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Publication Extents

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Magnitude and frequency of floods in small drainage basins in Idaho
C.A. Thomas, W. A. Harenberg, J.M. Anderson
1973, Water-Resources Investigations Report 73-7
A method is presented in this report for determining magnitude and frequency of floods on streams with drainage areas between 0.5 and 200 square miles. The method relates basin characteristics, including drainage area, percentage of forest cover, percentage of water area, latitude, and longitude, with peak flow characteristics. Regression equations...
Index of time-of-travel studies of the US Geological Survey
Charles W. Boning
1973, Water-Resources Investigations Report 73-34
This index identifies locations on streams where the U. S. Geological Survey has investigated the time of travel of a highly soluble material moving through a reach of stream channel. This index provides information only on the location of studied stream reaches; it contains no basic data. It does contain,...
United States mineral resources
Donald A. Brobst, Walden P. Pratt, editor(s)
1973, Professional Paper 820
The work on this volume began in January 1972, but in a broader sense its production began many years ago. The chapters were written by geologists most of whom have had many years of experience studying the geology of mineral deposits, and more particularly the commodities about which they have...
Effects of Urbanization on Floods in the Houston, Texas Metropolitan Area
Steven L. Johnson, Douglas M. Sayre
1973, Water-Resources Investigations Report 73-3
Rainfall and runoff data from drainage basins in the Houston metropolitan area and a 60-year rainfall record for the National Weather Service station, Houston-City, were used to simulate 60 annual flood peaks at 26 sites. Selected frequency characteristics, based on these simulated annual peaks, are related to drainage area and...
Water facts and figures for planners and managers
John Henry Frederick Feth
1973, Circular 601-I
Water is defined in terms of its chemical composition and dominant physical properties, such as expansion on freezing and high surface tension. Water on the earth is about 97 percent in the seas, 2 percent in glacier ice, principally Greenland and Antarctica. Man is left with less than 1 percent...