Sites (Siberia and the Russian Far East). Doklady Earth Sciences, 522(3). https://doi.org/10.1134/s1028334x25606662
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Ecological and Geographical Structure and Dynamics of Spring Migration of Passeriform Birds on the Putorana Plateau
Spring migration of passeriform birds on the Putorana Plateau follows distinct ecological and geographical patterns, characterized by asynchronous migratory waves with one dominant peak. Research spanning 1988–2007 identified 58 species migrating along river or lake shorelines, with population densities averaging 231 individuals/km². Migration timing varies significantly, from early arrivals like the horned lark (May 25–June 4) to late migrants such as the sand martin (June 7–16), with most species showing an 8-day interval between first appearances. The study highlights that migratory outbreaks coincide with low temperatures and precipitation, while closely related species exhibit varying synchronization in their migration peaks. This long-term analysis provides critical insights into the dynamics of avian spring migration in this UNESCO-listed region.
Romanov, A. A. (2025). Ecological and Geographical Structure and Dynamics of Spring Migration of Passeriform Birds on the Putorana Plateau. Contemporary Problems of Ecology, 18(5), 670–686. https://doi.org/10.1134/s1995425525700362
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Migrations of Passeriformes on the Putorana Plateau
The Putorana Plateau serves as a critical junction for passerine bird migrations, with distinct seasonal patterns and varying intensities. Spring migration occurs from late May to mid-June, lasting 8–17 days, while autumn migration spans late July to late August, lasting up to 31 days. Bird population density peaks in the south of the plateau (440 individuals/km²) and is lowest in the north (231 individuals/km²). Migration dynamics are wave-like, with bursts of activity influenced by temperature, showing higher intensity on colder days. Asynchronous migration patterns are observed among species and even within the same species, with spring migration synchronization varying annually from complete alignment to no overlap. The study employed route census methods on transects to analyze these migratory behaviors, revealing complex, temperature-dependent migration strategies.
Romanov, A. A. (2025). Migrations of Passeriformes on the Putorana Plateau. Vestnik of North-Eastern Federal University, 22(3), 7–22. https://doi.org/10.25587/2222-5404-2025-22-3-7-22
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