The continental equivalent of the chimere is thezimarraorsimarre, which is defined by foreign ecclesiologists (Moroni, Barbier de Montault) as a kind ofsoutane(cassock), from which it is distinguished by having a small cape and short, open arms (manches-fausses) reaching to the middle of the upper arm and decorated with buttons. In France and Germany it is fitted more or less to the figure; in Italy it is wider and falls down straight in front. Like thesoutane, thezimarrais not proper to any particular rank of clergy, but in the case of bishops and prelates it is ornamented with red buttons and bindings. It never has a train (cauda). It is not universally worn,e.g.in Germany apparently only by prelates. G. Moroni identifies thezimarrawith theepitogiumwhich Domenico Magri, in hisHierolexicon(ed. 1677), calls the uppermost garment of the clergy, worn over thesoutane(toga) instead of themantellum(vestis suprema clericorum loco pallii), with a cross-reference toTabardum, the “usual” upper garment (pallium usuale); and this definition is repeated in the 8th edition of the work (1732). From this it appears that so late as the middle of the 18th century thezimarrawas still in common use as an out-of-doors overcoat. But, according to Moroni, by the latter half of the 19th century thezimarra, though still worn by certain civilians (e.g.notaries and students), had become in Italy chiefly the domestic garment of the clergy, notably of superiors, parish priests, rectors, certain regulars, priests of congregations, bishops, prelates and cardinals. It was worn also by the Roman senators, and is still worn by university professors. A blackzimarralined with white, and sometimes ornamented with a white binding and gold tassels, is worn by the pope.More analogous to the Anglican chimere in shape, though not in significance, is the purplemantelletumworn over the rochet by bishops, and by others authorized to wear the episcopal insignia, in presence of the pope or his legates. This symbolizes the temporary suspension of the episcopal jurisdiction (symbolized by the rochet) so long as the pope or his representative is present. Thus at the Curia cardinals and prelates wear themantelletum, while the pope wears thezimarra, and the first act of the cardinal camerlengo after the pope’s death is to expose his rochet by laying aside themantelletum, the other cardinals following his example, as a symbol that during the vacancy of the papacy the pope’s jurisdiction is vested in the Sacred College. On the analogy of themantelletumcertain Anglican prelates, American and colonial, have from time to time appeared in purple chimeres; which, as the Rev. N.F. Robinson justly points out, is a most unhappy innovation, since it has no historical justification, and its symbolism is rather unfortunate.Authorities.—See theReportof the sub-committee of Convocation on the ornaments of the church and its ministers, p. 31 (London, 1908); the Rev. N.F. Robinson, “The black chimere of Anglican Prelates: a plea for its retention and proper use,” inTransactions of the St Paul’s Ecclesiological Soc.vol. iv. pp. 181-220 (London, 1898); Herbert Druitt,Costume on Brasses(London, 1906); G. Moroni,Dizionario dell’ erudizione storico-ecclesiastica(Venice, 1861), vol. 103, s.v. “Zimarra”: X. Barbier de Montault,Traité pratique de la construction, &c., des églises, ii. 538 (Paris, 1878).
The continental equivalent of the chimere is thezimarraorsimarre, which is defined by foreign ecclesiologists (Moroni, Barbier de Montault) as a kind ofsoutane(cassock), from which it is distinguished by having a small cape and short, open arms (manches-fausses) reaching to the middle of the upper arm and decorated with buttons. In France and Germany it is fitted more or less to the figure; in Italy it is wider and falls down straight in front. Like thesoutane, thezimarrais not proper to any particular rank of clergy, but in the case of bishops and prelates it is ornamented with red buttons and bindings. It never has a train (cauda). It is not universally worn,e.g.in Germany apparently only by prelates. G. Moroni identifies thezimarrawith theepitogiumwhich Domenico Magri, in hisHierolexicon(ed. 1677), calls the uppermost garment of the clergy, worn over thesoutane(toga) instead of themantellum(vestis suprema clericorum loco pallii), with a cross-reference toTabardum, the “usual” upper garment (pallium usuale); and this definition is repeated in the 8th edition of the work (1732). From this it appears that so late as the middle of the 18th century thezimarrawas still in common use as an out-of-doors overcoat. But, according to Moroni, by the latter half of the 19th century thezimarra, though still worn by certain civilians (e.g.notaries and students), had become in Italy chiefly the domestic garment of the clergy, notably of superiors, parish priests, rectors, certain regulars, priests of congregations, bishops, prelates and cardinals. It was worn also by the Roman senators, and is still worn by university professors. A blackzimarralined with white, and sometimes ornamented with a white binding and gold tassels, is worn by the pope.
More analogous to the Anglican chimere in shape, though not in significance, is the purplemantelletumworn over the rochet by bishops, and by others authorized to wear the episcopal insignia, in presence of the pope or his legates. This symbolizes the temporary suspension of the episcopal jurisdiction (symbolized by the rochet) so long as the pope or his representative is present. Thus at the Curia cardinals and prelates wear themantelletum, while the pope wears thezimarra, and the first act of the cardinal camerlengo after the pope’s death is to expose his rochet by laying aside themantelletum, the other cardinals following his example, as a symbol that during the vacancy of the papacy the pope’s jurisdiction is vested in the Sacred College. On the analogy of themantelletumcertain Anglican prelates, American and colonial, have from time to time appeared in purple chimeres; which, as the Rev. N.F. Robinson justly points out, is a most unhappy innovation, since it has no historical justification, and its symbolism is rather unfortunate.
Authorities.—See theReportof the sub-committee of Convocation on the ornaments of the church and its ministers, p. 31 (London, 1908); the Rev. N.F. Robinson, “The black chimere of Anglican Prelates: a plea for its retention and proper use,” inTransactions of the St Paul’s Ecclesiological Soc.vol. iv. pp. 181-220 (London, 1898); Herbert Druitt,Costume on Brasses(London, 1906); G. Moroni,Dizionario dell’ erudizione storico-ecclesiastica(Venice, 1861), vol. 103, s.v. “Zimarra”: X. Barbier de Montault,Traité pratique de la construction, &c., des églises, ii. 538 (Paris, 1878).
(W. A. P.)
CHIMESYAN(Tsimshian), a tribe of North American Indians, now some 3000 in number, living around the mouth of the Skeena river, British Columbia, and on the islands near the coast. They are a powerfully built people, who tattoo and wear labrets and rings in noses and ears. They are skilful fishermen, and live in large communal houses. They are divided into clans and distinct social orders.
CHIMKENT, a town of Asiatic Russia, in the province of Syr-darya, 70 m. by rail N.N.E. of Tashkent. Pop. (1897) 10,756, mostly Sarts. It occupies a strategical position at the west end of the valley between the Alexander range and the Ala-tau (or Talas-tau), at the meeting of commercial routes from (1) Vyernyi and Siberia beyond, from the north-east, (2) the Aral Sea and Orenburg (connected with it by rail since 1905) to the north-west, and (3) Ferghana and Bokhara to the south. The citadel, which was stormed by the Russians in 1864, stands on high ground above the town, but is now in ruins. Chimkent is visited by consumptive patients who wish to try the koumiss cure. It has cotton mills and soap-works.
CHIMNEY(through the Fr.cheminée, fromcaminata, sc.camera, a Lat. derivative ofcaminus, an oven or furnace), in architecture, that portion of a building, rising above the roof, in which are the flues conveying the smoke to the outer air. Originally the term included the fireplace as well as the chimney shaft. At Rochester Castle (1130) and Heddington, Essex, there were no external chimney shafts, and the flue was carried through the wall at some height above the fireplace. In the early examples the chimney shaft was circular, with one flue only, and was terminated with a conical cap, the smoke issuing from openings in the side, which at Sherborne Abbey (A.D.1300) were treated decoratively. It was not till the 15th century that the smoke issued at the top, and later in the century that more than one flue was carried up in the same shaft. There are a few examples of the clustered shaft in stone, but as a rule they are contemporaneous with the general use of brick. The brick chimney shafts, of which there are fine specimens at Hampton Court, were richly decorated with chevrons and other geometrical patterns. One of the best examples is that at Thornton Castle, Gloucestershire.
In the 15th and 16th centuries in France the chimney shaft was recognized as an important architectural feature, and was of considerable elevation in consequence of the great height of the roofs. In the château of Meillant (1503) the chimney shafts are decorated with angle buttresses, niches and canopies, in the late Flamboyant style; and at Chambord and Blois they are carved with pilasters and niches with panelling above, carved with the salamander and other armorial devices. In the Roman palaces they are sometimes masked by the balustrades, and (when shown) take the form of sepulchral urns, as if to disguise their real purpose. Though not of a very architectural character, the chimneys at Venice present perhaps the greatest variety of terminations, and as a rule the smoke comes out on the sides and not through the top.
(R. P. S.)
Factory Chimneys.—Chimneys, besides removing the products of combustion, also serve to provide the fire with the air requisite for burning the fuel. The hot air in the shaft, being lighter than the cold air outside it, tends to rise, and as it does so air flows in at the bottom to take its place. An ascending current is thus established in the chimney, its velocity, other things being equal, varying as the square root of the height of the shaft above the grate. The velocity also increases with increase of temperature in the gas column, but since the weight of each cubic foot grows less as the gases expand, the amount of smoke discharged by a chimney does not increase indefinitely with the temperature; a maximum is reached when the difference in temperature between the gases in the shaft and the outside air is about 600° F., but the rate of increase is very slow after the difference has passed about 300° F. In designing a chimney the dimensions (height and sectional area) have to be so proportioned to the amount of fuel to be burnt in the various furnaces connected with it that at the temperature employed the products of combustion are effectively removed, due allowance being made for the frictional retardation of the current against the sides of the flues and shafts and in passing through the fire. The velocity of the current in actual chimneys varies widely, from 3 or 4 to 50 or 60 ft. a second. Increased velocity, obtainable by increasing the height of the shaft, gives increased delivering capacity, but a speed of 10 or 12 ft. a second is regarded as good practice. Ordinary factory chimneys do not in general exceed 180 or 200 ft. in height, but in some cases, especially when, as in chemical works, they are employed to get rid of objectionable vapours, they have been made double that height, or even more. In section they are round, octagonal or square. The circular form offers the least resistance to wind pressure, and for a given height and sectional area requires less material to secure stability than the octagonal and still less than the square; on the other hand, there is more liability to cracking. Brick is the material commonly used, but many chimneys are now made of iron or steel. Reinforced concrete is also employed.
Factory Chimneys.—Chimneys, besides removing the products of combustion, also serve to provide the fire with the air requisite for burning the fuel. The hot air in the shaft, being lighter than the cold air outside it, tends to rise, and as it does so air flows in at the bottom to take its place. An ascending current is thus established in the chimney, its velocity, other things being equal, varying as the square root of the height of the shaft above the grate. The velocity also increases with increase of temperature in the gas column, but since the weight of each cubic foot grows less as the gases expand, the amount of smoke discharged by a chimney does not increase indefinitely with the temperature; a maximum is reached when the difference in temperature between the gases in the shaft and the outside air is about 600° F., but the rate of increase is very slow after the difference has passed about 300° F. In designing a chimney the dimensions (height and sectional area) have to be so proportioned to the amount of fuel to be burnt in the various furnaces connected with it that at the temperature employed the products of combustion are effectively removed, due allowance being made for the frictional retardation of the current against the sides of the flues and shafts and in passing through the fire. The velocity of the current in actual chimneys varies widely, from 3 or 4 to 50 or 60 ft. a second. Increased velocity, obtainable by increasing the height of the shaft, gives increased delivering capacity, but a speed of 10 or 12 ft. a second is regarded as good practice. Ordinary factory chimneys do not in general exceed 180 or 200 ft. in height, but in some cases, especially when, as in chemical works, they are employed to get rid of objectionable vapours, they have been made double that height, or even more. In section they are round, octagonal or square. The circular form offers the least resistance to wind pressure, and for a given height and sectional area requires less material to secure stability than the octagonal and still less than the square; on the other hand, there is more liability to cracking. Brick is the material commonly used, but many chimneys are now made of iron or steel. Reinforced concrete is also employed.
CHIMNEYPIECE, the term given to the projecting hood which in medieval times was built over a fireplace to catch the smoke, and at a later date to the decorative framework, often carried up to the ceiling. “Chimneypiece” or “mantelpiece” is now the general term for the jambs, mantelshelf and external accessories of a fireplace. For many centuries the chimneypiece was the most ornamental and most artistic feature of a room, but as fireplaces have become smaller, and modern methods of heating have been introduced, its artistic as well as its practical significance has grown less.
Up to the 12th century rooms were warmed entirely by a hypocaust, or with braziers, or by fires on the hearth, the smoke finding its way up to a lantern in the roof. The earliest chimneypiece known is that in the King’s House at Southampton, with Norman shafts in the joints carrying a segmental arch, which is attributed to the first half of the 12th century. At a later date, in consequence of the greater width of the fireplace, flat or segmental arches were thrown across and constructed with voussoirs, sometimes joggled, the thrust of the arch being resisted by bars of iron at the back. In domestic work of the 14th century the chimneypiece was greatly increased in order to allow of the members of the family sitting on either side of the fire on the hearth, and in these cases great beams of timber were employed to carry the hood; in such cases the fireplace was sodeeply recessed as to become externally an important architectural feature, as at Haddon Hall. The largest chimneypiece existing is in the great hall of the Palais des Comtes at Poitiers, which is nearly 30 ft. wide, having two intermediate supports to carry the hood; the stone flues are carried up between the tracery of an immense window above. In the early Renaissance style, the chimneypiece of the Palais de Justice at Bruges is a magnificent example; the upper portion, carved in oak, extends the whole width of the room, with statues of nearly life size of Charles V. and others of the royal family of Spain. The most prolific modern designer of chimneypieces was J.B. Piranesi, who in 1765 published a large series, on which at a later date the Empire style in France was based. In France the finest work of the early Renaissance period is to be found in the chimneypieces, which are of infinite variety of design.The English chimneypieces of the early 17th century, when the purer Italian style was introduced by Inigo Jones, were extremely simple in design, sometimes consisting only of the ordinary mantelpiece, with classic architraves and shelf, the upper part of the chimney breast being panelled like the rest of the room. In the latter part of the century the classic architrave was abandoned in favour of a much bolder and more effective moulding, as in the chimneypieces at Hampton Court, and the shelf was omitted.In the 18th century the architects returned to the Inigo Jones classic type, but influenced by the French work of Louis XIV. and XV. Figure sculpture, generally represented by graceful figures on each side, which assisted to carry the shelf, was introduced, and the overmantel developed into an elaborate frame for the family portrait over the chimneypiece. Towards the close of the 18th century the designs of the brothers Adam superseded all others, and a century later they came again into fashion. The Adam mantels are in wood enriched with ornament, cast in moulds, sometimes copied from the carved wood decoration of old times.
