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Terekty River
The Terekty River ( kk, Теректi өзенi, russian: река Теректы), also known under the Sinified spelling Tielieketi (), is a small river that flows from China to Kazakhstan. In its lower course the river is also known as the Kusak ( kz, Қусақ, russian: Кусак, ). Along most of its course, the river flows through the very sparsely populated mountainous terrain of the southern part of Xinjiang's Yumin County; by the time it crosses the China–Kazakhstan border and enters a flat desert east of Lake Zhalanashkol, its bed is usually dry, with little water ever reaching Lake Zhalanashkol. The Terekty is mainly known as the site of a Sino-Soviet border conflict that occurred in August 1969. Geography According to topographic maps, the Terekty rises in the Kertau or Barlik (巴尔鲁克) Mountains at around The river's source area can be seen e.g. on thiSoviet topo mapabout 2 km NE from Peak Kertau (which is marked with its elevation, 3282 m). After flowing ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alluvial Fan
An alluvial fan is an accumulation of sediments that fans outwards from a concentrated source of sediments, such as a narrow canyon emerging from an escarpment. They are characteristic of mountainous terrain in arid to semiarid climates, but are also found in more humid environments subject to intense rainfall and in areas of modern glaciation. They range in area from less than to almost . Alluvial fans typically form where flow emerges from a confined channel and is free to spread out and infiltrate the surface. This reduces the carrying capacity of the flow and results in deposition of sediments. The flow can take the form of infrequent debris flows or one or more ephemeral or perennial streams. Alluvial fans are common in the geologic record, such as in the Triassic basins of eastern North America and the New Red Sandstone of south Devon. Such fan deposits likely contain the largest accumulations of gravel in the geologic record. Alluvial fans have also been found on Mars ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Baiyang River
The Baiyang River (), also known under a Mongolian name transcribed in Chinese as Namuguolei (), is a river in Xinjiang Uighur Autonomous Region of China. It flows through the region's Tacheng Prefecture and the Urho District of Karamay City. The river's total length is estimated at , and the average annual flow at . The river's basin occupies , The Baiyang River starts in a massif near the junction of the Tarbagatai and Saur mountain ranges, near Xinjiang's border with Kazakhstan. It flows in a general southeastern direction, toward the endorheic Dzungarian Basin. Along much of its length it forms the border between Hoboksar Mongol Autonomous County in the east and Emin and Toli Counties in the west. It crosses Urho District of Karamay City, and then re-enters Hoboksar County. The Baiyang River is dammed at ； the dam creates the Baiyang River Reservoir (白杨河水库) with an area of . The Irtysh–Karamay Canal crosses the Baiyang River on an aqueduct at , upstream of Ur ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Adjective
In linguistics, an adjective (list of glossing abbreviations, abbreviated ) is a word that generally grammatical modifier, modifies a noun or noun phrase or describes its referent. Its semantic role is to change information given by the noun. Traditionally, adjectives were considered one of the main part of speech, parts of speech of the English language, although historically they were classed together with Noun, nouns. Nowadays, certain words that usually had been classified as adjectives, including ''the'', ''this'', ''my'', etc., typically are classed separately, as Determiner (class), determiners. Here are some examples: * That's a funny idea. (attributive) * That idea is funny. (predicate (grammar), predicative) * * The good, the bad, and the funny. (substantive adjective, substantive) Etymology ''Adjective'' comes from Latin ', a calque of grc, ἐπίθετον ὄνομα, epítheton ónoma, additional noun (whence also English ''epithet''). In the grammatical traditi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kazakh Language
The Kazakh or simply Qazaq (Latin: or , Cyrillic: or , Arabic Script: or , , ) is a Turkic language of the Kipchak branch spoken in Central Asia by Kazakhs. It is closely related to Nogai, Kyrgyz and Karakalpak. It is the official language of Kazakhstan and a significant minority language in the Ili Kazakh Autonomous Prefecture in Xinjiang, north-western China and in the Bayan-Ölgii Province of western Mongolia. The language is also spoken by many ethnic Kazakhs throughout the former Soviet Union (some 472,000 in Russia according to the 2010 Russian Census), Germany, and Turkey. Like other Turkic languages, Kazakh is an agglutinative language and employs vowel harmony. '' Ethnologue'' recognizes three mutually intelligible dialect groups, Northeastern Kazakh, the most widely spoken variety which also serves as the basis for the standard language, Southern Kazakh and Western Kazakh. The language share a degree of mutual intelligiblity with closely related Karakalpak ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Reinforced Concrete
Reinforced concrete (RC), also called reinforced cement concrete (RCC) and ferroconcrete, is a composite material in which concrete's relatively low tensile strength and ductility are compensated for by the inclusion of reinforcement having higher tensile strength or ductility. The reinforcement is usually, though not necessarily, steel bars ( rebar) and is usually embedded passively in the concrete before the concrete sets. However, post-tensioning is also employed as a technique to reinforce the concrete. In terms of volume used annually, it is one of the most common engineering materials. In corrosion engineering terms, when designed correctly, the alkalinity of the concrete protects the steel rebar from corrosion. Description Reinforcing schemes are generally designed to resist tensile stresses in particular regions of the concrete that might cause unacceptable cracking and/or structural failure. Modern reinforced concrete can contain varied reinforcing materials made of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Granite
