In his report, published by order of Parliament, Mr. Dawson says that while gold is so generally distributed over the province that scarcely a stream of any importance fails to show at least "colors" of the metal, the principal discoveries clearly indicate that the most important mining districts are in the systems of mountains and high plateaus lying to the south-west of the Rocky Mountains and parallel in direction with them. This mountain system next to and south-west of the Rockies is called, for convenience, the Gold Range, but it comprises a complex belt "of several more or less distinct and partly overlapping ranges"--the Purcell, Selkirk, and Columbia ranges in the south, and in the north the Cariboo, Omenica, and Cassiar ranges. "This series or system constitutes the most important metalliferous belt of the province. The richest gold fields are closely related to it, and discoveries of metalliferous lodes are reported in abundance from all parts of it which have been explored. The deposits already made known are very varied in character, including highly argentiferous galenas and other silver ores and auriferous quartz veins." This same authority asserts that the Gold Range is continued by the Cabinet, Coeur d'Alene, and Bitter Root mountains in our country. While there is no single well-developed gold field as in California, the extent of territory of a character to occasion a hopeful search for gold is greater in the province than in California. The average man of business to whom visitors speak of the mining prospects of the province is apt to declare that all that has been lacking is the discovery of one grand mine and the enlistment of capital (from the United States, they generally say) to work it. Mr. Dawson speaks to the same point, and incidentally accounts for the retarded development in his statement that one noteworthy difference between practically the entire area of the province and that of the Pacific States has been occasioned by the spread and movement of ice over the province during the glacial period. This produced changes in the distribution of surface materials and directions of drainage, concealed beneath "drifts" the indications to which prospectors farther south are used to trust, and by other means obscured the outcrops of veins which would otherwise be well marked. The dense woods, the broken navigation of the rivers, in detached reaches, the distance from the coast of the richest districts, and the cost of labor supplies and machinery--all these are additional and weighty reasons for the slowness of development. But this was true of the past and is not of the present, at least so far as southern British Columbia is concerned. Railroads are reaching up into it from our country and down from the transcontinental Canadian Railway, and capital, both Canadian and American, is rapidly swelling an already heavy investment in many new and promising mines. Here it is silver-mining that is achieving importance.