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Publication Extents

Not all publications have extents, not all extents are completely accurate
Transit traverse in Missouri, 1900-1937. Part 1, Southeastern Missouri, 1903-37
John G. Staack
1939, Bulletin 916-A
This bulletin, which for convenience is to be published in eight parts, contains the results of all transit traverse* done In Missouri through 1937 by the Geological Survey, United States Department of the Interior, including those heretofore published. (See page X.) Each of the parts deals with one of eight...
Subsurface geology and oil and gas resources of Osage County, Oklahoma. Part 2, Townships 22 and 23 north, ranges 8 and 9 east
C. T. Kirk, H. D. Jenkins, Otto Leatherock, W. R. Dillard, L. E. Kennedy, N. W. Bass
1939, Bulletin 900-B
This report on the subsurface geology of Osage County, Okla., describes the structural features, the character of the oil- and gas-producing beds, and the localities where additional oil and gas may be found. It embodies a part of the results of a subsurface geologic investigation of the Osage Indian Reservation,...
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...