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Instructions for measuring the rate of evaporation from water surfaces
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 in different seasons.
Authors
Map of Alaska showing known gold-bearing rocks with descriptive text containing sketches of the geography, geology, and gold deposits and routes to the gold fields.
No abstract available.
Authors
Samuel Franklin Emmons
New tests of certain pumps and water lifts used in irrigation
No abstract available.
Authors
Ozni Porter Hood
Nineteenth annual report of the United States Geological Survey to the Secretary of the Interior 1897 - 1898: Part I. Director's report, including triangulation and spirit leveling
No abstract available.
Authors
Charles D. Walcott
Nineteenth Annual Report of the United States Geological Survey to the Secretary of the Interior 1897 - 1898: Part VI - Mineral Resources of the United States, 1897, Metallic Products, Coal and Coke
No abstract available.
Authors
Charles D. Walcott
Nineteenth Annual Report of the United States Geological Survey to the Secretary of the Interior 1897 - 1898: Part VI (cont.) - Mineral resources of the United States, 1897, nonmetallic products, except coal and coke
No abstract available.
Authors
Charles D. Walcott, F.H. Oliphant, Edward Wheeler Parker, William C. Day, A.C. Peale, George F. Becker