The Info List - Gobi

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The Gobi Desert
(/ˈɡoʊ.bi/) is a large desert region in Asia.[1] It covers parts of northern and northwestern China, and of southern Mongolia. The desert basins of the Gobi are bounded by the Altai Mountains and the grasslands and steppes of Mongolia
on the north, by the Taklamakan Desert
to the west, by the Hexi Corridor
Hexi Corridor
and Tibetan Plateau
to the southwest, and by the North China
Plain to the southeast. The Gobi is notable in history as part of the great Mongol Empire, and as the location of several important cities along the Silk Road. The Gobi is a rain shadow desert, formed by the Tibetan Plateau blocking precipitation from the Indian Ocean reaching the Gobi territory.


1 Geography 2 Climate 3 Conservation, ecology, and economy 4 Desertification 5 Ecoregions
of the Gobi

5.1 Eastern Gobi desert steppe 5.2 Alashan Plateau
semi-desert 5.3 Dzungarian Basin
Dzungarian Basin

6 European exploration up to 1911 7 See also 8 Notes 9 References 10 Further reading 11 External links

Geography[edit] The Gobi measures over 1,600 km (1,000 mi) from southwest to northeast and 800 km (500 mi) from north to south. The desert is widest in the west, along the line joining the Lake Bosten and the Lop Nor
Lop Nor
(87°–89° east). It occupies an arc of land 1,295,000 km2 (500,000 sq mi)[2] in area as of 2007; it is the fifth-largest desert in the world and Asia's second largest. Much of the Gobi is not sandy but has exposed bare rock. In its broadest definition, the Gobi includes the long stretch of desert extending from the foot of the Pamirs
(77° east) to the Greater Khingan
Greater Khingan
Mountains, 116°-118° east, on the border of Manchuria; and from the foothills of the Altay, Sayan, and Yablonoi mountain ranges on the north to the Kunlun, Altyn-Tagh, and Qilian mountain ranges, which form the northern edges of the Tibetan Plateau, on the south.[3] A relatively large area on the east side of the Greater Khingan
Greater Khingan
range, between the upper waters of the Songhua
(Sungari) and the upper waters of the Liao-ho, is reckoned to belong to the Gobi by conventional usage. Some geographers and ecologists prefer to regard the western area of the Gobi region (as defined above): the basin of the Tarim in Xinjiang
and the desert basin of Lop Nor
Lop Nor
and Hami (Kumul), as forming a separate and independent desert, called the Taklamakan Desert. Archeologists and paleontologists have done excavations in the Nemegt Basin in the northwestern part of the Gobi Desert
(in Mongolia), which is noted for its fossil treasures, including early mammals, dinosaur eggs, and prehistoric stone implements, some 100,000 years old.[4] Climate[edit]

Gobi by NASA World

Sand dunes in Inner Mongolia
Autonomous Region, China

A summer monsoon produces a flash flood, 2004

Bactrian camels
Bactrian camels
by the sand dunes of Khongoryn Els, Gurvansaikhan NP, Mongolia.

The sand dunes of Khongoryn Els, Gurvansaikhan NP, Mongolia

Remains of Great Chinese Wall in Gobi Desert

The Gobi is a cold desert, with frost and occasionally snow occurring on its dunes. Besides being quite far north, it is also located on a plateau roughly 910–1,520 metres (2,990–4,990 ft) above sea level, which contributes to its low temperatures. An average of approximately 194 millimetres (7.6 in) of rain falls annually in the Gobi. Additional moisture reaches parts of the Gobi in winter as snow is blown by the wind from the Siberian Steppes. These winds may cause the Gobi to reach −40 °C (−40 °F) in winter to 45 °C (113 °F) in summer.[5] The climate of the Gobi is one of great extremes, combined with rapid changes of temperature of as much as 35 °C (63 °F). These can occur not only seasonally but within 24 hours.


