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Page 2749, results 68701 - 68725

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Publication Extents

Not all publications have extents, not all extents are completely accurate
Instructions for measuring the rate of evaporation from water surfaces
Water Resources Division, U.S. Geological Survey
1898, Division of Hydrography Circular 4
The ·rate of evaporation from water surfaces varies with the temperature of the water, the velocity of the wind at the water surface, and the dryness of the air. Consequently, the rate of evaporation from rivers, lakes, canals, or reservoirs varies widely in different localities and for the same locality...
Eighteenth annual report of the United States Geological Survey to the Secretary of the Interior, 1896-1897: Part IV - Hydrography
Arthur Powell Davis, Frank Leverett, N. H. Darton, J.D. Schuyler
1897, Annual Report 18-4
The completion of this volume marks the revival of extended systematic investigation of the hydrography of the United State. This book is, in effect, the ninth annual report of what has been known as the Irrigation Survey. Its preparation and publication has been made possible by the act of June...
Seepage water of northern Utah
Samuel Fortier
1897, Water Supply Paper 7
The term “seepage water” is used by the irrigators of the West to designate the water which reaches the lowest grounds or the stream channels, swelling the latter by imperceptible degrees and keeping up the flow long after the rains have ceased and the snow has melted. The word “seepage”...
Natural mineral water of the United States: Section in Fourteenth Annual Report of the United States Geological Survey to the Secretary of the Interior, 1892-1893: Part 2 - Accompanying papers
A.C. Peale
1894, Annual Report 14
Aside from the geological interest attached to the subject of mineral waters the facts that within the limits of the United States there are between 8,000 and 10,000 mineral springs, and that the waters from nearly 300 are annually placed upon the market to the extent of over 21,000,000 gallons,...