K. S. Muir
1964, Water Supply Paper 1664
Search Results
68807 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 2559, results 63951 - 63975
Publication Extents
Not all publications have extents, not all extents are completely accurateD.D. Harris, E.V. Richardson
1964, Water Supply Paper 1369-E
W. O. Smith, A.N. Sayre
1964, Professional Paper 402-E
Kenneth Lyle Walters
1964, Water Supply Paper 1779-A
G. H. Davis, B. E. Lofgren, Seymour Mack
1964, Water Supply Paper 1618
The San Joaquin Valley includes roughly the southern two-thirds of the Central Valley of California, extending 250 miles from Stockton on the north to Grapevine at the foot of the Tehachapi Mountains. The valley floor ranges in width from 25 miles near Bakersfield to about 55 miles near Visalia; it...
Ward Sundt Motts, Robert L. Cushman
1964, Water Supply Paper 1785
Edwin P. Weeks
1964, Water Supply Paper 1783
Lloyd A. Hershey, Paul A. Schneider
1964, Water Supply Paper 1669-X
Christian F. Davis, Durward H. Boggess
1964, Hydrologic Atlas 132
E. L. Hendricks
1964, Water Supply Paper 1750-A
R.H. Meade
1964, Professional Paper 497-B
E. L. Hendricks
1964, Water Supply Paper 1728
No abstract available....
John K. Adams, Durward H. Boggess
1964, Hydrologic Atlas 101
Water Resources Division, U.S. Geological Survey
1964, Professional Paper 501-D
This collection of 43 short papers is the last of the chapters of Geological Survey Research 1964. The papers report on scientific and economic results of current work by members of the Geologic, Conservation, Water Resources, and Topographic Divisions of the U.S. Geological Survey. Some of the papers present results...
A. Murray Fallis, Daniel O. Trainer Jr.
1964, Book chapter, Waterfowl tomorrow
No abstract available....
Water Resources Division, U.S. Geological Survey
1964, Report
The surface-water records for the 1964 water year for gaging stations, partial-record stations, and miscellaneous sites within the State of Indiana are given in this report. For convenience there are also included records for a few pertinent gaging stations in bordering States. The records were collected and computed by the...
J. H. Feth
1964, Ground Water (2) 14-17
“Hidden recharge” is defined as subsurface percolation of water from basin‐margin mountains directly into aquifers of the valley basins. It is an important, and sometimes neglected, item in hydrologic equations. Locally, geologic conditions permit inter‐basin circulation of ground water. The concept that ground‐water basins necessarily terminate at the contact between...
Edward Bradley
1964, International Association of Scientific Hydrology - Bulletin (9) 12-23
The biblical Jordan River Valley, which extends from Lake Tiberias (the Sea of Galilee) to the Dead Sea, is decidedly similar to the Jordan River Valley of Utah, which joins Lake Utah and Great Salt Lake. Both Jordan Rivers drain relatively large fresh-water lakes and also are major sources of discharge into large salty lakes that have no outlets to the ocean.The...
Donald E. White
1964, Bulletin Volcanologique (27) 369-370
A well drilled for geothermal power near Salton Sea in Imperial Valley, Calif., is 5,232 feet deep; it is the deepest well in the world (1962) in a high-temperature hot spring area. In the lower half of the hole temperatures are too high to measure with available equipment, but are...
George Plafker
1964, GSA Bulletin (75) 503-522
Strongly oriented lineaments, defined by lake shores and stream and vegetation alignments, are distributed throughout more than 45,000 square miles of the Beni basin in northeastern Bolivia. The area in which these features occur is a flat, poorly drained, lake-studded plain. It is underlain by flat-lying, poorly consolidated, continental clastic...
Harold E. Malde, Asher P. Schick
1964, American Antiquity (30) 60-73
Geologic interest in Thorne Cave stems from its link with valley alluvium along Cliff Creek, which accumulated to a height of 48 ft., continued to build up another 13 ft. while men lived here, and then reached 30 ft. higher-sealing in the signs of man. Mineralogic study shows that ground water then circulated...
J. V. Skinner, V.C. Colby
1964, Report M
No abstract available....
J. L. Jolly, A. V. Heyl
1964, Economic Geology (59) 596-624
The Central Kentucky mineral district occupies the greater part of the Blue Grass lowland of Kentucky, which lies astride the Lexington dome and the Cincinnati arch. The oldest exposed rocks of the mineralized area are limestones of Middle Ordovician age. The paragenesis throughout the district is constant and traceable, although the relative abundance of minerals varies from vein to vein....
O. M. Hackett
1964, Groundwater (2) 2-5
No abstract available. ...
Ernest L. Paynter, W.J.D. Stephen
1964, Book chapter, Waterfowl Tomorrow
No abstract available....