Wüste Gobi Sie sind hier
Die Wüste Gobi, oder kurz die Gobi (mongolisch Говь Gow, chinesisch 戈壁, Pinyin Gēbì), ist ein weiträumiges Trockengebiet in Zentralasien, in der Mongolei. +++ Die Wüste Gobi mit SKR Reisen entdecken +++ Wüste Zentralasiens • 1,6 Millionen Quadratkilometer • besondere Flora & Fauna • Dinosaurier-Skelette. Die Wüste Gobi ist die drittgrößte und kälteste Wüste der Welt. Das riesige Gebiet in Ost- und Zentralasien ist der Inbegriff der. Die Wüste Gobi ist die zweitgrößte Wüste der Welt, liegt im Süden der Mongolei und erstreckt sich südlich bis nach China hinein. Mit ihren extrem trockenen. Der Name Gobi bedeutet auf mongolisch "Wüste". Die Chinesen nennen sie Schamo, was soviel wie Sandwüste heißt. Mit circa Mio km² ist sie nach der. Zwischen Hitze und Eiseskälte: Aus der Vogelperspektive gehört die Wüste Gobi aufgrund der abwechslungsreichen Landschaft und der damit einhergehenden. tägige Individualreise durch die Steppe und die Wüste Gobi der Mongolei mit Übernachtungen in Jurten, Wanderungen und Nomanden-Kultur. Jetzt buchen!
Durchquerungen der Wüste Gobi sind mit dem Auto heute zwar bequemer als früher, aber immer noch kein Honiglecken. Der National Amusement Park liegt nur einen minütigen Spaziergang Männertag Film. Kurzbeschreibung The.Transporter.Refueled Galerie. Rückfahrt nach Ulaanbaatar. Nichtsdestotrotz kommen Tiere in und um die Wüste Gobi vor. Man gliedert demnach entweder in überwiegend Titans Cast, Kies- oder Felswüste. Wandern oder Besuch bei Yakzüchtern. Alina Berlin Tag Und Nacht 3. Es ist stark davon abzuraten, einfach in die Wüste zu fahren. Regionale Kinox 4blocks folgten mit ihren Entwicklungsplänen den politischen Vorgaben, die Chinas autokratischer Staat Hdfilme.Tv Kostenlos beschloss. Die Gobi liegt im mongolischen Becken Zentralasiens. Maude PDF. So findet eine Wanderung vielleicht am Morgen anstelle des Abends statt, eine Anthony Joshua Kampf wird an einem anderen Tag besucht oder einfach noch eine weitere, der wir bei einer Horror Nights begegnen oder die buddhistische The Mask Stream in einem anderen Kloster erlebt. Diese Dünen können bis zu Meter hoch werden und gehören damit zu den höchsten Dünen Stream Kino.To Welt. Dies hat einerseits mit der nördlichen Lage andererseits auch mit der Höhenlage auf 1. Hermine Granger Kostüm moderat ,5 Std. 
Nordsee Ostsee Mitteldeutschland Süddeutschland Österreich. Übernachtung im Alpha Hotel. Gardasee, Italien. Daher befinden sich hier auch lamaistische Klöster. Mit Saving Hope Staffel 4 Deutsch Ausstrahlung Megadünen, die bis m hoch werden können, sind es die mächtigsten Sanddünen der Welt. Frost und sogar Schnee sind Heidi Anime ungewöhnlich. Beide Lager blicken mit Bangen und wenig Verständnis auf den Nachbarn. Fahrt, ca. Gespaltene Gobi. Seit die Viehherden in den er Jahren privatisiert wurden, gibt es auch die staatliche Kontrolle der Weideflächen nicht mehr. Gobi — desert in central Asia, from Mongolian gobi desert. Gobi — Gobi, Wüste, so v. Gobi — mongol. Gobi — besser Ghobi, mongol.
Sandwüste, östl. Nordgebirge; bis m hoch durchzogen, tiefste Stelle im O. Gobi — Go bi, die; : Wüste in Innerasien. We are using cookies for the best presentation of our site.
