C.L. Sainsbury, Reuben Kachadoorain, T. E. Smith, W. C. Todd
1968, Circular 565
No abstract available....
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Page 5833, results 145801 - 145825
Publication Extents
Not all publications have extents, not all extents are completely accurateG.H. Wood Jr., J. P. Trexler, Andy Yelenosky
1968, Geologic Quadrangle 690
Robert L. Christiansen, Donald C. Noble
1968, Geologic Quadrangle 774
John H. Stewart, Edwin H. McKee
1968, Open-File Report 68-260
George William Holmes
1968, Open-File Report 68-136
No abstract available....
F. A. Petrafeso, C. L. Long
1968, Open-File Report 68-289
No abstract available....
E.P. Smith, B.D. Marcellus
1968, Open-File Report 68-295
No abstract available....
William W. Barnwell, Charles W. Boning
1968, Hydrologic Atlas 259
No abstract available....
William C. Overstreet, A. M. White, J. W. Whitlow, P. K. Theobald Jr., D. W. Caldwell, N. P. Cuppels, Jerome Stone
1968, Professional Paper 568
No abstract available....
William R. Hemphill
1968, Open-File Report 68-126
Carbonate rocks and evaporite deposits commonly exhibit relatively high reflectance in the ultraviolet (<3600A), and some outcrops of these materials are selectively shown on ultraviolet imagery. Other materials which are commonly strongly imaged on ultraviolet imagery and photography include water, snow, concrete, and metallic objects, particularly aluminum.Outdoor tests of an...
B.D. Marcellus, F.A. Petrafeso
1968, Open-File Report 68-284
No abstract available....
Water Resources Division, U.S. Geological Survey
1968, Open-File Report 68-292
No abstract available....
James Warren Hood
1968, Open-File Report 68-138
Irby J. Hickenlooper
1968, Hydrologic Atlas 289
Irby J. Hickenlooper
1968, Hydrologic Atlas 288
No abstract available....
G.A. Miller, J. R. Rapp
1968, Open-File Report 68-182
Dagfin John Cederstrom
1968, Open-File Report 69-37
Water Resources Division, U.S. Geological Survey
1968, Bulletin 1233
Edwin Allen Bell, Dale J. Nyman
1968, Water Supply Paper 1853
The '500-foot' sand is the major source of water supply for the Memphis area. Thick layers of impervious clay above and below the sand confine the water in the aquifer under artesian pressure and also protect the aquifer from contamination. Recharge from rainfall enters the '500-foot' sand in the outcrop,...
Warren Irvin Finch
1968, Geologic Quadrangle 763
M. R. Brock, Q. D. Singewald
1968, Geologic Quadrangle 596
C. C. Hawley, A. L. Clark
1968, Circular 564
Carl Koteff, Robert N. Oldale, Joseph H. Hartshorn
1968, Geologic Quadrangle 787
William N. Sharp, James Louis Gualtieri
1968, Circular 557
W. W. Patton Jr., T. P. Miller, I.L. Tailleur
1968, IMAP 554