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Kodar Mountains
The Kodar Mountains ( rus, Кода́р) are a mountain range in the Transbaikal region of Siberia, Russia. The name Kodar is derived from "khada", an Evenki word for rock. The range is part of the Udokan Ore Region that includes the Kalar and Udokan ranges.Udokan Ore Region / '':'' in 30 vols. / Ch. ed. A.M. Prokhorov. - 3rd ed. - M. Soviet Encyclopedia, 1969-1978. Geography The Kodar Mountains are part of the , which range from the northern tip of |
Russia
Russia (, , ), or the Russian Federation, is a List of transcontinental countries, transcontinental country spanning Eastern Europe and North Asia, Northern Asia. It is the List of countries and dependencies by area, largest country in the world, with its internationally recognised territory covering , and encompassing one-eighth of Earth's inhabitable landmass. Russia extends across Time in Russia, eleven time zones and shares Borders of Russia, land boundaries with fourteen countries, more than List of countries and territories by land borders, any other country but China. It is the List of countries and dependencies by population, world's ninth-most populous country and List of European countries by population, Europe's most populous country, with a population of 146 million people. The country's capital and List of cities and towns in Russia by population, largest city is Moscow, the List of European cities by population within city limits, largest city entirely within E ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Northern Muya Range
The Northern Muya Range (russian: Се́веро-Му́йский хребе́т, translit=Severo-Muyskiy khrebet) is a mountain range in Buryatia, Russia, part of the Stanovoy Highlands.Google Earth The Baikal Amur Mainline (BAM) railway traverses the southern end of the mountain range via the Severomuysky Tunnel. Geography The Northern Muya Range stretches from the valley of the Svetlaya river, a left tributary of the Upper Angara, in the southwest, to the valley of the Vitim in the northeast. The Upper Angara Depression lies to the northwest and the Muya-Kuanda Depression to the southeast. To the north it runs parallel with the Delyun-Uran Range just south of it, and to the south with the Muyakan Range. The highest summit of the range is a high mountain located in its extreme southwestern part. Peaks and ridges have sharp glacial shapes in the central sector of the range, while flat summits predominate on the periphery. In its southwestern part the Northern Muya Range is b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Snow Line
The climatic snow line is the boundary between a snow-covered and snow-free surface. The actual snow line may adjust seasonally, and be either significantly higher in elevation, or lower. The permanent snow line is the level above which snow will lie all year. Background Snow line is an umbrella term for different interpretations of the boundary between snow-covered surface and snow-free surface. The definitions of the snow line may have different temporal and spatial focus. In many regions the changing snow line reflect seasonal dynamics. The final height of the snow line in a mountain environment at the end of the melting season is subject to climatic variability, and therefore may be different from year to year. The snow line is measured using automatic cameras, aerial photographs, or satellite images. Because the snow line can be established without on-the-ground measurements, it can be measured in remote and difficult to access areas. Therefore, the snow line has become an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Siberian High
The Siberian High (also Siberian Anticyclone; russian: Азиатский антициклон (''Aziatsky antitsiklon'')) is a massive collection of cold dry air that accumulates in the northeastern part of Eurasia from September until April. It is usually centered on Lake Baikal.“The Siberian High and Climate Change over Middle to High-Latitude Asia” It reaches its greatest size and strength in the when the air temperature near the center of the is often lower than . The |
Subarctic Climate
The subarctic climate (also called subpolar climate, or boreal climate) is a climate with long, cold (often very cold) winters, and short, warm to cool summers. It is found on large landmasses, often away from the moderating effects of an ocean, generally at latitudes from 50° to 70°N, poleward of the humid continental climates. Subarctic or boreal climates are the source regions for the cold air that affects temperate latitudes to the south in winter. These climates represent Köppen climate classification ''Dfc'', ''Dwc'', ''Dsc'', ''Dfd'', ''Dwd'' and ''Dsd''. Description This type of climate offers some of the most extreme seasonal temperature variations found on the planet: in winter, temperatures can drop to below and in summer, the temperature may exceed . However, the summers are short; no more than three months of the year (but at least one month) must have a 24-hour average temperature of at least to fall into this category of climate, and the coldest month should ave ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Global And Planetary Change
''Global and Planetary Change'' is a monthly peer-reviewed scientific journal covering research into the earth sciences, particularly pertaining to changes in aspects thereof such as sea level and the chemical composition of the atmosphere. It has been published by Elsevier since it was established in 1989. The editors-in-chief are Alan Haywood, Jed Kaplan, Trude Storelvmo, Liviu Matenco, Zhengtang Guo, Maoyan Zhu, Fabienne Marret-Davies, Howard Falcon-Lang. According to the ''Journal Citation Reports'', the journal has a 2021 impact factor The impact factor (IF) or journal impact factor (JIF) of an academic journal is a scientometric index calculated by Clarivate that reflects the yearly mean number of citations of articles published in the last two years in a given journal, as i ... of 5.114. References External links * {{Official website, http://www.journals.elsevier.com/global-and-planetary-change/ Earth and atmospheric sciences journals Planetary science journals ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glacier
