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Pekulney Range
The Pekulney Range (russian: Пэкульней) is a range of mountains in far North-eastern Russia. Administratively the range is part of the Chukotka Autonomous Okrug of the Russian Federation. The area of the range is desolate and uninhabited.Пэкульней , in 30 vols. / Ch. ed. A.M. Prokhorov . - 3rd ed. - M, 1969 The term "Pekulney" means "knife mountain" in the . Geography The Pekulney Range is a southern prolongation of the |
Google Earth
Google Earth is a computer program that renders a 3D computer graphics, 3D representation of Earth based primarily on satellite imagery. The program maps the Earth by superimposition, superimposing satellite images, aerial photography, and geographic information system, GIS data onto a 3D globe, allowing users to see cities and landscapes from various angles. Users can explore the globe by entering addresses and coordinates, or by using a Computer keyboard, keyboard or computer mouse, mouse. The program can also be downloaded on a smartphone or Tablet computer, tablet, using a touch screen or stylus to navigate. Users may use the program to add their own data using Keyhole Markup Language and upload them through various sources, such as forums or blogs. Google Earth is able to show various kinds of images overlaid on the surface of the earth and is also a Web Map Service client. In 2019, Google has revealed that Google Earth now covers more than 97 percent of the world, and has c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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] |
Mountain Tundra
Alpine tundra is a type of natural region or biome that does not contain trees because it is at high elevation, with an associated harsh climate. As the latitude of a location approaches the poles, the threshold elevation for alpine tundra gets lower until it reaches sea level, and alpine tundra merges with polar tundra. The high elevation causes an adverse climate, which is too cold and windy to support tree growth. Alpine tundra transitions to sub-alpine forests below the tree line; stunted forests occurring at the forest-tundra ecotone are known as ''Krummholz''. With increasing elevation it ends at the snow line where snow and ice persist through summer. Alpine tundra occurs in mountains worldwide. The flora of the alpine tundra is characterized by dwarf shrubs close to the ground. The cold climate of the alpine tundra is caused by adiabatic cooling of air, and is similar to polar climate. Geography Alpine tundra occurs at high enough altitude at any latitude. Portions ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dwarf Cedar
''Pinus sibirica'', or Siberian pine, in the family Pinaceae is a species of pine tree that occurs in Siberia from 58°E in the Ural Mountains east to 126°E in the Stanovoy Range in southern Sakha Republic, and from Igarka at 68°N in the lower Yenisei River, Yenisei valley, south to 45°N in central Mongolia. Description ''Pinus sibirica'' is a member of the Pinus classification, white pine group, ''Pinus'' subgenus ''Strobus'', and like all members of that group, the leaves ('needles') are in fascicles (bundles) of five, with a deciduous sheath. They are 5–10 cm long. Siberian pine conifer cone, cones are 5–9 cm long. The 9–12 mm long seeds have only a vestigial wing and are dispersed by spotted nutcrackers. Siberian pine is treated as a variety or subspecies of the very similar Swiss pine (''Pinus cembra'') by some botanists. It differs in having slightly larger cones, and needles with three resin canals instead of two in Swiss pine. Like other European ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Operational Navigation Chart C-7, 5th Edition
An operational definition specifies concrete, replicable procedures designed to represent a construct. In the words of American psychologist S.S. Stevens (1935), "An operation is the performance which we execute in order to make known a concept." For example, an operational definition of "fear" (the construct) often includes measurable physiologic responses that occur in response to a perceived threat. Thus, "fear" might be operationally defined as specified changes in heart rate, galvanic skin response, pupil dilation, and blood pressure. Overview An operational definition is designed to model or represent a concept or theoretical definition, also known as a construct. Scientists should describe the operations (procedures, actions, or processes) that define the concept with enough specificity such that other investigators can replicate their research. Operational definitions are also used to define system states in terms of a specific, publicly accessible process of preparation ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Snow Field
