William Peters Brosge, H. N. Reiser
1977, Open-File Report 77-29
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Page 5301, results 132501 - 132525
Publication Extents
Not all publications have extents, not all extents are completely accurateJerry E. Carr, Melvin V. Marcher
1977, Open-File Report 77-278
The Garber-Wellington aquifer, which dips westward at 30 to 40 feet per mile, consists of about 900 feet of interbedded sandstone, shale, and siltstone. Sandstone comprises 35 to 75 percent of the aquifer and averages about 50 percent. Water-table conditions generally exist in the upper 200 feet in the outcrop...
David P. Adam
1977, Open-File Report 77-489
Bernard Dunn, Richard Lumia
1977, Open-File Report 77-484
Henry Nicholas Halberg
1977, Open-File Report 76-791
Gary S. Fuis, Martin E. Friedman, James A. Hileman
1977, Open-File Report 77-181
Reuben James Ross, Charles W. Naeser, Glen Arthur Izett
1977, Open-File Report 77-348
Joseph A. Caggiano
1977, Open-File Report 77-633
Till and stratified drift overlie maturely dissected topography in the Belchertown quadrangle, an area that straddles the New England Upland and Connecticut Valley Lowland in central Massachusetts. Lower Paleozoic, massive quartzo-feldspathic gneiss, quartzite and schist of the Pelham dome and Devonian granodiorite and quartz diorite of the Belchertown intrusive complex...
Stephen J. Stankowski, John Thomas Limerinos, S. Eugene Buell
1977, Open-File Report 77-646
B. E. Law
1977, Open-File Report 77-41
Carleen D. Holloway
1977, Open-File Report 77-169-I
No abstract available....
Charles G. Cunningham, Charles W. Naeser, Richard F. Marvin
1977, Open-File Report 77-573
Eileen M. Pera, E. G. Allen, Gale Alex Lutz
1977, Open-File Report 77-603
No abstract available....
P. D. Snavely, H. D. Gower, J. C. Yount, R.A. Tagg, J.W. Lee, D.L. Lander
1977, Open-File Report 77-195
David S. McCulloch, Rodger H. Chapman
1977, Open-File Report 77-79
No abstract available....
J.H. Sass, J.P. Ziagos, H.A. Wollenberg, R. J. Munroe, D. E. di Somma, A.H. Lachenbruch
1977, Open-File Report 77-762
H.D. Buckner
1977, Open-File Report 77-72
Mountain Creek drains the northeast corner of Johnson County, the northwest corner of Ellis County, the southeast corner of Tarrant County, and part of the southwest corner of Dallas County, Tex. The basin is 30 miles long and averages 10 miles in width. The total drainage area at the mouth...
Eileen M. Pera, E. G. Allen, Nancy L. Curtis
1977, Open-File Report 77-602
No abstract available....
Stuart W. McKenzie
1977, Open-File Report 77-740
The bottom material of the Willamette River, Portland Harbor, was sampled in duplicate on February 1, 1977. Results are reported on the following analyses of the material: immediate and long-term oxygen demand; particle size; percent moisture; residue, loss on ignition; and chemical....
William H. Langer, C. J. Recny
1977, Miscellaneous Field Studies Map 452-F
This map describes the type, thickness, and distribution of unconsolidated materials. It is intended to serve as an aid in planning and evaluation of areas and in identifying areas of potential economic deposits....
Carleen D. Holloway
1977, Open-File Report 77-169-D
No abstract available....
M.B. Scott
1977, Open-File Report 77-398
This report traces by text, maps, and photographs, the development of the water supply in the Santa Ana River basin from its beginning in 1810 or 1811 to 1968. The value of the report lies in the fact that interpretation of the hydrologic systems in the basin requires knowledge of...
J.H. Barks
1977, Water-Resources Investigations Report 77-75
No abstract available. ...
William E. Scott
1977, Open-File Report 77-507
John Skelton
1977, Open-File Report 77-605
Low-flow and peak-flow frequency data and flow-duration-data, based on records from 21 gaging stations in the Joplin area of southwestern Missouri, are presented. Generalized equations and graphs based on gaging-station records are-shown so that estimates of frequency data and the effects of urbanization on peak flows can be made at...