Sivantse (1190 m) Ulaanbaatar
(1150 m)

Annual mean −2.5 °C (27.5 °F) −0.4 °C (31.3 °F)

January mean −26.5 °C (−15.7 °F) −21.6 °C (−6.9 °F)

July mean 17.5 °C (63.5 °F) 18.2 °C (64.8 °F)

Extremes −43 to 38 °C (−45 to 100 °F) −42.2 to 39.0 °C (−44.0 to 102.2 °F)

In southern Mongolia, the temperature has been recorded as low as −32.8 °C (−27.0 °F). In contrast, in Alxa, Inner Mongolia, it rises as high as 37 °C (99 °F) in July. Average winter minimums are a frigid −21 °C (−6 °F), while summertime maximums are a warm 27 °C (81 °F). Most of the precipitation falls during the summer.[6] Although the southeast monsoons reach the southeast parts of the Gobi, the area throughout this region is generally characterized by extreme dryness, especially during the winter, when the Siberian anticyclone is at its strongest. The southern and central parts of the Gobi Desert have variable plant growth due to this monsoon activity. The more northern areas of the Gobi are very cold and dry, making it unable to support much plant growth; this cold and dry weather is attributed to Siberian-Mongolian high pressure cells.[1] Hence, the icy sandstorms and snowstorms of spring and early summer plus early January (winter). Conservation, ecology, and economy[edit] The Gobi Desert
is the source of many important fossil finds, including the first dinosaur eggs. Despite the harsh conditions, these deserts and the surrounding regions sustain many animals, including black-tailed gazelles, marbled polecats, wild Bactrian camels, Mongolian wild ass
Mongolian wild ass
and sandplovers. They are occasionally visited by snow leopards, brown bears, and wolves. Lizards are especially well-adapted to the climate of the Gobi Desert, with approximately 30 species distributed across its southern Mongolian border.[7] The most common vegetation in the Gobi desert are shrubs adapted to drought.[8] These shrubs included gray sparrow's saltwort (Salsola passerina), gray sagebrush, and low grasses such as needle grass and bridlegrass. Due to livestock grazing, the amount of shrubs in the desert has decreased.[8] Several large nature reserves have been established in the Gobi, including Gobi Gurvansaikhan National Park, Great Gobi A and Great Gobi B Strictly Protected Area. The area is vulnerable to trampling by livestock and off-road vehicles (effects from human intervention are greater in the eastern Gobi Desert, where rainfall is heavier and may sustain livestock). In Mongolia, grasslands have been degraded by goats, which are raised by nomadic herders as source of cashmere wool.[9] The economic trends of livestock privatization and the collapse of the urban economy have caused people to return to subsistence rural lifestyles, away from urbanization. Large copper and gold deposits located at Oyuu Tolgoi, about 80 kilometres from the Chinese border into Mongolia, are being investigated for development as mining operations.[10] The Oyu Tolgoi copper and gold mine, under construction by Rio Tinto in the South Gobi Desert, is expected to begin operation in early 2013, and is the biggest economic undertaking in the country's history. Rio Tinto estimates that taxes, royalties and dividends generated by the Oyu Tolgoi project is expected to add a third to the country's gross domestic product by 2020. Rio Tinto forecasts average annual production of 450,000 tonnes of copper and 330,000 ounces of gold, and with 1.4 billion tonnes of reserves and a resource of 3.1 billion tonnes, the mine is expected to last for more than 50 years.[11] The mine has been and remains controversial. There is significant opposition in Mongolia's parliament to the terms under which the mine will proceed, and some are calling for the terms to be renegotiated. Specifically, the contention revolves primarily around the question of whether negotiations were fair (Rio Tinto is far better resourced) and whether Rio Tinto will pay adequate taxes on the revenues it derives from the mine (an agreement was reached whereby the operation will be exempt from windfall tax.[12] Desertification[edit] The Gobi Desert
is expanding at an alarming rate, in a process known as desertification. The expansion is particularly rapid on the southern edge into China, which has seen 3,600 km2 (1,390 sq mi) of grassland overtaken every year by the Gobi Desert. Dust storms, which used to occur regularly in China, have increased in frequency in the past 20 years, mainly due to desertification. They have caused further damage to China's agriculture economy. The northern and eastern boundaries between desert and grassland are constantly changing. This is mostly due to the climate conditions before the growing season, which influence the rate of evapotranspiration and subsequent plant growth.[13] The expansion of the Gobi is attributed mostly to human activities, notably deforestation, overgrazing, and depletion of water resources. China
has tried various plans to slow the expansion of the desert, which have met with some small degree of success, but no major effects. The most recent plan involves the planting of the Green Wall of China, a huge ring of newly planted forests; the government hopes the forests will help stabilize the soil, retain moisture, and act as a buffer against further desertification.[14] Ecoregions
of the Gobi[edit] The Gobi, broadly defined, can be divided into five distinct dry ecoregions, based on variations in climate and topography.

