John R. Dyni
1966, Open-File Report 66-38
No abstract available....
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Publication Extents
Not all publications have extents, not all extents are completely accurateGeorge Plafker, Reuben Kachadoorian
1966, Professional Paper 543-D
Kodiak Island and the nearby islands constitute a mountainous landmass with an aggregate area of 4,900 square miles that lies at the western border of the Gulf of Alaska and from 20 to 40 miles off the Alaskan mainland. Igneous and metamorphic rocks underlie most of the area except for...
Edward W. Wolfe
1966, Open-File Report 69-321
E. H. Cordes, J. R. Wall, Joe A. Moreland
1966, Open-File Report 66-19
James L. Patterson, William P. Somers
1966, Water Supply Paper 1683
This report outlines methods by which the magnitude and frequency of expected floods of any recurrence interval from 1.1 to 50 years can be determined at most points in the Colorado River basin.Composite frequency curves were drawn showing the relation of the mean annual flood to floods having recurrence intervals...
R. Theodore Hurr, J.E. Moore, David B. Richards
1966, Open-File Report 66-66
Robert H. Tschudy, Sharon D. Van Loenen
1966, Open-File Report 66-133
As a part of continuing studies to provide palynological data from critical sequences for comparative biostratigraphic studies, the microfossils found in two Paleocene samples have been examined and photographed....
Division Of Wildlife Research
1966, Wildlife Leaflet 474
M. R. Collings, R. M. Myrick
1966, Professional Paper 491-B
F. Geukens
1966, Professional Paper 560-B
Farrell F. Barnes
1966, Bulletin 1202-C
No abstract available....
Thomas Seward Lovering
1966, Bulletin 1222-F
Bureau Of Sport Fisheries And Wildlife, University Of Alaska
1966, Resource Publication 16
No abstract available....
R.G. Reeves
1966, Professional Paper 341-E
E. R. Hampton
1966, Open-File Report 66-56
Stanley Eugene Norris, Andrew Maute Spieker
1966, Water Supply Paper 1808
The principal aquifers of the Dayton area are sand and gravel layers in the 150- to 250-foot thick glacial deposits filling the river valleys (Miami River and its tributaries), which were originally cut in bedrock by preglacial streams. The upper and lower aquifers are separated by a poorly permeable till-rich...
Perry C. Olcott
1966, Water Supply Paper 1814
Sources or water in Winnebago County include surface water from the Fox and Wolf Rivers and their associated lakes, and ground water from sandstone, dolomite, and sand and gravel deposits. Surface water is hard and generally requires treatment, but is then suitable for municipal and most industrial uses. Pollution is...
Donald L. Coffin, Edward J. Jenkins
1966, Open-File Report 66-15
J.M. Weigle, Richard Kranes
1966, Open-File Report 66-152
G. Arthur Cooper, Richard E. Grant
1966, Bulletin 1244-E
James A. Pitkin, Bernard L. White
1966, Open-File Report 66-105
David L. Durham
1966, Bulletin 1221-B
George Vincent Cohee, Walter S. West
1966, Bulletin 1244-A
No abstract available....
J. H. McCarthy Jr., G. B. Gott
1966, Open-File Report 66-83
No abstract available....
Preston E. Cloud Jr.
1966, Bulletin 1199-O
No abstract available....