TheKumtag Desert (Chinese:库姆塔格沙漠;pinyin:Kùmǔtǎgé Shāmò;Uyghur:قۇمتاغ قۇملۇقى,romanized: Qumtagh Qumluqi) is an arid landform innorthwestern China. It was proclaimed as anational park in 2002.
The ovalTarim Basin with its centralTaklamakan Desert is bounded on the north, west, and south by mountains. On the east side the Kumtag is an unbroken plain about 100 miles from north to south that runs from the Taklamakan toGansu province and Mongolia. Many modern maps do not show a Kumtag in this sense, which implies that the usage may be out of date.
The Kumtag Desert is a section of theTaklamakan Desert that lies east-southeast of theDesert of Lop. It is bordered byDunhuang in the east,Tian Shan in the north and has an area of more than 22,800 square kilometers. Its southern rim is marked by a labyrinth of hills, dotted in groups and irregular clusters. Between these and theAltyn-Tagh is a broad latitudinal valley, seamed with watercourses that come down from the foothills of the Altyn-tagh. Grapes and other crops are grown in oases in low-lying areas. Elsewhere, the desert supports scrubby desert plants, water reaching them in some instances at intervals of years only. This part of the desert has a general slope northwest towards the relative depression of theKara-koshun. A noticeable feature of the Kumtag is the presence of large accumulations of drift-sand, especially along the foot of the desert ranges, where it rises into dunes sometimes as much as 250 feet (76 m) in height and climbs the flanks of ranges themselves.[1]
Administratively, the desert is located in theRuoqiang (Qakilik) County of Xinjiang andAksai Kazakh Autonomous County andDunhuang City ofGansu, near their border withQinghai.
A map published by the National Geographic Society[2] shows a much smaller Kumtag. This is a rectangle with a northwest corner south ofLop Nor, a southern edge along theAltyn-Tagh and an eastern edge just beyond the Gansu border. Near the northeast corner is theJade Gate which is often taken as the western end of the Great Wall. From space it appears as a belt of orange sand dunes. This is probably the 2500 square kilometer area mentioned below.
The Kumtag Desert is expanding and threatening to engulf previously productive lands with its arid wasteland character.[3] Several years prior the estimated size of the desert was 2500 square kilometres, but with recent expansion, the Kumtag Desert is already considerably larger as of 2008.
The Kumtag Desert is continuing a process of expansion that is the result of centuries ofovergrazing of this region that is beyond its carrying capacity. According to the AFP news report of November, 2007: "Towering sand dunes [of the Kumtag Desert] loom over the ancient Chinese city ofDunhuang".[3] According to Hogan: "Rapid expansion of the Kumtag Desert and other dunes formations threaten to engulfYungang and other archaeological sites"; moreover, thedesertification adjacent to the Kumtag Desert is part of a larger problem in northern China where the present rate of desertification in this single region of China (e.g. Northern China) now exceeds 1,000 square miles (2,600 km2) per annum.[4] To mitigate the desertification, the town of Dunhuang has placedsevere limitations on immigration, and has also placed restrictions on new water-well development or new farm additions.[3]
The prevailing winds in this region blow from the west and northwest during the summer, winter and autumn. Though in spring, when they are more violent, they come from the northeast, as in the desert of Lop. The arrangement of the sand here agrees perfectly with the law laid down byGrigory Potanin, that in the basins ofCentral Asia the sand is heaped up in greater mass on the south, all along the bordering mountain ranges where the floor of the depressions lies at the highest level. The country to the north of the desert ranges is thus summarily described bySven Hedin: "The first zone of drift sand is succeeded by a region that exhibits proofs of wind modelling on an extraordinarily energetic and well-developed scale, the results corresponding to the jardangs and the wind-eroded gullies of theDesert of Lop. Both sets of phenomena lie parallel to one another; from this we may infer that the winds which prevail in the two deserts are the same. Next comes, sharply demarcated from the zone just described, a more or less thin kamishsteppe growing on level ground; and this in turn is followed by another very narrow belt ofsand, immediately south of Achik-kuduk Finally in the extreme north we have the characteristic and sharply defined belt of kamish steppe, stretching from east-northeast to west-southwest and bounded on north and south by high, sharp cut clay terraces.
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"At the points where we measured them the northern terrace was 113 feet (34 m) high and the southern 853/4 feet....Both terraces belong to the same level, and would appear to correspond to the shore lines of a big bay of the last surviving remnant of the Central Asian Mediterranean. At the point where I crossed it the depression was 6 to 7 miles (11 km), wide, and thus resembled a flat valley or immense river-bed."[1][5]
The moving sands of the Kumtag are of a concern for the designers of theGolmud–Dunhuang Railway, which will cross the eastern edge of this desert in the Shashangou area, between Dunhuang and theAltyn-Tagh-Qilian mountain system. There was a concern that the "megadunes" characteristic of this area may shift, burying the railway. However, geological research indicated that the "megadunes" are mostly formed by solid subsoil, rather than just sand. Although there is still the issue of drifting sand, it is thought by the experts that the sand is mostly blown along the direction of the future railway rather than across it, and can be handled with certain precautions.[6]
One or more of the preceding sentences incorporates text from a publication now in thepublic domain: Bealby, John Thomas (1911). "Gobi,s.v.Desert of Kum-Tagh". InChisholm, Hugh (ed.).Encyclopædia Britannica. Vol. 12 (11th ed.). Cambridge University Press. p. 166.
42°42′00″N90°16′00″E / 42.7°N 90.2667°E /42.7; 90.2667
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