Eastern Gobi desert steppe, the easternmost of the Gobi ecoregions, covering an area of 281,800 km2 (108,804 sq mi). It extends from the Inner Mongolian Plateau
in China
northward into Mongolia. It includes the Yin Mountains and many low-lying areas with salt pans and small ponds. It is bounded by the Mongolian-Manchurian grassland to the north, the Yellow River
Yellow River
Plain to the southeast, and the Alashan Plateau
semi-desert to the southeast and east. Alashan Plateau
semi-desert, lies west and southwest of the Eastern Gobi desert steppe. It consists of the desert basins and low mountains lying between the Gobi Altai range on the north, the Helan Mountains to the southeast, and the Qilian Mountains
Qilian Mountains
and northeastern portion of the Tibetan Plateau
Tibetan Plateau
on the southwest. Gobi Lakes Valley desert steppe, ecoregion lies north of Alashan Plateau
semi-desert, between the Gobi Altai range to the south and the Khangai Mountains
Khangai Mountains
to the north. Dzungarian Basin
Dzungarian Basin
semi-desert, includes the desert basin lying between the Altai mountains on the north and the Tian Shan
Tian Shan
range on the south. It includes the northern portion of China's Xinjiang
province and extends into the southeastern corner of Mongolia. The Alashan Plateau semi-desert lies to the east, and the Emin Valley steppe to the west, on the China- Kazakhstan
border. Tian Shan
Tian Shan
range, separates the Dzungarian Basin
Dzungarian Basin
semi-desert from the Taklamakan Desert, which is a low, sandy desert basin surrounded by the high mountain ranges of the Tibetan Plateau
Tibetan Plateau
to the south and the Pamirs
to the west. The Taklamakan Desert
ecoregion includes the Desert
of Lop.

Eastern Gobi desert steppe[edit]

A Khulan (Mongolian wild ass) on a hill in the eastern Gobi of Mongolia
at sunset.

The surface is extremely diversified, although there are no great differences in vertical elevation. Between Ulaanbaatar
(48°00′N 107°00′E / 48.000°N 107.000°E / 48.000; 107.000) and the small lake of Iren-dubasu-nor (43°45′N 111°50′E / 43.750°N 111.833°E / 43.750; 111.833), the surface is greatly eroded. Broad flat depressions and basins are separated by groups of flat-topped mountains of relatively low elevation 150 to 180 m (490 to 590 ft)), through which archaic rocks crop out as crags and isolated rugged masses. The floors of the depressions lie mostly between 900 to 1,000 m (3,000 to 3,300 ft) above sea-level. Farther south, between Iren-dutiasu-nor and the Yellow River, comes a region of broad tablelands alternating with flat plains, the latter ranging at altitudes of 1000–1100 m and the former at 1,070 to 1,200 m (3,510 to 3,940 ft). The slopes of the plateaus are more or less steep, and are sometimes penetrated by "bays" of the lowlands. As the border-range of the Hyangan is approached, the country steadily rises up to 1,370 m (4,490 ft) and then to 1,630 m (5,350 ft). Here small lakes frequently fill the depressions, though the water in them is generally salt or brackish. Both here and for 320 km (199 mi) south of Ulaanbaatar, streams are frequent and grass grows more or less abundantly. Through all the central parts, until the bordering mountains are reached, trees and shrubs are utterly absent. Clay and sand are the predominant formations; the watercourses, especially in the north, being frequently excavated 2 to 3 m (6 ft 7 in to 9 ft 10 in) deep. In many places in the flat, dry valleys or depressions farther south, beds of loess, 5 to 6 m (16 to 20 ft) thick, are exposed. 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 altitudes are higher, those of the lowlands ranging from 1,000 to 1,700 m (3,300 to 5,600 ft), and those of the ranges from 200 to 500 m (660 to 1,640 ft) higher, though in a few cases they reach altitudes of 2,400 m (7,900 ft). 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 Takla Makan
Takla Makan
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 taana wild onion Allium
polyrrhizum is the main browse eaten by many herd animals, and Mongolians claim that this is essential to produce the correct, slightly hazelnut-like flavour of camel airag (fermented milk). This great desert country of Gobi is crossed by several trade routes, some of which have been in use for thousands of years. Among the most important are those from Kalgan
(at the Great Wall) to Ulaanbaatar (960 km (597 mi)); from Jiuquan
(in Gansu) to Hami 670 km (416 mi); from Hami to Beijing (2,000 km (1,243 mi)); from Hohhot
to Hami and Barkul; and from Lanzhou
(in Gansu) to Hami. Alashan Plateau
semi-desert[edit] The southwestern portion of the Gobi, known also as the Hsi-tau and the Little Gobi, fills the space between the great north loop of the Yellow River
Yellow River
on the east, the Ejin River
Ejin River
on the west, and the Qilian Mountains and narrow rocky chain of Longshou, 3,200 to 3,500 m (10,500 to 11,500 ft) in altitude, on the southwest. 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. "Topographically," says Nikolai Przhevalsky, "it is a perfectly level plain, which in all probability once formed the bed of a huge lake or inland sea." He concludes this based on the level area of the region as a whole, the hard saldgine clay and the sand-strewn surface and, lastly, the salt lakes which occupy its lowest parts. 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.e. sky). 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. Although on the whole a level country with a general altitude of 1,000 to 1,500 m (3,300 to 4,900 ft), this section, like most other parts of the Gobi, is crowned by a chequered network of hills and broken ranges going up 300 m higher. 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, 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.g. the sandgrouse, lark, stonechat, sparrow, crane, Henderson's ground jay ( Podoces
hendersoni), horned lark (Eremophila alpestris), and crested lark (Galerida cristata). Dzungarian Basin
Dzungarian Basin

