Reed W. Mower, J. W. Hood, R.L. Cushman, R.L. Borton, S.E. Galloway
1964, Water Supply Paper 1659
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Publication Extents
Not all publications have extents, not all extents are completely accurateG. R. Boynton, Francis P. Gilbert
1964, Open-File Report 64-20
No abstract available....
Edward A. Sammel, Richard A. Brackley, Wilbur Nathaniel Palmquist
1964, Hydrologic Atlas 196
E. J. McKay, William P. Williams
1964, Open-File Report 64-111
Edward G. Sable
1964, Geologic Quadrangle 302
Gordon H. VanSickle, William H. Dennen, Edwin Van Horn Post
1964, Open-File Report 64-156
Roland George Henderson, Alphonso Wilson
1964, Open-File Report 64-76
Christian F. Davis, Durward H. Boggess
1964, Hydrologic Atlas 136
Peter Popenoe, G. R. Boynton, G. L. Zandle
1964, Geophysical Investigations Map 450
No abstract available....
O. M. Hackett
1964, Water Supply Paper 1781
H. T. Morris
1964, Bulletin 1142-L
J. H. Johnson
1964, Professional Paper 403-G
No abstract available....
D. R. Mabey
1964, Geophysical Investigations Map 415
No abstract available....
J. A. MacKallor
1964, Geophysical Investigations Map 462
S. K. Love
1964, Water Supply Paper 1942
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...
Hilton H. Cooper
1964, Water Supply Paper 1613-C
Investigations in the coastal part of the Biscayne aquifer, a highly productive aquifer of limestone and sand in the Miami area, Florida, show that the salt-water front is dynamically stable as much as 8 miles seaward of the position computed according to the Ghyben-Herzberg principle. This discrepancy results, at least...
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)...
William Stewart Eisenlohr
1964, Water Supply Paper 1779-L
Wallace De Witt Jr., G. W. Colton
1964, Bulletin 1173
Norman F. Sohl, Erle G. Kauffman
1964, Professional Paper 483-H
Two unusually massive ostreid species, representing the largest and youngest Mesozoic members of their respective lineages, occur in Upper Cretaceous sediment of the gulf coast and Caribbean areas. Their characteristics and significance, as well as the morphologic terminology of ostreids in general, are discussed. Crassostrea cusseta Sohl and Kauffman n. sp....
F. S. MacNeil
1964, Professional Paper 399-B
J. L. Meuschke, J. L. Vargo
1964, Geophysical Investigations Map 487
R. G. Yates
1964, IMAP 412