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Page 6469, results 161701 - 161725

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Publication Extents

Not all publications have extents, not all extents are completely accurate
Major Texas floods of 1935
Tate Dalrymple
1939, Water Supply Paper 796-G
In localities where highly mineralized water is present in beds above and below the beds that yield the supplies of fresh water it is necessary to be able to locate leaks in wells in order to know whether the wells are being contaminated through holes in the casings or whether...
Geology of some dam sites on Little Colorado and its tributaries, Arizona
Edwin B. Eckel
1939, Open-File Report 40-5
This report contains descriptions of the geology of 10 dam and reservoir sites on the Little Colorado River and several of its larger tributaries in northern Arizona. All of the streams examined are intermittent in character and are dry during the greater part of every year. At times they all...
Fluctuations in artesian pressure produced by passing railroad‐trains as shown in a well on Long Island, New York
C. E. Jacob
1939, Eos, Transactions, American Geophysical Union (20) 666-674
Perhaps one of the chief interests of ground‐water hydrologists is the study of water‐level fluctuations. Since the beginning of the science of hydrology attempts have been made to interpret these phenomena and determine their significance. On the basis of actual observations and “with special reference to Long Island, New York,”...
A conception of runoff‐phenomena
F. Snyder
1939, Eos, Transactions, American Geophysical Union (20) 725-738
The problem of transforming observed precipitation into stream‐flow for a natural drainage‐basin can be divided into two parts. The first part requires a procedure for determining the amount and kind of runoff that occurs under various conditions. The second part is concerned with the shaping of the runoff into a...
Earth‐tides shown by fluctuations of water‐levels in wells in New Mexico and Iowa
T. W. Robinson
1939, Eos, Transactions, American Geophysical Union 656-665
It is quite generally known that ocean‐tides produce fluctuations of the water‐level in wells of the artesian type located close to the seashore by periodically changing the external load on the aquifer [see 1 of “References” at end of paper]. Fluctuations of ground‐water as a result of earth‐tides, however, are...
Some features of the Livingston Formation near Nye, Montana
J.S. Vhay
1939, Eos, Transactions, American Geophysical Union (20) 433-437
The Livingston Formation is a series of pyroclastic rocks several thousand feet thick cropping out on the north side of the Beartooth Mountains. These pyroclastic rocks grade laterally into the Claggett, Judith River, Bearpaw, and Lennep formations of the Montana Group, according to Stone and Calvert [see 1 of references...