Up to the 12th century rooms were warmed entirely by a hypocaust, or with braziers, or by fires on the hearth, the smoke finding its way up to a lantern in the roof. The earliest chimneypiece known is that in the King’s House at Southampton, with Norman shafts in the joints carrying a segmental arch, which is attributed to the first half of the 12th century. At a later date, in consequence of the greater width of the fireplace, flat or segmental arches were thrown across and constructed with voussoirs, sometimes joggled, the thrust of the arch being resisted by bars of iron at the back. In domestic work of the 14th century the chimneypiece was greatly increased in order to allow of the members of the family sitting on either side of the fire on the hearth, and in these cases great beams of timber were employed to carry the hood; in such cases the fireplace was sodeeply recessed as to become externally an important architectural feature, as at Haddon Hall. The largest chimneypiece existing is in the great hall of the Palais des Comtes at Poitiers, which is nearly 30 ft. wide, having two intermediate supports to carry the hood; the stone flues are carried up between the tracery of an immense window above. In the early Renaissance style, the chimneypiece of the Palais de Justice at Bruges is a magnificent example; the upper portion, carved in oak, extends the whole width of the room, with statues of nearly life size of Charles V. and others of the royal family of Spain. The most prolific modern designer of chimneypieces was J.B. Piranesi, who in 1765 published a large series, on which at a later date the Empire style in France was based. In France the finest work of the early Renaissance period is to be found in the chimneypieces, which are of infinite variety of design.
The English chimneypieces of the early 17th century, when the purer Italian style was introduced by Inigo Jones, were extremely simple in design, sometimes consisting only of the ordinary mantelpiece, with classic architraves and shelf, the upper part of the chimney breast being panelled like the rest of the room. In the latter part of the century the classic architrave was abandoned in favour of a much bolder and more effective moulding, as in the chimneypieces at Hampton Court, and the shelf was omitted.
In the 18th century the architects returned to the Inigo Jones classic type, but influenced by the French work of Louis XIV. and XV. Figure sculpture, generally represented by graceful figures on each side, which assisted to carry the shelf, was introduced, and the overmantel developed into an elaborate frame for the family portrait over the chimneypiece. Towards the close of the 18th century the designs of the brothers Adam superseded all others, and a century later they came again into fashion. The Adam mantels are in wood enriched with ornament, cast in moulds, sometimes copied from the carved wood decoration of old times.
(R. P. S.)
CHIMPANZEE(Chimpanzi), the vernacular name of the highest species of the man-like apes, forming the typical representatives of the genusAnthropopithecus. Chimpanzees, of which there appear to be at least two species, range through the tropical forest-zone of Africa from the west coast to Uganda. The typicalA. troglodyteshas been long known to European science, Dr Tyson, a celebrated surgeon and anatomist of his time, having dissected a young individual, and described it, as a pigmy orHomo sylvestris, in a book published in 1699. Of this baby chimpanzee the skeleton may be seen in the Natural History branch of the British Museum alongside the volume in which it is described. It was not, however, till 1788 that the chimpanzee received what is now recognized as a scientific name, having been christened in that yearSimia troglodytesby the naturalist Johann Friedrich Gmelin. In his classification it was included in the same genus as the orang-utan; and it has recently been suggested that the nameSimiapertains of right to the chimpanzee rather than to the orang-utan. Between the typical West African chimpanzee and the gorilla (q.v.) there is no difficulty in drawing a distinction; the difficulty comes in when we have to deal with the aberrant races, or species, of chimpanzee, some of which are so gorilla-like that it is by no means easy to determine to which group they really pertain. In height the adult male chimpanzee of the typical form does not exceed 5 ft., and the colour of the hair is a full black, while the skin, especially that of the face, is light-coloured; the ears are remarkably large and prominent, and the hands reach only a short distance below the knees. The head is rounded and short, without prominent beetling ridges above the eyes, or a strong crest along the middle line of the back of the skull; and the tusks of the old males are of no very great length and prominence. Moreover, there is no very marked difference in the size of the two sexes. Gentleness and docility are specially characteristic of the species, even when full-grown; while in the native state its habits are thoroughly arboreal.
In central Africa the chimpanzees assume more or less marked gorilla-like traits. The first of these aberrant types is Schweinfurth’s chimpanzee (Anthropopithecus troglodytes schweinfurthi), which inhabits the Niam-Niam country, and, although evidently belonging to the same species as the typical race, exhibits certain gorilla-like features. These traits are still more developed in the bald chimpanzee (A. tschego) of Loango, the Gabun, and other regions of French Congo, which takes its English name from the sparse covering of hair on the head. The most gorilla-like of all the races is, however, the kulu-kamba chimpanzee (A. kulu-kamba) of du Chaillu, which inhabits central Africa. The celebrated ape “Mafuka,” which lived in the Dresden zoological gardens during 1875, and came from Loango, was apparently a member of this species, although it was at one time regarded as a hybrid between a chimpanzee and a gorilla. These gorilla-like traits were still more pronounced in “Johanna,” a female chimpanzee living in Barnum & Bailey’s show in 1899, which has been described and figured by Dr A. Keith. The heavy ridges over the brow, originally supposed to be distinctive of the gorilla, are particularly well marked in “Johanna,” and they would doubtless be still more noticeable in the male of the same race, which seems to be undoubtedly du Chaillu’s kulu-kamba. Still the large size and prominence of the ears proclaim that both “Mafuka” and “Johanna” were chimpanzees and not gorillas. A gorilla-like feature in “Johanna” is, however, the presence of large folds at the sides (ala) of the nostrils, which are absent in the typical chimpanzee, but in the gorilla extend down to the upper lip. Chimpanzees exhibit great docility in confinement, where, however, they seldom survive for any great length of time. They likewise display a much higher degree of intelligence than any of the other man-like apes. (SeePrimates.)
In central Africa the chimpanzees assume more or less marked gorilla-like traits. The first of these aberrant types is Schweinfurth’s chimpanzee (Anthropopithecus troglodytes schweinfurthi), which inhabits the Niam-Niam country, and, although evidently belonging to the same species as the typical race, exhibits certain gorilla-like features. These traits are still more developed in the bald chimpanzee (A. tschego) of Loango, the Gabun, and other regions of French Congo, which takes its English name from the sparse covering of hair on the head. The most gorilla-like of all the races is, however, the kulu-kamba chimpanzee (A. kulu-kamba) of du Chaillu, which inhabits central Africa. The celebrated ape “Mafuka,” which lived in the Dresden zoological gardens during 1875, and came from Loango, was apparently a member of this species, although it was at one time regarded as a hybrid between a chimpanzee and a gorilla. These gorilla-like traits were still more pronounced in “Johanna,” a female chimpanzee living in Barnum & Bailey’s show in 1899, which has been described and figured by Dr A. Keith. The heavy ridges over the brow, originally supposed to be distinctive of the gorilla, are particularly well marked in “Johanna,” and they would doubtless be still more noticeable in the male of the same race, which seems to be undoubtedly du Chaillu’s kulu-kamba. Still the large size and prominence of the ears proclaim that both “Mafuka” and “Johanna” were chimpanzees and not gorillas. A gorilla-like feature in “Johanna” is, however, the presence of large folds at the sides (ala) of the nostrils, which are absent in the typical chimpanzee, but in the gorilla extend down to the upper lip. Chimpanzees exhibit great docility in confinement, where, however, they seldom survive for any great length of time. They likewise display a much higher degree of intelligence than any of the other man-like apes. (SeePrimates.)
(R. L.*)
CHINA, a country of eastern Asia, the principal division of the Chinese empire. In addition to China proper the Chinese Empire includes Manchuria, Mongolia, Tibet and Sin-kiang (East Turkestan, Kulja, Dzungaria, &c.,i.e.all the Chinese dependencies lying between Mongolia on the north and Tibet on the south). Its most southern point is in 18° 50′ N.; its most northern in 53° 25′ N.; its most western in 74° E., and its most eastern in 135° E. It lies, however, mainly between 20° and 50° N. and 80° and 130° E. It is considerably larger than the whole of Europe. Though its area has not been exactly ascertained the various estimates closely approximate, varying between 4,277,000 and 4,300,000 sq. m. It is bounded N.W., N. and N.E. by Asiatic Russia, along a frontier extending some 6000 m.; E. by Korea and those parts of the Pacific known as the Yellow Sea and China Sea; S. and S.W. by the China Sea, French Indo-China, Upper Burma and the Himalayan states. It is narrowest in the extreme west. Chinese Turkestan along the meridian of Kashgar (76° E.) has a breadth of but 250 m. It rapidly broadens and for the greater part of its area is over 1800 m. across in a direct N. and S. line. Its greatest length is from the N.E. corner of Manchuria to the S.W. confines of Tibet, a distance of 3100 m. in a direct line. Its seaboard, about 5000 m. following the indentations of the coast, is almost, wholly in China proper, but the peninsula of Liao-tung and also the western shores of the Gulf of Liao-tung are in Manchuria.
China1proper or the Eighteen Provinces (Shih-pa-shêng) occupies the south-eastern part of the empire. It is bounded N. by Mongolia, W. by Turkestan and Tibet, S.W. by Burma, S. by Tongking and the gulf of that name, S.E. by the South China Sea, E. by the East China Sea, the Yellow Sea, Gulf of Chih-li and Manchuria. Its area is approximately 1,500,000 sq. m.
This vast country is separated from the rest of continental Asia by lofty tablelands and rugged mountain ranges, which determine the general course—west to east—of its principal rivers. On the north and west the Mongolian and Tibetan tablelands present towards China steep escarpments across which are very few passes. On the S.W. and S., on the borders of Yun-nan, high mountains and deep valleys separate China from Burma and Tongking. On the narrow N.E. frontier the transition from the Manchurian plateau to the alluvial plain of northern China is not abrupt, but, before the advent of railways, Manchuria afforded few and difficult means of access to other regions. Thus China was almost cut off from the rest of the world save by sea routes.
I. The Country
Western China consists of highlands often sparsely, and eastern China of lowlands densely peopled. Western China contains the only provinces where the population is under 100 per sq. m. From the Tibetan and Mongolian tablelands project mountain ranges which, ramifying over the western region, enclose elevated level tracts and lower basins and valleys. East of this mountainous region, which extends into central China and covers probablyfully half of the kingdom, are, in the north a great alluvial plain and in the south a vast calcareous tableland traversed by hill ranges of moderate elevation (see §§MountainsandGeology). In north-eastern China there is only one mountain system, the group of hills—-highest peak 5060 ft.—-forming the Shan-tung peninsula. This peninsula was formerly an island, but has been attached to the mainland by the growth of the alluvial plain. Besides the broad division of the country into western and eastern China it may also be considered as divided into three regions by the basins of its chief rivers, the Hwang-ho (Yellow river) in the north, the Yangtsze-kiang in the centre, and the Si-kiang (West river) in the south. In the northern provinces of Kan-suh and Shen-si the basins of the Hwang-ho and Yangtsze-kiang are separated by a mountain chain with various names— the eastern termination of the Kuen-lun range of central Asia. These mountains, in China, attain, in the Tsing-ling Shan, a maximum elevation of 13,000 ft. East of Shen-si, in Ho-nan the Fu-niu-shan continue the range, but with decreasing elevation, and beyond this the deltaic plain is entered.
The watershed between the Yangtsze-kiang and that of the Si-kiang is less clearly marked. It traverses the immense tableland which occupies a great part of the south-west provinces of Yun-nan and Kwei-chow and is continued eastward by the lower tableland of Kwang-si and the Nanshan hills (whose elevation seldom exceeds 6000 ft.). The basin of the Yangtsze-kiang forms the whole of central China. Its western border, in Sze-ch‘uen and Yun-nan, is wholly mountainous, with heights exceeding 19,000 ft. Central Sze-ch‘uen, which is shut in by these mountains on the west, by the Yun-nan and Kwei-chow plateau on the south, by the Kiu-lung range on the north, and by highlands eastward (save for the narrow valley through which the Yangtsze-kiang forces its way), is a vast red sandstone tableland of about 1600 ft. elevation. It is exceedingly fertile and supports a dense population. Eastward of Sze-ch‘uen the Yangtsze valley is studded with lakes. Finally it enters the deltaic plain. The basin of the Si-kiang fills the two southern provinces of Kwang-si and Kwang-tung and contains no very striking orographic features. It may be added that in the extreme S.W. portion of China is part of a fourth drainage area. Here the Mekong, Salween, Song-koi (Red river), &c. flow south to Indo-China.
