The only considerable lake connected with the Yellow River is the Hungtsih in Kiangsu, situated near the junction of that river and the Grand Canal, into which it discharges the drainings of the Hwai River; it is more remarkable for the fleets of boats upon it than for scenery in the vicinity. The larger part of the country between the mouths of the two rivers is so marshy and full of lakes, as to suggest the idea that the whole was once an enormous estuary where their waters joined, or else that their deposits have filled up a huge lake which once occupied this tract, leaving only a number of lesser sheets. Besides these, there are small lakes in Chihlí and Shantung; also the Tien, the Sien, and the Tali, of moderate extent, in Yunnan; all of them support an aquatic population upon the fish taken from their waters.
The largest lake in Manchuria is the Hinkai-nor in Kirin, near the source of the Usuri; the two lakes Hurun and Puyur, or Pir, in the basin of the Nonni River, give their name to Hurun-pir, the western district of Tsitsihar; but of the extent and productions of these sheets of water little is known.
The regions lying north and south of Gobi contain many salt lakes, none of them individually comparing with the Aral Sea, but collectively covering a much larger extent, and most of them receiving the waters of the streams which drain their own isolated basins. The peculiarities of these little known parts, especially the depression on each side of the Tien shan, are such as to render them among the most interesting fields for geographical and geological research in the world. The largest one in Turkestan is Lob-nor, stated to be a great marsh overgrown with tall reeds and having a length of 75 miles and width of 15 miles.[13] Bostang-nor, said to connect with this lake, is placed on Chinese maps some 30 miles north of it. North of the Tien shan the lakes are larger and more numerous; the Dzaisang, Kisil-bash and Issik-kul are the most important. All these lakes are salt.
The whole region of Koko-nor is a country of lakes. The Oling and Dzaring are among the sources of the Yellow River; and the Tsing hai, or Azure Sea, better known as Koko-nor, gives its name to the province. The Tengkiri-nor in Tibet lies to the north of H’lassa, and is the largest sheet of water within the frontiers of the empire. In its neighborhood are numerous small lakes extending northward into Koko-nor. The Palti or Yamorouk is shaped like a ring, an island in its centre occupying nearly the whole surface. Ulterior Tibet possesses many lakes on both sides of the Gang-dis-ri range; the Yik and Paha, near Gobi, are the largest, being only two of a long row of them south of the Kwănlun range.
BOUNDARIES OF THE PROVINCES.
The Eighteen Provinces are bounded on the north-east by the colony of Shingking, from which they are separated by the line of a former palisade marking the boundary from the town of Shan-hai kwan to the Hwang ho. Following this stream to its sources in the Ín shan, the boundary then crosses these mountains and pursues a west and south-west course, through the territories of roving Mongol tribes, until it finds the Yellow River at the settlement of Hokiuh in Shensí. West of this the Great Wall divides the provinces of Shensí and Kansuh from the Mongolian deserts as far as the Kiayü Pass, beyond which lies the desert of Gobi, called Peh hai (North Sea) and Hah hai (Black Sea). On the east are the Gulf of Pechele and the Yellow Sea or Hwang hai, also called Tung hai (Eastern Sea) as far south as the Channel of Formosa. This channel and the China Sea lie on the south-east and south, as far as the Gulf of Tongking and the confines of Annam. Kwangsí and Yunnan border on Annam and Siam on their south sides, while Burmah marks the western frontier, but nearly the whole south-west and western frontiers beyond Yunnan and Sz’chuen are possessed by small tribes of uncivilized people, over whom neither the Chinese nor Burmese have much real control. Koko-nor bounds Sz’chuen and Kansuh on their western and south-western sides.
CHARACTER OF THE COAST.
The coast of China, from Hainan to the mouth of the Yangtsz’, is bordered with multitudes of islands and rocky islets; from that point northward to Liautung, the shores are low, and, except in Shantung, the coast is rendered dangerous by shoals.
South of the Pei ho, along to the end of Shantung Promontory, the coast is bolder, increasing in height after passing the Miautau Islands, though neither side of the promontory presents any point of remarkable elevation; Cape Macartney, at the eastern end, is a conspicuous bluff when approaching it from sea. From this cape to the mouth of the Tsientang River, near Chapu, a distance of about 400 miles, the coast is low, especially between the mouths of the Yangtsz’ and Yellow rivers, and has but few good harbors. Quicksands in the regions near these rivers and the Bay of Hangchau render the navigation dangerous to native junks. From Kitto Point, near Ningpo, down to Hongkong, the shores assume a bolder aspect, and numerous small bays and coves occur among the islands, affording safe refuge for vessels. The aspect along this part is uninviting in the extreme, consisting principally of a succession of yellowish cliffs and naked headlands, giving little promise of the highly cultivated country beyond them. This bleak appearance is caused by the rains washing the decomposed soil off the surface; the rock being granite in a state of partial and progressive disintegration, the loose soil is easily carried down into the intervals. Another reason for its treeless surface is owing to the practice of annually cutting the coarse grass for fuel, and after the crop is gathered setting the stubble on fire, in order to manure the ground for the coming year; the fire and thinness of the soil together effectually prevent any large growth of trees or shrubbery upon the hills.