Robert Wayne Schnabel
1962, Geologic Quadrangle 147
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Page 6043, results 151051 - 151075
Publication Extents
Not all publications have extents, not all extents are completely accurateJ. L. Meuschke, A. J. Petty, F. P. Gilbert
1962, Geophysical Investigations Map 299
No abstract available....
Roy O. Jackson, R.G. Bogue, Glen F. Brown, Ruel D. Gierhart
1962, IMAP 211-B
Prepared by the U.S. Geological Survey and the Arabian American Oil Company under the joint sponsorship of the Kingdom of Saudi Arabia and the U.S. Department of State....
H. E. Thomas
1962, Circular 469
J. L. Meuschke, A. J. Petty, W. E. McCaslin
1962, Geophysical Investigations Map 303
No abstract available....
Richard A. Bramkamp, Glen F. Brown, Donald A. Holm, Newton M. Layne Jr.
1962, IMAP 200-B
Prepared by the U.S. Geological Survey and the Arabian American Oil Company under the joint sponsorship of the Kingdom of Saudi Arabia and the U.S. Department of State....
Bruce William Maxwell, Robert Washburn Devaul
1962, Hydrologic Atlas 26
Edwin Thor McKnight, Allen Van Heyl, William Louis Newman
1962, Mineral Investigations Resource Map 15
The productive lead districts in the United States (exclusive of Alaska and Hawaii) are shown on the accompanying map. The map is at a scale of 1: 3,168,000, (50 miles to the inch). Only those districts known or believed to contain 1,000 short tons or more of lead are shown;...
Anna Hietanen
1962, Professional Paper 344-A
D.M. Lemmon, Ogden L. Tweto
1962, Mineral Investigations Resource Map 25
The accompanying map shows the tungsten deposits of the United States (exclusive of Alaska and Hawaii). The relative importance of the deposits, groups, or districts is shown by four symbols, indicating tungsten contents of: (1) greater than 10,000 short tons of tungsten metal, (2) 10,000 to 500 tons, (3) 500...
Albert Herbert Koschmann, M.H. Bergendahl
1962, Mineral Investigations Resource Map 24
The accompanying map shows the distribution of the principal gold mining districts in the United States (excluding Alaska and Hawaii). Only those districts that have produced 10,000 ounces of gold or more are shown. Gold ore reserves were not considered, and the types of deposits are not shown. Based on...
R. W. Bromery, F. P. Gilbert
1962, Geophysical Investigations Map 297
Arthur R. Kinkel Jr., N. P. Peterson
1962, Mineral Investigations Resource Map 13
The copper districts in the United States (exclusive of Alaska and Hawaii) are shown on the accompanying map. In compiling the map, the estimated total quantity of copper present before mining was used to assign districts to size categories, and both production and reserves are included without distinction as to...
J. L. Meuschke, A. J. Petty, F. P. Gilbert
1962, Geophysical Investigations Map 302
No abstract available....
William E. Price, D. S. Mull, Chabot Kilburn
1962, Water Supply Paper 1607
In the Eastern Coal Field region of Kentucky, water is obtained from consolidated sedimentary rocks ranging in age from Devonian to Pennsylvanian and from unconsolidated sediments of Quaternary age. About 95 percent of the area is underlain by shale, sandstone, and coal of Pennsylvanian age. Principal factors governing the availability...
J. L. Meuschke, A. J. Petty, F. P. Gilbert
1962, Geophysical Investigations Map 301
Eugene T. Oborn, John David Hem
1962, Water Supply Paper 1459-I
E. L. Hendricks, S. K. Love
1962, Water Supply Paper 1720
G. E. Andreasen, J. L. Vargo
1962, Geophysical Investigations Map 342
No abstract available....
Edward A. Sammel, John A. Baker
1962, Ground-water Series 2
The lower Ipswich River basin is that part of the Ipswich River drainage basin below the Geological Survey stream-gaging station at South Middleton in northeastern Massachusetts (fig. 1). It includes about 110 square miles between the gaging station at South Middleton and the Atlantic Ocean. This report presents basic data collected...
Water Resources Division, U.S. Geological Survey
1962, Report
The surface-water records for the 1962 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...
Richard A. Robie
1962, Trace Elements Investigations 816
In the ten years since the publication of the national Bureau of Standards comprehensive tables of thermochemical properties, by Rossini and other (1952), a very large body of modern calorimetric and equilibrium data has become available. Because of the complex interrelations among many thermochemical data and the necessity for internal...
B.J. Kallman
1962, Chemist-Analyst (51) 75-76
Carboxylic esters and lactones react with alkaline hydroxylamine to yield hydroxamates; these in acidic solution form colored iron(III) complexes. A photometric determination of such esters and lactones is thus permitted and has been extensively applied ( I-6). Hestrin ( 3) utilized this method for the microdetermination of acetylcholine and his...
Harold Meisler
1962, Geological Society of America Bulletin (73) 1071-1082
Summit elevations in the Lebanon Valley, part of the Great Valley, range from 440 to 720 feet above msl (mean sea level). This range cannot be accounted for adequately by the peneplain concept. Although accordant summits, the chief evidence for peneplains, occur over large areas, summits are not accordant between...
Warren Hamilton
1962, Geological Society of America Bulletin (73) 511-516
The massive Salmon River Mountains of interior Idaho are bounded on the west by a belt 30 miles wide of post-Miocene, west-tilted normal-fault blocks and west-dipping monoclines. The belt is coincident with the western border zone of the middle Cretaceous Idaho batholith, as it extends from the west edge of the massive...