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Page 6643, results 166051 - 166075

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Fluvial sediment of the Mississippi River at St. Louis, Missouri
Paul Robert Jordan
1965, Water Supply Paper 1802
An investigation of the fluvial sediment of the Mississippi River at St. Louis, Mo., was begun in 1948. Most data have been obtained only to determine the daily suspended-sediment discharge and the particle-size distribution of suspended sediment and bed material, but a few data have been obtained to study the...
Specific yield - laboratory experiments showing the effect of time on column drainage
Robert C. Prill, A.I. Johnson, Donald Arthur Morris
1965, Water Supply Paper 1662-B
The increasing use of ground water from many major aquifers in the United States has required a more thorough understanding of gravity drainage, or specific yield. This report describes one phase of specific yield research by the U.S. Geological Survey's Hydrologic Laboratory in cooperation with the California Department of Water...
Summary of floods in the United States during 1961
J.O. Rostvedt
1965, Water Supply Paper 1810
This report describes the most outstanding floods in the United States during 1961. The most damaging floods during the year were those caused by snowmelt in March and April in the upper Mississippi River basin and those accompanying Hurricane Carla in September.Hurricane Carla traveled northward along the east edge of...
Hydrologic conditions near Glendo, Platte County, Wyoming
G. E. Welder, Edwin P. Weeks
1965, Water Supply Paper 1791
The Glendo area of Platte and Carbon Counties, Wyo., about 250 square miles in extent, is in the Great Plains physiographic province. It is bordered on the west by the Laramie Range and on the east by the Hartville uplift. The North Platte River and Horseshoe and Middle Bear Creeks...
Geology and water resources of Portage County, Wisconsin
Charles Lee Roy Holt
1965, Water Supply Paper 1796
Portage County has abundant resources of generally good quality water and, although water problems exist locally, depletion or general scarcity of water is not likely in the foreseeable future. The county receives annually about 31 inches of precipitation, of which about 21 inches is lost as evaportranspiration. The average annual water...