A snow field, snowfield or neve is an accumulation of permanent snow and ice, typically found above the snow line, normally in mountainous and glacial terrain. Glaciers originate in snowfields. The lower end of a glacier is usually free from snow and névé in summer. In the upper end and above the upper boundary of a glacier, the snow field is an ice field An ice field (also spelled icefield) is a mass of interconnected valley glaciers (also called mountain glaciers or alpine glaciers) on a mountain mass with protruding rock ridges or summits. They are often found in the colder climates and highe ... covered with snow. The glacier upper boundary, where it emerges from under a snow field, is ill-defined because of gradual transition.Thomas Chrowder Chamberlin, Rollin D. Salisbury (1904) "Geology"p. 258 References Bodies of ice Landforms {{glaciology-stub it:Formazioni nevose perenni#Nevaio ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cirque Glacier
A cirque glacier is formed in a cirque, a bowl-shaped depression on the side of or near mountains. Snow and ice accumulation in corries often occurs as the result of avalanching from higher surrounding slopes. If a cirque glacier advances far enough, it may become a valley glacier. Additionally, if a valley glacier retreats enough that it is within the cirque, it becomes a cirque glacier again. In these depressions, snow persists through summer months, and becomes glacier ice. Snow may be situated on the leeward slope of a mountain, where it is sheltered from wind. Rock fall from above slopes also plays an important role in sheltering the snow and ice from sunlight. If enough rock falls onto the glacier, it may become a rock glacier. Randklufts may form beneath corrie glaciers as open space between the ice and the bedrock, where meltwater Meltwater is water released by the melting of snow or ice, including glacial ice, tabular icebergs and ice shelves over oceans. Meltwater ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Anadyr Lowland
The Anadyr Lowlands (russian: Ана́дырская ни́зменность) are a low alluvial plain located in the Chukotka Autonomous Okrug, Far Eastern Federal District, Russia. Geography The lowlands are crossed by the Anadyr River in the middle and the Velikaya in the south. They are bound by the Pekulney Range of the Chukotka Mountains to the northwest, west of which lie the Parapol-Belsky Lowlands (Парапольско-Бельская низменность) beyond which rise the Anadyr Highlands, and by the Rarytkin and Ukvushvuynen ranges of the Koryak Mountains to the south. The mouth of the Anadyr River flows into the Anadyr Gulf of the Bering Sea to the east. The harbor city of Anadyr is located by the mouth on the shore of Onemen Bay in the estuarine area of the river.Google Earth The lowlands are a flat, mostly marshy tundra plain with a maximum height of above sea level. The whole area is dotted with lakes, the largest of which is Lake Krasnoye.Ана́ ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tanyurer River
The Tanyurer (russian: Танюрер) is a river in Chukotka in Russia, a left tributary of the Anadyr. The length of the river is . The area of its drainage basin is . The whole basin of the Tanyurer and its tributaries belongs to the Chukotka Autonomous Okrug. Course It flows roughly southwards from the Pekulney Range of the Chukotka Mountains and passes through the sparsely populated areas of Chukotka. This river meets the Anadyr in the lower stretch of its course, being the last large tributary of the Anadyr.Танюрер, Great Soviet Encyclopedia in 30 vols. / Ch. ed. A.M. Prokhorov - 3rd ed. - M, 1969-1978. 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 drained into ... References External links Ice extent in the Tanyurer River Valley * ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Belaya River (Chukotka)
The Belaya (russian: Бе́лая, in its upper course Юрумкувеем ''Yurumkuveyem'') Great Soviet Encyclopedia is a south-flowing tributary of the Anadyr (river), Anadyr in the Chukotka Autonomous Okrug administrative region of Russia. Course The source of the Yurumkuveyem is in the northern Anadyr Mountains. Its main tributaries are the Bolshoy Pykarvaam, Chaavaam and Bolshaya Osinovaya from the left, and the Enmyvaam, which drains Lake Elgygytgyn, from the right. Its basin is and its length is (487 km from its furthest source, that of the Bolshoy Pykarvaam). Downstream from its confluence with the Enmyvaam it is named ''Belaya''. The Belaya flows through sparsely populated areas of Chukotka, flows southwards across the eastern edge of the Anadyr Highlands and the Pekulney Range, and joins with the Enmyvaam i ...[...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Osinov Range
Mikhail Svyatoslavovich Osinov (russian: Михаил Святославович Осинов; born 8 October 1975) is a Russian football coach and a former midfielder. He works as an assistant coach with FC Rostov. Career Born in Arti, Sverdlovsk Oblast, Mikhail Osinov started his professional career at the Gornyak Kachkanar in 1993. In 1994-1995, he played for Uralets Nizhny Tagil. Next year, Osinov was invited to Uralmash, the biggest club in the region. After two seasons in Yekaterinburg, Osinov moved to Israel for a spell with Maccabi Tel Aviv. He later returned to the Russian Top Division side Rotor Volgograd. In 2001, Osinov was transferred to FC Rostov and stayed there for 9 years, suffering a relegation and helping the ''yellow-blues'' to return to the Premier League. He also holds the club record for league appearances with 239 games. In 2010, he returned to Yekaterinburg to play in the Russian First Division. In 2011, Osinov went to a lower league joining MITOS No ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
