Mexico, an immense cornucopia, hangs upon the Tropic of Cancer and opens toward the north pole. The distance across its mouth is about the same as that between Boston and Omaha, and the line of its western coast would probably reach from New York to Salt Lake City. Nearly twenty states like Ohio could be laid down within its limits, and in 1845 it included also New Mexico, Arizona, Utah, Nevada, California and portions of Colorado and Wyoming. On its eastern side the ground rises almost imperceptibly from the Gulf of Mexico for a distance varying from ten to one hundred miles, and ascends then into hills that soon become lofty ranges, while on the western coast series of cordilleras tower close to the ocean. Between the two mountain systems lies a plateau varying in height from 4000 to 8000 feet, so level—we are told—that one could drive, except where deep gullies make trouble, from the capital of Montezuma to Santa Fe, New Mexico. The country is thus divided into three climatic zones, in one or another of which, it has been said, every plant may be found that grows between the pole and the equator. Except near the United States the coast lands are tropical or semi-tropical; and the products of the soil, which in many quarters is extraordinarily deep and rich, are those which naturally result from extreme humidity and heat. Next comes an intermediate zone varying in general height from about 2000 to about 4000 feet, where the rainfall, though less abundant than on the coast, is ample, and the climate far more salubrious than below. Here, in view of superb mountains and even of perpetual snows, one finds a sort of eternal spring and a certain blending of the tropical and the temperate zones. Wheat and sugar sometimes grow on the same plantation, and both of them luxuriantly; while strawberries and coffee are not far apart.
Mexico, an immense cornucopia, hangs upon the Tropic of Cancer and opens toward the north pole. The distance across its mouth is about the same as that between Boston and Omaha, and the line of its western coast would probably reach from New York to Salt Lake City. Nearly twenty states like Ohio could be laid down within its limits, and in 1845 it included also New Mexico, Arizona, Utah, Nevada, California and portions of Colorado and Wyoming. On its eastern side the ground rises almost imperceptibly from the Gulf of Mexico for a distance varying from ten to one hundred miles, and ascends then into hills that soon become lofty ranges, while on the western coast series of cordilleras tower close to the ocean. Between the two mountain systems lies a plateau varying in height from 4000 to 8000 feet, so level—we are told—that one could drive, except where deep gullies make trouble, from the capital of Montezuma to Santa Fe, New Mexico. The country is thus divided into three climatic zones, in one or another of which, it has been said, every plant may be found that grows between the pole and the equator. Except near the United States the coast lands are tropical or semi-tropical; and the products of the soil, which in many quarters is extraordinarily deep and rich, are those which naturally result from extreme humidity and heat. Next comes an intermediate zone varying in general height from about 2000 to about 4000 feet, where the rainfall, though less abundant than on the coast, is ample, and the climate far more salubrious than below. Here, in view of superb mountains and even of perpetual snows, one finds a sort of eternal spring and a certain blending of the tropical and the temperate zones. Wheat and sugar sometimes grow on the same plantation, and both of them luxuriantly; while strawberries and coffee are not far apart.