The Coast.—The coast-line, following all the minor indentations, is reckoned at over 4500 m.; if only the larger inlets and promontories be regarded, the coast-line is about 2150 m. in length. Its shape is that of a semicircle, with its most easterly point midway (30° N.) between its northern and southern extremities. At either end of this semicircular sweep lies a peninsula, and beyond the peninsula a gulf. In the north are the peninsula of Shan-tung and the gulf of Chih-li; in the south the Lien-chow peninsula and the gulf of Tongking. Due south of Lien-chow peninsula, separated rom it by a narrow strait, is Hai-nan, the only considerable island of China. From the northern point of the gulf of Chih-li to 30° N., where is Hang-chow bay, the shores are flat and alluvial save where the Shan-tung peninsula juts out. Along this stretch there are few good natural harbours, except at the mouths of rivers and in the Shan-tung promontory; the sea is shallow and has many shoals. The waters bordering the coast of Chih-li are partly frozen in winter; at 10 m. from the shore the water is only 20 ft. deep. The proximity of Peking gives its few ports importance; that of Taku is at the mouth of the Peiho. In Shan-tung, deeply indented on its southern coast, are the ports of Chi-fu, Wei-hai-wei and Tsing-tao (the last in Kiao-chow bay). South of Shan-tung and north of the mouth of the Yangtsze huge sandbanks border the coast, with narrow channels between them and the shore. The estuary of the Yangtsze is 60 m. across; it contains islands and sandbanks, but there is easy access to Wusung (Shanghai) and other river ports. The bay of Hangchow, as broad at its entrance as the Yangtsze estuary, forms the mouth of the Tsien-tang-kiang. The Chusan and other groups of islands lie across the entrance of the bay.South of Hang-chow bay the character of the coast alters. In place of the alluvial plain, with flat, sandy and often marshy shores, the coast is generally hilly, often rocky and abrupt; it abounds in small indentations and possesses numerous excellent harbours; in this region are Fu-chow, Amoy, Swatow, Hongkong, Macao, Canton and other well-known ports. The whole of this coast is bordered by small islands. Formosa lies opposite the S.E. coast, the channel between it and Fu-kien province being about 100 m. wide. Formosa protects the neighbouring regions of China from the typhoons experienced farther north and farther south.Surface.—-As already indicated, one of the most noticeable features in the surface of China is the immense deltaic plain in the north-eastern portion of the country, which, curving round the mountainous districts of Shan-tung, extends for about 700 m. in a southerly direction from the neighbourhood of Peking and variesDeltaic Plain.from 150 to 500 m. in breadth. This plain is the delta of the Yellow river and, to some extent, that of the Yangtsze-kiang also. Beginning in the prefecture of Yung-p‘ing Fu, in the province of Chih-li, its outer limit passes in a westerly direction as far as Ch‘ang-p‘ing Chow, north-west of Peking. Thence running a south-south-westerly course it passes westward of Chêng-ting Fu and Kwang-p‘ing Fu till it reaches the upper waters of the Wei river in Ho-nan. From this point it turns westward and crosses the Hwang-ho or Yellow river in the prefecture of Hwai-k‘ing. Leaving this river it takes a course a little to the east of south, and passing west of Ju-ning Fu, in the province of Ho-nan, it turns in a more easterly direction as far as Luchow Fu. From this prefecture an arm of the plain, in which lies the Chao Lake, stretches southward from the Hwai river to the Yangtsze-kiang, and trending eastward occupies the region between that river and Hangchow Bay. To the north of this arm rises a hilly district, in the centre of which stands Nanking. The greater part of this vast plain descends very gently towards the sea, and is generally below the level of the Yellow river, hence the disastrous inundations which so often accompany the rise of that river. Owing to the great quantity of soil which is brought down by the waters of the Yellow river, and to the absence of oceanic currents, this delta is rapidly increasing and the adjoining seas are as rapidly becoming shallower. As an instance, it is said that the town of P‘utai was one Chinese mile2west of the seashore in the year 200B.C., and in 1730 it was 140 m. inland, thus giving a yearly encroachment upon the sea of about 100 ft. Again, Sien-shwuy-kow on the Peiho was on the seashore inA.D.500, and it is now about 18 m. inland.Some of the ranges connected with the mountain system of central Asia which enter the western provinces of China have been mentioned above, others may be indicated here. In the eastern portion of Tibet the Kuen-lun range throws offMountains.a number of branches, which spread first of all in a south-easterly direction and eventually take a north and south course, partly in the provinces of Sze-ch‘uen and Yun-nan, where they divide the beds of the rivers which flow into Siam and French Indo-China, as well as the principal northern tributaries of the Yangtsze-kiang. In the north-west, traversing the western portion of the province of Kan-suh, are parallel ranges running N.W. and S.E. and forming a prolongation of the northern Tibetan mountains. They are known as the Lung-shan, Richthofen and Nan-shan, and join on the south-east the Kuen-lun range. The Richthofen range (locally called Tien-shan, or Celestial Mountains) attains elevations of over 20,000 ft. Several of its peaks are snowclad, and there are many glaciers. Forming the northern frontier of the province of Sze-ch‘uen run the Min-shan and the Kiu-lung (or Po-mêng) ranges, which, entering China in 102° E., extend in a general easterly course as far as 112° E. in the province of Hu-peh. These ranges have an average elevation of 8000 and 11,000 ft. respectively. In the south a number of parallel ranges spread from the Yun-nan plateau in an easterly direction as far as the province of Kwang-tung. Then turning north-eastward they run in lines often parallel with the coast, and cover large areas of the provinces of Fu-kien, Kiang-si, Cheh-kiang, Hu-nan and southern Ngan-hui, until they reach the Yangtsze-kiang; the valley of that river from the Tung-ting Lake to Chin-kiang Fu forming their northern boundary. In Fu-kien these hills attain the character of a true mountain range with heights of from 6500 to nearly 10,000 ft. Besides the chief ranges there are the Tai-hang Mountains in Shan-si, and many others, among which may be mentioned the ranges—part of the escarpment of the Mongolian plateau—which form the northern frontier of Chih-li. Here the highest peak is Ta-kuang-ting-tzu (6500 ft.), about 300 m. N.N.E. of Peking and immediately north of Wei Ch‘ang (the imperial hunting grounds).Rivers and Canals.—The rivers of China are very numerous and there are many canals. In the north the rivers are only navigable by small craft; elsewhere they form some of the most frequented highways in the country. The two largest rivers,The Yellow River.the Yangtsze-kiang and the Hwang-ho (Yellow river), are separately noticed. The Hwang-ho (length about 2400 m.) has only one important tributary in China, the Wei-ho, which rises in Kan-suh and flows through the centre of Shen-si. Below the confluence the Hwang-ho enters the plains. According to the Chinese records this portion of the river has changed its course nine times during 2500 years, and has emptied itself into the sea at different mouths, the most northerly of which is represented as having been in about 39° N., or in the neighbourhood of the present mouth of the Peiho, and the most southerly being that which existed before the change in 1851-1853, in 34° N. Owing to its small value as a navigable highway and to its propensity to inundate the regions in its neighbourhood, there are no considerable towns on its lower course.The Yangtsze-kiang is the chief waterway of China. The river, flowing through the centre of the country, after a course of 2900 m., empties itself into the Yellow Sea in about 31° N. Unlike the Yellow river, the Yangtsze-kiang is dotted along its navigable portions with many rich and populous cities, among which are Nanking, An-ch‘ing (Ngank‘ing), Kiu-kiang, Hankow and I-ch‘ang.From its mouth to I-ch‘ang, about 1000 m., the river is navigable by large steamers. Above this last-named city the navigation becomesThe Yangtsze-kiang.impossible for any but light native craft or foreign vessels specially constructed for the navigation, by reason of the rapids which occur at frequent intervals in the deep mountain gorges through which the river runs between Kwei-chow and I-ch‘ang. Above Kwei-chow it receives from the north many tributaries, notably the Min, which water the low table-land of central Sze-ch‘uen. The main river itself has in this province a considerable navigable stretch, while below I-ch‘ang it receives the waters of numerous navigable affluents. The Yangtsze system is thus all important in the economic and commercial development of China.Perhaps the most remarkable of the affluents of the Yangtsze is the Han-kiang or Han river. It rises in the Po-mêng mountains to the north of the city of Ning-kiang Chow in Shen-si. Taking a generally easterly course from its source as far as Fan-cheng, it from that point takes a more southerly direction and empties itself into the Yangtsze-kiang at Han-kow, “the mouth of the Han.” Here it is only 200 ft. wide, while higher up it widens to 2600 ft. It is navigable by steamers for 300 m. The summer high-water line is for a great part of its course, from I-ch‘eng Hien to Han-kow, above the level of its banks. Near Sien-t‘ao-chên the elevation of the plain above low water is no more than 1 ft., and in summer the river rises about 26 ft. above its lowest level. To protect themselves against inundations the natives have here, as elsewhere, thrown up high embankments on both sides of the river, but at a distance from the natural banks of about 50 to 100 ft. This intervening space is flooded every year, and by the action of the water new layers of sand and soil are deposited every summer, thus strengthening the embankments from season to season.The Hwai-ho is a large river of east central China flowing between the Hwang-ho and the Yangtsze-kiang. The Hwai-ho and its numerous affluents (it is said to have 72 tributaries) rise in Ho-nan. The main river flows through the centre of Ngan-hui, in which province it receives from the N.W. the Sha-ho, Fei-ho and other important affluents. Formerly it received through the Sha-ho part of the waters of the Hwang-ho. The Hwai-ho flows into the Hungtso lake, through which it feeds the Grand Canal, not far from the old course of the Hwang-ho, and probably at one time joined that river not far from its mouth. It has a length of about 800 m. and is navigable from the point where it leaves the hill country of Ho-nan to Lake Hungtso. It is subject to violent floods, which inundate the surrounding country for a distance of 10 to 20 m. Many of its tributaries are also navigable for considerable distances.Next in importance to the Yangtsze-kiang as a water highway is the Yun-ho, or, as it is generally known in Europe, the Grand Canal. This magnificent artificial river reaches from Hang-chow Fu in the province of Cheh-kiang to Tientsin in Chih-li,Grand Canal.where it unites with the Peiho, and thus may be said to extend to Tung-chow in the neighbourhood of Peking. According to the itineraries published by Père Gandar, the total length of the canal is 3630li, or about 1200 m. A rough measurement, taking account only of the main bends of the canal, makes its length 850 m. After leaving Hang-chow the canal passes round the eastern border of the Tai-hu or Great Lake, surrounding in its course the beautiful city of Su-chow, and then trends in a generally north-westerly direction through the fertile districts of Kiang-su as far as Chin-kiang on the Yangtsze-kiang. In this, the southern section, the slope is gentle and water is plentiful (from 7 ft. at low water to 11 ft., and occasionally 13 ft. at high water). Between Su-chow and Chin-kiang the canal is often over 100 ft. wide, and its sides are in many places faced with stone. It is spanned by fine stone bridges, and near its banks are many memorial arches and lofty pagodas. In the central portion of the canal, that is between Chin-kiang and Tsing-kiang-pu, at which latter place it crosses the dry channel which marks the course of the Yellow river before 1852, the current is strong and difficult to ascend in the upward (northern) journey. This part of the canal skirts several lakes and is fed by the Hwai-ho as it issues from the Hungtso lake. The country lying west of the canal is higher than its bed; while the country east is lower than the canal. The two regions are known respectively as Shang-ho (above the river) and Ssia-ho (below the river). Waste weirs opening on the Ssia-ho (one of the great rice-producing areas of China) discharge the surplus water in flood seasons. The northern and considerably the longest section of the canal extends from the old bed of the Yellow river to Tientsin. It largely utilizes existing rivers and follows their original windings. Between Tsing-kiang-pu and the present course of the Yellow river the canal trends N.N.W., skirting the highlands of Shan-tung. In this region it passes through a series of lagoons, which in summer form one lake—Chow-yang. North of that lake on the east bank of the canal, is the city of Tsi-ning-chow. About 25 m. N. of that city the highest level of the canal is reached at the town of Nan Wang. Here the river Wen enters the canal from the east, and about 30 m. farther N. the Yellow river is reached. On the west side of the canal, at the point where the Yellow river now cuts across it, there is laid down in Chinese maps of the 18th century a dry channel which is described as being that once followed by the Yellow river,i.e.before it took the channel it abandoned in 1851-1853. The passage of the Yellow river to the part of the canal lying north of that stream is difficult, and can only be effected at certain levels of the river. Frequently the waters of the river are either too low or the current is too strong to permit a passage. Leaving this point the canal passes through a well-wooded and hilly country west of Tung-p‘ing Chow and east of Tung-ch‘ang Fu. At Lin-ching Chow it is joined at right angles by the Wei river in the midst of the city. Up to this point,i.e.from Tsing-kiang-pu to Lin-ching Chow, a distance of over 300 m., navigation is difficult and the water-supply often insufficient. The differences of level, 20 to 30 ft., are provided for by barrages over which the boats—having discharged their cargo—are hauled by windlasses. Below the junction with the Wei the canal borrows the channel of the river and again becomes easily navigable. Crossing the frontier into Chih-li, between Te Chow and Tsang Chow, which it passes to the west, it joins the Peiho at Tientsin, after having received the waters of the Keto river in the neighbourhood of Tsing Hien.3The most ancient part of the canal is the section between the Yangtsze and the Hwai-ho. This part is thought, on the strength of a passage in one of the books of Confucius, to have been built c. 486B.C.It was repaired and enlarged in the 3rd centuryA.D.The southern part, between the Yangtsze and Hang-chow, was built early in the 7th centuryA.D.The northern part is stated to have been constructed in the three years 1280-1283. The northern portion of the canal is now of little use as a means of communication between north and south.4It is badly built, neglected and charged with the mud-laden waters of the Yellow river. The “tribute fleet” bearing rice to Peking still uses this route; but the rice is now largely forwarded by sea. The central and southern portions of the canal are very largely used.The Peiho (length about 350 m.) is of importance as being the high waterway to Peking. Taking its rise in the Si-shan, or Western Mountains, beyond Peking, it passes the city of T‘sung-chow, the port of Peking, and Tientsin, where it meets the waters of the Hun-ho and empties itself into the gulf of Chih-li at the village of Taku. The Peiho is navigable for small steamers as far as Tientsin during the greater part of the year, but from the end of November to the beginning of March it is frozen up.In the southern provinces the Si-kiang, or Western river, is the most considerable. It has a length of over 1000 m. This river takes its rise in the prefecture of Kwang-nan Fu in Yun-nan, whence it reaches the frontier of Kwang-si at a distanceThe Si-kiang.of about 90 li from its source. Then trending in a north-easterly direction it forms the boundary between the two provinces for about 150 li. From this point it takes a generally south-easterly course, passing the cities of Tsien Chow, Fung-e Chow, Shang-lin Hien, Lung-ngan Hien, Yung-kang Chow and Nan-ning Fu to Yung-shan Hien. Here it makes a bend to the north-east, and continues this general direction as far as Sin-chow Fu, a distance of 800 li, where it meets and joins the waters of the Kien-kiang from the north. Its course is then easterly, and after passing Wu-chow Fu it crosses the frontier into Kwang-tung. In this part of its course it flows through a gorge 3 m. long and in places but 270 yds. in width. Both above and below this gorge it is 1 m. wide. Some 30 m. above Canton it divides into two main and several small branches. The northern branch, called Chu-kiang, or Pearl river, flows past Fat-shan and Canton and reaches the sea through the estuary called the Bocca Tigris or Bogue, at the mouth of which is the island of Hong-Kong. The southern branch, which retains the name of Si-kiang, reaches the sea west of Macao. Near the head of its delta the Si-kiang receives the Pei-kiang, a considerable river which flows through Kwang-tung in a general N. to S. direction. Like the Yangtsze-kiang the Si-kiang is known by various names in different parts of its course. From its source to Nan-ning Fu in Kwang-si it is called the Si-yang-kiang, or river of the Western Ocean; from Nan-ning Fu to Sin-chow Fu it is known as the Yu-kiang, or the Bending river; and over the remainder of its course it is recognized by the name of the Si-kiang, or Western river. The Si-kiang is navigable as far as Shao-king, 130 m., for vessels not drawing more than 15 ft. of water, and vessels of a light draught may easily reach Wu-chow Fu, in Kwang-si, which is situated 75 m. farther up. In winter the navigation is difficult above Wu-chow Fu. Above that place there is a rapid at low water, but navigation is possible to beyond Nan-ning Fu.Click to see detailed left-side.Click to see detailed right-side.Lakes.