Extending Darcy's concept of ground-water motion
H.E. Skibitzke
1964, Professional Paper 411-F
The tensor nature of permeability and its effect in a given ground-water flow regime have been acknowledged by various investigators. The effect on the spread of a given dissolved substance can be qualitatively discussed on the basis of the tensor characteristic of the permeability coefficient. The correlation between the dispersion...
Hydrology and hydrogeology of Navajo Lake, Kane County, Utah
Milton Theurer Wilson, Harold E. Thomas
1964, Professional Paper 417-C
Navajo Lake, whose entire outflow disappears underground, is on the high Markagurit Plateau where the average annual precipitation is more than 30 inches. It nestles among the headwaters of several streams that flow into arid regions where competition for municipal, industrial, and irrigation water sup- plies is very keen. Several...
Geology of the Tell City quadrangle, Kentucky-Indiana
Frank Darwyn Spencer
1964, Geologic Quadrangle 356
Middle Bajocian ammonites from the Cook Inlet region, Alaska
R. W. Imlay
1964, Professional Paper 418-B
Geology of parts of the Rockport and Lewisport quadrangles, Kentucky
Frank Darwyn Spencer
1964, Geologic Quadrangle 315
Phreatophyte research in the Western States, March 1959 to July 1964
Thomas William Robinson
1964, Circular 495
Geology and mineral deposits of the Thomas and Dugway Ranges, Juab and Tooele Counties, Utah
Mortimer Hay Staatz, Wilfred James Carr
1964, Professional Paper 415
Surficial geology of the Niantic quadrangle, Connecticut
Richard Goldsmith
1964, Geologic Quadrangle 329
Geology of the Grand Rivers quadrangle, Kentucky
William Henry Hays
1964, Geologic Quadrangle 328
Geology of the Sulphur Lick quadrangle, Kentucky
Leonard D. Harris
1964, Geologic Quadrangle 323
Crystal chemistry of beryllium
Malcolm Ross
1964, Professional Paper 468
Geology of the Cane Valley quadrangle, Kentucky
Charles Henry Maxwell, W.B. Turner
1964, Geologic Quadrangle 369
Growing importance of urban geology
John T. McGill
1964, Circular 487
Geology of the Summit quadrangle, Kentucky
Frank R. Moore
1964, Geologic Quadrangle 298
Bedrock geologic map of the Big Lake quadrangle, Washington County, Maine
David M. Larrabee
1964, Geologic Quadrangle 358
Channel geometry of Piedmont streams as related to frequency of floods
F. A. Kilpatrick, Harry Hawthorne Barnes Jr.
1964, Professional Paper 422-E
Bedrock geology of the Salem quadrangle and vicinity, Massachusetts
Priestley Toulmin
1964, Bulletin 1163-A
Aeromagnetic map of the Bergland and part of the White Pine quadrangles, Ontonagon and Gogebic Counties, Michigan
James R. Balsley, Joseph L. Vargo
1964, Open-File Report 64-8
No abstract available....
Geology of Lost River mine area, Alaska
C.L. Sainsbury
1964, Bulletin 1129
Geologic map of New England
Richard Goldsmith
1964, Open-File Report 64-62
Preliminary report on the phosphate deposits and stratigraphy of Permian rocks in Dry Bread Hollow, Weber County, Utah
Elmer M. Schell, Willard Calvin Gere
1964, Open-File Report 64-138
Water-table, surface-drainage, and engineering soils map of the Smyrna area, Delaware
Durward H. Boggess, John K. Adams, Christian F. Davis
1964, Hydrologic Atlas 81
Geology of the Andover Granite and surrounding rocks, Massachusetts
Robert O. Castle
1964, Open-File Report 64-33
Field and petrographic studies of the Andover Granite and surrounding rocks have afforded an opportunity for an explanation of its emplacement and crystallization. The investigation has contributed secondarily to an understanding of the geologic history of southeastern New England, particularly as it is revealed in the Lawrence, Wilmington, South Groveland,...
Water resources of the Flint area, Michigan
Sulo Werner Wiitala, K.E. Vanlier, Robert A. Krieger
1964, Water Supply Paper 1499-E
This report describes the water resources of Genesee County, Mich., whose principal city is Flint. The sources of water available to the county are the Flint and Shiawassee Rivers and their tributaries, inland lakes, ground water, and Lake Huron. The withdrawal use of water in the county in 1958 amounted...
Geologic reconnaissance of the Antelope-Ashwood area, north-central Oregon, with emphasis on the John Day Formation of late Oligocene and early Miocene age
Dallas L. Peck
1964, Bulletin 1161-D
This report briefly describes the geology of an area of about 750 square miles in Jefferson, Wasco, Crook, and Wheeler Counties, Oregon. About 16,000 feet of strata that range in age from pre-Tertiary to Quaternary are exposed. These include the following units: pre-Tertiary slate, graywacke, conglomerate, and meta-andesite; Clarno Formation...
