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Publication Extents

Not all publications have extents, not all extents are completely accurate
Hydrologic effects of area B flood control plan on urbanization of Dade County, Florida
F. A. Kohout, J.H. Hartwell
1967, Florida Geological Survey Report of Investigations 47
Swampy low land (Area B) that fringes the Everglades west of Metropolitan Miami, Florida (Area A) probably will be urbanized in the future. Area B will be protected from flooding by huge pumps that will pump water westward from Area B over a levee system into Conservation Area 3B. The...
Hydrogeologic data for the Shetucket River basin, Connecticut
Chester E. Thomas Jr., Gene A. Bednar, Mendall P. Thomas, William E. Wilson
1967, Connecticut Water Resources Bulletin 12
This report presents hydrologic and geologic data collected by the U.S. Geological Survey during an investigation of water resources in the Shetucket River basin of Connecticut in cooperation with the Connecticut Water Resources Commission. The Shetucket River basin occupies about 507 square miles in the eastern part of the State,...
Hydrologic effects of the earthquake of March 27, 1964, outside Alaska, with sections on Hydroseismograms from the Nunn-Bush Shoe Co. well, Wisconsin, and Alaska earthquake effects on ground water in Iowa: Chapter C in The Alaska earthquakes, March 27, 1964: effects on hydrologic regimen
Robert C. Vorhis, Elmer E. Rexin, R. W. Coble
1967, Professional Paper 544-C
The Alaska earthquake of March 27, 1964, had widespread hydrologic effects throughout practically all of the United States. More than 1,450 water-level recorders, scattered throughout all the 50 States except Connecticut, Delaware, and Rhode Island, registered the earthquake. Half of the water-level records were obtained from ground-water observation wells and...
Effects of the March 1964 Alaska earthquake on glaciers
Austin Post
1967, Professional Paper 544-D
The 1964 Alaska earthquake occurred in a region where there are many hundreds of glaciers, large and small. Aerial photographic investigations indicate that no snow and ice avalanches of large size occurred on glaciers despite the violent shaking. Rockslide avalanches extended onto the glaciers in many localities, seven very large...
Preliminary report on the geology, geophysics and hydrology of USBM/AEC Colorado core hole No. 2, Piceance Creek Basin, Rio Blanco County, Colorado
J. R. Ege, R. D. Carroll, F.A. Welder
1967, Open-File Report 67-87
Approximately 1,400 feet of continuous core was taken .between 800-2,214 feet in depth from USBM/AEC Colorado core hole No. 2. The drill, site is located in the Piceance Creek basin, Rio Blanco County, Colorado. From ground surface the drill hole penetrated 1,120 feet of the Evacuation Creek Member and 1,094...
Water resources of the Roseau River Watershed, Northwestern Minnesota
Thomas C. Winter, R.W. Maclay, G.M. Pike
1967, Hydrologic Atlas 241
The drainage area of the Roseau River consists of 2,060 square miles above its confluence with the Red River of the North. About 1,150 square miles lie in the United States and 910 square miles in Canada. This report deals only with that portion within the United States, except for...
Water resources of the Two Rivers Watershed, Northwestern Minnesota
R.W. Maclay, Thomas C. Winter, G.M. Pike
1967, Hydrologic Atlas 237
The Two Rivers watershed includes two physiographic areas a lake plain and a till plain – within its 1,232 square miles. It lies in parts of Kittson and Roseau counties and includes the drainage basins of the Two Rivers and Joe River. The flat lake plain which extends 15 to 20...