—There are numerous lakes in the central provinces of China. The largest of these is the Tung-t‘ing in Hu-nan, which, according to the Chinese geographers, is upwards of 800 li, or 266 m., in circumference. In native gazetteers its various portions are known under distinct names; thus it is said to include the Ts‘ing-ts‘ao, or Green Grass Lake; the Ung, or Venerable Lake; the Chih-sha, or Red Sand Lake; the Hwang-yih, or Imperial Post-house Lake; the Ngan-nan, or Peaceful Southern Lake; and the Ta-tung, orGreat Deep Lake. In ancient times it went by the name of the Kiu-kiang Hu, or Lake of the Nine Rivers, from the fact that nine rivers flowed into it. Its chief affluents are the Siang-kiang, which rises in the highlands in the north of Kwang-si and flows in a general N.N.E. direction, and the Yuen-kiang, which flows N. and then E. from the eastern border of Kwei-chow. The lake is connected with the Yangtsze-kiang by two canals, the Taping and the Yochow Fu. In summer it is fed by the overflow from the Yangtsze-kiang; in winter it pours its waters into that river through the Yochow Fu canal. During the winter and spring the water of the lake is so low that the shallow portions become islands, separated by rivers such as the Siang and Yuen, and numberless streams; but in summer, owing to the rise in the waters of the Yangtsze-kiang, the whole basin of the lake is filled. It is then about 75 m. long and 60 m. broad. About 180 m. E. of the Tung-t‘ing lake is the Poyang lake, which occupies the low-lying part of the province of Kiang-si, and is connected with the Yangtsze by the Hu-kow canal. The Poyang lake is also subject to a wide difference between high and low water, but not quite to the same extent as the Tung-t‘ing lake, and its landmarks are more distinctly defined. It is about 90 m. long by 20 broad. The T‘ai lake, in the neighbourhood of Su-chow Fu, is also celebrated for its size and the beauty of its surroundings. It is about 150 m. in circumference, and is dotted over with islands, on which are built temples for the devotees of religion, and summer-houses for the votaries of pleasure from the rich and voluptuous cities of Hang-chow and Su-chow. The boundary line between the provinces of Cheh-kiang and Kiang-su crosses its blue waters, and its shores are divided among thirteen prefectures. Besides these lakes there are, among others, two in Yun-nan, the Kun-yang-hai (Tien-chi) near Yun-nan Fu, which is 40 m. long and is connected with the Yangtsze-kiang by the Pu-to river, and the Erh-hai (Urh-hai) to the east of the city of Tali.The Great Wall.—Along the northern provinces of Chih-li, Shan-si, Shen-si and Kan-suh, over 22° of longitude (98° to 120° E.), stretches the Great Wall of China, built to defend the country against foreign aggression. It was begun in the 3rd centuryB.C., was repaired in the 15th century, and in the 16th century was extended by 300 m. Following the windings the wall is 1500 m. long. Starting near the seashore5at Shan-hai-kwan on the gulf of Liao-tung, where the Chinese and Manchurian frontiers meet, it goes eastward past Peking (which is about 35 m. to the south) and then trends S. and E. across Shan-si to the Hwang-ho. From the neighbourhood of Peking to the Hwang-ho there is an inner and an outer wall. The outer (northern) wall passes through Kalgan, thus guarding the pass into Mongolia. A branch wall separates the greater part of the western frontier of Chih-li from Shan-si. West of the Hwang-ho the Great Wall forms the northern frontier of Shen-si, and west of Shen-si it keeps near the northern frontier of Kan-suh, following for some distance in that province the north bank of the Hwang-ho. It ends at Kiayu-kwan (98° 14′E.) just west of Su-chow. This part of the wall was built to protect the one main artery leading from central Asia to China through Kan-suh and Shen-si by the valley of the Wei-ho, tributary of the Hwang-ho. There is a branch wall in Kan-suh running west and south to protect the Tibetan frontier. The height of the wall is generally from 20 to 30 ft., and at intervals of some 200 yds. are towers about 40 ft. high. Its base is from 15 to 25 ft. thick and its summit 12 ft. wide. The wall is carried over valleys and mountains, and in places is over 4000 ft. above sea-level. Military posts are still maintained at the chief gates or passes—at Shan-hai-kwan, the Kalgan pass, the Yenmun pass (at the N. of Shan-si) and the Kaiyu pass in the extreme west, through which runs the caravan route to Barkal in Turkestan. Colonel A.W.S. Wingate, who in the opening years of the 20th century visited the Great Wall at over twenty places widely apart and gathered many descriptions of it in other places, states that its position is wrongly shown “on the maps of the day” (1907) in a number of places; while in others it had ceased to exist, “the only places where it forms a substantial boundary being in the valley bottoms, on the passes and where it crosses main routes. These remarks apply with particular force to the branch running south-west from the Nan-k‘ow pass and forming the boundary of Chih-li and Shan-si provinces.” In Colonel Wingate’s opinion the wall was originally built by degrees and in sections, not of hewn stone, but of round boulders and earth, the different sections being repaired as they fell into ruin. “Only in the valley bottoms and on the passes was it composed of masonry or brickwork. The Mings rebuilt of solid masonry all those sections through which led a likely road for invading Tatars to follow, or where it could be seen at a distance from the sky-line.” The building of the wall “was a sufficiently simple affair,” not to be compared with the task of building the pyramids of Egypt.6Climate.—The climate over so vast an area as China necessarily varies greatly. The southern parts of Yun-nan, Kwang-si and Kwang-tung (including the city of Canton) lie within the tropics. The northern zone (in which lies Peking) by contrast has a climate which resembles that of northern Europe, with winters of Arctic severity. The central zone (in which Shanghai is situated) has a generally temperate climate. But over both northern and central China the influence of the great plateau of Mongolia tends to establish uniform conditions unusual in so large an area. The prevailing winds during summer—the rainy season—are south-easterly, caused by heat and the ascending current of air over the sandy deserts of central Asia, thus drawing in a current from the Pacific Ocean. In the winter the converse takes place, and the prevailing winds, descending from the Mongolian plateau, are north and north-west, and are cold and dry. From October to May the climate of central China is bracing and enjoyable. The rainfall is moderate and regular.In northern China the inequalities both of temperature and rainfall are greater than in the central provinces. In the province of Chih-li, for example, the heat of summer is as intense as is the cold of winter. In summer the rains often render the plain swampy, while the dry persistent westerly winds of spring create dust storms (experienced in Peking from March to June). The rainfall is, however, uncertain, and thus the harvests are precarious. The provinces of Shan-tung and Shan-si are peculiarly liable to prolonged periods of drought, with consequent severe famines such as that of 1877-1878, when many millions died. In these regions the air is generally extremely dry, and the daily variations of temperature consequent on excessive radiation are much greater than farther south.Accurate statistics both of heat and rainfall are available from a few stations only. The rainfall on the southern coasts is said to be about 100 in. yearly; at Peking the rainfall is about 24 in. a year. In the coast regions the temperatures of Peking, Shanghai and Canton may be taken as typical of those of the northern, central and southern zones. In Peking (39° N.) the mean annual temperature is about 53° F., the mean for January 23°, for July 79°. In Shanghai (31° 11′ N.)7the mean annual temperature is 59°, the mean for January 36.2°, for July 80.4°. In Canton (23° 15′ N.) the mean annual temperature is 70°, the mean for January 54°, for July 82°. The range of temperature, even within the tropics, is noteworthy. At Peking and Tientsin the thermometer in winter falls sometimes to 5° below zero and rises in summer to 105° (at Taku 107° has been recorded); in Shanghai in winter the thermometer falls to 18° and in summer rises to 102°. In Canton frost is said to have been recorded, but according to theChina Sea Directorythe extreme range is from 38° to 100°.8The climate of Shanghai, which resembles, but is not so good as, that of the Yangtsze-kiang valley generally, is fairly healthy, but there is an almost constant excess of moisture. The summer months, July to September, are very hot, while snow usually falls in December and January.At Canton and along the south coast the hot season corresponds with the S.W. monsoon; the cool season—mid October to end of April—with the N.E. monsoon. Farther north, at Shanghai, the S.W. monsoon is sufficiently felt to make the prevailing wind in summer southerly.Provinces.—China proper is divided into the following provinces: Cheh-kiang, Chih-li, Fu-kien, Ngan-hui (An-hui), Ho-nan, Hu-nan, Hu-peh, Kan-suh, Kiang-si, Kiang-su, Kwang-si, Kwang-tung, Kwei-chow, Shan-si, Shan-tung, Shen-si, Sze-ch‘uen and Yun-nan. See the separate notices of each province and the article on Shêng-king, the southern province of Manchuria.(X.)Geology.The Palaeozoic formations of China, excepting only the upper part of the Carboniferous system, are marine, while the Mesozoic and Tertiary deposits are estuarine and freshwater or else of terrestrial origin. From the close of the Palaeozoic period down to the present day the greater part of the empire has been dry land, and it is only in the southern portion of Tibet and in the western Tian Shan that any evidence of a Mesozoic sea has yet been found. The geological sequence may be summarized as follows:—Archean.—Gneiss, crystalline schists, phyllites, crystalline limestones. Exposed in Liao-tung, Shan-tung, Shan-si, northern Chih-li and in the axis of the mountain ranges,e.g.the Kuen-lun and the ranges of southern China.Sinian.—Sandstones, quartzites, limestones. Sometimes rests unconformably upon the folded rocks of the Archaen system; but sometimes, according to Lóczy, there is no unconformity. Covers a large area in the northern part of China proper; absent in the eastern Kuen-lun; occurs again in the ranges of S.E. China. In Liao-tung Cambrian fossils have been found near the summit of the series; they belong to the oldest fauna known upon the earth, the fauna of theOlenelluszone. It is, however, not improbable that in many places beds of considerably later date have been included in the Sinian system.Ordovician.—Ordovician fossils have been found in the Lung-shan, Kiang-su (about 50 m. east of Nan-king), in the south-west of Cheh-kiang and in the south-east of Yun-nan. Ordovician beds probably occur also in the Kuen-lun.Silurian.—Limestones and slates with Silurian corals and other fossils have been found in Sze-ch‘uen.Devonian.—Found in Kan-suh and in the Tsing-ling-shan, but becomes much more important in southern China. Occurs also on the south of the Tian-shan, in the Altyn-tagh, the Nan-shan and the western Kuen-lun.Carboniferous.—Covers a large area in northern China, in the plateau of Shen-si and Shan-si, extending westwards in tongues between the folds of the Kuen-lun. In this region it consists of a lower series of limestones and an upper series of sandstones with seams of coal, which may perhaps be in part of Permian age. This is probably the most extensive coalfield in the world.In south China the whole series consists chiefly of limestones, and the coal seams are comparatively unimportant. Carboniferous beds are also found in the Tian-shan, the Nan-shan, Kan-suh, on the southern borders of the Gobi, &c.Mesozoic.—Marine Triassic beds containing fossils similar to those of the German Muschelkalk have been found by Lóczy near Chung-tien, on the eastern border of the Tibetan plateau. Elsewhere, however, the Mesozoic is represented chiefly by a red sandstone, which covers the greater part of Sze-ch‘uen and fills also a number of troughs amongst the older beds of southern China. No marine fossils are found in this sandstone, but remains of plants are numerous, and these belong to the Rhaetic, Lias and Lower Oolite. No Cretaceous beds are known in China excepting in S. Tibet (on the shores of the Tengri-nor) and in the western portion of the Tian-shan.Cainozoic and Recent.—No marine deposits of this age are known. Although the loess of the great plain and the sand of the desert are still in process of formation, the accumulation of these deposits probably began in the Tertiary period.Volcanic Rocks.—Amongst the Archean rocks granitic and other intrusions are abundant, but of more modern volcanic activity the remains are comparatively scanty. In south China there is no evidence of Tertiary or Post-Tertiary volcanoes, but groups of volcanic cones occur in the great plain of north China. In the Liao-tung and Shan-tung peninsulas there are basaltic plateaus, and similar outpourings occur upon the borders of Mongolia. All these outbursts appear to be of Tertiary or later data.Loess.—One of the most characteristic deposits of China is the loess, which not merely imparts to north China the physical character of the scenery, but also determines the agricultural products, the transport, and general economic life of the people of that part of the country. It is peculiar to north China and it is not found south of the Yangtsze. The loess is a solid but friable earth of brownish-yellow colour, and when triturated with water is not unlike loam, but differs from the latter by its highly porous and tubular structure. The loess soil is extremely favourable to agriculture. (SeeLoessandinfra, § Agriculture.)The loess is called by the ChineseHwang-t‘u, or yellow earth, and it has been suggested that the imperial titleHwang-ti, Yellow Emperor or Ruler of the Yellow, had its origin in the fact that the emperor is lord of the loess or yellow earth.Structurally, China proper may be divided into two regions, separated from each other by the folded range of the Tsing-ling-shan, which is a continuation of the folded belt of the Kuen-lun. North of this chain the Palaeozoic beds areStructure.in general nearly horizontal, and the limestones and sandstones of the Sinian and Carboniferous systems form an extensive plateau which rises abruptly from the western margin of the great plain of northern China. The plateau is deeply carved by the rivers which flow through it; and the strata are often faulted, but they are never sharply folded. South of the Tsing-ling-shan, on the other hand, the Palaeozoic beds are thrown into a series of folds running from W. 30° S. to E. 30° N., which form the hilly region of southern China. Towards Tongking these folds probably bend southwards and join the folds of Further India. Amongst these folded beds lie trough-like depressions filled with the Mesozoic red sandstone which lies unconformably upon the Palaeozoic rocks.The present configuration of China is due, in a very considerable degree, to faulting. The abrupt eastern edge of the Shan-si plateau, where it overlooks the great plain, is a line of fault, or rather a series of step faults, with the downthrow on the east; and von Richthofen has shown reason to believe that this line of faulting is continued far to the south and to the north. He believed also that the present coast-line of China has to a large extent been determined by similar faults with their downthrow on the east.Concerning the structure of the central Asian plateau our knowledge is still incomplete. The great mountain chains, the Kuen-lun, the Nan-shan and the Tian-shan, are belts of folding; but the Mongolian Altai is a horst—a strip of ancient rock lying between two faults and with a depressed area upon each side. In the whole of this northern region faulting, as distinct from folding, seems to have played an important part. Along the southern margin of the Tian-shan there is a remarkable trough-like depression which appears to lie between two approximately parallel faults.