A glacier (; ) is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its Ablation#Glaciology, ablation over many years, often Century, centuries. It acquires distinguishing features, such as Crevasse, crevasses and Serac, seracs, as it slowly flows and deforms under stresses induced by its weight. As it moves, it abrades rock and debris from its substrate to create landforms such as cirques, moraines, or fjords. Although a glacier may flow into a body of water, it forms only on land and is distinct from the much thinner sea ice and lake ice that form on the surface of bodies of water. On Earth, 99% of glacial ice is contained within vast ice sheets (also known as "continental glaciers") in the polar regions, but glaciers may be found in mountain ranges on every continent other than the Australian mainland, including Oceania's high-latitude oceanic island countries such as New Zealand. Between lati ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Apsat River
The Apsat (russian: Апсат) is a river in the Kodar Range, on the eastern side of Lake Baikal in Siberia, Russia. It is a left tributary of the Chara (Lena basin). It is long, and has a drainage basin of . See also *List of rivers of Russia Russia can be divided into a European and an Asian part. The dividing line is generally considered to be the Ural Mountains. The European part is drained into the Arctic Ocean, Baltic Sea, Black Sea, and Caspian Sea. The Asian part is drain ... References Rivers of Zabaykalsky Krai Stanovoy Highlands {{Russia-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chara (river)
, image = 2000 Charoite 613.jpg , image_size = , image_caption = View of the river and piece of charoite , pushpin_map = Russia Sakha Republic , pushpin_map_size = , pushpin_map_caption= Location in the Sakha Republic, Russia , source1_location = Bolshoye Leprindo Lake , source1_coordinates = , source1_elevation = , mouth = Olyokma , mouth_coordinates = , mouth_elevation = , progression = Olyokma→ , subdivision_type1 = Country , subdivision_name1 = Yakutia, Russia , length = , discharge1_avg = , basin_size = The Chara (russian: Ча́ра; sah, Чаара, ''Çaara'') is a left tributary of the Olyokma in Eastern Siberia, Russia. It is long, and has a drainage basin of . Together with the Olyokma, river Chara gives its name to the Olyokma-Chara Plateau (Олёкмо-Чарское плоскогорье), located to the east of its east ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Olyokma-Chara Plateau
The Olyokma-Chara Plateau ( rus, Олёкмо-Чарское плоскогорье; sah, Өлүөхүмэ-Чаара хаптал хайалаах сир) is a mountainous area in the Sakha Republic and Irkutsk Oblast, Far Eastern Federal District, Russia.Google Earth A small section is in Kalarsky District, northernmost Zabaykalsky Krai. Charoite, a rare mineral, is found in the Murun Massif area of the plateau, rising between rivers Chara and Tokko. Geography The Olyokma-Chara Plateau is located to the south of the Lena, at the southwestern end of the Sakha Republic in Olyokminsky District, and the eastern end of Irkutsk Oblast, Bodaybinsky District. The plateau is bound by the Chara River, a left tributary of the Olyokma river to the west and the Olyokma, a left tributary of the Lena, to the east. The Tokko River, the largest tributary of the Chara, crosses the uplands from south to north. To the south rises the Udokan Range of the Stanovoy Highlands and to the north ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lena River
The Lena (russian: Ле́на, ; evn, Елюенэ, ''Eljune''; sah, Өлүөнэ, ''Ölüöne''; bua, Зүлхэ, ''Zülkhe''; mn, Зүлгэ, ''Zülge'') is the easternmost of the three great Siberian rivers that flow into the Arctic Ocean (the other two being the Ob and the Yenisey). Permafrost underlies most of the catchment, 77% of which is continuous. It is long, and has a drainage basin of . The Lena is the eleventh-longest river in the world, and the longest river entirely within Russia. Course Originating at an elevation of at its source in the Baikal Mountains south of the Central Siberian Plateau, west of Lake Baikal, the Lena flows northeast across the Lena-Angara Plateau, being joined by the Kirenga, Vitim and Olyokma. From Yakutsk it enters the Central Yakutian Lowland and flows north until joined by its right-hand tributary the Aldan and its most important left-hand tributary, the Vilyuy. After that, it bends westward and northward, flowing between the K ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chara River
, image = 2000 Charoite 613.jpg , image_size = , image_caption = View of the river and piece of charoite , pushpin_map = Russia Sakha Republic , pushpin_map_size = , pushpin_map_caption= Location in the Sakha Republic, Russia , source1_location = Bolshoye Leprindo Lake , source1_coordinates = , source1_elevation = , mouth = Olyokma , mouth_coordinates = , mouth_elevation = , progression = Olyokma→ , subdivision_type1 = Country , subdivision_name1 = Yakutia, Russia , length = , discharge1_avg = , basin_size = The Chara (russian: Ча́ра; sah, Чаара, ''Çaara'') is a left tributary of the Olyokma in Eastern Siberia, Russia. It is long, and has a drainage basin of . Together with the Olyokma, river Chara gives its name to the Olyokma-Chara Plateau (Олёкмо-Чарское плоскогорье), located to the east of its east ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
