Variations in the chemical character of the Susquehanna River at Harrisburg, Pennsylvania
Peter W. Anderson
1963, Water Supply Paper 1779-B
The chemical quality of the Susquehanna River at Harrisburg is influenced by three major factors: streamflow, anthracite and bituminous coal-mine drainage, and geology. Water samples collected at Harrisburg near the west bank of the Susquehanna River and those of western tributaries that drain limestone terranes are similar in chemical quality....
Geology and promising areas for ground-water development in the Hualapai Indian Reservation, Arizona
F. R. Twenter
1963, Water Supply Paper 1576-A
Occurrence and distribution of strontium in natural water
Marvin W. Skougstad, Horr C. Albert
1963, Water Supply Paper 1496-D
Geology and hydrology of Valle Grande and Valle Toledo, Sandoval County, New Mexico
Clyde Stuart Conover, C.V. Theis, Roy L. Griggs
1963, Water Supply Paper 1619-Y
Compilation of records of surface waters of the United States, October 1950 to September 1960, part 13. Snake River basin
E. L. Hendricks, W. T. Miller, Leon A. Wiard, K. N. Phillips, W. I. Travis, F. M. Veatch, M. T. Wilson
1963, Water Supply Paper 1737
No abstract available....
Water-resources reconnaissance in southeastern part of Honey Lake Valley, Lassen County, California
George Stockbridge Hilton
1963, Water Supply Paper 1619-Z
No abstract available....
Geology and ground-water conditions in southern Nassau and southeastern Queens Counties, Long Island, N.Y.
N. M. Perlmutter, J. J. Geraghty
1963, Water Supply Paper 1613-A
Test drilling, electrical logging, and water sampling of 'outpost' and other wells have revealed the existence of a deep confined body of salt water in the Magothy(?) formation beneath southwestern Nassau and southeastern Queens Counties, Long Island, N.Y. In connection with a test-drilling program, cooperatively sponsored by the U.S. Geological...
Quality of surface waters of the United States, 1959, Parts 5 & 6, Hudson Bay and upper Mississippi River basins and Missouri River basin
S. K. Love
1963, Water Supply Paper 1643
Ground-water geology of Karnes County, Texas
Robert B. Anders
1963, Water Supply Paper 1539-G
The exposed rocks and those underlying Karnes County dip toward the Gulf of Mexico at average rates ranging from 20 to more than 200 feet per mile. The oil fields are on structures associated with faulting; the effect of faulting on the occurrence of ground water has not been determined. The...
Geology and ground-water resources of Hale County, Texas
J.G. Cronin, Lloyd C. Wells
1963, Water Supply Paper 1539-U
Hale County, in the southern High Plains of Texas, has an area of 1,033 square miles. The land surface is one of low relief, and the regional slope is about 10 feet per mile toward the southeast. Surface runoff drains into numerous playa lakes and two intermittent streams: Running Water...
Ground-water resources of the Alma area, Michigan
Kenneth E. Vanlier
1963, Water Supply Paper 1619-E
The Alma area consists of 30 square miles in the northwestern part of Gratiot County, Mich. It is an area of slight relief gently rolling hills and level plains and is an important agricultural center in the State.The Saginaw formation, which forms the bedrock surface in part of the area,...
Water resources of Red River Parish, Louisiana
Roy Newcome, Leland Vernon Page
1963, Water Supply Paper 1614
Red River Parish is on the eastern flank of the Sabine uplift in northwestern Louisiana. The 'area is underlain by lignitic clay and sand of Paleocene and Eocene age which dip to the east at the rate of about 30 feet per mile. The Red River is entrenched in these...
Effects of hydraulic and geologic factors on streamflow of the Yakima River Basin, Washington
Hallard B. Kinnison, Jack E. Sceva
1963, Water Supply Paper 1595
The Yakima River basin, in south-central Washington, is the largest single river system entirely within the confines of the State. Its waters are the most extensively utilized of all the rivers in Washington. The river heads high on the eastern slope of the Cascade Mountains, flows for 180 miles in a...
Geology and ground-water appraisal of the Naval Air Missile Test Center area, Point Mugu, California
R. W. Page
1963, Water Supply Paper 1619-S
Application of electrical and radioactive well logging to ground-water hydrology
Eugene P. Patten Jr., Gordon D. Bennett
1963, Water Supply Paper 1544-D
Ground water in the Prineville area, Crook County, Oregon
J. W. Robinson, Don Price
1963, Water Supply Paper 1619-P
Geology and ground-water resources of Bartow County, Georgia
M.G. Croft
1963, Water Supply Paper 1619-FF
Hydrogeologic reconnaissance of San Nicolas Island, California
W. L. Burnhan, Fred Kunkel, Walter Hofmann, W. C. Peterson
1963, Water Supply Paper 1539-O
No abstract available....
Water in the Dakota and Purgatoire Formations in Otero County and the southern part of Crowley County, Colorado
William G. Weist
1963, Water Supply Paper 1669-P
The hardness of available shallow ground water in Otero County and in the southern part of Crowley County generally exceeds 1,000 parts per million, and the water requires treatment for most uses. To obtain a supply of softer water, wells have been drilled into the Dakota Sandstone and the Cheyenne...
Reconnaissance study of the chemical quality of surface waters in the Sacramento River Basin, California
Robert Brennan
1963, Water Supply Paper 1619-Q
Hydrology of stock-water development on the public domain of western Utah
Charles T. Snyder
1963, Water Supply Paper 1475-N
A geologic and hydrologic reconnaissance was made on the public domain of western Utah to appraise the water resources of the area and to provide a basis for locating and developing sources of stock water. The study area includes the Bonneville, Pahvant, and Virgin Grazing Districts, in parts of Tooele,...
Geochemical aspects of artificial recharge in the Grand Prairie region, Arkansas
Richard T. Sniegocki
1963, Water Supply Paper 1615-E
Sediment characteristics of small streams in southern Wisconsin, 1954-59
Charles R. Collier
1963, Water Supply Paper 1669-B
The results of investigations of the sediment and water discharge characteristics of Black Earth Creek, Mount Vernon Creek, and Yellowstone River from 1954 to 1959 and Dell Creek for 1958 and 1959 indicate large differences in annual runoff and sediment yields. The suspended-sediment discharge of Black Earth Creek averaged 3,260...
Causes of depletion of the Pecos River in New Mexico
Harold E. Thomas
1963, Water Supply Paper 1619-G
Chemical equilibria and rates of manganese oxidation
John David Hem
1963, Water Supply Paper 1667-A