(P. La.)Fauna.China lies within two zoological provinces or regions, its southern portion forming a part of the Oriental or Indian region and having a fauna close akin to that of the western Himalaya, Burma and Siam, whereas the districts to the north of Fu-chow and south of the Yangtsze-kiang lie within the eastern Holarctic (Palaearctic) region, or rather the southern fringe of the latter, which has been separated as the Mediterranean transitional region. Of these two divisions of the Chinese fauna, the northern one is the more interesting, since it forms the chief home of a number of peculiar generic types, and also includes types represented elsewhere at the present day (exclusive in one case of Japan) only in North America. The occurrence in China of these types common to the eastern and western hemispheres is important in regard to the former existence of a land-bridge between Eastern Asia and North America by way of Bering Strait.Of the types peculiar to China and North America the alligator of the Yangtsze-kiang is generically identical with its Mississippi relative. The spoon-beaked sturgeon of the Yangtsze and Hwang-ho is, however, now separated, asPsephurus, from the closely allied AmericanPolyodon. Among insectivorous mammals the Chinese and Japanese shrew-moles, respectively forming the generaUropsilusandUrotrichus, are represented in America byNeurotrichus. The giant salamander of the rivers of China and Japan and the Chinese mandarin duck are by some included in the same genera as their American representatives, while by others they are referred to genera apart. Whichever view we take does not alter their close relationship. One wapiti occurs on the Tibetan frontier, and others in Manchuria and Amurland.As regards mammals and birds, the largest number of generic and specific types peculiar to China are met with in Sze-ch‘uen. Foremost among these is the great panda (Aeluropus melanoleucus), representing a genus by itself, probably related to bears and to the true panda (Aelurus), the latter of which has a local race in Sze-ch‘uen. Next come the snub-nosed monkeys (Rhinopithecus), of which the typical species is a native of Sze-ch‘uen, while a second is found on the upper Mekong, and a third in the mountains of central China. In the Insectivora the swimming-shrew (Nectogale) forms another generic type peculiar to Sze-ch‘uen, which is also the sole habitat of the mole-likeScaptochirus, ofUropsilus, near akin to the JapaneseUrotrichus, ofScaptonyx, which connects the latter with the moles (Talpa), and ofNeotetracus, a relative of the Malay rat-shrews (Gymnura). Here also may be mentioned the raccoon-dog, forming the subgenusNyctereutes, common to China and Japan. The Himalayan black and the Malay bear have each a local race in Sze-ch‘uen, where the long-haired Fontanier’s cat (Felis tristis) and the Tibet cat (F. scripta) connect Indo-Malay species with the American ocelots, while the bay cat (F. temmincki), a Malay type, is represented by local forms in Sze-ch‘uen and Fu-chow. The Amurland leopard and Manchurian tiger likewise constitute local races of their respective species.Among ruminants, the Sze-ch‘uen takin represents a genus (Budorcas) found elsewhere in the Mishmi Hills and Bhutan, while serows (Nemorhaedus) and gorals (Urotragus), allied to Himalayan and Burmo-Malay types, abound. The Himalayan fauna is also represented by a race of the Kashmir hangul deer. Of other deer, the original habitat of Père David’s milu (Elaphurus), formerly kept in the Peking park, is unknown. The sika group, which is peculiar to China, Japan and Formosa, is represented byCervus hortulorumin Manchuria and the smallerC. manchuricusandsikain that province and the Yangtsze valley; while musk-deer (Moschus) abound in Kan-suh and Sze-ch‘uen. The small water-deer (HydropotesorHydrelaphus) of the Yangtsze valley represents a genus peculiar to the country, as do the three species of tufted deer (Elaphodus), whose united range extends from Sze-ch‘uen to Ning-po and I-ch‘ang. Muntjacs (Cervulus) are likewise very characteristic of the country, to which the white-tailed, plum-coloured species, like the TenasserimC. crinifrons, are peculiar. The occurrence of races of the wapiti in Manchuria and Amurland has been already mentioned.To refer in detail to the numerous forms of rodents inhabiting China is impossible here, and it must suffice to mention that the flying-squirrels (Pteromys) are represented by a large and handsome species in Sze-ch‘uen, where is also found the largest kind of bamboo-rat (Rhizomys), the other species of which are natives of the western Himalaya and the Malay countries. Dwarf hamsters of the genusCricetulusare natives of the northern provinces. In the extreme south, in Hai-nan, is found a gibbon ape (Hylobates), while langur (Semnopithecus) and macaque monkeys (Macacus) likewise occur in the south, one of the latter also inhabiting Sze-ch‘uen.To give an adequate account of Chinese ornithology would require space many times the length of this article. The gorgeous mandarin duck (Aix galerita) has already been mentioned among generic types common to America. In marked distinction to this is the number of species of pheasants inhabiting north-western China, whence the group ranges into the eastern Himalaya. Among Chinese species are two of the three species of blood-pheasants (Ithagenes), two tragopans (CeriornisorTragopan), a monal (Lophophorus), three out of the five species ofCrossoptilum, the other two being Tibetan, two kinds ofPucrasia, the gorgeous golden and Amherst’s pheasants alone representing the genusChrysolophus, together with several species of the typical genusPhasianus, among which it will suffice to mention thelong-tailedP. reevesi. The Himalayan bamboo-partridges (Bambusicola) have also a Chinese representative. The only other large bird that can be mentioned is the Manchurian crane, misnamedGrus japonensis. Pigeons include the peculiar subgenusDendroteron; while among smaller birds, warblers, tits and finches, all of an Eastern Holarctic type, constitute the common element in the avifauna. Little would be gained by naming the genera, peculiar or otherwise.China has a few peculiar types of freshwater tortoises, among whichOcadia sinensisrepresents a genus unknown elsewhere, while there is also a species of the otherwise Indian genusDamonia. The Chinese alligator,Alligator sinensis, has been already mentioned. Among lizards, the generaPlestiodon,Mabuia,TachydromusandGecko, of which the two latter are very characteristic of the Oriental region, range through China to Japan; and among snakes, the Malay python (Python reticulatus) is likewise Chinese. The giant salamander (Cryptobranchus, orMegalobatrachus, maximus) represents, as mentioned above, a type found elsewhere only in North America, whileHynobiusandOnychodactylusare peculiar generic types of salamanders. Among fishes, it must suffice to refer to the spoon-beaked sturgeon (Psephurus) of the Yangtsze-kiang, and the numerous members of the carp family to be found in the rivers of China. From these native carp the Chinese have produced two highly coloured breeds, the goldfish and the telescope-eyed carp.Among the invertebrates special mention may be made of the great ailanthus silk-moth (Attacus cynthia) of northern China and Japan, and also of its Manchurian relativeA. pernyi; while it may be added that the domesticated “silkworm” (Bombyx mori) is generally believed to be of Chinese origin, although this is not certain. Very characteristic of China is the abundance of handsomely coloured swallow-tailed butterflies of the familyPapilionidae. The Chinese kermes (Coccus sinensis) is also worth mention, on account of it yielding wax. As regards land and freshwater snails, China exhibits a marked similarity to Siam and India; the two groups in which the Chinese province displays decided peculiarities of its own beingHelix(in the wider sense) andClausilia. There are, for instance, nearly half a score of subgenera ofHelixwhose headquarters are Chinese, while among these, forms with sinistral shells are relatively common. The genusClausiliais remarkable on account of attaining a second centre of development in China, where its finest species, referable to several subgenera, occur. Carnivorous molluscs include a peculiar slug (Rathouisia) and the shelled generaEnneaandStreptaxis. In the western provinces species ofBuliminusare abundant, and in the operculate groupHeudeiaforms a peculiar type akin toHelicina, but with internal foldings to the shell.Lastly, it has to be mentioned that the waters of the Yangtsze-kiang are inhabited by a small jelly-fish, or medusa (Limnocodium kawaii), near akin toL. sowerbii, which was discovered in the hot-house tanks in the Botanical Gardens in the Regent’s Park, London, but whose real home is probably the Amazon.(R. L.*)Flora.The vegetation of China is extremely rich, no fewer than 9000 species of flowering plants having been already enumerated, of which nearly a half are endemic or not known to occur elsewhere. Whole provinces are as yet only partially explored; and the total flora is estimated to comprise ultimately 12,000 species. China is the continuation eastward of the great Himalayan mass, numerous chains of mountains running irregularly to the sea-board. Thousands of deep narrow valleys form isolated areas, where peculiar species have been evolved. Though the greater part of the country has long ago been cleared of its primeval forest and submitted to agriculture, there still remain some extensive forests and countless small woods in which the original flora is well preserved. Towards the north the vegetation is palaearctic, and differs little in its composition from that of Germany, Russia and Siberia. The flora of the western and central provinces is closely allied to that of the Himalayas and of Japan; while towards the south this element mingles with species derived from Indo-China, Burma and the plain of Hindostan. Above a certain elevation, decreasing with the latitude, but approximately 6000 ft. in the Yangtsze basin, there exist in districts remote from the traffic of the great rivers, extensive forests of conifers, like those of Central Europe in character, but with different species of silver fir, larch, spruce and Cembran pine. Below this altitude the woods are composed of deciduous and evergreen broad-leafed trees and shrubs, mingled together in a profusion of species. Pure broad-leafed forests of one or two species are rare, though small woods of oak, of alder and of birch are occasionally seen. There is nothing comparable to the extensive beech forests of Europe, the two species of Chinese beech being sporadic and rare trees. The heaths,CallunaandErica, which cover great tracts of barren sandy land in Europe, are absent from China, where the Ericaceous vegetation is made up of numerous species ofRhododendron, which often cover vast areas on the mountain slopes. Pine forests occur at low levels, but are always small in extent.The appearance of the vegetation is very different from that of the United States, which is comparable to China in situation and in extent. Though there are 60 species of oak in China, many with magnificent foliage and remarkable cupules, the red oaks, so characteristic of North America, with their bristle-pointed leaves, turning beautiful colours in autumn, are quite unknown. The great coniferous forest west of the Rocky Mountains has no analogue in China, the gigantic and preponderant Douglas fir being absent, while the giantSequoiasare represented only on a small scale byCryptomeria, which attains half their height.Certain remnants of the Miocene flora which have disappeared from Europe are still conspicuous and similar in North America and China. In both regions there are several species ofMagnolia; one species each ofLiriodendron, LiquidambarandSassafras; and curious genera likeNyssa, Hamamelis, DecumariaandGymnocladus. The swamps of the south-eastern states, in which still survive the once widely spreadTaxodiumor deciduous cypress, are imitated on a small scale by the marshy banks of rivers near Canton, which are clad withGlyptostrobus, the “water-pine” of the Chinese.Pseudolarix, CunninghamiaandKeteleeriaare coniferous genera peculiar to China, which have become extinct elsewhere. The most remarkable tree in China, the only surviving link between ferns and conifers,Ginkgo biloba, has only been seen in temple gardens, but may occur wild in some of the unexplored provinces. Its leaves have been found in the tertiary beds of the Isle of Mull.Most of the European genera occur in China, though there are curious exceptions like the plane tree, and the whole family of theCistaceae, which characterize the peculiarmaquisof the Mediterranean region. The rhododendrons, of which only four species are European, have their headquarters in China, numbering 130 species, varying in size from miniature shrubs 6 in. high to tall trees.Lysimachia, Primula, Clematis, RubusandGentianahave each a hundred species, extraordinary variable in habit, in size and in colour of the flowers. The ferns are equally polymorphic, numbering 400 species, and including strange genera likeArchangiopterisandCheiropteris, unknown elsewhere. About 40 species of bamboos have been distinguished; the one with a square stem from Fu-kien is the most curious.With a great wealth of beautiful flowering shrubs and herbaceous plants, the Chinese at an early period became skilled horticulturists. The emperor Wu Ti established in 111B.C.a botanic garden at Ch‘ang-an, into which rare plants were introduced from the west and south. Many garden varieties originated in China. The chrysanthemum, perhaps the most variable of cultivated flowers, is derived from two wild species (small and inconspicuous plants), and is mentioned in the ancient Chinese classics. We owe to the skill of the Chinese many kinds of roses, lilies, camellias and peonies; and have introduced from China some of the most ornamental plants in our gardens, asWistaria, Diervilla, Kerria, Incarvillea, Deutzia, Primula sinensis, Hemerocallis, &c. The peach and several oranges are natives of China. The varnish tree (Rhus vernicifera), from which lacquer is obtained; the tallow tree (Sapium sebiferum); the white mulberry, on which silkworms are fed; and the tea plant were all first utilized by the Chinese. The Chinese have also numerous medicinal plants, of which ginseng and rhubarb are best known. Nearly all our vegetables and cereals have their counterpart in China, where there are numerous varieties not yet introduced into Europe, though some, like the Soy bean, are now attracting great attention.(A. He.*)Authorities.—L. Richard (S.J.),Géographie de l’empire de Chine(Shanghai, 1905)—the first systematic account of China as a whole in modern times. The work, enlarged, revised and translated into English by M. Kennelly (S.J.), was reissued in 1908 as Richard’sComprehensive Geography of the Chinese Empire and Dependencies. This is the standard authority for the country and gives for each section bibliographical notes. It has been used in the revision of the present article. Valuable information on northern, central and western China is furnished by Col. C.C. Manifold and Col. A.W.S. Wingate in theGeog. Journ.vol. xxiii. (1904) and vol. xxix. (1907). Consult also Marshall Broomhall (ed.),The Chinese Empire: a General and Missionary Survey(London, 1907); B. Willis, E. Blackwelder and others,Research in China, vol. i. part i. “Descriptive Topography and Geology,” part ii. “Petrography and Zoology,” and Atlas (Washington, Carnegie Institution, 1906-1907); Forbes and Hemsley, “Enumeration of Chinese Plants,” inJourn. Linnean Soc. (Bot.), vols. xxiii. and xxxvi.; Bretschneider,History of European Botanical Discoveries in China; E. Tiessen,China das Reich der achtzehn Provinzen, Teil i. “Die allgemeine Geographie des Landes” (Berlin, 1902); andThe China Sea Directory(published by the British Admiralty), a valuable guide to the coasts: vol. ii. (5th ed., 1906) deals with Hong-Kong and places south thereof, vol. iii. (4th ed., 1906, supp. 1907) with the rest of the Chinese coast; vol. i. (5th ed., 1906) treats of the islands and straits in the S.W. approach to the China Sea. Much of China has not been surveyed, but considerable progress has been made since 1900.The Atlas of the Chinese Empire(London, 1908), a good general atlas, which, however, has no hill shading, gives maps of each province on the scale of 1:3,000,000. The preface contains a list of the best regional maps.The Journal af the China Branch of the Royal Asiatic Societycontains papers on all subjects relating to China.
The Coast.—The coast-line, following all the minor indentations, is reckoned at over 4500 m.; if only the larger inlets and promontories be regarded, the coast-line is about 2150 m. in length. Its shape is that of a semicircle, with its most easterly point midway (30° N.) between its northern and southern extremities. At either end of this semicircular sweep lies a peninsula, and beyond the peninsula a gulf. In the north are the peninsula of Shan-tung and the gulf of Chih-li; in the south the Lien-chow peninsula and the gulf of Tongking. Due south of Lien-chow peninsula, separated rom it by a narrow strait, is Hai-nan, the only considerable island of China. From the northern point of the gulf of Chih-li to 30° N., where is Hang-chow bay, the shores are flat and alluvial save where the Shan-tung peninsula juts out. Along this stretch there are few good natural harbours, except at the mouths of rivers and in the Shan-tung promontory; the sea is shallow and has many shoals. The waters bordering the coast of Chih-li are partly frozen in winter; at 10 m. from the shore the water is only 20 ft. deep. The proximity of Peking gives its few ports importance; that of Taku is at the mouth of the Peiho. In Shan-tung, deeply indented on its southern coast, are the ports of Chi-fu, Wei-hai-wei and Tsing-tao (the last in Kiao-chow bay). South of Shan-tung and north of the mouth of the Yangtsze huge sandbanks border the coast, with narrow channels between them and the shore. The estuary of the Yangtsze is 60 m. across; it contains islands and sandbanks, but there is easy access to Wusung (Shanghai) and other river ports. The bay of Hangchow, as broad at its entrance as the Yangtsze estuary, forms the mouth of the Tsien-tang-kiang. The Chusan and other groups of islands lie across the entrance of the bay.