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.[15]

The Yulduz valley or valley of the Haidag-gol (43°N 83°E / 43°N 83°E / 43; 83–43°N 86°E / 43°N 86°E / 43; 86) is a mini desert enclosed by two prominent members of the Shanashen Trahen Osh mountain range, namely the chucis and the kracenard pine rallies, running perpendicular and far from one another. As they proceed south, they transcend and transpose, sweeping back on east and west respectively, with Lake Bosten
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. On its northern side, the Chol-tagh descends steeply, and its foot is fringed by a string of deep depressions, ranging from Lukchun (130 m (427 ft) below sea level) to Hami (850 m (2,789 ft) above sea-level). 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". It is some 130 to 160 km (81 to 99 mi) across from north to south, and is traversed by a number of minor parallel ranges, ridges and chains of hills. Down its middle runs a broad stony valley, 40 to 80 km (25 to 50 mi) wide, at an elevation of 900 to 1,370 m (2,950 to 4,490 ft). The Chol-tagh, which reaches an average altitude of 1,800 m (5,900 ft), is absolutely sterile, and its northern foot rests upon a narrow belt of barren sand, which leads down to the depressions mentioned above. 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
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 these chequered 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. To the highest range on the great swelling Grumm-Grzhimailo gives the name of Tuge-tau, its altitude being 2,700 m (8,858 ft) above the level of the sea and some 1,200 m (3,937 ft) above the crown of the swelling itself. This range he considers to belong to the Choltagh system, whereas Sven Hedin
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. In 91° east, while the principal range of the Kuruk-tagh system wheels to the east-northeast, four of its subsidiary ranges terminate, or rather die away somewhat suddenly, on the brink of a long narrow depression (in which Sven Hedin sees a northeast bay of the former great Central Asian lake of Lop-nor), having over against them the écheloned terminals of similar subordinate ranges of the Pe-shan (Boy-san) system (see below). 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 relatively favoured spots, is of the scantiest and is mainly confined to bushes of saxaul (Haloxylon), anabasis, reeds (kamish), tamarisks, poplars, and Ephedra. European exploration up to 1911[edit] 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 only very imperfectly known to outsiders, information being confined to observations by individual travellers from their respective itineraries across the desert. Among the European explorers who contributed to early-20th-century understanding of the Gobi, the most important were:

