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Moma Natural Park
Moma Natural Park or Moma Nature Park (russian: Момский природный парк, ''Momsky Pryrodny Park''; sah, Аан Айылгы, ''Aan Aiylgy'') is a protected area of the Momsko-Chersk Region of Yakutia in the upper part of the Moma River basin. Administratively the park is a part of the Moma District, Sakha Republic, Far Eastern Russia. The nearest city is Khonuu, served by Moma Airport, and the nearest village Sasyr. Attractions The park includes part of the mostly mountainous area of the Ulakhan-Chistay Range, featuring pristine ridges and lakes of environmental and aesthetic value. Visitors may find a whole array of educational and recreational purposes in the area. Some of the main features are: * Mount Pobeda (), rising in the Buordakh Massif, is the highest point of the Ulakhan-Chistay, as well as of the Chersky mountain system. Climbing routes of varying difficulty are marked —up to category 5A. *Moma River valley, featuring the extinct cinder cone vo ...
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Sakha Republic
Sakha, officially the Republic of Sakha (Yakutia),, is the largest republic of Russia, located in the Russian Far East, along the Arctic Ocean, with a population of roughly 1 million. Sakha comprises half of the area of its governing Far Eastern Federal District, and is the world's largest country subdivision, covering over 3,083,523 square kilometers (1,190,555 sq mi). ''Sakha'' following regular sound changes in the course of development of the Yakut language) as the Evenk and Yukaghir exonyms for the Yakuts. It is pronounced as ''Haka'' by the Dolgans, whose language is either a dialect or a close relative of the Yakut language.Victor P. Krivonogov, "The Dolgans’Ethnic Identity and Language Processes." ''Journal of Siberian Federal University'', Humanities & Social Sciences 6 (2013 6) 870–888. Geography * ''Borders'': ** ''internal'': Chukotka Autonomous Okrug (660 km)(E), Magadan Oblast (1520 km)(E/SE), Khabarovsk Krai (2130 km)(SE), Amur Oblast (S ...
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Climbing Route
A climbing route is a path by which a climber reaches the top of a mountain, rock, or ice wall. Routes can vary dramatically in difficulty and grade; once committed to that ascent, it can sometimes be difficult to stop or return. Choice of route can be critically important. Guidebooks, if available, are helpful in providing detailed diagrams and photographs of routes. In the earliest days of hillwalking and mountaineering, climbers got to the top by whatever means got them there. Little information about how they did it is available. During the 19th century, as explorers of the Alps tried ever harder summits, it became clear that choosing an eastern face over a southwestern ridge could spell the difference between success or failure. One example was the first ascent of the Matterhorn, which had been repeatedly and unsuccessfully attempted via the southern side. The strata there tended to slope down and away while the rocks of the northeastern ridge (the one closest to Ze ...
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Protected Areas Of The Russian Far East
Protection is any measure taken to guard a thing against damage caused by outside forces. Protection can be provided to physical objects, including organisms, to systems, and to intangible things like civil and political rights. Although the mechanisms for providing protection vary widely, the basic meaning of the term remains the same. This is illustrated by an explanation found in a manual on electrical wiring: Some kind of protection is a characteristic of all life, as living things have evolved at least some protective mechanisms to counter damaging environmental phenomena, such as ultraviolet light. Biological membranes such as bark (botany), bark on trees and skin on animals offer protection from various threats, with skin playing a key role in protecting organisms against pathogens and excessive water loss. Additional structures like Scale (anatomy), scales and hair offer further protection from the elements and from predators, with some animals having features such ...
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East Siberian Mountains
The East Siberian Mountains or East Siberian Highlands ( rus, Восточно-Сибирское нагорье) are one of the largest mountain systems of the Russian Federation. They are located between the Central Yakutian Lowland and the Bering Strait in the Far Eastern Federal District and Northeast Siberia. The whole area of the East Siberian System has a very low population density. The territory of the mountain system is one of the Great Russian Regions. In some areas of the East Siberian Mountains, such as the Kisilyakh Range and the Oymyakon Plateau there are kigilyakhs, the rock formations that are highly valued in the culture of the Yakuts. Geography The East Siberian System consists of several separate sections of mountain ranges rising to the north and south of the Arctic Circle. The main group of ranges stretches for a distance of nearly from the Lena River valley to Cape Dezhnev, at the eastern end of the Chukotka Peninsula. Although it reaches a width of roughly ...