South of Hang-chow bay the character of the coast alters. In place of the alluvial plain, with flat, sandy and often marshy shores, the coast is generally hilly, often rocky and abrupt; it abounds in small indentations and possesses numerous excellent harbours; in this region are Fu-chow, Amoy, Swatow, Hongkong, Macao, Canton and other well-known ports. The whole of this coast is bordered by small islands. Formosa lies opposite the S.E. coast, the channel between it and Fu-kien province being about 100 m. wide. Formosa protects the neighbouring regions of China from the typhoons experienced farther north and farther south.
Surface.—-As already indicated, one of the most noticeable features in the surface of China is the immense deltaic plain in the north-eastern portion of the country, which, curving round the mountainous districts of Shan-tung, extends for about 700 m. in a southerly direction from the neighbourhood of Peking and variesDeltaic Plain.from 150 to 500 m. in breadth. This plain is the delta of the Yellow river and, to some extent, that of the Yangtsze-kiang also. Beginning in the prefecture of Yung-p‘ing Fu, in the province of Chih-li, its outer limit passes in a westerly direction as far as Ch‘ang-p‘ing Chow, north-west of Peking. Thence running a south-south-westerly course it passes westward of Chêng-ting Fu and Kwang-p‘ing Fu till it reaches the upper waters of the Wei river in Ho-nan. From this point it turns westward and crosses the Hwang-ho or Yellow river in the prefecture of Hwai-k‘ing. Leaving this river it takes a course a little to the east of south, and passing west of Ju-ning Fu, in the province of Ho-nan, it turns in a more easterly direction as far as Luchow Fu. From this prefecture an arm of the plain, in which lies the Chao Lake, stretches southward from the Hwai river to the Yangtsze-kiang, and trending eastward occupies the region between that river and Hangchow Bay. To the north of this arm rises a hilly district, in the centre of which stands Nanking. The greater part of this vast plain descends very gently towards the sea, and is generally below the level of the Yellow river, hence the disastrous inundations which so often accompany the rise of that river. Owing to the great quantity of soil which is brought down by the waters of the Yellow river, and to the absence of oceanic currents, this delta is rapidly increasing and the adjoining seas are as rapidly becoming shallower. As an instance, it is said that the town of P‘utai was one Chinese mile2west of the seashore in the year 200B.C., and in 1730 it was 140 m. inland, thus giving a yearly encroachment upon the sea of about 100 ft. Again, Sien-shwuy-kow on the Peiho was on the seashore inA.D.500, and it is now about 18 m. inland.
Some of the ranges connected with the mountain system of central Asia which enter the western provinces of China have been mentioned above, others may be indicated here. In the eastern portion of Tibet the Kuen-lun range throws offMountains.a number of branches, which spread first of all in a south-easterly direction and eventually take a north and south course, partly in the provinces of Sze-ch‘uen and Yun-nan, where they divide the beds of the rivers which flow into Siam and French Indo-China, as well as the principal northern tributaries of the Yangtsze-kiang. In the north-west, traversing the western portion of the province of Kan-suh, are parallel ranges running N.W. and S.E. and forming a prolongation of the northern Tibetan mountains. They are known as the Lung-shan, Richthofen and Nan-shan, and join on the south-east the Kuen-lun range. The Richthofen range (locally called Tien-shan, or Celestial Mountains) attains elevations of over 20,000 ft. Several of its peaks are snowclad, and there are many glaciers. Forming the northern frontier of the province of Sze-ch‘uen run the Min-shan and the Kiu-lung (or Po-mêng) ranges, which, entering China in 102° E., extend in a general easterly course as far as 112° E. in the province of Hu-peh. These ranges have an average elevation of 8000 and 11,000 ft. respectively. In the south a number of parallel ranges spread from the Yun-nan plateau in an easterly direction as far as the province of Kwang-tung. Then turning north-eastward they run in lines often parallel with the coast, and cover large areas of the provinces of Fu-kien, Kiang-si, Cheh-kiang, Hu-nan and southern Ngan-hui, until they reach the Yangtsze-kiang; the valley of that river from the Tung-ting Lake to Chin-kiang Fu forming their northern boundary. In Fu-kien these hills attain the character of a true mountain range with heights of from 6500 to nearly 10,000 ft. Besides the chief ranges there are the Tai-hang Mountains in Shan-si, and many others, among which may be mentioned the ranges—part of the escarpment of the Mongolian plateau—which form the northern frontier of Chih-li. Here the highest peak is Ta-kuang-ting-tzu (6500 ft.), about 300 m. N.N.E. of Peking and immediately north of Wei Ch‘ang (the imperial hunting grounds).
Rivers and Canals.—The rivers of China are very numerous and there are many canals. In the north the rivers are only navigable by small craft; elsewhere they form some of the most frequented highways in the country. The two largest rivers,The Yellow River.the Yangtsze-kiang and the Hwang-ho (Yellow river), are separately noticed. The Hwang-ho (length about 2400 m.) has only one important tributary in China, the Wei-ho, which rises in Kan-suh and flows through the centre of Shen-si. Below the confluence the Hwang-ho enters the plains. According to the Chinese records this portion of the river has changed its course nine times during 2500 years, and has emptied itself into the sea at different mouths, the most northerly of which is represented as having been in about 39° N., or in the neighbourhood of the present mouth of the Peiho, and the most southerly being that which existed before the change in 1851-1853, in 34° N. Owing to its small value as a navigable highway and to its propensity to inundate the regions in its neighbourhood, there are no considerable towns on its lower course.
The Yangtsze-kiang is the chief waterway of China. The river, flowing through the centre of the country, after a course of 2900 m., empties itself into the Yellow Sea in about 31° N. Unlike the Yellow river, the Yangtsze-kiang is dotted along its navigable portions with many rich and populous cities, among which are Nanking, An-ch‘ing (Ngank‘ing), Kiu-kiang, Hankow and I-ch‘ang.From its mouth to I-ch‘ang, about 1000 m., the river is navigable by large steamers. Above this last-named city the navigation becomesThe Yangtsze-kiang.impossible for any but light native craft or foreign vessels specially constructed for the navigation, by reason of the rapids which occur at frequent intervals in the deep mountain gorges through which the river runs between Kwei-chow and I-ch‘ang. Above Kwei-chow it receives from the north many tributaries, notably the Min, which water the low table-land of central Sze-ch‘uen. The main river itself has in this province a considerable navigable stretch, while below I-ch‘ang it receives the waters of numerous navigable affluents. The Yangtsze system is thus all important in the economic and commercial development of China.
Perhaps the most remarkable of the affluents of the Yangtsze is the Han-kiang or Han river. It rises in the Po-mêng mountains to the north of the city of Ning-kiang Chow in Shen-si. Taking a generally easterly course from its source as far as Fan-cheng, it from that point takes a more southerly direction and empties itself into the Yangtsze-kiang at Han-kow, “the mouth of the Han.” Here it is only 200 ft. wide, while higher up it widens to 2600 ft. It is navigable by steamers for 300 m. The summer high-water line is for a great part of its course, from I-ch‘eng Hien to Han-kow, above the level of its banks. Near Sien-t‘ao-chên the elevation of the plain above low water is no more than 1 ft., and in summer the river rises about 26 ft. above its lowest level. To protect themselves against inundations the natives have here, as elsewhere, thrown up high embankments on both sides of the river, but at a distance from the natural banks of about 50 to 100 ft. This intervening space is flooded every year, and by the action of the water new layers of sand and soil are deposited every summer, thus strengthening the embankments from season to season.
The Hwai-ho is a large river of east central China flowing between the Hwang-ho and the Yangtsze-kiang. The Hwai-ho and its numerous affluents (it is said to have 72 tributaries) rise in Ho-nan. The main river flows through the centre of Ngan-hui, in which province it receives from the N.W. the Sha-ho, Fei-ho and other important affluents. Formerly it received through the Sha-ho part of the waters of the Hwang-ho. The Hwai-ho flows into the Hungtso lake, through which it feeds the Grand Canal, not far from the old course of the Hwang-ho, and probably at one time joined that river not far from its mouth. It has a length of about 800 m. and is navigable from the point where it leaves the hill country of Ho-nan to Lake Hungtso. It is subject to violent floods, which inundate the surrounding country for a distance of 10 to 20 m. Many of its tributaries are also navigable for considerable distances.
Next in importance to the Yangtsze-kiang as a water highway is the Yun-ho, or, as it is generally known in Europe, the Grand Canal. This magnificent artificial river reaches from Hang-chow Fu in the province of Cheh-kiang to Tientsin in Chih-li,Grand Canal.where it unites with the Peiho, and thus may be said to extend to Tung-chow in the neighbourhood of Peking. According to the itineraries published by Père Gandar, the total length of the canal is 3630li, or about 1200 m. A rough measurement, taking account only of the main bends of the canal, makes its length 850 m. After leaving Hang-chow the canal passes round the eastern border of the Tai-hu or Great Lake, surrounding in its course the beautiful city of Su-chow, and then trends in a generally north-westerly direction through the fertile districts of Kiang-su as far as Chin-kiang on the Yangtsze-kiang. In this, the southern section, the slope is gentle and water is plentiful (from 7 ft. at low water to 11 ft., and occasionally 13 ft. at high water). Between Su-chow and Chin-kiang the canal is often over 100 ft. wide, and its sides are in many places faced with stone. It is spanned by fine stone bridges, and near its banks are many memorial arches and lofty pagodas. In the central portion of the canal, that is between Chin-kiang and Tsing-kiang-pu, at which latter place it crosses the dry channel which marks the course of the Yellow river before 1852, the current is strong and difficult to ascend in the upward (northern) journey. This part of the canal skirts several lakes and is fed by the Hwai-ho as it issues from the Hungtso lake. The country lying west of the canal is higher than its bed; while the country east is lower than the canal. The two regions are known respectively as Shang-ho (above the river) and Ssia-ho (below the river). Waste weirs opening on the Ssia-ho (one of the great rice-producing areas of China) discharge the surplus water in flood seasons. The northern and considerably the longest section of the canal extends from the old bed of the Yellow river to Tientsin. It largely utilizes existing rivers and follows their original windings. Between Tsing-kiang-pu and the present course of the Yellow river the canal trends N.N.W., skirting the highlands of Shan-tung. In this region it passes through a series of lagoons, which in summer form one lake—Chow-yang. North of that lake on the east bank of the canal, is the city of Tsi-ning-chow. About 25 m. N. of that city the highest level of the canal is reached at the town of Nan Wang. Here the river Wen enters the canal from the east, and about 30 m. farther N. the Yellow river is reached. On the west side of the canal, at the point where the Yellow river now cuts across it, there is laid down in Chinese maps of the 18th century a dry channel which is described as being that once followed by the Yellow river,i.e.before it took the channel it abandoned in 1851-1853. The passage of the Yellow river to the part of the canal lying north of that stream is difficult, and can only be effected at certain levels of the river. Frequently the waters of the river are either too low or the current is too strong to permit a passage. Leaving this point the canal passes through a well-wooded and hilly country west of Tung-p‘ing Chow and east of Tung-ch‘ang Fu. At Lin-ching Chow it is joined at right angles by the Wei river in the midst of the city. Up to this point,i.e.from Tsing-kiang-pu to Lin-ching Chow, a distance of over 300 m., navigation is difficult and the water-supply often insufficient. The differences of level, 20 to 30 ft., are provided for by barrages over which the boats—having discharged their cargo—are hauled by windlasses. Below the junction with the Wei the canal borrows the channel of the river and again becomes easily navigable. Crossing the frontier into Chih-li, between Te Chow and Tsang Chow, which it passes to the west, it joins the Peiho at Tientsin, after having received the waters of the Keto river in the neighbourhood of Tsing Hien.3
The most ancient part of the canal is the section between the Yangtsze and the Hwai-ho. This part is thought, on the strength of a passage in one of the books of Confucius, to have been built c. 486B.C.It was repaired and enlarged in the 3rd centuryA.D.The southern part, between the Yangtsze and Hang-chow, was built early in the 7th centuryA.D.The northern part is stated to have been constructed in the three years 1280-1283. The northern portion of the canal is now of little use as a means of communication between north and south.4It is badly built, neglected and charged with the mud-laden waters of the Yellow river. The “tribute fleet” bearing rice to Peking still uses this route; but the rice is now largely forwarded by sea. The central and southern portions of the canal are very largely used.
The Peiho (length about 350 m.) is of importance as being the high waterway to Peking. Taking its rise in the Si-shan, or Western Mountains, beyond Peking, it passes the city of T‘sung-chow, the port of Peking, and Tientsin, where it meets the waters of the Hun-ho and empties itself into the gulf of Chih-li at the village of Taku. The Peiho is navigable for small steamers as far as Tientsin during the greater part of the year, but from the end of November to the beginning of March it is frozen up.
In the southern provinces the Si-kiang, or Western river, is the most considerable. It has a length of over 1000 m. This river takes its rise in the prefecture of Kwang-nan Fu in Yun-nan, whence it reaches the frontier of Kwang-si at a distanceThe Si-kiang.of about 90 li from its source. Then trending in a north-easterly direction it forms the boundary between the two provinces for about 150 li. From this point it takes a generally south-easterly course, passing the cities of Tsien Chow, Fung-e Chow, Shang-lin Hien, Lung-ngan Hien, Yung-kang Chow and Nan-ning Fu to Yung-shan Hien. Here it makes a bend to the north-east, and continues this general direction as far as Sin-chow Fu, a distance of 800 li, where it meets and joins the waters of the Kien-kiang from the north. Its course is then easterly, and after passing Wu-chow Fu it crosses the frontier into Kwang-tung. In this part of its course it flows through a gorge 3 m. long and in places but 270 yds. in width. Both above and below this gorge it is 1 m. wide. Some 30 m. above Canton it divides into two main and several small branches. The northern branch, called Chu-kiang, or Pearl river, flows past Fat-shan and Canton and reaches the sea through the estuary called the Bocca Tigris or Bogue, at the mouth of which is the island of Hong-Kong. The southern branch, which retains the name of Si-kiang, reaches the sea west of Macao. Near the head of its delta the Si-kiang receives the Pei-kiang, a considerable river which flows through Kwang-tung in a general N. to S. direction. Like the Yangtsze-kiang the Si-kiang is known by various names in different parts of its course. From its source to Nan-ning Fu in Kwang-si it is called the Si-yang-kiang, or river of the Western Ocean; from Nan-ning Fu to Sin-chow Fu it is known as the Yu-kiang, or the Bending river; and over the remainder of its course it is recognized by the name of the Si-kiang, or Western river. The Si-kiang is navigable as far as Shao-king, 130 m., for vessels not drawing more than 15 ft. of water, and vessels of a light draught may easily reach Wu-chow Fu, in Kwang-si, which is situated 75 m. farther up. In winter the navigation is difficult above Wu-chow Fu. Above that place there is a rapid at low water, but navigation is possible to beyond Nan-ning Fu.
Click to see detailed left-side.Click to see detailed right-side.
