Everything about Gobi Desert totally explained
The
Gobi (
Chinese:
Gēbì (Shāmò);,
Govi or
Gov', meaning, gravel-covered plain) is the largest
desert region in
Asia. It covers area in China and 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
Tibetan Plateau to the southwest, and by the
North China Plain to the southeast. The Gobi is made up of several distinct ecological and geographic regions based on variations in climate and topography. This desert is the
fourth largest in the world.
The Gobi is most 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 Himalaya range blocking rain-carrying clouds from reaching the Gobi.
Geography
The Gobi measures over from southwest to northeast and from north to south. The desert is widest in the west, along the line joining the
Baghrash Kol and the
Lop Nor (87°-89° east). It occupies an arc of land in area, making it fourth largest in the world and Asia's largest. Much of the Gobi isn't sandy but is covered with bare rock.
The Gobi has several different Chinese names, including 沙漠 (shāmò, actually a generic term for deserts in general) and 旱海 (hànhǎi, dry sea). In its broadest definition, the Gobi includes the long stretch of desert and semidesert country extending from the foot of the
Pamirs, 77° east, to the
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 Shan,
Altun Shan, and
Qilian shan ranges, which form the northern edges of the Tibetan Plateau, on the south.
A relatively large area on the east side of the Greater Khingan range, between the upper waters of the
Songhua (Sungari) and the upper waters of the Liao-ho, is also reckoned to belong to the Gobi by conventional usage. On the other hand,
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 and Hami (
Kumul) as forming a separate and independent desert, called the
Taklamakan Desert.
The
Nemegt Basin in the northwestern part of the Gobi Desert (in Mongolia) is famous for its
dinosaur fossil treasures.
Climate
The Gobi desert is a cold desert, and it isn't uncommon to see frost and occasionally snow on its dunes. Besides being quite far north, it's also roughly 900 meters (2,953 ft) above sea level, which further contributes to its low temperatures. An average of approximately 194 millimeters (7.6 in) of rain falls per year 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 cause the Gobi to reach extremes of temperature ranging from –40°C (-15°F) in Winter to +50°C in Summer.
Climate (as of 1911)
The
climate of the Gobi is one of great extremes, combined with rapid changes of
temperature, not only through the year but even within 24 hours (by as much as 32 °C or 58 °F).
Temperature>
|
Ulaanbaatar (1150 m) |
Sivantse (1190 m) |
| Annual mean |
-2.5 °C (27 °F) |
2.8 °C (37 °F) |
| January mean |
-26.5 °C (-15.7 °F) |
-16.5 °C (2 °F) |
| July mean |
17.5 °C (63.5 °F) |
19.0 °C (66 °F) |
| Extremes |
38.0 °C and -43 °C (100 °F and -45 °F) |
33.9 °C and -47 °C (93 °F and -52 °F) |
Even in southern Mongolia the
thermometer goes down as low as -32.8 °C (-27 °F), and in Ala-shan it rises as high as 37 °C (98.6 °F) in July.
Average winter minimals are a frigid -40 °C (-40 °F) while summertime temperatures are warm to hot, highs range up to 50 °C (112 °F). Most of the
precipitation falls during the summer.
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. Hence, the icy
sandstorms and
snowstorms of spring and early summer plus early January (winter)
Conservation, ecology, economy
The Gobi Desert is the source of many important fossil finds, including the first dinosaur
eggs.
These deserts and the surrounding regions sustain many animals, including
black-tailed gazelles,
marbled polecats,
bactrian camels and
sandplovers, and are occasionally visited by
snow leopards,
brown bears, and
wolves. The desert features a number of drought-adapted shrubs such as
gray sparrow's saltwort,
gray sagebrush, and low grasses such as
needle grass and
bridlegrass.
The area is vulnerable to trampling by
livestock and off-road vehicles (human impacts are greater in the eastern Gobi Desert, where rainfall is heavier and may sustain livestock). In Mongolia, grasslands have been degraded by goats, raised by nomadic herders as source of
cashmere wool. Economic trends of livestock privatization and the collapse of the
urban economy have caused people to return to
rural lifestyles, a movement contrary to
urbanization. This movement has resulted in a great increase of nomadic herder population and livestock raising.
Large copper and gold deposits are located at
Oyuu Tolgoi, about 80 kilometers from the Chinese border into Mongolia and the feasibility of setting up a mining operation is being investigated.
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Desertification
Currently, 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 of grassland overtaken every year by the Gobi Desert. This loss of farmland has caused an estimated $50 billion in losses each year for China's economy. Dust storms, which were once a rarity, are springing up all over China, and could cause even further damage to China's agriculture economy.
The expansion of the Gobi is attributed mostly to human activities, notably
deforestation,
overgrazing, overconsumption of water resources, and
global warming. China has made various plans to try to slow the expansion of the desert, which have met with some small degree of success, but usually have no major impact. The most recent plan involves the planting of the
Green Wall of China, a huge ring of newly-planted forests that the Chinese government hopes will act as a buffer against further expansion.
Ecoregions of the Gobi
The Gobi, broadly defined, can be divided into five distinct dry
ecoregions.
The
'Eastern Gobi desert steppe' is the easternmost of the Gobi ecoregions, covering an area of . 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 Plain to the southeast, and the Alashan Plateau semi-desert to the southeast and east.
