Louis H. Motz
1974, Open-File Report 74-257
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Page 594, results 14826 - 14850
Publication Extents
Not all publications have extents, not all extents are completely accurateH. W. Anderson Jr., D.F. Farrell, W.L. Broussard, P.E. Felsheim
1974, Hydrologic Atlas 522
The 1,462 square miles of land surface in the Cannon River watershed varies considerably from areas of low hills and plains to areas dominated by streams deeply incised into bedrock. Much of the south-central part of the area consists of a till plain that ranges in altitude from 1,100 to...
Chester Zenone, Henry R. Schmoll, Ernest Dobrovolny
1974, Open-File Report 74-57
The Eagle River — Chugiak area is a rapidly growing residential part of the Greater Anchorage Area Borough, south-central Alaska. High-density, urban development in some parts of the area may be restricted because of the nature of the surficial geologic materials and their hydrologic characteristics. This report assembles all information...
H. L. Young, Earl L. Skinner
1974, Hydrologic Atlas 524
This report describes the physical environment, availability, distribution, movement, quality, and use of water in the upper Wisconsin River basin as an aid in planning and water management. The report presents general information on the basin derived from data obtained from Federal, State, and local agencies, New field data were...
Frederick B. Gay, L.G. Toler, Bruce P. Hansen
1974, Hydrologic Atlas 506
T. E. Kelly
1974, Hydrologic Atlas 510
No abstract available....
Robert E. Faye
1974, Water-Resources Investigations Report 73-58
A mathematical model study of the San Juan Valley ground-water basin in San Benito County, Calif., has quantitatively described the ground-water hydrology of the basin under past, present, and future conditions of development. An analysis of conditions in the basin prior to large-scale ground-water development indicates that net recharge equaled...
John B. Weeks, George H. Leavesley, Frank A. Welder, George J. Saulnier Jr.
1974, Open-File Report 74-255
The Piceance and Yellow Creeks drainage area is about 900 square miles (2,330 square kilometres) and is referred to as the Piceance basin, or simply as the basin. The surface-water and ground-water systems in the Piceance basin are intimately related. The annual volume of runoff from the basin (Piceance and...
George R. Dempster Jr.
1974, Water-Resources Investigations Report 73-60
The effects of urbanization on flood characteristics of streams in the Dallas metropolitan area were studied by use of a digital model of the hydrologic system. The model was calibrated by using observed rainfall and runoff data from 19 storms in six basins having various degrees of urbanization. The calibrated...
F. Butler Shaffer, Kenneth J. Braun
1974, Hydrologic Atlas 503
Water Resources Division, U.S. Geological Survey
1974, Hydrologic Unit 16
H.W. Anderson, D.F. Farrell, W.L. Broussard
1974, Hydrologic Atlas 526
The lower Minnesota River watershed, an area of 2,005 square miles, is fairly flat west of the Minnesota River, but rises to a hilly ridge along the east side of the watershed. Most of the area is covered by ground moraine cut deeply by the Minnesota River and less deeply...
R.G. Simpson
1974, Water-Resources Investigations Report 73-55
Gerald F. Lindholm, J. O. Helgesen, W.L. Broussard, D.F. Farrell
1974, Hydrologic Atlas 490
The lower St. Croix River watershed is an elongate area of about 930 square miles bounded on the east by the St. Croix River. The St. Croix River forms the Minnesota-Wisconsin boundary along the eastern side of the watershed. Additional drainage to the St. Croix River includes areas of about 2,500...
Karl G. Johnson
1974, Hydrologic Atlas 532
H.W. Anderson, D.F. Farrell, W.L. Broussard
1974, Hydrologic Atlas 525
The Blue Earth River Watershed in Minnesota includes 3,106 square miles of land surface, which varies from fairly flat to gently rolling. The drainage extends south to include an additional 450 square miles in Iowa. The western, southern, and eastern boundaries are end moraines formed by Pleistocene glaciers. Major streams...
Water Resources Division, U.S. Geological Survey
1974, Hydrologic Unit 44
This map and accompanying table show Hydrologic Units that are basically hydrographic in nature. The Cataloging Units shown will supplant the Cataloging Units previously used by the U.S. Geological Survey in its Catalog of Information on Water Data (1966-72). The previous U.S. Geological Survey Catalog-Indexing System was by map number...
Water Resources Division, U.S. Geological Survey
1974, Hydrologic Unit 17
This map and accompanying table show Hydrologic Units that are basically hydrographic in nature. The Cataloging Units shown will supplant the Cataloging Units previously used by the U.S. Geological Survey in its Catalog of Information on Water Data (1966-72). The previous U.S. Geological Survey Catalog-Indexing System was by map number...
Water Resources Division, U.S. Geological Survey
1974, Hydrologic Unit 19
No abstract available....
Gerald F. Lindholm, D.F. Farrell, John O. Helgesen
1974, Hydrologic Atlas 528
The Crow River watershed, an area of about 2,760 square miles, is covered entirely by glacial deposits. A topographically high, east-west-trending end moraine divides most of the watershed into two drainage areas of approximately equal size. The North Fork Crow River drains a mixture of glacial outwash and till deposits,...
H.M. Jensen, Julian Soren
1974, Hydrologic Atlas 501
Gerald S. Runner
1974, Hydrologic Atlas 547
John R. Williams, Gary D. Tasker
1974, Hydrologic Atlas 504
James R. Marie, L.G. Davis
1974, Hydrologic Atlas 508
Don Price, Thomas E. Eakin
1974, Hydrologic Atlas 487
The Great Basin Region is defined to include the drainage of the Great Basin physiographic section (Fennman, 1931) in Idaho, Nevada, Utah, and Wyoming. In October 1966, the President’s Water Resources Council requested that a comprehensive framework study be made in the Great Basin Region under the leadership of the...