Lakes.—There are numerous lakes in the central provinces of China. The largest of these is the Tung-t‘ing in Hu-nan, which, according to the Chinese geographers, is upwards of 800 li, or 266 m., in circumference. In native gazetteers its various portions are known under distinct names; thus it is said to include the Ts‘ing-ts‘ao, or Green Grass Lake; the Ung, or Venerable Lake; the Chih-sha, or Red Sand Lake; the Hwang-yih, or Imperial Post-house Lake; the Ngan-nan, or Peaceful Southern Lake; and the Ta-tung, orGreat Deep Lake. In ancient times it went by the name of the Kiu-kiang Hu, or Lake of the Nine Rivers, from the fact that nine rivers flowed into it. Its chief affluents are the Siang-kiang, which rises in the highlands in the north of Kwang-si and flows in a general N.N.E. direction, and the Yuen-kiang, which flows N. and then E. from the eastern border of Kwei-chow. The lake is connected with the Yangtsze-kiang by two canals, the Taping and the Yochow Fu. In summer it is fed by the overflow from the Yangtsze-kiang; in winter it pours its waters into that river through the Yochow Fu canal. During the winter and spring the water of the lake is so low that the shallow portions become islands, separated by rivers such as the Siang and Yuen, and numberless streams; but in summer, owing to the rise in the waters of the Yangtsze-kiang, the whole basin of the lake is filled. It is then about 75 m. long and 60 m. broad. About 180 m. E. of the Tung-t‘ing lake is the Poyang lake, which occupies the low-lying part of the province of Kiang-si, and is connected with the Yangtsze by the Hu-kow canal. The Poyang lake is also subject to a wide difference between high and low water, but not quite to the same extent as the Tung-t‘ing lake, and its landmarks are more distinctly defined. It is about 90 m. long by 20 broad. The T‘ai lake, in the neighbourhood of Su-chow Fu, is also celebrated for its size and the beauty of its surroundings. It is about 150 m. in circumference, and is dotted over with islands, on which are built temples for the devotees of religion, and summer-houses for the votaries of pleasure from the rich and voluptuous cities of Hang-chow and Su-chow. The boundary line between the provinces of Cheh-kiang and Kiang-su crosses its blue waters, and its shores are divided among thirteen prefectures. Besides these lakes there are, among others, two in Yun-nan, the Kun-yang-hai (Tien-chi) near Yun-nan Fu, which is 40 m. long and is connected with the Yangtsze-kiang by the Pu-to river, and the Erh-hai (Urh-hai) to the east of the city of Tali.
The Great Wall.—Along the northern provinces of Chih-li, Shan-si, Shen-si and Kan-suh, over 22° of longitude (98° to 120° E.), stretches the Great Wall of China, built to defend the country against foreign aggression. It was begun in the 3rd centuryB.C., was repaired in the 15th century, and in the 16th century was extended by 300 m. Following the windings the wall is 1500 m. long. Starting near the seashore5at Shan-hai-kwan on the gulf of Liao-tung, where the Chinese and Manchurian frontiers meet, it goes eastward past Peking (which is about 35 m. to the south) and then trends S. and E. across Shan-si to the Hwang-ho. From the neighbourhood of Peking to the Hwang-ho there is an inner and an outer wall. The outer (northern) wall passes through Kalgan, thus guarding the pass into Mongolia. A branch wall separates the greater part of the western frontier of Chih-li from Shan-si. West of the Hwang-ho the Great Wall forms the northern frontier of Shen-si, and west of Shen-si it keeps near the northern frontier of Kan-suh, following for some distance in that province the north bank of the Hwang-ho. It ends at Kiayu-kwan (98° 14′E.) just west of Su-chow. This part of the wall was built to protect the one main artery leading from central Asia to China through Kan-suh and Shen-si by the valley of the Wei-ho, tributary of the Hwang-ho. There is a branch wall in Kan-suh running west and south to protect the Tibetan frontier. The height of the wall is generally from 20 to 30 ft., and at intervals of some 200 yds. are towers about 40 ft. high. Its base is from 15 to 25 ft. thick and its summit 12 ft. wide. The wall is carried over valleys and mountains, and in places is over 4000 ft. above sea-level. Military posts are still maintained at the chief gates or passes—at Shan-hai-kwan, the Kalgan pass, the Yenmun pass (at the N. of Shan-si) and the Kaiyu pass in the extreme west, through which runs the caravan route to Barkal in Turkestan. Colonel A.W.S. Wingate, who in the opening years of the 20th century visited the Great Wall at over twenty places widely apart and gathered many descriptions of it in other places, states that its position is wrongly shown “on the maps of the day” (1907) in a number of places; while in others it had ceased to exist, “the only places where it forms a substantial boundary being in the valley bottoms, on the passes and where it crosses main routes. These remarks apply with particular force to the branch running south-west from the Nan-k‘ow pass and forming the boundary of Chih-li and Shan-si provinces.” In Colonel Wingate’s opinion the wall was originally built by degrees and in sections, not of hewn stone, but of round boulders and earth, the different sections being repaired as they fell into ruin. “Only in the valley bottoms and on the passes was it composed of masonry or brickwork. The Mings rebuilt of solid masonry all those sections through which led a likely road for invading Tatars to follow, or where it could be seen at a distance from the sky-line.” The building of the wall “was a sufficiently simple affair,” not to be compared with the task of building the pyramids of Egypt.6
Climate.—The climate over so vast an area as China necessarily varies greatly. The southern parts of Yun-nan, Kwang-si and Kwang-tung (including the city of Canton) lie within the tropics. The northern zone (in which lies Peking) by contrast has a climate which resembles that of northern Europe, with winters of Arctic severity. The central zone (in which Shanghai is situated) has a generally temperate climate. But over both northern and central China the influence of the great plateau of Mongolia tends to establish uniform conditions unusual in so large an area. The prevailing winds during summer—the rainy season—are south-easterly, caused by heat and the ascending current of air over the sandy deserts of central Asia, thus drawing in a current from the Pacific Ocean. In the winter the converse takes place, and the prevailing winds, descending from the Mongolian plateau, are north and north-west, and are cold and dry. From October to May the climate of central China is bracing and enjoyable. The rainfall is moderate and regular.
In northern China the inequalities both of temperature and rainfall are greater than in the central provinces. In the province of Chih-li, for example, the heat of summer is as intense as is the cold of winter. In summer the rains often render the plain swampy, while the dry persistent westerly winds of spring create dust storms (experienced in Peking from March to June). The rainfall is, however, uncertain, and thus the harvests are precarious. The provinces of Shan-tung and Shan-si are peculiarly liable to prolonged periods of drought, with consequent severe famines such as that of 1877-1878, when many millions died. In these regions the air is generally extremely dry, and the daily variations of temperature consequent on excessive radiation are much greater than farther south.
Accurate statistics both of heat and rainfall are available from a few stations only. The rainfall on the southern coasts is said to be about 100 in. yearly; at Peking the rainfall is about 24 in. a year. In the coast regions the temperatures of Peking, Shanghai and Canton may be taken as typical of those of the northern, central and southern zones. In Peking (39° N.) the mean annual temperature is about 53° F., the mean for January 23°, for July 79°. In Shanghai (31° 11′ N.)7the mean annual temperature is 59°, the mean for January 36.2°, for July 80.4°. In Canton (23° 15′ N.) the mean annual temperature is 70°, the mean for January 54°, for July 82°. The range of temperature, even within the tropics, is noteworthy. At Peking and Tientsin the thermometer in winter falls sometimes to 5° below zero and rises in summer to 105° (at Taku 107° has been recorded); in Shanghai in winter the thermometer falls to 18° and in summer rises to 102°. In Canton frost is said to have been recorded, but according to theChina Sea Directorythe extreme range is from 38° to 100°.8The climate of Shanghai, which resembles, but is not so good as, that of the Yangtsze-kiang valley generally, is fairly healthy, but there is an almost constant excess of moisture. The summer months, July to September, are very hot, while snow usually falls in December and January.
At Canton and along the south coast the hot season corresponds with the S.W. monsoon; the cool season—mid October to end of April—with the N.E. monsoon. Farther north, at Shanghai, the S.W. monsoon is sufficiently felt to make the prevailing wind in summer southerly.
Provinces.—China proper is divided into the following provinces: Cheh-kiang, Chih-li, Fu-kien, Ngan-hui (An-hui), Ho-nan, Hu-nan, Hu-peh, Kan-suh, Kiang-si, Kiang-su, Kwang-si, Kwang-tung, Kwei-chow, Shan-si, Shan-tung, Shen-si, Sze-ch‘uen and Yun-nan. See the separate notices of each province and the article on Shêng-king, the southern province of Manchuria.
(X.)
Geology.
The Palaeozoic formations of China, excepting only the upper part of the Carboniferous system, are marine, while the Mesozoic and Tertiary deposits are estuarine and freshwater or else of terrestrial origin. From the close of the Palaeozoic period down to the present day the greater part of the empire has been dry land, and it is only in the southern portion of Tibet and in the western Tian Shan that any evidence of a Mesozoic sea has yet been found. The geological sequence may be summarized as follows:—
Archean.—Gneiss, crystalline schists, phyllites, crystalline limestones. Exposed in Liao-tung, Shan-tung, Shan-si, northern Chih-li and in the axis of the mountain ranges,e.g.the Kuen-lun and the ranges of southern China.
Sinian.—Sandstones, quartzites, limestones. Sometimes rests unconformably upon the folded rocks of the Archaen system; but sometimes, according to Lóczy, there is no unconformity. Covers a large area in the northern part of China proper; absent in the eastern Kuen-lun; occurs again in the ranges of S.E. China. In Liao-tung Cambrian fossils have been found near the summit of the series; they belong to the oldest fauna known upon the earth, the fauna of theOlenelluszone. It is, however, not improbable that in many places beds of considerably later date have been included in the Sinian system.
Ordovician.—Ordovician fossils have been found in the Lung-shan, Kiang-su (about 50 m. east of Nan-king), in the south-west of Cheh-kiang and in the south-east of Yun-nan. Ordovician beds probably occur also in the Kuen-lun.
Silurian.—Limestones and slates with Silurian corals and other fossils have been found in Sze-ch‘uen.
Devonian.—Found in Kan-suh and in the Tsing-ling-shan, but becomes much more important in southern China. Occurs also on the south of the Tian-shan, in the Altyn-tagh, the Nan-shan and the western Kuen-lun.
Carboniferous.—Covers a large area in northern China, in the plateau of Shen-si and Shan-si, extending westwards in tongues between the folds of the Kuen-lun. In this region it consists of a lower series of limestones and an upper series of sandstones with seams of coal, which may perhaps be in part of Permian age. This is probably the most extensive coalfield in the world.
In south China the whole series consists chiefly of limestones, and the coal seams are comparatively unimportant. Carboniferous beds are also found in the Tian-shan, the Nan-shan, Kan-suh, on the southern borders of the Gobi, &c.
Mesozoic.—Marine Triassic beds containing fossils similar to those of the German Muschelkalk have been found by Lóczy near Chung-tien, on the eastern border of the Tibetan plateau. Elsewhere, however, the Mesozoic is represented chiefly by a red sandstone, which covers the greater part of Sze-ch‘uen and fills also a number of troughs amongst the older beds of southern China. No marine fossils are found in this sandstone, but remains of plants are numerous, and these belong to the Rhaetic, Lias and Lower Oolite. No Cretaceous beds are known in China excepting in S. Tibet (on the shores of the Tengri-nor) and in the western portion of the Tian-shan.
Cainozoic and Recent.—No marine deposits of this age are known. Although the loess of the great plain and the sand of the desert are still in process of formation, the accumulation of these deposits probably began in the Tertiary period.
Volcanic Rocks.—Amongst the Archean rocks granitic and other intrusions are abundant, but of more modern volcanic activity the remains are comparatively scanty. In south China there is no evidence of Tertiary or Post-Tertiary volcanoes, but groups of volcanic cones occur in the great plain of north China. In the Liao-tung and Shan-tung peninsulas there are basaltic plateaus, and similar outpourings occur upon the borders of Mongolia. All these outbursts appear to be of Tertiary or later data.
Loess.—One of the most characteristic deposits of China is the loess, which not merely imparts to north China the physical character of the scenery, but also determines the agricultural products, the transport, and general economic life of the people of that part of the country. It is peculiar to north China and it is not found south of the Yangtsze. The loess is a solid but friable earth of brownish-yellow colour, and when triturated with water is not unlike loam, but differs from the latter by its highly porous and tubular structure. The loess soil is extremely favourable to agriculture. (SeeLoessandinfra, § Agriculture.)
The loess is called by the ChineseHwang-t‘u, or yellow earth, and it has been suggested that the imperial titleHwang-ti, Yellow Emperor or Ruler of the Yellow, had its origin in the fact that the emperor is lord of the loess or yellow earth.
Structurally, China proper may be divided into two regions, separated from each other by the folded range of the Tsing-ling-shan, which is a continuation of the folded belt of the Kuen-lun. North of this chain the Palaeozoic beds areStructure.in general nearly horizontal, and the limestones and sandstones of the Sinian and Carboniferous systems form an extensive plateau which rises abruptly from the western margin of the great plain of northern China. The plateau is deeply carved by the rivers which flow through it; and the strata are often faulted, but they are never sharply folded. South of the Tsing-ling-shan, on the other hand, the Palaeozoic beds are thrown into a series of folds running from W. 30° S. to E. 30° N., which form the hilly region of southern China. Towards Tongking these folds probably bend southwards and join the folds of Further India. Amongst these folded beds lie trough-like depressions filled with the Mesozoic red sandstone which lies unconformably upon the Palaeozoic rocks.
The present configuration of China is due, in a very considerable degree, to faulting. The abrupt eastern edge of the Shan-si plateau, where it overlooks the great plain, is a line of fault, or rather a series of step faults, with the downthrow on the east; and von Richthofen has shown reason to believe that this line of faulting is continued far to the south and to the north. He believed also that the present coast-line of China has to a large extent been determined by similar faults with their downthrow on the east.
Concerning the structure of the central Asian plateau our knowledge is still incomplete. The great mountain chains, the Kuen-lun, the Nan-shan and the Tian-shan, are belts of folding; but the Mongolian Altai is a horst—a strip of ancient rock lying between two faults and with a depressed area upon each side. In the whole of this northern region faulting, as distinct from folding, seems to have played an important part. Along the southern margin of the Tian-shan there is a remarkable trough-like depression which appears to lie between two approximately parallel faults.
(P. La.)
Fauna.
China lies within two zoological provinces or regions, its southern portion forming a part of the Oriental or Indian region and having a fauna close akin to that of the western Himalaya, Burma and Siam, whereas the districts to the north of Fu-chow and south of the Yangtsze-kiang lie within the eastern Holarctic (Palaearctic) region, or rather the southern fringe of the latter, which has been separated as the Mediterranean transitional region. Of these two divisions of the Chinese fauna, the northern one is the more interesting, since it forms the chief home of a number of peculiar generic types, and also includes types represented elsewhere at the present day (exclusive in one case of Japan) only in North America. The occurrence in China of these types common to the eastern and western hemispheres is important in regard to the former existence of a land-bridge between Eastern Asia and North America by way of Bering Strait.