Jean-François Gerbillon
Jean-François Gerbillon
(1688–1698) Eberhard Isbrand Ides (1692–1694) Lorenz Lange (1727–1728 and 1736) Fuss and Alexander G. von Bunge (1830–1831) Hermann Fritsche (1868–1873) Pavlinov
and Z.L. Matusovski (1870) Ney Elias
Ney Elias
(1872–1873) Nikolai Przhevalsky
Nikolai Przhevalsky
(1870–1872 and 1876–1877) Zosnovsky (1875) Mikhail V. Pevtsov (1878) Grigory Potanin (1877 and 1884–1886) Count Béla Széchenyi and Lajos Lóczy (1879–1880) The brothers G. E. Grumm-Grshimailo (1889–1890) and ? Grumm-Grshimailo. Pyotr Kuzmich Kozlov
Pyotr Kuzmich Kozlov
(1893–1894 and 1899–1900) Vsevolod I. Roborovsky (1894) Vladimir Obruchev
Vladimir Obruchev
(1894–1896) Karl Josef Futterer and Dr. Holderer (1896) Charles-Etienne Bonin (1896 and 1899) Sven Hedin
Sven Hedin
(1897 and 1900–1901) K. Bogdanovich (1898) Ladyghin (1899–1900) and Katsnakov (1899–1900) Count Jacques Bouly de Lesdain and Martha Mailey, 1902.[16]

See also[edit]

Asian Dust Geography
of Mongolia Geography
of China Green Wall of China Legendary Mongolian death worm
Mongolian death worm
(olgoi khorkhoi), said to inhabit the Gobi in Mongolia List of deserts by area


^ a b Sternberg, Troy; Rueff, Henri; Middleton, Nick (2015-01-26). "Contraction of the Gobi Desert, 2000–2012". Remote Sensing. 7 (2): 1346–1358. doi:10.3390/rs70201346.  ^ Wright, John W., ed. (2006). The New York Times Almanac (2007 ed.). New York, New York: Penguin Books. p. 456. ISBN 0-14-303820-6.  ^ Hare, John (2009-11-01). "The Mysteries of the Gobi Desert". Asian Affairs. 40 (3): 408–417. doi:10.1080/03068370903195196. ISSN 0306-8374.  ^ Kielan-Jaworowska, Zofia (1975). "Late Cretaceous Mammals and Dinosaurs from the Gobi Desert: Fossils excavated by the Polish-Mongolian Paleontological Expeditions of 1963–71 cast new light on primitive mammals and dinosaurs and on faunal interchange between Asia
and North America". American Scientist. 63 (2): 150–159. doi:10.2307/27845359.  ^ Planet Earth, BBC TV series 2006 UK, 2007 US, "Episode 5". ^ "Climate". The Gobi Desert.  ^ Keqin, Gao; Norell, Mark A. (2000-03-01). "Taxonomic composition and systematics of late Cretaceous lizard assemblages from Ukhaa Tolgod and adjacent localities". Bulletin of the American Museum of Natural History. 249: 1–118. doi:10.1206/0003-0090(2000)2492.0.CO;2. ISSN 0003-0090.  ^ a b Liu, Ji-Liang; Li, Feng-Rui; Liu, Chang-An; Liu, Qi-Jun (2012-09-01). "Influences of shrub vegetation on distribution and diversity of a ground beetle community in a Gobi desert ecosystem". Biodiversity and Conservation. 21 (10): 2601–2619. doi:10.1007/s10531-012-0320-4. ISSN 0960-3115.  ^ Yiruhan, I. (2001). Changes in floristic composition of grasslands according to grazing intensity in inner Mongolia, China. Journal of Japanese Society of Grassland Science, 47, 362-369. ^ "Oyu Tolgoi Gold and Copper Project, Southern Mongolia". Archived from the original on February 21, 2009. Retrieved 2009-08-08.  ^ "Oyu Tolgoi". Archived from the original on 2013-02-01. Retrieved 2012-11-20.  ^ "Rio set to open mammoth Mongolian mine". Retrieved 2012-11-20.  ^ F. Yu, K. P. Price, J. Ellis, J. J. Feddema, P. Shi (2004). "Interannual variations of the grassland boundaries bordering the eastern edges of the Gobi Desert
in central Asia". International Journal of Remote Sensing. 25: 327–346. ^ Parungo, Farn; Zhe, Li; Xingsheng, LI; Yang, Dongzeng; Harris, Joyce (1994-06-01). "Gobi dust storms and The Great Green Wall". Geophysical Research Letters. 21 (11): 999–1002. doi:10.1029/94GL00879. ISSN 1944-8007.  ^ Lattimore (1973), p. 238. ^ "Romance Gone, Given Divorce". The Evening News. Harrisburg, Pennsylvania. July 28, 1926. p. 1. Retrieved October 4, 2016 – via Newspapers.com. (Registration required (help)). In 1902, while Lesdain was leading an expedition through the Gobi desert, he crossed the path of another explorer. This latter proved to be Miss Mailey who, dressed in men's clothes, commanded her expedition with assurance borne of the safe culmination of many adventures. 


