Louis C. Conant
1964, Bulletin 1160-F
Search Results
184899 results.
Alternate formats: RIS file of the first 3000 search results | Download all results as CSV | TSV | Excel | RSS feed based on this search | JSON version of this page of results
Page 6679, results 166951 - 166975
Publication Extents
Not all publications have extents, not all extents are completely accurateRobert Vittum Cushman, D. Tanski, M. P. Thomas
1964, Water Supply Paper 1499-H
The Hartford-New Britain area includes the metropolitan areas of Hartford and New Britain and parts of several adjoining towns. Water used in the area is withdrawn from the principal streams and aquifers at an average rate of 463.5 mgd (million gallons per day). Sufficient water is available from these sources...
Peter Zubovic, Taisia Maximovna Stadnichenko, Nola B. Sheffey
1964, Bulletin 1117-B
R.C. Gilstrap, R.C. Christensen
1964, Open-File Report 64-60
On July 16, 1963, the city of Hot Springs had severe flooding, which, from all reports, was exceeded only by a flood that occurred in May 1923. The storm, which caused the flooding, was centered in the vicinity of Hot Springs and covered an area including most of Garland County...
Charles Sherwood Robinson, W. J. Mapel, M.H. Bergendahl
1964, Professional Paper 404
William Stewart Eisenlohr
1964, Water Supply Paper 1779-L
James H. Criner, P-C. P. Sun, Dale J. Nyman
1964, Water Supply Paper 1779-O
The Memphis area as described in .this report comprises about 1,300 square miles of the Mississippi embayment part of the Gulf Coastal Plain. The area is underlain by as much as 3,000 feet of sediments ranging in age from Cretaceous through Quaternary. In 1960, 150 mgd (million gallons per day)...
Mark W. Busby
1964, Water Supply Paper 1669-S
J.G. Cronin, B. N. Myers
1964, Water Supply Paper 1693
The Southern High Plains of Texas occupies an area of about 22,000 square miles in northwest Texas, extending from the Canadian River southward. about 250 miles and from the New Mexico line eastward an average distance of about 120 miles. The economy of the area is dependent largely upon irrigated...
Wallace De Witt Jr., G. W. Colton
1964, Bulletin 1173
R. C. Baker, Leon S. Hughes, I. D. Yost
1964, Water Supply Paper 1669-CC
The average daily load of the Brazos River at Possum Kingdom Reservoir is about 2,800 tons of dissolved solids, of which 1,000 tons is chloride. More than 85 percent of the chloride load is contributed by the Salt Fork Brazos River, and more than 50 percent of the chloride load...
John Augustus Baker
1964, Water Supply Paper 1669-Y
Ivan Barnes
1964, Water Supply Paper 1535-H
The behavior of electrometric pH equipment under field conditions departs from the behavior predicted from Nernst's law. The response is a linear function of pH, and hence measured pH values may be corrected to true pH if the instrument is calibrated with two reference solutions for each measurement. Alkalinity titrations...
John Augustus Baker, H.G. Healy, O. M. Hackett
1964, Water Supply Paper 1694
The Wilmington-Reading area, as defined for this report, contains the headwaters of the Ipswich River in northeastern Massachusetts. Since World War II the growth of communities in this area and the change in character of some of them from rural to suburban have created new water problems and intensified old...
Alvin J. Feulner
1964, Water Supply Paper 1809-E
Robert Vittum Cushman
1964, Water Supply Paper 1752
The term 'north-central Connecticut' in this report refers to an area of about 640 square miles within the central lowland of the Connecticut River basin north of Middletown. The area is mostly a broad valley floor underlain by unconsolidated deposits of Pleistocene and Recent age which mantle an erosional surface...
Mackenzie Gordon Jr.
1964, Professional Paper 483-A
Charles L. McGuinness
1964, Circular 492
No abstract available....
Leo T. McCarthy Jr., Walter B. Keighton
1964, Water Supply Paper 1779-X
Water in the Delaware River at Trenton, NJ, is a mixture of several types--water from the mountainous headwater region, water from the coal-mining regions, and water from the limestone valleys. The quantities of these types of water, in relation to the total quantity of water at Trenton, vary with changes...
G.M. Hogenson
1964, Water Supply Paper 1620
R.A. Sheppard
1964, Miscellaneous Field Studies Map 280
Grover Cleveland Goddard
1964, Water Supply Paper 1761
Robert Schneider
1964, Water Supply Paper 1608-F
The Cenomanian-Turonian formations constitute a highly permeable dolomite and limestone aquifer in central Israel. The aquifer is on the west limb of an anticlinorium that trends north-northeast. In places it may be as much as 800 meters thick, but in the report area, largely the foothills of the Judean-Ephraim Mountains...
Roy Edwin Oltman, H. O’R. Sternberg, F.C. Ames, L.C. Davis
1964, Circular 486
The first measurements of the flow of the Amazon River were made in July 1963 as a joint project of the University of Brazil, the Brazilian Navy, and the U.S. Geological Survey. The discharge of the Amazon River at Obidos was 7,640,000 cfs at an annual flood stage somewhat lower...
John R. Williams
1964, Open-File Report 64-163