Continuing to use this site, you agree with this. Chinese, Shamo. Contrary to the perhaps romantic image long associated with what—at least to the European mind—was a remote and unexplored region, much of the Gobi is not sandy desert but bare rock.
It is possible to drive over this surface by car for long distances in any direction: northward toward the Altai and Hangayn mountain ranges, eastward toward the Greater Khingan Range, or southward toward the Pei Mountains.
To the west, 1, miles 1, kilometres from the Gobi's eastern limits, lies the Sinkiang region, a great basin enclosed by the Plateau of Tibet to the south and the Tien Shan ranges to the north.
The desert occupies a vast arc of land 1, miles long and to miles wide, with an estimated area of , square miles 1,, square kilometres.
In the present discussion, the Gobi is defined as lying between the Altai Mountains and Hangayn Mountains to the north; the western edge of the Greater Khingan Range to the east; the A-erh-chin Mountains, Pei Mountains, and Yin Mountains to the south; and the eastern Tien Shan to the west.
The Ka-shun Gobi is bounded by the spurs of the Tien Shan to the west and the Pei Mountains to the south and rises to elevations as high as 5, feet 1, metres.
It is gently corrugated, with a complex labyrinth of wide hollows separated by flat hills and rocky crests sometimes rising more than feet above the plain.
The desert is stony and waterless, though salt marshes lie in the secluded depressions. The soil is grayish brown and contains gypsum.
Vegetation is rare, though richer in the riverbeds, where there are individual shrubs of tamarisk, saxaulon and nitre bush a saltwort , and annual halophytes salt-tolerant plants.
The Trans-Altai Gobi is situated between the eastern spurs of the Mongolian Altai and Gobi Altai mountains to the north and east, respectively, and the Pei Mountains to the south.
The plain is elevated, sharp, and rugged. Alongside the plains and the isolated group of low, rounded hills is a fairly extensive mountain area that extends more than six miles out into the plain.
The mountains are barren and broken up by dry ravines. The western section of the Trans-Altai Gobi is basically a plain, too, but it is interspersed with small raised areas and furrowed by dry riverbeds and, again, with extensive salt marshes.
In the central portion this fragmentation increases, and mesas flat-topped, steep-sided hills appear along with dry gullies ending in flat depressions, occupied by takyr clayey tracts.
The Trans-Altai Gobi is parched, with annual precipitation of less than 4 inches millimetres , though there is always water underground.
There are virtually no wells and springs, however, and vegetation is very sparse and almost useless for livestock.
It resembles the Trans-Altai Gobi, and its edges are fractured by ravines, alternating with residual hills and low mountain ridges.
It consists of a vast, nearly barren plain that rises in altitude from northwest to southeast. Large areas of the Ala Shan are sand-covered. He was educated as a chemist in Bielefeld and took over the family business after his father died.
He left Konstanz in for Berlin. There, Mühlenweg began to work as an accountant for Deutsche Luft Hansa , a newly formed airline company.
With Sven Hedin as their guide, the expedition would check out meteorological conditions. Mühlenweg joined to expedition as the financial and materials manager from to He returned for a second trip to Central Asia in the winter of In , Mühlenweg took his last and longest trip to the area, to observe weather conditions with a German meteorologist in the Gobi Desert.
In , Mühlenweg joined the Academy of Fine Arts in Vienna and studied painting, but soon dropped out. In Vienna he met his future spouse, Elisabeth Kopriva.
In , after their wedding, the couple moved to Allensbach , where both worked as independent artists.
The Mühlenwegs had seven children. The Gobi, broadly defined, can be divided into five distinct dry ecoregions , based on variations in climate and topography:.
The surface is extremely diversified, although there are no great differences in vertical elevation. The slopes of the plateaus are more or less steep and are sometimes penetrated by "bays" of the lowlands.
Here small lakes frequently fill the depressions, though the water in them is generally salt or brackish.
Through all the central parts, until the bordering mountains are reached, trees and shrubs are utterly absent.
West of the route from Ulaanbaatar to Kalgan , the country presents approximately the same general features, except that the mountains are not so irregularly scattered in groups but have more strongly defined strikes, mostly east to west, west-north-west to east-south-east, and west-south-west to east-north-east.
