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Page 5647, results 141151 - 141175

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Publication Extents

Not all publications have extents, not all extents are completely accurate
Water resources of the Crow Wing River watershed, central Minnesota
Gerald F. Lindholm, E.L. Oakes, D.W. Ericson, J. O. Helgesen
1972, Hydrologic Atlas 380
The Crow Wing River, a tributary of the Mississippi River, drains an area of about 3,760 square miles, essentially all of which is covered by glacial deposits. Topography of most of the watershed is slightly- to moderately-undulating and has local relief of up to about 50 feet. The margin of the...
Reconnaissance of the Manistee River, a cold-water river in the northwestern part of Michigan's Southern Peninsula
G. E. Hendrickson, C. J. Doonan
1972, Hydrologic Atlas 436
The cold-water streams of the northern states provide unique recreational values to the American people (wilderness or semi-wilderness atmosphere, fast-water canoeing, trout fishing), but expanding recreational needs must be balanced against the growing demand of water for public and industrial supplies, irrigation, and dilution of sewage and other wastes. In...
Water resources of the Minnesota River-Hawk Creek watershed, southwestern Minnesota
Wayne A. Van Voast, W.L. Broussard, D.E. Wheat
1972, Hydrologic Atlas 391
The Minnesota River – Hawk Creek watershed is located in southwestern Minnesota. The watershed has an area of 1,479 square miles and is drained along its southwestern edge by the Minnesota River (Minnesota Division of Waters, 1959). The major watercourse within the watershed is Hawk Creek, having a drainage area...
Reconnaissance geology of the Bi'r Al Badriyah quadrangle, Kingdom of Saudi Arabia
William C. Overstreet, J. W. Whitlow, V.P. Kahr, A.O. Ankary
1972, Open-File Report 72-283
The Bi'r al Badriyah quadrangle covers an area of 2843 sq km in the extreme eastern part of the Precambrian Shield in central Saudi Arabia. The Precambrian rocks in the southeastern part of the area are unconformably overlain by limestone of Permian age, which occupies only a small part of...
Reconnaissance engineering geology of the Skagway area, Alaska, with emphasis on evaluation of earthquake and other geologic hazards
Lynn A. Yehle, Richard Walter Lemke
1972, Open-File Report 72-454
A program to study the engineering geology of most of the larger Alaska coastal communities and to evaluate their earthquake and other geologic hazards was started promptly after the 1964 Alaska earthquake; this report is a product of that program. Field-study methods were largely reconnaissance, and thus the interpretations in...
Interim results of geological investigations in the vicinity of the Ergani-Maden massive copper deposits near Maden, Elazig, Turkey
A.E. Weisseborn, Omer Oner, Metin Sengun
1972, Open-File Report 72-446
As a result of geologic studies and geochemical reconnaissance by Griffitts, Albers, and brier in 1969 in the Ergani-Maden district of eastern Turkey, seven areas were recommended for more detailed investigation. Two of these, here termed Areas 1 and 2, were mapped geologically and sampled geochemically in June and July...
A quick transcribing technique for oral data
David Schleicher
1972, Open-File Report 72-330
Stenographic techniques offer a means for transcribing oral data accurately and efficiently. In one such application, during five Appolo lunar missions, a rough but helpful transcript was produced within minutes. Similarly, lectures, conferences, and audio tapes can be accurately transcribed as promptly as necessary. Computer programs for translating shorthand notes...
Geology of the Konakpinar--Sarica area, Sivas Province, Turkey
Patrick James Barosh, Salim Sermin, Ilker Gencel, Metin Sengun, Frank Ekren
1972, Open-File Report 72-25
The junction of several major structures and stratigraphic sequences is in the Konakpinar-Sarica area of central Turkey. Most of the area is underlain by Upper Jurassic to Cretaceous limeston and siltstone, early Tertiary sedimentary rock, and remnants of younger volcanic rocks and lacustrine deposits. The northeastern part of the area,...