The
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 Altay range on the north, the
Helan Mountains to the southeast, and the
Qilian Mountains and northeastern portion of the Tibetan Plateau on the southwest.
The
Gobi Lakes Valley desert steppe ecoregion lies north of Alashan Plateau semi-desert, between the Gobi Altay range to the south and the
Khangai Mountains to the north.
The
Junggar Basin semi-desert includes the desert basin lying between the Altay mountains on the north and the
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.
The
Tian Shan range separates the Junggar Basin semi-desert from the
Taklamakan Desert, which is a low, sandy desert basin surrounded by the high mountain ranges of the Tibetan Plateau to the south and the
Pamirs to the west. The Taklamakan Desert ecoregion includes the
Desert of Lop.
Eastern Gobi desert steppe
Here the surface is extremely diversified, although there are no great differences in vertical elevation. Between Ulaanbaatar (48° N 107° E) and the little lake of Iren-dubasu-nor the surface is greatly eroded, and consists of broad flat depressions and basins separated by groups of flat-topped mountains of relatively low elevation (150-180 m), through which archaic rocks crop out as crags and isolated rugged masses. The floors of the depressions lie mostly between 900-1000 m above sea-level. Farther south, between Iren-dutiasu-nor and the
Hwang-ho comes a region of broad tablelands alternating with flat plains, the latter ranging at altitudes of 1000-1100 m and the former at 1070-1200 m. 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 1370 m and then to 1630 m. Here small lakes frequently fill the depressions, though the water in them is generally salt or brackish. Both here and for south of Ulaanbaatar, streams are frequent and grass grows more or less abundantly. There is, however, through all the central parts, until the bordering mountains are reached, an utter absence of trees and shrubs. Clay and sand are the predominant formations, the watercourses, especially in the north, being frequently excavated 2-3 m deep, and in many places in the flat, dry valleys or depressions farther south beds of
loess, 5-6 m 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 too are higher, those of the lowlands ranging from 1000-1700 m, and those of the ranges from 200-500 m higher, though in a few cases they reach altitudes of 2400 m. The elevations do not, however, 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 tablelards, built up of the horizontal red deposits of the Han-gai (Ohruchev'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, and are then greatly intersected by gullies or dry watercourses. Here there is, however, a great dearth of water, no streams, no lakes, no wells, arid precipitation falls but seldom. The prevailing winds blow from the west and northwest and the pall of dust overhangs the country as in the 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 on the frontier of China to Ulaanbaatar, from
Jiuquan (in
Gansu) to Hami from Hami to Beijing, from
Hohhot to Hami and Barkul, and from
Lanzhou (in Gansu) to Hami.
Ala Shan Plateau semi-desert
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 on the east, the
Ejin River on the west, and the
Qilian Mountains and narrow rocky chain of
Longshou (Ala-shan), 3200-3500 m in altitude, on the southwest. The
Ordos Desert, which covers the northeastern portion of the Ordos Plateau, in the great north loop of the Huang He, 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
Przhevalsky, "it is a perfectly level plain, which in all probability once formed the bed of a huge lake or inland sea." The data upon which he bases this conclusion are 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 there's nothing to be seen but bare sands; in some places they continue so far without a break that the Mongols call them Tengger (for example 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 1000 to 1500 m, 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 else except antelopes, the wolf, fox, hare, hedgehog, marten, numerous lizards and a few birds, for example the sandgrouse, lark, stonechat, sparrow, crane,
Henderson's Ground Jay (Podoces hendersoni),
Horned Lark (Eremophila alpestris), and
Crested Lark (Galerida cristata). The only human inhabitants of Ala-shan are the
Torguud Mongols.
The Gobi is also home to the rare Bactrian camel. This eats snow to maintain its fluid level and must limit itself to 10 litres a day of snow if it isn't to prove fatal. Poaching has made these animals highly fearful of people.
Junggar Basin semi-desert
The Yulduz valley or valley of the Haidag-gol (43° N 83°-86° E) 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 transend and transpose, sweeping back on east and west, respectively so as to leave room for the
Baghrash-kol. 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 (below sea level) to
Hami (above sea-level). To the south of the Kuruk-tagh lie the
desert of Lop (= desert of
Lop Nur), the desert of
Kum-tagh, 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 across from north to south, and is traversed by a number of minor parallel ranges, ridges and chains of hills, and down its middle runs a broad stony valley, 40-80 km wide, at an elevation of 900 to 1370 m. The Chol-tagh, which reaches an average altitude of 1800 m, 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 formerly was of incomparably greater magnitude. In the west, between
Baghrash-kol 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's 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've cut their way through one or more of the transverse barrier ranges. To the highest range on the great swelling
Gruni-Grzhimailo gives the name of
Tuge-tau, its altitude being above the level of the sea and some above the crown of the swelling itself. 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 Baghrash-kol, though parted from it by the drift-sand desert of
Ak-bel-kum (White Pass Sands), has at first a westnorthwest to eastsoutheast strike, but it gradually curves round like a scimitar towards the eastnortheast and at the same time gradually decreases in elevation. In 91° east, while the principal range of the Kuruk-tagh system wheels to the eastnortheast, 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
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 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 the observations which individual travellers had made from their respective itineraries across the desert. Amongst the European explorers who contributed to early 20th century understanding of the Gobi, the most important were:
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