An unusual Lower Cambrian trilobite fauna from Nevada
Allison R. Palmer
1964, Professional Paper 483-F
Channel geometry of Piedmont streams as related to frequency of floods
F. A. Kilpatrick, Harry Hawthorne Barnes Jr.
1964, Professional Paper 422-E
Preliminary surficial geologic map of the Mesabi-Vermilion Iron Range area, northeastern Minnesota
R. D. Cotter, H. L. Young, T. C. Winter
1964, IMAP 403
No abstract available....
Geologic map of the south half of the Baylor, Larslan, West Fork, Police Creek, Kahle, and Lundville quadrangles, Valley, Roosevelt, and Daniels Counties, Montana
R. B. Colton
1964, IMAP 361
No abstract available. ...
Topographic mapping: A challenging future
U.S. Geological Survey
1964, Report
The United States Geological Survey was established by Congress in 1879 to make a systematic study of the geology and natural resources of the United States. To provide the essential base maps for these studies, the Survey immediately began a program of topographic mapping. In 1882 a general plan was adopted for a standard series...
Surface water records of Indiana, 1964
Water Resources Division, U.S. Geological Survey
1964, Report
The surface-water records for the 1964 water year for gaging stations, partial-record stations, and miscellaneous sites within the State of Indiana are given in this report. For convenience there are also included records for a few pertinent gaging stations in bordering States. The records were collected and computed by the...
Gravel resources in the Patuxent Formation of Cretaceous age in the Beltsville quadrangle, Prince Georges and Montgomery Counties, Maryland
C. F. Withington
1964, Report
No abstract available....
Late quaternary sea-level change and crustal rise at Boston, Massachusetts, with notes on the autocompaction of peat
C. A. Kaye, E.S. Barghoorn
1964, Geological Society of America Bulletin (75) 63-80
The compression of peat beneath its own weight (autocompaction) is discussed, and it is shown that because of this process radiocarbondated samples of salt-marsh peat or peaty sediment, other than very thin samples cut from the base of the deposit, cannot be correlated with sea level without construction of a...
Boulder train of silicified paleozoic wood, southeastern Massachusetts
C. A. Kaye
1964, Geological Society of America Bulletin (75) 233-236
Pebbles of silicified gymnospermous wood occur widely in the drift of southeastern Massachusetts. An investigation of the distribution of these pebbles shows the bedrock source of the wood to be tuffaceous beds that apparently overlie older granite in the Middleboro-Plympton area, Massachusetts, and are at the base of the Carboniferous...
Exploration for mineral deposits in White County, Georgia
Vernon J. Hurst
1964, Report
White County is in the Northeast Georgia Highland. It comprises 243 square miles and has abouit 7,000 Inhabitants. The county seat is Cleveland.Although the scene of considerable mining activity in the past, White County now has few operating mines: a small production of clay1 for the manufacture of miscellaneous potter...
Manufacturers of chemical animal repellents
U.S. Bureau of Sport Fisheries and Wildlife
1964, Wildlife Leaflet 464
No abstract available....
Recreational policy on National Wildlife Refuges
U.S. Bureau of Sport Fisheries and Wildlife
1964, Wildlife Leaflet 463
No abstract available....
Low-amplitude aeromagnetic anomalies in Southeastern Missouri
J.W. Allingham
1964, Geophysics (29) 537-552
This study shows that aeromagnetic anomalies of less than 200 gammas are associated with topographic relief of exposed Precambrian granitic and volcanic rocks of the St. François Mountains. Anomalies resulting from hills coarsely crystalline granite are as high as 100 gammas in amplitude, whereas anomalies over comparable hills of fine-grained rocks, such as granophyre or devitrified volcanic rock, are...
Principal features and origin of podiform chro-mite deposits, and some observations on the Guleman-Soridag District, Turkey
T. P. Thayer
1964, Economic Geology (59) 1497-1524
Podiform chromite deposits occur in alpine peridotite and mafic complexes and fundamentally are tabular, pencil-shaped, or irregular in form. The chromite characteristically is anhedral and commonly shows effects of granulation and magmatic corrosion. Flow-layering, foliation, and lineation are parallel in most chromite deposits and peridotite host rocks, and normally pass through major...
Pasteurella sp. from an epizootic of white perch (Roccus americanus) in Chesapeake Bay Tidewater areas
S. F. Snieszko, G. L. Bullock, E. Hollis, J.G. Boone
1964, Journal of Bacteriology (88) 1814-1815
No abstract available. ...