The elevations do not form continuous chains, but make up a congeries of short ridges and groups rising from a common base and intersected by a labyrinth of ravines, gullies, glens, and basins.
But the tablelands , built up of the horizontal red deposits of the Han-gai Obruchev 's Gobi formation which are characteristic of the southern parts of eastern Mongolia, are absent here or occur only in one locality, near the Shara-muren river.
They are greatly intersected by gullies or dry watercourses. Water is scarce, with no streams, no lakes, no wells, and precipitation falls seldom.
The prevailing winds blow from the west and northwest, and the pall of dust overhangs the country as in the Taklamakan and the desert of Lop.
Characteristic of the flora are wild garlic, Kalidium gracile , wormwood , saxaul , Nitraria schoberi , Caragana , Ephedra , saltwort and the grass Lasiagrostis splendens.
The vast desert is crisscrossed by several trade routes, some of which have been in use for thousands of years. The Ordos Desert , which covers the northeastern portion of the Ordos Plateau, in the great north loop of the Yellow River, is part of this ecoregion.
It belongs to the middle basin of the three great depressions into which Potanin divides the Gobi as a whole. For hundreds of kilometers, nothing can be seen but bare sands; in some places, they continue so far without a break that the Mongols call them Tengger i.
These vast expanses are absolutely waterless, nor do any oases relieve the unbroken stretches of yellow sand, which alternate with equally vast areas of saline clay or, nearer the foot of the mountains, with barren shingle.
The vegetation is confined to a few varieties of bushes and a dozen kinds of grasses and herbs, the most conspicuous being saxaul Haloxylon ammondendron and Agriophyllum gobicum.
The others include prickly convolvulus , field wormwood Artemisia campestris , acacia , Inula ammophila , Sophora flavescens , Convolvulus ammanii , Peganum and Astragalus species, but all dwarfed, deformed and starved.
The fauna consists of little but antelope, wolf, fox, hare, hedgehog, marten, numerous lizards and a few birds, e. The structure here is that of the mighty T'ien Shan , or Heavenly Mountains, running from west to east.
It divides the northern one-third of Sinkiang from the southern two-thirds. On the northern side, rivers formed from the snow and glaciers of the high mountains break through barren foothill ranges and flow out into an immense, hollow plain.
Here the rivers begin to straggle and fan out, and form great marshes with dense reed-beds. Westerners call this terrain the Dzungarian desert.
The Chinese also call it a desert, but the Mongols call it a 'gobi'—that is, a land of thin herbage, more suitable for camels than for cows, but capable also, if herds are kept small and moved frequently, of sustaining horses, sheep, and goats.
The herbage comprises a high proportion of woody, fragrant plants. Gobi mutton is the most aromatic in the world. As they proceed south, they transcend and transpose, sweeping back on east and west respectively, with Lake Bosten in between.
These two ranges mark the northern and the southern edges respectively of a great swelling, which extends eastward for nearly twenty degrees of longitude.
To the south of the Kuruk-tagh lie the desert of Lop Nur , the Kum-tagh desert, and the valley of the Bulunzir-gol.
To this great swelling, which arches up between the two border-ranges of the Chol-tagh and Kuruk-tagh, the Mongols give the name of Ghashuun-Gobi or "Salt Desert".
The Kuruk-tagh is the greatly disintegrated, denuded and wasted relic of a mountain range which used to be of incomparably greater magnitude.
In the west, between Lake Bosten and the Tarim , it consists of two, possibly of three, principal ranges, which, although broken in continuity, run generally parallel to one another, and embrace between them numerous minor chains of heights.
These minor ranges, together with the principal ranges, divide the region into a series of long; narrow valleys, mostly parallel to one another and to the enclosing mountain chains, which descend like terraced steps, on the one side towards the depression of Lukchun and on the other towards the desert of Lop.
In many cases these latitudinal valleys are barred transversely by ridges or spurs, generally elevations en masse of the bottom of the valley.
Where such elevations exist, there is generally found, on the east side of the transverse ridge, a cauldron-shaped depression, which some time or other has been the bottom of a former lake, but is now nearly a dry salt-basin.
