C. P. Ross
1941, Open-File Report 41-2
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Page 7166, results 179126 - 179150
Publication Extents
Not all publications have extents, not all extents are completely accurateWater Resources Division, U.S. Geological Survey
1941, Water Supply Paper 909
R.E. Spratt
1941, Report
REGULATIONS PRESCRIBING PERCENT OF ROYALTY Section 17 of General Land Office Circular 1386, dated May 7, 1936, states: 17. Royalties.--Royalties, as follows, shall be paid on the amount or value of all production from the leased lands (except that portion thereof used for production purposes on said lands or unavoidably lost): (1) When...
L.L. Ray, J.F. Smith Jr.
1941, Geological Society of America Bulletin (52) 177-210
The Moreno Valley, located along the complex eastern boundary between the Sangre de Cristo Mountains and the Great Plains, is structurally a broad, northwardplunging syncline, disrupted by smaller folds and faults. This major synclinal structure is the result of the Laramide disturbance. Deformation, however, has continued possibly into the Quaternary....
E.S. Larsen, C.S. Hurlbut, Bennett Frank Buie, C.H. Burgess
1941, GSA Bulletin (52) 1841-1856
The minerals of the igneous rocks of the Highwood Mountains are described. The primary hornblende of the quartz latites is basaltic and it has been partly replaced by a common green hornblende. Hornblende is rare in the alkalic rocks. Augite is an abundant mineral of the alkalic rocks; in the...
E. S. Larsen Jr., C.S. Hurlbut, C.H. Burgess, Bennett Frank Buie
1941, GSA Bulletin (52) 1857-1868
In the shonkinite series olivine, leucite, and analcime crystallized only from magmas with over 20 per cent of mafites. At this stage the leucite and analcime inverted to pseudoleucite. Pyroxene crystallized over the whole range of rocks and changed little in composition until the magma reached the composition of nepheline...
Esper Signius Larsen Jr., Bennett Frank Buie
1941, GSA Bulletin (52) 1829-1840
Very near the contacts of the stocks the sediments have been replaced by sanidine and diopside, through magmatic reaction. An irregular zone of indurated sediments, produced largely by hydrothermal agents, extends outward from the stocks for as much as half a mile. Locally, more intense hydrothermal metamorphism has formed orthoclase...
E. S. Larsen Jr.
1941, GSA Bulletin (52) 1733-1752
Early eruptions of quartz latites, rather rich in potash, built up a volcanic mountain over 30 miles across on an irregular surface of late Cretaceous sediments. Erosion then removed much of the quartz latite. Renewed volcanism formed a volcano made up of basaltic rocks (mafic phonolite) that covered the quartz...
Section of Fur Resources U.S. Division Of Wildlife Research
1941, Wildlife Leaflet 203
No abstract available....
George S. Templeton
1941, Wildlife Leaflet 202
No abstract available....
Franklin H. May
1941, Wildlife Leaflet 205
No abstract available....
Charles Francis Bassett
1941, Wildlife Leaflet 206
No abstract available....
P.W. Wetmore
1941, Journal of Parasitology (27) 379-393
Recently a number of surveys of blood parasites of birds have been made in different parts of this country by different workers, the general purpose of which was to further the knowledge of the distribution andpathogenicity of these protozoa. This paper treats the distribution of parasites found in sampling miscellaneous...
W.L. McAtee
1941, Wildlife Leaflet 200
No abstract available....
C. E. Jacob
1941, Eos, Transactions, American Geophysical Union 783-787
The Lloyd sand is a productive artesian aquifer underlying all of Long Island except the westernmost part. It rests unconformably upon a floor of crystalline rock that slopes toward the southeast at about 100 feet to the mile. Locally the bed‐rock surface has a relief of more than 100 feet....
Walter B. Lang
1941, Science (94) 390-391
No abstract available....
Walter B. Lang
1941, Science (94) 414-414
No abstract available....
S.F. Turner, L.C. Halpenny
1941, Eos, Transactions, American Geophysical Union (22) 738-744
The Division of Ground Water of the Geological Survey, United States Department of the Interior, has been making an inventory of the water‐resources of the upper Gila River since January 1, 1940. Funds for the project are furnished under a cooperative agreement with the Arizona State Water Commissioner, supplemented by...
C. E. Jacob
1941, Eos, Transactions, American Geophysical Union (22) 744-756
An investigation of the ground‐water supply of the Houston District, in Texas, has been in progress since December, 1930, under the general direction of O. E. Meinzer, Geologist‐in‐Charge of the Division of Ground Water of the Geological Survey. The Houston District, as the term is used here, comprises all of...
Roland W. Brown
1941, Psyche: A Journal of Entomology (48) 105-110
No abstract available....
Francois E. Matthes
1941, Polar Record (333) 451-453
No abstract available....
G.A. LaRocque Jr.
1941, Eos, Transactions, American Geophysical Union (22) 374-386
Numerous ground‐water hydrologists have obtained records of water‐level surges in wells during earthquakes and of heightened or lowered levels after those earthquakes. Many of these surges and changes of level are undoubtedly direct effects of the several earthquake‐waves that are recorded on seismographs. Thus, water‐level recorders on observation‐wells promise to...
David G. Thompson
1941, Eos, Transactions, American Geophysical Union (22) 948-950
The membership of the Committee during the past year has continued as it was a year ago [see Trans. Amer. Geophys. Union, p. 433, 1940].During a large part of the year, particularly during the last few months, many of the members of the Committee have been engaged in activities more...
W.F. Guyton
1941, Eos, Transactions, American Geophysical Union 756-770
The Houston District, as the term is used in this paper, comprises an area between the Trinity and Brazos rivers in Harris County and parts of Montgomery, Waller, and Fort Bend counties, Texas. It consists of a plain of low relief that lies not far above sea‐level, and is a...
Arthur M. Morgan
1941, Eos, Transactions, American Geophysical Union (22) 779-783
The Pecos River Drainage‐Basin is underlain by a thick series of Permian rocks consisting largely of limestone, gypsum (or anhydrite), and halite. The beds have a regional eastward or southeastward dip of 40 to 80 feet to the mile and successively younger beds are exposed at the surface from west...