Watson H. Monroe
1938, Open-File Report 38-3
Search Results
164468 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 6419, results 160451 - 160475
Publication Extents
Not all publications have extents, not all extents are completely accurateR.O. Helland
1938, Open-File Report 38-2
R.O. Helland
1938, Open-File Report 38-1
W. Ayvazoglou (compiler)
1938, Bulletin 909-A
W. Ayvazoglou (compiler)
1938, Bulletin 895-C
W. Ayvazoglou (compiler)
1938, Bulletin 895-D
Water Resources Division, U.S. Geological Survey
1938, Bulletin 898-A
Water Resources Division, U.S. Geological Survey
1938, Bulletin 898-B
Water Resources Division, U.S. Geological Survey
1938, Bulletin 898-C
Water Resources Division, U.S. Geological Survey
1938, Bulletin 898-D
N. W. Bass, L. E. Kennedy, W. R. Dillard, Otto Leatherock, J. H. Hengst
1938, Bulletin 900-A
No abstract available....
C. H. Dane, H. E. Rothrock, J. S. Williams
1938, Bulletin 874-C
No abstract available....
W. Ayvazoglou (compiler)
1938, Bulletin 895-B
C. Milton, W. D. Johnston Jr.
1938, Economic Geology (33) 749-771
Seventeen representative samples of supergene sulphates from old workings on the Comstock Lode are described. They range from simple minerals such as gypsum and epsomite to complex aggregates of four or more distinct species. All are well known species except a mineral of the copper (chalcanthite) or magnesium sulphate pentahydrate...
Charles Frederick Park
1938, Economic Geology (33) 709-729
The replacement ore bodies of the Metaline zinc-lead district, in northeastern Washington are limited to the greatly disturbed fault block through which the Pend Oreille River flows and are associated with the major faults but are not in them. They are mostly near the top of the Metaline limestone, of...
U.S. Bureau of Biological Survey
1938, Wildlife Leaflet 121
No abstract available....
E.R. Kalmbach
1938, Wildlife Leaflet 120
No abstract available....
C. S. Ross
1938, Eos, Transactions, American Geophysical Union (19) 263-264
The igneous rocks and the minerals of Magnet Cove, Arkansas, have long interested geologists and mineralogists, but in much of the area rock‐exposures are so sparse that many of the geologic, relations have remained obscure. However, recent prospecting and the mining of titanium ores have uncovered rocks that throw new...
F. C. Calkins
1938, Eos, Transactions, American Geophysical Union (19) 262-262
The oldest igneous rocks in the Comstock District are amphibolites probably derived from basalts and of Triassic age. These are intruded by pre‐Tertiary quartz monzonlte and by granodiorite of Sierran facies, the latter not being exposed on the surface but found on mine‐dumps. Igneous activity recorded mainly in volcanic rocks...
C. Milton
1938, Eos, Transactions, American Geophysical Union (19) 264-264
Two of the numerous small dikes mapped on the areal geology sheet of the Franklin Furnace Folio (U.S. Geological Survey 161) as “Mostly basic, including nepheline tinguaite, leucite tinguaite, and camptonite” of post‐Ordovician age, have been found to be quite distinct from these alkalic rocks, and the two dikes in...
George R. Mansfield
1938, Economic Geology (32) 335-549
Stratigraphy is concerned mainly with the genesis and interpretation of stratified rocks, which include some of wide extent and of great scientific as well as economic interest that are largely of chemical rather than of detrital origin. Chemical agencies have been recognized to some extent in genetic studies of these...
Ralf R. Woolley, J.C. Alter
1938, Eos, Transactions, American Geophysical Union (19) 804-807
As time marches on, historians are usually quite faithful in recording the activities of man, and it will usually be found that Mother Nature is even more meticulous in reflecting and preserving her experiences, more especially with regard to climate and vegetation. Just how much the activities of man have...
J. Oliver, N.W. Cummings
1938, Eos, Transactions, American Geophysical Union (19) 609-612
The instrument herein described was originally designed and built to record the evaporation‐loss from a standard Weather Bureau pan for use in a study of the variation of flow in Santa Ana River. Valuable suggestions were made by various members of the Water Resources Branch of the Geological Survey in...
R.M. Leggette, M.L. Brashears Jr.
1938, Eos, Transactions, American Geophysical Union (19) 412-418
During the last five years ground‐water has been more and more extensively used for air‐conditioning on Long Island, New York. The wide‐spread occurrence of highly permeable water‐bearing material and the relatively small cost of installation and operation of a ground‐water, air‐conditioning system has resulted in many such installations by theaters,...
John Calvin Reed
1938, Economic Geology (33) 53-78
Prospecting in the Glacier Bay National Monument has been confined so far to granitic rocks near contacts with Paleozoic sediments, which they intrude.Near Reid Glacier thin veins, a few of which are traceable for about 300 feet both horizontaliy and vertically, trend northerly and carry sphalerite, galena, and pyrite. Gold...