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Kyun-Tas Range
Kyun-Tas ( rus, Кюн-Тас; sah, Күн Таас) is a mountain range in the Sakha Republic, Far Eastern Federal District, Russia. The Kyun-Tas is one of the mountain areas of Yakutia where there are kigilyakh rock formations. Geography The Kyun-Tas is located northeast of Deputatsky, between the Selennyakh Range and the western end of the Polousny Range. It rises at the southern limit of the Yana-Indigirka Lowland, northwest of the Aby Lowland. It is a broad massif with mountains of middle height and smooth slopes. The main ridge stretches in a roughly southeast/northwest direction west of the eastern slopes of the Selennyakh Range for about .Google Earth Although the range is smaller, the highest summits of the Kyun-Tas are higher than those of the neighboring Polousny Range. The highest peak, located in the northern part, is high; there is another high peak at the southeastern end that is . Hydrography The long Nuchcha, a tributary of the Chondon, originates in ...
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Russia
Russia (, , ), or the Russian Federation, is a transcontinental country spanning Eastern Europe and Northern Asia. It is the largest country in the world, with its internationally recognised territory covering , and encompassing one-eighth of Earth's inhabitable landmass. Russia extends across eleven time zones and shares land boundaries with fourteen countries, more than any other country but China. It is the world's ninth-most populous country and Europe's most populous country, with a population of 146 million people. The country's capital and largest city is Moscow, the largest city entirely within Europe. Saint Petersburg is Russia's cultural centre and second-largest city. Other major urban areas include Novosibirsk, Yekaterinburg, Nizhny Novgorod, and Kazan. The East Slavs emerged as a recognisable group in Europe between the 3rd and 8th centuries CE. Kievan Rus' arose as a state in the 9th century, and in 988, it adopted Orthodox Christianity from the ...
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Rock Formation
A rock formation is an isolated, scenic, or spectacular surface rock outcrop. Rock formations are usually the result of weathering and erosion sculpting the existing rock. The term ''rock formation'' can also refer to specific sedimentary strata or other rock unit in stratigraphic and petrologic studies. A rock structure can be created in any rock type or combination: * Igneous rocks are created when molten rock cools and solidifies, with or without crystallisation. They may be either plutonic bodies or volcanic extrusive. Again, erosive forces sculpt their current forms. * Metamorphic rocks are created by rocks that have been transformed into another kind of rock, usually by some combination of heat, pressure, and chemical alteration. * Sedimentary rocks are created by a variety of processes but usually involving deposition, grain by grain, layer by layer, in water or, in the case of terrestrial sediments, on land through the action of wind or sometimes moving i ...
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Mountain Ranges Of The Sakha Republic
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable ...
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Kigilyakh
Kigilyakh or kisiliyakh ( rus, кигиляхи; sah, киһилээх, meaning "stone person") are tall, pillar-like natural rock formations looking like tall monoliths standing more or less isolated. Usually they are composed of granite or sandstone shaped as a result of cryogenic weathering. Most kigilyakhs formed during the Cretaceous period and are about 120 million years old. Cultural significance and etymology These anthropomorphic rock pillars are an important feature in Yakut culture. Often they are slightly scattered, protruding from the surface of smooth mountains and giving the impression of a standing crowd of people. According to Yakut legends kigilyakhs originated in very ancient people. The Yakut word ''"kisiliy"'' means "a place where there are people". ''Kisilyakh'' means "mountain having a man" or "mountain married". The term "kigilyakh" is a distorted form of the original Yakut ''"kisilyakh"''. Locations Such stones are found in different places of Sakha ...
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Indigirka
The Indigirka ( rus, Индиги́рка, r=; sah, Индигиир, translit=Indigiir) is a river in the Sakha Republic in Russia between the Yana to the west and the Kolyma to the east. It is long. The area of its basin is . History The isolated village of Russkoye Ustye, located on the delta of the Indigirka, is known for the unique traditional culture of the Russian settlers whose ancestors came there several centuries ago. Some historians have speculated that Russkoye Ustye was settled by Pomors in the early 17th century. In 1638 explorer Ivan Rebrov reached the Indigirka. In 1636–42 Elisei Buza pioneered the overland route to the Indigirka river system. At about the same time, Poznik Ivanov ascended a tributary of the lower Lena, crossed the Verkhoyansk Range to the upper Yana, and then crossed the Chersky Range to the Indigirka. In 1642 Mikhail Stadukhin reached the Indigirka overland from the Lena. Zashiversk on the Indigirka was an important colonial outpo ...
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Uyandina
The Uyandina (russian: Уяндина; sah, Уйаандьы, translit=Uyaancı) is a river in Yakutia, Russia, a tributary of the Indigirka. The length of the Uyandina is . The area of its drainage basin is . Course The river is formed by the confluence of the long Irgichyan originating in the NW Selennyakh Range and the long Baky, which has its source in Lake Baky, located at the junction of the western end of the Polousny Range and the Kyun-Tas. After flowing in a roughly southern direction in its upper course, the Uyandina flows then eastwards through the Aby Lowland. Finally it meets the left bank of the Indigirka from its mouth. Google Earth The Uyandina freezes up in October and remains icebound until late May or early June. Tributaries The biggest tributaries of the Uyandina are the long Khatyngnakh and long Khachimcher from the left, as well as the long Buor-Yuryakh from the right. See also *List of rivers of Russia Russia can be divided into a European Russi ...
