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Tungsten deposits of the Atolia district, San Bernardino and Kern Counties, California
No abstract available.
Authors
D.M. Lemmon, John Van N. Dorr
Water levels and artesian pressure in observation wells in the United States in 1939
No abstract available.
Authors
Oscar Edward Meinzer, Leland Keith Wenzel
Protecting field crops from waterfowl damage by means of reflectors and revolving beacons
No abstract available.
Authors
F.M. Uhler, Stephen Creech
Fluctuations in artesian pressure produced by passing railroad‐trains as shown in a well on Long Island, New York
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,” Veatch [see 1 of “References” at end of paper] in 1906 considered in
Authors
C. E. Jacob
A conception of runoff‐phenomena
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 discharge‐hydrograph for a particular gaging station. (Rainfall‐eccentricities often
Authors
F. Snyder