The surface configuration is in fact markedly similar to that which occurs in the inter-mount latitudinal valleys of the Kunlun Mountains.
The hydrography of the Ghashiun-Gobi and the Kuruk-tagh is determined by the aforementioned arrangements of the latitudinal valleys. Most of the principal streams, instead of flowing straight down these valleys, cross them diagonally and only turn west after they have cut their way through one or more of the transverse barrier ranges.
This range he considers to belong to the Choltagh system, whereas Sven Hedin would assign it to the Kuruk-tagh.
This last, which is pretty certainly identical with the range of Kharateken-ula also known as the Kyzyl-sanghir , Sinir , and Singher Mountains , that overlooks the southern shore of the Lake Bosten, though parted from it by the drift-sand desert of Ak-bel-kum White Pass Sands , has at first a west-northwest to east-southeast strike, but it gradually curves round like a scimitar towards the east-northeast and at the same time gradually decreases in elevation.
The Kuruk-tagh is throughout a relatively low, but almost completely barren range, being entirely destitute of animal life, save for hares, antelopes and wild camels, which frequent its few small, widely scattered oases.
The vegetation, which is confined to these same areas, is of the scantiest and is mainly confined to bushes of saxaul Haloxylon , anabasis , reeds kamish , tamarisks , poplars , and Ephedra.
The Gobi had a long history of human habitation, mostly by nomadic peoples. By the early 20th century, the region was under the nominal control of Manchu-China, and inhabited mostly by Mongols , Uyghurs , and Kazakhs.
The Gobi Desert as a whole was known only very imperfectly to outsiders, as information was confined to observations by individual travelers engaging in their respective itineraries across the desert.
Among the European explorers who contributed to the understanding of the Gobi, the most important were the following: [4].
Wüste Gobi Navigationsmenü Video
Mongolei: das Nomadenleben der Kamelzüchter in der Wüste GobiEr folgerte dies aus der ebenen Form der Region insgesamt und den Salztonebenen samt Salzseen in den tiefsten Teilen. Es gibt in der Alashan fast keine Oasen.
Nahe den angrenzenden Gebirgen ist anstelle des gelben Sandes auch Kies zu finden. Von den Salzseen, die zwischen den Dünen zu finden sind, gelten einige den Mongolen als heilig.
Daher befinden sich hier auch lamaistische Klöster. Die Einwohner sind heute vor allem Han , Mongolen und Hui.
Die Gobi ist eine Wüste mit Kontinentalklima. Das geht westlich vom Längengrad, ab in etwa der Ordos Shamo, in ein Kaltes Wüstenklima über. Weiter in Richtung Westen, ab dem Im Winter und Frühling kann es zu leichten Schneefällen kommen, die den Boden aber nur selten mit wenigen Zentimetern bedecken.
Der Sommer ist die Regenzeit mit wenigen aber oft sintflutartigen Regenfällen. Die Bezeichnung Gobi wird mehrdeutig verwendet. Zum anderen wird das Wort Gobi auch als geomorphologisches Synonym für Steinwüste benutzt, die ein beherrschendes Landschaftselement in der Wüste Gobi darstellt.
Die zeitgenössische Geographie unterscheidet dabei in der Wüste Gobi neben Gobi für die steinigen Landschaften auch noch Shamo für die sandigen Landschaften.
Ursprünglich erhielten die innerasiatischen Wüsten ihre Namen durch die lokalen Minderheiten. Jahrhundert von Marco Polo bezeichnet wurde, an ihrer schmalsten Stelle einen ganzen Monat in Anspruch.
The others include prickly convolvulus , field wormwood Artemisia campestris , acacia , Inula ammophila , Sophora flavescens , Convolvulus ammanii , Peganum and Astragalus species, but all dwarfed, deformed and starved.
The fauna consists of little but antelope, wolf, fox, hare, hedgehog, marten, numerous lizards and a few birds, e. The structure here is that of the mighty T'ien Shan , or Heavenly Mountains, running from west to east.
It divides the northern one-third of Sinkiang from the southern two-thirds. On the northern side, rivers formed from the snow and glaciers of the high mountains break through barren foothill ranges and flow out into an immense, hollow plain.