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Baky (Uyandina)
The Baky (russian: Бакы; sah, Бакы) is a river in the Sakha Republic (Yakutia), Russia. It is one of the northern tributaries of the Yana. The river has a length of and a drainage basin area of . The river flows north of the Arctic Circle. Its basin falls within Verkhoyansky District. Course The Baky is a left tributary of the Yana. It has its sources in the northwestern slopes of the Khayrdakh Ridge (Хайырдахский кряж), part of the Kular Range of the Verkhoyansk system. The river flows first northeastwards, skirting the mountain area. It meanders within a wide valley heading in an eastern direction in its lower course. Osokhtokh village is located by the banks of the Baky in its last stretch, where the river meanders very strongly. Near the left bank of the Yana the Baky divides into three branches, joining the river from its mouth. Google Earth Tributaries The main tributaries of the Baky are the long Tulluk (Туллук), the long Yuyuteer ...
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Chondon
The Chondon ( rus, Чондон; sah, Чондоон) is a river in Ust-Yansky District, Sakha Republic (Yakutia), Russia. It is long, with a drainage basin of . The Chondon mammoth was discovered in 2013 in the Chondon basin, at the feet of the Polousny Range, 66 km south-west of the village of Tumat. It had died at the age of 47 to 50 years. Course The river begins in the northern slopes of the Selennyakh Range at an elevation of . It flows roughly northwards west of the Yana River across the Yana-Indigirka Lowland meandering strongly among marshy areas and lakes. In its lower course it flows parallel to the Sellyakh in the east.''Chondon'' // Great Soviet Encyclopedia, in 30 vols. / Ch. ed. A.M. Prokhorov . - 3rd ed. - M .: Soviet Encyclopedia, 1969-197 Yarok Island lies across its mouth, in the Chondon Bay, by the Yana Bay of the Laptev Sea. Google Earth There are over 6,600 lakes in the Chondon basin, with a total area of . The river freezes yearly between early O ...
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Nuchcha
The Nuchcha or Nuuchcha (russian: Нучча; sah, Нуучча) is a river in the Sakha Republic (Yakutia), Russia. It is the longest tributary of the Chondon. The river has a length of and a drainage basin area of . The Nuchcha flows north of the Arctic Circle, across desolate territories of the Ust-Yansky District. An abandoned village named "Batagay" was located by the riverside in its lower course. A 2021 Yakut fictional film which received and award at the Karlovy Vary International Film Festival was named Nuuchcha. Course The Nuchcha is a right tributary of the Chondon. It has its sources in the northern slopes of the Kyun-Tas range. The river flows roughly northwards within a valley. After it leaves the mountainous terrain it heads across the Yana-Indigirka Lowland floodplain to the southwest of the Sellyakh. It flows slowly through flat terrain where it meanders very strongly among numerous lakes. Finally the river joins the Chondon from its mouth. Tumat, the near ...
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Google Earth
Google Earth is a computer program that renders a 3D representation of Earth based primarily on satellite imagery. The program maps the Earth by superimposing satellite images, aerial photography, and 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 keyboard or mouse. The program can also be downloaded on a smartphone or 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 captured 10 million miles of Street View imagery. In addition to Earth navigation, Google Earth provides a series ...
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Aby Lowland
The Aby Lowland (russian: Абыйская низменность; sah, Абый Намтала, translit=Abıy Namtala) is a low alluvial plain located in the Sakha Republic, Far Eastern Federal District, Russia. Administratively most of the territory of the lowland is part of Aby District ''(Aby Ulus)''. Geography The lowland is crossed by the Indigirka River in its middle course. Besides many smaller rivers and streams, three large left hand tributaries of the great river flow into it, the Selennyakh, Uyandina (with the Khatyngnakh) and Druzhina rivers. The Badyarikha limits the area in the east. The area is flat and mostly marshy, the average height of the plain being between and above sea level. The rivers are generally slow-flowing and meandering, connected by channels and with very boggy shores. The Aby Lakes, mostly small and numbering over 15,000, are dotting the lowlands. The largest are Lake Ozhogino
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Yana-Indigirka Lowland
The Yana-Indigirka Lowland (russian: Яно-Индигирская низменность; sah, Дьааҥы - Индигир намтала) is a large, low alluvial plain located in northern Siberia, Far Eastern Federal District, Russia. Administratively most of the territory of the lowland is part of the Sakha Republic (Yakutia). There are inhabited centers of population in the lowlands such as Chokurdakh, Olenegorsk and Nizhneyansk, but these are very few and scattered. Geography The lowland is named after the Yana River in the west and the Indigirka River in the east and is crossed by both rivers in their middle and lower courses. The area is mostly flat and very marshy, its northern limits extending for over from the Buor Khaya Gulf of the Laptev Sea in the west to the delta of river Indigirka in the East Siberian Sea in the east. It is limited by the Kyundyulyun, the northern end of the Selennyakh Range and the Polousny Range in the south.
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