Nocardial infection in hatchery-reared fingerling rainbow trout (Salmo gairdneri)
S. F. Snieszko, G. L. Bullock, C. E. Dunbar, L.L. Pettijohn
1964, Journal of Bacteriology (88) 1809-1810
No abstract available. ...
Paleo-channels at the Guayacan copper mine, Cabildo District, Aconcagua Province, Chile
W. D. Carter, T. Aliste Nelson
1964, Economic Geology (59) 1283-1292
An uneven erosion surface separates calcareous sedimentary rocks above and vesicular andesite porphyry below at the Guayacan mine of central Chile. Channel-like depressions filled with sedimentary rock flank elongate, stratiform bodies of disseminated copper ore which impregnate the vesicular crests of andesite lava flows. The "channels" lie parallel to and mark the margins of tongues of lava. Erosional features...
Supergene iron ores of minas Gerais, Brazil
J. V.N. Dorr II
1964, Economic Geology (59) 1203-1240
The iron ores of Minas Gerais, Brazil, fall into two categories: (1) hypogene hematite ore averaging 66 percent or more Fe, and (2) lower-grade supergene ores. Most ore now extracted is high-grade hypogene ore; lower-grade supergene ores will be of much future value. All supergene ores formed by weathering of itabirite, a metamorphosed oxide-facies iron formation averaging about 38 percent Fe and 44 percent Si02. The Caue Itabirite crops out for...
Rigid plastic collars for marking geese
R.M. Ballou, F.W. Martin
1964, Journal of Wildlife Management (28) 846-847
Rigid plastic collars of one to three colors proved useful for recognition of individual Canada geese (Branta canadensis). The collars did not seem to affect the behavior of the geese, and there was little mortality caused by their use. In good light, bright colors are visible through a 20-power spotting...
Problems of the geographic and stratigraphic distribution of American Middle Eocene larger Foraminifera
W. Storrs Cole, Esther English Richards Applin
1964, Bulletins of American Paleontology (47) 1-48
Larger Foraminifera from the middle Eocene of Florida and southern Georgia are discussed, including 2 new species, and their geographic and stratigraphic distribution, not only in the U. S., but also at selected localities in the Caribbean region, is analyzed. Several species not previously reported from the U. S. are...
The international hydrological decade
R. L. Nace
1964, Eos, Transactions, American Geophysical Union (45) 413-421
Work toward establishing a program of international cooperative studies in scientific hydrology began about 4 years ago, and the IHD (International Hydrological Decade) will begin under international auspices in January 1965. This program will be highly important for hydrology and hydrologists, and it should contribute greatly to human welfare in the future. Fortuitously, the opening year...
Geohydrologic analogies between the Jordan Valleys of Utah and the holy land
Edward Bradley
1964, International Association of Scientific Hydrology - Bulletin (9) 12-23
The biblical Jordan River Valley, which extends from Lake Tiberias (the Sea of Galilee) to the Dead Sea, is decidedly similar to the Jordan River Valley of Utah, which joins Lake Utah and Great Salt Lake. Both Jordan Rivers drain relatively large fresh-water lakes and also are major sources of discharge into large salty lakes that have no outlets to the ocean.The...
Big game inventory for 1963
U.S. Bureau of Sport Fisheries and Wildlife
1964, Wildlife Leaflet 461
No abstract available....
Experimental determination of the reaction chalcopyrite + sulfur = pyrite + bornite from 350 to 500° C
P. B. Barton Jr., P. Toulmin III
1964, Economic Geology (59) 747-752
The fugacity of sulfur along the curve representing the univariant equilibrium assemblage, chalcopyrite + bornite + pyrite + vapor, has been determined by the electrum tarnish method (1). The conditions of the equilibrium may be expressed by the equation (TP) - /°s 2 (T, 1 atm) = -50,730 + 56.95T (cal.) (350 - 500° C) (T in °K). With gentle curvature, the line...
Officer's cave, a pseudokarst feature in altered tuff and volcanic ash of the John Day formation in eastern Oregon
Garald G. Parker, Lynn M. Shown, Karl W. Ratzlaff
1964, Geological Society of America Bulletin (75) 393-402
Officer's Cave is the uppermost of four rapidly eroding cave levels constituting a cavern complex about 700 feet long developed chiefly in clay and silt. Its outer room is 35 feet by 43.5 feet by 100 feet and slopes about 45° east into the western end of a narrow linear hill called Officer's Cave Ridge. Dry valleys, blind valleys, hanging valleys, sinkholes, pipes,...