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For the last nine years the United States Geological Survey has made a special study of the run-off of mountain streams, particularly in Colorado and Wyoming. The gradual installation of water-stage recorders on the larger streams has made available sufficient data to permit a study of the characteristics of these streams. During this period 40 or more stations, located in the mountains and above practically all diversions, have been maintained for periods ranging from two to eight years or more, and the records thus obtained, together with studies of the topography of the drainage basins, form the basis of this report.

Some characteristics of run-off in the Rocky Mountain region