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ft. above the neighbouring plain the coal-seams crop out in all directions. Mining is thus carried on by adits driven into the face of the formation, rendering the mining of the coal extremely easy. The coalfield is divided into two by a mountain range of ancient granitic formation running north-east and south-west, termed the Ho-shan. It is of anterior date to the limestone and coal formations, and has not affected the uniformity of the stratification, but it has this peculiarity, that the coal on the east side is anthracite, and that on the west side is bituminous. A concession to work coal and iron in certain specified districts in this area was granted to a British company, the Peking Syndicate, together with the right to connect the mines by railway with water navigation. The syndicate built a railway in Shan-si from P'ingyang to Tsi-chow-fu, the centre of a vast coalfield, and connected with the main Peking-Hankow line; lines to serve coal mines have also been built in Hu-nan and other provinces. The earliest in date was that to the K'aip'ing collieries in the east of the province of Chih-li, the railway connecting the mines with the seaport of Taku. The coal at K'aip'ing is a soft bituminous coal with a large proportion of dust. The output is about 1,500,000 tons per annum. A mine has also been opened in the province of Hu-peh, about 60 m. below Hankow, and near the Yangtsze, in connexion with iron-works. Iron. Iron ore of various qualities is found almost as widely diffused as coal. The districts where it is most worked at present lie within the coalfield of Shan-si, viz. at Tsi-chow-fu and P'ing-ting-chow. The ore is a mixture of clay iron ore and spathic ore, together with limonite and hematite. It is found abundantly in irregular deposits in the Coal Measures, and is easily smelted by the natives in crucibles laid in open furnaces. This region supplies nearly the whole of north China with the iron required for agricultural and domestic use. The out-turn must be very considerable, but no data are available for forming an accurate estimate. The province of Sze-ch'uen also yields an abundance of iron ores of various kinds. They are worked by the natives in numerous places, but always on a small scale and for local consumption only. The ores occur in the Coal Measures, predominant among them being a clay iron ore. Hu-nan, Fu-kien, Che
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