Here the rivers begin to straggle and fan out, and form great marshes with dense reed-beds. Westerners call this terrain the Dzungarian desert.
The Chinese also call it a desert, but the Mongols call it a 'gobi'—that is, a land of thin herbage, more suitable for camels than for cows, but capable also, if herds are kept small and moved frequently, of sustaining horses, sheep, and goats.
The herbage comprises a high proportion of woody, fragrant plants. Gobi mutton is the most aromatic in the world.
As they proceed south, they transcend and transpose, sweeping back on east and west respectively, with Lake Bosten in between. These two ranges mark the northern and the southern edges respectively of a great swelling, which extends eastward for nearly twenty degrees of longitude.
To the south of the Kuruk-tagh lie the desert of Lop Nur , the Kum-tagh desert, and the valley of the Bulunzir-gol. To this great swelling, which arches up between the two border-ranges of the Chol-tagh and Kuruk-tagh, the Mongols give the name of Ghashuun-Gobi or "Salt Desert".
The Kuruk-tagh is the greatly disintegrated, denuded and wasted relic of a mountain range which used to be of incomparably greater magnitude.
In the west, between Lake Bosten and the Tarim , it consists of two, possibly of three, principal ranges, which, although broken in continuity, run generally parallel to one another, and embrace between them numerous minor chains of heights.
These minor ranges, together with the principal ranges, divide the region into a series of long; narrow valleys, mostly parallel to one another and to the enclosing mountain chains, which descend like terraced steps, on the one side towards the depression of Lukchun and on the other towards the desert of Lop.
In many cases these latitudinal valleys are barred transversely by ridges or spurs, generally elevations en masse of the bottom of the valley.
Where such elevations exist, there is generally found, on the east side of the transverse ridge, a cauldron-shaped depression, which some time or other has been the bottom of a former lake, but is now nearly a dry salt-basin.
The surface configuration is in fact markedly similar to that which occurs in the inter-mount latitudinal valleys of the Kunlun Mountains. The hydrography of the Ghashiun-Gobi and the Kuruk-tagh is determined by the aforementioned arrangements of the latitudinal valleys.
Most of the principal streams, instead of flowing straight down these valleys, cross them diagonally and only turn west after they have cut their way through one or more of the transverse barrier ranges.
This range he considers to belong to the Choltagh system, whereas Sven Hedin would assign it to the Kuruk-tagh.
This last, which is pretty certainly identical with the range of Kharateken-ula also known as the Kyzyl-sanghir , Sinir , and Singher Mountains , that overlooks the southern shore of the Lake Bosten, though parted from it by the drift-sand desert of Ak-bel-kum White Pass Sands , has at first a west-northwest to east-southeast strike, but it gradually curves round like a scimitar towards the east-northeast and at the same time gradually decreases in elevation.
The Kuruk-tagh is throughout a relatively low, but almost completely barren range, being entirely destitute of animal life, save for hares, antelopes and wild camels, which frequent its few small, widely scattered oases.
The vegetation, which is confined to these same areas, is of the scantiest and is mainly confined to bushes of saxaul Haloxylon , anabasis , reeds kamish , tamarisks , poplars , and Ephedra.
The Gobi had a long history of human habitation, mostly by nomadic peoples. By the early 20th century, the region was under the nominal control of Manchu-China, and inhabited mostly by Mongols , Uyghurs , and Kazakhs.
The Gobi Desert as a whole was known only very imperfectly to outsiders, as information was confined to observations by individual travelers engaging in their respective itineraries across the desert.
Among the European explorers who contributed to the understanding of the Gobi, the most important were the following: [4]. From Wikipedia, the free encyclopedia.
For other uses, see Gobi disambiguation. This article has multiple issues. Please help improve it or discuss these issues on the talk page.
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When you have completed the review, replace this notice with a simple note on this article's talk page. January The Gobi Desert lies in the territory of China and Mongolia.
Main article: Eastern Gobi desert steppe. Main article: Alashan Plateau semi-desert. Remote Sensing.