 This article incorporates text from a publication now in the public domain: Chisholm, Hugh, ed. (1911). "Gobi". Encyclopædia Britannica. 12 (11th ed.). Cambridge University Press. p. 165.  Owen Lattimore. (1973) "Return to China's Northern Frontier". The Geographical Journal, Vol. 139, No. 2 (June 1973), pp. 233–242.

Further reading[edit]

Cable, Mildred and French, Francesca (1943) The Gobi Desert Landsborough Publications, London, OCLC 411792. Man, John (1997) Gobi: Tracking the Desert
Yale University Press, New Haven, ISBN 0-300-07609-6. Stewart, Stanley (2001) In the Empire of Genghis Khan: A Journey among Nomads HarperCollins Publishers, London, ISBN 0-00-653027-3. Thayer, Helen (2007) Walking the Gobi: 1,600 Mile-trek Across a Desert of Hope and Despair Mountaineer Books, Seattle, WA, ISBN 978-1-59485-064-6. Younghusband, Francis (1904) The Heart of a Continent, John Murray.

External links[edit]

Wikimedia Commons has media related to Gobi Desert.

Map, from " China
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Kopet Dag semi-desert

Iran Turkmenistan

Mesopotamian shrub desert

Iraq Jordan Syria

Paropamisus xeric woodlands


Rigestan-North Pakistan
sandy desert

Afghanistan Iran Pakistan

South Iran
Nubo-Sindian desert and semi-desert

Iran Iraq Pakistan

Central Asia

shrub desert and steppe

Azerbaijan Georgia Iran

Caspian lowland desert

Iran Kazakhstan Russia Turkmenistan

Central Asian northern desert

Kazakhstan Uzbekistan

Central Asian riparian woodlands


Central Asian southern desert

Kazakhstan Turkmenistan Uzbekistan

Kazakh semi-desert


Eastern Asia

Alashan Plateau

China Mongolia

Eastern Gobi desert steppe

China Mongolia

Gobi Lakes Valley desert steppe


Great Lakes Basin desert steppe

Mongolia Russia

Junggar Basin semi-desert

China Mongolia

Qaidam Basin
Qaidam Basin


Taklamakan Desert


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Desert Desertification List of deserts List of deserts by area


Algerian Bayuda Blue Chalbi Danakil Djurab Eastern Ferlo Farafra (White) Kalahari Libyan Moçâmedes Namib Nubian Nyiri Owami Richtersveld Sahara Tanezrouft Ténéré Western


Ad-Dahna Akshi Arabian Aral Karakum Aralkum Badain Jaran Betpak-Dala Cholistan Dasht-e Kavir Dasht-e Khash Dasht-e Leili Dasht-e Loot Dasht-e Margo Dasht-e Naomid Gurbantünggüt Gobi Hami Indus Valley Judaean Karakum Katpana Kharan Kumtag Kyzylkum Lop Maranjab Muyunkum Nefud Negev Polond Ordos Qaidam Ramlat al-Sab'atayn Rub' al Khali Russian Arctic Registan Saryesik-Atyrau Syrian Taklamakan Tengger Thal Thar Ustyurt Plateau Wahiba Sands


Gibson Great Sandy Great Victoria Little Sandy Nullarbor Plain Painted Pedirka Simpson Strzelecki Sturt's Stony Tanami Tirari


Accona Bardenas Reales Błędów Cabo de Gata Deliblatska Peščara Hálendi Monegros Oleshky Oltenian Sahara Ryn Stranja Tabernas