Granite () is a coarse-grained (phaneritic) intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase. It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies underground. It is common in the continental crust of Earth, where it is found in igneous intrusions. These range in size from dikes only a few centimeters across to batholiths exposed over hundreds of square kilometers. Granite is typical of a larger family of ''granitic rocks'', or ''granitoids'', that are composed mostly of coarse-grained quartz and feldspars in varying proportions. These rocks are classified by the relative percentages of quartz, alkali feldspar, and plagioclase (the QAPF classification), with true granite representing granitic rocks rich in quartz and alkali feldspar. Most granitic rocks also contain mica or amphibole minerals, though a few (known as leucogranites) contain almost no dark minerals. Granite is nearly alway ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Survey Marker
Survey markers, also called survey marks, survey monuments, or geodetic marks, are objects placed to mark key survey points on the Earth's surface. They are used in geodetic and land surveying. A ''benchmark'' is a type of survey marker that indicates elevation (vertical position). Horizontal position markers used for triangulation are also known as ''triangulation stations''. '' Benchmarking'' is the hobby of "hunting" for these marks. Types All sorts of different objects, ranging from the familiar brass disks to liquor bottles, clay pots, and rock cairns, have been used over the years as survey markers. Some truly monumental markers have been used to designate tripoints, or the meeting points of three or more countries. In the 19th century, these marks were often drill holes in rock ledges, crosses or triangles chiselled in rock, or copper or brass bolts sunk into bedrock. Today in the United States, the most common geodetic survey marks are cast metal disks with stamped l ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Delta
A river delta is a landform shaped like a triangle, created by deposition (geology), deposition of sediment that is carried by a river and enters slower-moving or stagnant water. This occurs where a river enters an ocean, sea, estuary, lake, reservoir, or (more rarely) another river that cannot carry away the supplied sediment. It is so named because its triangle shape resembles the Greek letter Delta. The size and shape of a delta is controlled by the balance between watershed processes that supply sediment, and receiving basin processes that redistribute, sequester, and export that sediment. The size, geometry, and location of the receiving basin also plays an important role in delta evolution. River deltas are important in human civilization, as they are major agricultural production centers and population centers. They can provide Coast, coastline defense and can impact drinking water supply. They are also Ecology, ecologically important, with different species' assemblages ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake Alakol
Alakol Lake ( kk, Алакөл, , from Turkic "motley lake") is a lake located in the Balkhash-Alakol Basin, part of the Almaty and Shyghyz regions, east central Kazakhstan. Its elevation is above sea level. The lake is the northwest extension of the region known as the Dzhungarian Gate (Alataw Pass), a narrow valley connects the southern uplands of Kazakhstan with arid northwest China. The Dzhungarian Gate is a fault-bounded valley (see vertical line on the image along the southwest side of the lake) where the elevation of the valley floor is between 350 and 450 m above sea level and the peaks of the Dzhungarsky Alatau range (lower left) reach above sea level. Two well-defined alluvial fans are visible where mountain streams cut through the faulted landscape to the southwest of the lake. The surface area of the lake is . It is deep at its maximum depth, with a volume of 58.6 km3. A swampy lowland (just above the center of the photo) connects the northwest end of Lake ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Zhalanashkol
Lake Zhalanashkol ( kz, Жалаңашкөл, literally "Bare Lake", or "Exposed Lake"; russian: Жаланашколь) is a freshwater lake in the eastern part of Kazakhstan, on the border of Almaty Province (Alakol District) and East Kazakhstan Province (Urzhar District). It is the smallest out of the four major lakes of the Alakol depression (the other three being the Alakol, the Sasykkol, and the Koshkarkol). It is also the southernmost of the four, the one closest to the Dzungarian Gate and the Aibi Lake on the other, Chinese, side of the Gate. On the maps compiled in the 18th and 19th century the Zhalanashkol is labeled Taskol (literally "Stone Lake"); this name is now obsolete. Description On the border with the mountain ranges formed depression, in which there was an accumulation of wastewater flowing into rivers, creating isolated water bodies. In these desert areas with a dry continental climate and very little precipitation, water consumption in the drainless lake ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tielieketi
Tielieketi () is located in Yumin County in Xinjiang, the People's Republic of China, adjacent to the border with Kazakhstan. The name comes from the Terekty River, an intermittent stream which flows China to Kazakhstan. Tielieketi Incident The Tielieketi military incident between Soviet and Chinese border troops (known in Soviet sources as "the border conflict near Lake Zhalanashkol" (russian: пограничный конфликт у озера Жаланашколь) occurred on August 13, 1969, during the Sino-Soviet split The Sino-Soviet split was the breaking of political relations between the China, People's Republic of China and the Soviet Union caused by Doctrine, doctrinal divergences that arose from their different interpretations and practical applications .... The Soviet force eliminated a unit of about 30 Chinese soldiers, capturing four. Soviet sources allege the August 13 clash between Soviet border guards and a Chinese force happened after persistent violat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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