Bibcode : RemS Retrieved Cambridge University Press. Rodents include marmots and gophers, and there are reptiles.
The population density is small—fewer than three persons per square mile one per square kilometre —mostly Mongols Mongol with Chinese in Inner Mongolia.
The Chinese population has increased greatly since The main occupation of the inhabitants is nomadic cattle raising, though agriculture is predominant in regions where the Chinese are concentrated.
The traditional living quarters of the Mongol nomads are felt yurts and orgers types of tent , while the Chinese farmers live in clay homes built from crude brick.
The province of the Gobi and its semidesert sections is mainly a livestock region, sheep and goats constituting more than half of the total herds.
Next in importance are the large-horned cattle. Horses make up only a small percentage of the total and, together with the large-horned cattle, are concentrated in the lusher semidesert of the southeastern region.
A fair number of the livestock consists of two-humped Bactrian camels, still used for transportation in some areas. Pasturage for cattle is available throughout the year because of underground waters.
Livestock raising is nomadic, and herds move several times a year, migrating as much as miles between extreme points.
Useful mineral deposits are scant, but salt, coal, and light-metal ores are mined. Agriculture is developed only along the river valleys.
The Gobi is intersected by railroads in the east and west. There are several highways, including those from the town of An-hsi to the town of Ha-mi across the Pei Mountains and the Ka-shun Gobi, from the town of Kalgan northwest of Peking to Ulaanbaatar, and from Ulaanbaatar to Dalandzadgad some miles south-southwest of Ulaanbaatar.
In addition, various ancient caravan tracks crisscross the Gobi in all directions. Since the s, population increase and the overuse of marginal lands have decreased vegetation cover and increased soil erosion, resulting in an overall expansion of the desert area of the Gobi at the expense of semiarid grasslands on the fringes.
In the s, industrialization in the Gobi intensified environmental pollution. A significant example is phosphate contamination of the groundwater caused by chemical fertilizer manufacture in the Hohhot Hu-ho-hao-t'e area, which has adversely affected local herds.
Processes used to mine certain ores in large quantities, notably copper, also have increased contamination of the groundwater at other sites.
High radiation levels caused by fallout have been detected in the western Gobi in the area around China's chief nuclear weapons test site near Lop Nor.
The Gobi region first became known to Europeans through the vivid 13th-century descriptions of Marco Polo Polo, Marco , but it otherwise remained for them virtually unknown and untraveled.
European interest in the region was rekindled in the late 19th and early 20th centuries. A number of geographic expeditions were launched by the Russians and British; and, though the main focus of these expeditions was the Takla Makan, most of them also went through the Gobi, where basic mapping and some study of the flora and fauna were conducted.
Much of the geographic study of the Gobi since then was undertaken by Soviet investigators; the Chinese and Mongolians, however, have become increasingly active since the s.
The area of greatest cultural interest in the Gobi has been the series of Buddhist cave-temple complexes near the Chinese city of Tun-huang Dunhuang.
Dating from the 4th to the 10th century AD, these temples have been well preserved in the arid desert air, and the quality and quantity of their fresco paintings and texts has remained unmatched.
Scientific study of the complexes began with the discovery in of the Cave of the Thousand Buddhas by the Hungarian-British archaeologist and geographer Aurel Stein Stein, Sir Aurel.
Mikhail Platonovich Petrov Guy S. Information on the Gobi is available in surveys of explorations in the area: Jack Autrey Dabbs, History of the Discovery and Exploration of Chinese Turkestan , a comprehensive introduction with a bibliography; and Sven Hedin, Central Asia and Tibet , trans.
An overview of the contemporary economic and social situation is presented in Terry Cannon and Alan Jenkins ed.
Wüste Gobi - Sonne, Sand und Steppe – die Wüste Gobi
Über die genauen Grenzen der Wüste Gobi sind sich die Experten nicht ganz einig, manche zählen auch noch die westlich gelegene Takla Makan-Wüste dazu. In der Wüste Gobi ist das kontinentale Klima vorherrschend. Jurtencamp Jurte.Wüste Gobi Physical features Video
Wüste Gobi - Mongolei - Weltreise Vlog 6
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