North America

Alvord Amargosa Baja California Black Rock Carcross Carson Channeled scablands Chihuahuan Colorado Escalante Forty Mile Gran Desierto de Altar Great Basin Great Salt Lake Great Sandy Jornada del Muerto Kaʻū Lechuguilla Mojave North American Arctic Owyhee Painted Desert Red Desert Sevier Smoke Creek Sonoran Tonopah Desert Tule (Arizona) Tule (Nevada) Yp Yuha Yuma

South America

Atacama La Guajira Los Médanos de Coro Monte Patagonian Sechura Tatacoa


Rangipo Desert

Polar Regions

Antarctica Arctic Greenland North American Arctic Russian Arctic

Project Category Commons

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History Index Outline



Agricultural Behavioral Cultural Development Economic Health Historical Political Population Settlement

Regional Urban



Ecology Phytogeography Zoogeography

Coastal / Oceanography Earth science

Atmospheric science
Atmospheric science
/ Meteorology Environmental science Climatology
/ Paleoclimatology
/ Palaeogeography Geobiology Geophysics
/ Geodesy

Earth system science Geomorphology
/ Geology Glaciology Hydrology
/ Limnology Pedology (Edaphology/Soil science) Quaternary science


Integrated / Environmental

Environmental social science Environmental studies Landscape architecture Landscape ecology

Time geography

Techniques and tools

/ Geomathematics

Cartography Geologic modelling Geostatistics Geographic information system

Geochronology Geomatics Hydrography

Photogrammetry Remote sensing


Geographic data and information organizations Geographical societies Geoscience societies National mapping agency



Geo-literacy International Geography
Olympiad MSc in Geographic Information Science/Systems Spatial citizenship

Category Portal Commons WikiProject

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Physical geography

Atmospheric science
Atmospheric science
/ Meteorology Biogeography
/ Phytogeography Climatology
/ Paleoclimatology
/ Palaeogeography Coastal geography
Coastal geography
/ Oceanography Edaphology
/ Pedology or Soil science Geobiology Geology Geomorphology Geostatistics Glaciology Hydrology
/ Limnology Landscape ecology Quaternary science

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Mongolia articles


Timeline Prehistoric Mongolia Proto-Mongols Xiongnu Xianbei Rouran Khaganate Liao dynasty Medieval tribes Mongol
Empire Yuan rule Northern Yuan dynasty Four Oirat Dzungar Khanate Qing rule 1911 Revolution Bogd Khanate Occupation of Mongolia 1921 Revolution Mongolian People's Republic 1990 Revolution Modern Mongolia Anthem Flag Soyombo symbol



Ulaanbaatar Historical cities and towns

Climate Fauna

Birds Mammals

Flora Gobi Desert Grassland Lakes

Khövsgöl Uvs


Altai Khangai Khentii

National parks Rivers

Selenga Orkhon


Administrative divisions

Aimags Sums

Constitution Elections Foreign relations

Third neighbor policy

Human rights Military

Nuclear-Weapons-Free Status

Political parties President


Prime Minister

list Mongolian People's Party Democratic Party

State Great Khural
State Great Khural
(parliament) Supreme Court Visa policy


Economic history 1921–92 Agriculture Banking

Central Golomt

Companies International rankings Stock Exchange Tögrög (currency) Tourism Transportation


Demographics Mongols

Khalkha Buryats Oirats Southern Mongols

Education Language Public holidays List of Mongolians Women Writing systems


Architecture Biyelgee
(dance) Cinema Cuisine Goyol Fashion Festival Literature Media Traditional medicine Music

Morin khuur Long song Throat singing

(festival) Religion

Buddhism Islam Christianity

Tsagaan Sar
Tsagaan Sar
(New Year's Day) Sport

Mongolian wrestling

Outline Index

Book Category Portal

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Inner Mongolia



History Politics Independence movement Economy Administrative divisions


Cities Gobi Desert Tengger Desert Climate


Inner Mongolia
University Inner Mongolia
Normal University Chifeng University


Music of Inner Mongolia Mongolian language Mongolian script Northeastern Mandarin Plain Blue Banner


Hot pot

Visitor attractions

Shiretu Juu Zhaojun Tomb Mausoleum of Genghis Khan Hexigten Global Geopark

Category Commons

Authority control

WorldCat Identities VIAF: 243456761 GND: 4093637-5 NDL: 00628517

Coordinates: 42°35′N 103°26′E / 42.59°N 103.43°E / 4