AGRICULTURAL AND MINERAL PRODUCTIONS. 159 Other coal-fields occur in Illinois and Missouri, in Texas, Michigan, Rhode Island, and New Brunswick and Nova Scotia. The area of the coal-fields of Western Europe is estimated by Dana at about 20,000 square miles, while the total area of those of the United States probably exceeds 125,000 square miles. In the United States, Pennsylvania possesses the most extensive and the richest deposits, the total area of the deposits in this State being nearly 20,000 square miles, or equal to those of Western Europe. The richness of the American coal-fields cannot fail to exert an import- ant influence on the future development of the country. 418. Peat-Bogs of Massachusetts——Peat con- sists of a black, carbonaceous deposit which ac- cumulates in badly-drained regions of humid climates. The surfaces of the peat-marshes are often covered with a thin crust, formed. by the interlacing roots of vegetable growths. Below this crust is a treacherous, oozy quagmire. When peat is dried it is suitable for fuel. Dana estimates that Massachusetts contains fifteen ‘billion cubic feet of peat. Large deposits occur in _ the Great Dismal Swamp, in North Carolina and Virginia. 419. Petroleum, or Coal Oil, is found in various Fig, 138, Oil Well and Tank. sections. ‘The most valuable deposits occur in a region embracing Western Pennsylvania, Vir- ginia, Ohio, and Michigan. Petroleum is found also in the West. The oil is obtained by boring. The wells so produced are similar to artesian wells, except in the material discharged. In many instances the oil issues in powerful streams, which continue to flow for considerable periods. The crude oil is generally stored in huge tanks, from which it is transferred to barrels or iron tanks for trans- portation. Much is also distributed for great dis- tances through lines of pipes called pipe-lines. For most commercial uses it is necessary to re- fine or purify the oil. 420. Natural Gas.——Accumulations of natural or rock-gas occur in nearly all portions of the United States, but such deposits are especially rich in the regions where coal oil is found. Western Pennsylvania, and the adjoining States, yield great quantities of such gas. ‘The gas is obtained by borings similar to those made for artesian wells or coal-oil wells. From the gas wells thus formed the gas issues forth with great velocity. When lighted it burns with a flame similar to that of ordinary illuminating gas. Like ordinary gas it burns with a pale bluish flame when mixed with air, and affords an excellent source of artificial heat. - Natural gas has been known for many years past, but it is only recently that its great extent and quantity have been ascertained. In many districts—notably in the city of Pittsburgh and vicinity—natural gas has practically superseded illuminating gas as a source of light, and has almost entirely replaced ordinary coal as a source of heat. The value of such a natural product in any manufacturing centre can scarcely be overestimated, and its successful in- troduction in any locality has in. all cases been attended with a marked growth in the extent and variety of its manufactures. Although such deposits must in perhaps a comparatively short time become exhausted, as yet they show but little signs of failure. The gas escapes from the well under great pressure. Before its delivery to consumers, through pipes like ordi- nary gas-pipes, the pressure is reduced by suitable contri- vances; so that its consumption is not attended with any greater risk than that attending ordinary illuminating gas. 421. Salt——Beds of rock-salt occur in Louisi- ana, Virginia, and in various parts of the West. Large quantities are obtained by evaporating the waters of saline or brine springs. These are of common occurrence. The most valuable are found in New York, in the neighborhood of Salina and Syracuse; in Virginia, Michigan, Ken- tucky, and in the Far West. 422. Building Stones.—Large deposits of valu- able building stones are found in all parts of the country. Among the most common are various kinds of sandstone, marble, granite, slate, mag- nesian limestone, serpentine, gneiss, and mica