Of the types peculiar to China and North America the alligator of the Yangtsze-kiang is generically identical with its Mississippi relative. The spoon-beaked sturgeon of the Yangtsze and Hwang-ho is, however, now separated, asPsephurus, from the closely allied AmericanPolyodon. Among insectivorous mammals the Chinese and Japanese shrew-moles, respectively forming the generaUropsilusandUrotrichus, are represented in America byNeurotrichus. The giant salamander of the rivers of China and Japan and the Chinese mandarin duck are by some included in the same genera as their American representatives, while by others they are referred to genera apart. Whichever view we take does not alter their close relationship. One wapiti occurs on the Tibetan frontier, and others in Manchuria and Amurland.
As regards mammals and birds, the largest number of generic and specific types peculiar to China are met with in Sze-ch‘uen. Foremost among these is the great panda (Aeluropus melanoleucus), representing a genus by itself, probably related to bears and to the true panda (Aelurus), the latter of which has a local race in Sze-ch‘uen. Next come the snub-nosed monkeys (Rhinopithecus), of which the typical species is a native of Sze-ch‘uen, while a second is found on the upper Mekong, and a third in the mountains of central China. In the Insectivora the swimming-shrew (Nectogale) forms another generic type peculiar to Sze-ch‘uen, which is also the sole habitat of the mole-likeScaptochirus, ofUropsilus, near akin to the JapaneseUrotrichus, ofScaptonyx, which connects the latter with the moles (Talpa), and ofNeotetracus, a relative of the Malay rat-shrews (Gymnura). Here also may be mentioned the raccoon-dog, forming the subgenusNyctereutes, common to China and Japan. The Himalayan black and the Malay bear have each a local race in Sze-ch‘uen, where the long-haired Fontanier’s cat (Felis tristis) and the Tibet cat (F. scripta) connect Indo-Malay species with the American ocelots, while the bay cat (F. temmincki), a Malay type, is represented by local forms in Sze-ch‘uen and Fu-chow. The Amurland leopard and Manchurian tiger likewise constitute local races of their respective species.
Among ruminants, the Sze-ch‘uen takin represents a genus (Budorcas) found elsewhere in the Mishmi Hills and Bhutan, while serows (Nemorhaedus) and gorals (Urotragus), allied to Himalayan and Burmo-Malay types, abound. The Himalayan fauna is also represented by a race of the Kashmir hangul deer. Of other deer, the original habitat of Père David’s milu (Elaphurus), formerly kept in the Peking park, is unknown. The sika group, which is peculiar to China, Japan and Formosa, is represented byCervus hortulorumin Manchuria and the smallerC. manchuricusandsikain that province and the Yangtsze valley; while musk-deer (Moschus) abound in Kan-suh and Sze-ch‘uen. The small water-deer (HydropotesorHydrelaphus) of the Yangtsze valley represents a genus peculiar to the country, as do the three species of tufted deer (Elaphodus), whose united range extends from Sze-ch‘uen to Ning-po and I-ch‘ang. Muntjacs (Cervulus) are likewise very characteristic of the country, to which the white-tailed, plum-coloured species, like the TenasserimC. crinifrons, are peculiar. The occurrence of races of the wapiti in Manchuria and Amurland has been already mentioned.
To refer in detail to the numerous forms of rodents inhabiting China is impossible here, and it must suffice to mention that the flying-squirrels (Pteromys) are represented by a large and handsome species in Sze-ch‘uen, where is also found the largest kind of bamboo-rat (Rhizomys), the other species of which are natives of the western Himalaya and the Malay countries. Dwarf hamsters of the genusCricetulusare natives of the northern provinces. In the extreme south, in Hai-nan, is found a gibbon ape (Hylobates), while langur (Semnopithecus) and macaque monkeys (Macacus) likewise occur in the south, one of the latter also inhabiting Sze-ch‘uen.
To give an adequate account of Chinese ornithology would require space many times the length of this article. The gorgeous mandarin duck (Aix galerita) has already been mentioned among generic types common to America. In marked distinction to this is the number of species of pheasants inhabiting north-western China, whence the group ranges into the eastern Himalaya. Among Chinese species are two of the three species of blood-pheasants (Ithagenes), two tragopans (CeriornisorTragopan), a monal (Lophophorus), three out of the five species ofCrossoptilum, the other two being Tibetan, two kinds ofPucrasia, the gorgeous golden and Amherst’s pheasants alone representing the genusChrysolophus, together with several species of the typical genusPhasianus, among which it will suffice to mention thelong-tailedP. reevesi. The Himalayan bamboo-partridges (Bambusicola) have also a Chinese representative. The only other large bird that can be mentioned is the Manchurian crane, misnamedGrus japonensis. Pigeons include the peculiar subgenusDendroteron; while among smaller birds, warblers, tits and finches, all of an Eastern Holarctic type, constitute the common element in the avifauna. Little would be gained by naming the genera, peculiar or otherwise.
China has a few peculiar types of freshwater tortoises, among whichOcadia sinensisrepresents a genus unknown elsewhere, while there is also a species of the otherwise Indian genusDamonia. The Chinese alligator,Alligator sinensis, has been already mentioned. Among lizards, the generaPlestiodon,Mabuia,TachydromusandGecko, of which the two latter are very characteristic of the Oriental region, range through China to Japan; and among snakes, the Malay python (Python reticulatus) is likewise Chinese. The giant salamander (Cryptobranchus, orMegalobatrachus, maximus) represents, as mentioned above, a type found elsewhere only in North America, whileHynobiusandOnychodactylusare peculiar generic types of salamanders. Among fishes, it must suffice to refer to the spoon-beaked sturgeon (Psephurus) of the Yangtsze-kiang, and the numerous members of the carp family to be found in the rivers of China. From these native carp the Chinese have produced two highly coloured breeds, the goldfish and the telescope-eyed carp.
Among the invertebrates special mention may be made of the great ailanthus silk-moth (Attacus cynthia) of northern China and Japan, and also of its Manchurian relativeA. pernyi; while it may be added that the domesticated “silkworm” (Bombyx mori) is generally believed to be of Chinese origin, although this is not certain. Very characteristic of China is the abundance of handsomely coloured swallow-tailed butterflies of the familyPapilionidae. The Chinese kermes (Coccus sinensis) is also worth mention, on account of it yielding wax. As regards land and freshwater snails, China exhibits a marked similarity to Siam and India; the two groups in which the Chinese province displays decided peculiarities of its own beingHelix(in the wider sense) andClausilia. There are, for instance, nearly half a score of subgenera ofHelixwhose headquarters are Chinese, while among these, forms with sinistral shells are relatively common. The genusClausiliais remarkable on account of attaining a second centre of development in China, where its finest species, referable to several subgenera, occur. Carnivorous molluscs include a peculiar slug (Rathouisia) and the shelled generaEnneaandStreptaxis. In the western provinces species ofBuliminusare abundant, and in the operculate groupHeudeiaforms a peculiar type akin toHelicina, but with internal foldings to the shell.
Lastly, it has to be mentioned that the waters of the Yangtsze-kiang are inhabited by a small jelly-fish, or medusa (Limnocodium kawaii), near akin toL. sowerbii, which was discovered in the hot-house tanks in the Botanical Gardens in the Regent’s Park, London, but whose real home is probably the Amazon.
(R. L.*)
Flora.
The vegetation of China is extremely rich, no fewer than 9000 species of flowering plants having been already enumerated, of which nearly a half are endemic or not known to occur elsewhere. Whole provinces are as yet only partially explored; and the total flora is estimated to comprise ultimately 12,000 species. China is the continuation eastward of the great Himalayan mass, numerous chains of mountains running irregularly to the sea-board. Thousands of deep narrow valleys form isolated areas, where peculiar species have been evolved. Though the greater part of the country has long ago been cleared of its primeval forest and submitted to agriculture, there still remain some extensive forests and countless small woods in which the original flora is well preserved. Towards the north the vegetation is palaearctic, and differs little in its composition from that of Germany, Russia and Siberia. The flora of the western and central provinces is closely allied to that of the Himalayas and of Japan; while towards the south this element mingles with species derived from Indo-China, Burma and the plain of Hindostan. Above a certain elevation, decreasing with the latitude, but approximately 6000 ft. in the Yangtsze basin, there exist in districts remote from the traffic of the great rivers, extensive forests of conifers, like those of Central Europe in character, but with different species of silver fir, larch, spruce and Cembran pine. Below this altitude the woods are composed of deciduous and evergreen broad-leafed trees and shrubs, mingled together in a profusion of species. Pure broad-leafed forests of one or two species are rare, though small woods of oak, of alder and of birch are occasionally seen. There is nothing comparable to the extensive beech forests of Europe, the two species of Chinese beech being sporadic and rare trees. The heaths,CallunaandErica, which cover great tracts of barren sandy land in Europe, are absent from China, where the Ericaceous vegetation is made up of numerous species ofRhododendron, which often cover vast areas on the mountain slopes. Pine forests occur at low levels, but are always small in extent.
The appearance of the vegetation is very different from that of the United States, which is comparable to China in situation and in extent. Though there are 60 species of oak in China, many with magnificent foliage and remarkable cupules, the red oaks, so characteristic of North America, with their bristle-pointed leaves, turning beautiful colours in autumn, are quite unknown. The great coniferous forest west of the Rocky Mountains has no analogue in China, the gigantic and preponderant Douglas fir being absent, while the giantSequoiasare represented only on a small scale byCryptomeria, which attains half their height.
Certain remnants of the Miocene flora which have disappeared from Europe are still conspicuous and similar in North America and China. In both regions there are several species ofMagnolia; one species each ofLiriodendron, LiquidambarandSassafras; and curious genera likeNyssa, Hamamelis, DecumariaandGymnocladus. The swamps of the south-eastern states, in which still survive the once widely spreadTaxodiumor deciduous cypress, are imitated on a small scale by the marshy banks of rivers near Canton, which are clad withGlyptostrobus, the “water-pine” of the Chinese.Pseudolarix, CunninghamiaandKeteleeriaare coniferous genera peculiar to China, which have become extinct elsewhere. The most remarkable tree in China, the only surviving link between ferns and conifers,Ginkgo biloba, has only been seen in temple gardens, but may occur wild in some of the unexplored provinces. Its leaves have been found in the tertiary beds of the Isle of Mull.
Most of the European genera occur in China, though there are curious exceptions like the plane tree, and the whole family of theCistaceae, which characterize the peculiarmaquisof the Mediterranean region. The rhododendrons, of which only four species are European, have their headquarters in China, numbering 130 species, varying in size from miniature shrubs 6 in. high to tall trees.Lysimachia, Primula, Clematis, RubusandGentianahave each a hundred species, extraordinary variable in habit, in size and in colour of the flowers. The ferns are equally polymorphic, numbering 400 species, and including strange genera likeArchangiopterisandCheiropteris, unknown elsewhere. About 40 species of bamboos have been distinguished; the one with a square stem from Fu-kien is the most curious.
With a great wealth of beautiful flowering shrubs and herbaceous plants, the Chinese at an early period became skilled horticulturists. The emperor Wu Ti established in 111B.C.a botanic garden at Ch‘ang-an, into which rare plants were introduced from the west and south. Many garden varieties originated in China. The chrysanthemum, perhaps the most variable of cultivated flowers, is derived from two wild species (small and inconspicuous plants), and is mentioned in the ancient Chinese classics. We owe to the skill of the Chinese many kinds of roses, lilies, camellias and peonies; and have introduced from China some of the most ornamental plants in our gardens, asWistaria, Diervilla, Kerria, Incarvillea, Deutzia, Primula sinensis, Hemerocallis, &c. The peach and several oranges are natives of China. The varnish tree (Rhus vernicifera), from which lacquer is obtained; the tallow tree (Sapium sebiferum); the white mulberry, on which silkworms are fed; and the tea plant were all first utilized by the Chinese. The Chinese have also numerous medicinal plants, of which ginseng and rhubarb are best known. Nearly all our vegetables and cereals have their counterpart in China, where there are numerous varieties not yet introduced into Europe, though some, like the Soy bean, are now attracting great attention.
(A. He.*)
Authorities.—L. Richard (S.J.),Géographie de l’empire de Chine(Shanghai, 1905)—the first systematic account of China as a whole in modern times. The work, enlarged, revised and translated into English by M. Kennelly (S.J.), was reissued in 1908 as Richard’sComprehensive Geography of the Chinese Empire and Dependencies. This is the standard authority for the country and gives for each section bibliographical notes. It has been used in the revision of the present article. Valuable information on northern, central and western China is furnished by Col. C.C. Manifold and Col. A.W.S. Wingate in theGeog. Journ.vol. xxiii. (1904) and vol. xxix. (1907). Consult also Marshall Broomhall (ed.),The Chinese Empire: a General and Missionary Survey(London, 1907); B. Willis, E. Blackwelder and others,Research in China, vol. i. part i. “Descriptive Topography and Geology,” part ii. “Petrography and Zoology,” and Atlas (Washington, Carnegie Institution, 1906-1907); Forbes and Hemsley, “Enumeration of Chinese Plants,” inJourn. Linnean Soc. (Bot.), vols. xxiii. and xxxvi.; Bretschneider,History of European Botanical Discoveries in China; E. Tiessen,China das Reich der achtzehn Provinzen, Teil i. “Die allgemeine Geographie des Landes” (Berlin, 1902); andThe China Sea Directory(published by the British Admiralty), a valuable guide to the coasts: vol. ii. (5th ed., 1906) deals with Hong-Kong and places south thereof, vol. iii. (4th ed., 1906, supp. 1907) with the rest of the Chinese coast; vol. i. (5th ed., 1906) treats of the islands and straits in the S.W. approach to the China Sea. Much of China has not been surveyed, but considerable progress has been made since 1900.The Atlas of the Chinese Empire(London, 1908), a good general atlas, which, however, has no hill shading, gives maps of each province on the scale of 1:3,000,000. The preface contains a list of the best regional maps.
The Journal af the China Branch of the Royal Asiatic Societycontains papers on all subjects relating to China.
II. The People
China is noted for the density of its population, but no accurate statistics are forthcoming. The province of Shan-tung is reputedto have a population of 680 per sq. m. The provinces of central China, in the basin of the Yangtsze-kiang—namely Sze-ch‘uen, Hu-peh, Ngan-hui, Kiang-su and Cheh-kiang—containPopulation.probably a third of thes total population, the density of the people in these provinces being represented as from 490 to 310 per sq. m. Ho-nan, which belongs partly to the basin of the Hwang-ho and partly to that of the Yangtsze-kiang, as well as the S.E. coast provinces of Fu-kien and Kwang-tung, are also densely peopled, Ho-nan being credited with 520 persons per sq. m., Fu-kien with 490 and Kwang-tung with about 320.