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Moma Range
The Moma Range (russian: Момский хребет, ''Momsky Khrebet''; sah, Муома сиһэ) is a range of mountains in far North-eastern Russia. Administratively the range is part of the Sakha Republic of the Russian Federation.''Momsky Khrebet'' / Great Soviet Encyclopedia; in 35 vols. / Ch. ed. Yu. S. Osipov. 2004—2017. The nearest town is Khonuu, served by Moma Airport. Etymology The name originated in the Evenki language, where "мома" means wood, timber or tree. Geography The Moma Range extends from NW to SE for almost southeast of the southern end of the Selennyakh Range and north of the Ulakhan-Chistay Range, the highest subrange of the Chersky Range system. It is parallel to the latter and separated from it by a wide intermontane basin, where the Moma River flows from the southeast and joins the Indigirka. Turning northwards, the Indigirka River cuts deeply across the range in its northwestern part. The Aby Lowland, part of the Yana-Indigirka Lowland, lies t ...
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Aufeis
Aufeis, ( ), (German for "ice on top") is a sheet-like mass of layered ice that forms from successive flows of ground or river water during freezing temperatures. This form of ice is also called overflow, icings, or the Russian term, naled. The term was first used in 1859 by Alexander von Middendorff following his observations of the phenomenon in northern Siberia. When thawed, ''aufeis'' leave footprints in the form of ''aufeis'' glades or, perhaps more accurately in tundra habitats, “''aufeis'' barrens, because of the near absence of vascular plants due to ice cover during much of the growing season. Etymology Aufeis literally translates from German to “on ice”. In 1859 the Baltic German scientist and explorer Alexander von Middendorff used this term to describe his observations of the phenomenon in northern Siberia.Ashton, George D. 1986. River and lake ice engineering. Chelsea, Michigan, USA: Book Crafters, Inc. It is also called ''overflow'', ''icings'', or the Russia ...
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Balagan-Tas
Balagan-Tas ( sah, Балаҕан Таас, russian: Балаган-Тас) is a cinder cone volcano in Russia. It was discovered by V.A. Zimin in 1939 and is one of the main features of the Moma Natural Park. Description This volcano is located in the Chersky Range, in the Moma River valley and is the only clearly Quaternary volcano in the area; the existence of another volcano active in the 1770s has not been confirmed. The supposed Indighirsky volcano may be actually Balagan-Tas. Its location has often been given incorrectly. Balagan-Tas is a volcanic cone with a crater of which little remains. It covers a surface area of . The crater is wide and deep, the cone is high and has a base diameter of . It may be considered a composite volcano. The volcano has generated three lava flows which cover a surface area of . They reach a thickness of . The volcano has erupted alkali basalts typical for rift zone volcanoes. Its composition has been characterized as hawaiite. Titanium d ...
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Cinder Cone
A cinder cone (or scoria cone) is a steep conical hill of loose pyroclastic fragments, such as volcanic clinkers, volcanic ash, or scoria that has been built around a volcanic vent. The pyroclastic fragments are formed by explosive eruptions or lava fountains from a single, typically cylindrical, vent. As the gas-charged lava is blown violently into the air, it breaks into small fragments that solidify and fall as either cinders, clinkers, or scoria around the vent to form a cone that often is symmetrical; with slopes between 30 and 40°; and a nearly circular ground plan. Most cinder cones have a bowl-shaped crater at the summit. Mechanics of eruption Cinder cones range in size from tens to hundreds of meters tall and often have a bowl-shaped crater at the summit. They are composed of loose pyroclastic material (cinder or scoria), which distinguishes them from ''spatter cones'', which are composed of agglomerated volcanic bombs. The pyroclastic material making up a cinder ...
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