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Vink, Gregory E.; And Others – Scientific American, 1985
Hot spots are isolated areas of geologic activity where volcanic eruptions, earthquakes, and upwelling currents occur far from plate boundaries. These mantle plumes are relatively stable and crustal plates drift over them. The nature and location of hot spots (with particular attention to the Hawaiian Islands and Iceland) are discussed. (DH)
Descriptors: College Science, Earthquakes, Geology, Geophysics
United Nations Educational, Scientific, and Cultural Organization, Paris (France). Div. of Marine Sciences. – 1985
This report introduces oceanographers to the International System of Units (SI) in physical oceanography. The SI constitutes a universal language, designed to be understood by all scientists. It facilitates their mutual comprehension and exchange of views and results of their work. The first part of the report is devoted to physical quantities,…
Descriptors: Chemistry, College Science, Geophysics, Higher Education
Anderson, Don L.; Dziewonski, Adam M. – Scientific American, 1984
Describes how seismic tomography is used to analyze the waves produced by earthquakes. The information obtained from the procedure can then be used to map the earth's mantle in three dimensions. The resulting maps are then studied to determine such information as the convective flow that propels the crustal plates. (JN)
Descriptors: College Science, Earthquakes, Geology, Geophysics

Schramm, David N. – Physics Today, 1983
Many properties of new particle field theories can only be tested by comparing their predictions about the physical conditions immediately after the big bang with what can be reconstructed about this event from astronomical data. Facts/questions about big bang, unified field theories, and universe epochs/mass are among the topics discussed. (JN)
Descriptors: Astronomy, College Science, Geophysics, Higher Education
Burchfiel, B. Clark – Scientific American, 1983
Continental crust underlies the continents, their margins, and also small shallow regions in oceans. The nature of the crust (much older than oceanic crust) and its dynamics are discussed. Research related to and effects of tectonics, volcanism, erosion, and sedimentation on the crust are considered. (JN)
Descriptors: College Science, Earth Science, Geology, Geophysics
Jeanloz, Raymond – Scientific American, 1983
The nature of the earth's core is described. Indirect evidence (such as that determined from seismological data) indicates that it is an iron alloy, solid toward its center but otherwise liquid. Evidence also suggests that it is the turbulent flow of the liquid that generates the earth's magnetic field. (JN)
Descriptors: College Science, Earth Science, Geology, Geophysics
McKenzie, D. P. – Scientific American, 1983
The nature and dynamics of the earth's mantle is discussed. Research indicates that the silicate mantle is heated by the decay of radioactive isotopes and that the heat energizes massive convention currents in the upper 700 kilometers of the ductile rock. These currents and their consequences are considered. (JN)
Descriptors: College Science, Earth Science, Geology, Geophysics
Francheteau, Jean – Scientific American, 1983
The earth's oceanic crust is created and destroyed in a flow outward from midocean ridges to subduction zones, where it plunges back into the mantle. The nature and dynamics of the crust, instrumentation used in investigations of this earth feature, and research efforts/findings are discussed. (JN)
Descriptors: College Science, Earth Science, Geology, Geophysics

Brush, Stephen G. – Journal of Geological Education, 1982
Refutes scientific creationists' arguments that the earth is less than 10,000 years old by presenting information related to the time scales for creation and evolution models, times from stellar distances, Kelvin's estimate of the earth's age, radioactive decay, radiometric dating, and the decay of the earth's magnetic field. (DC)
Descriptors: College Science, Creationism, Elementary Secondary Education, Evolution
Siever, Raymond – Scientific American, 1983
Discusses how the earth is a dynamic system that maintains itself in a steady state. Areas considered include large/small-scale earth motions, geologic time, rock and hydrologic cycles, and other aspects dealing with the changing face of the earth. (JN)
Descriptors: College Science, Earth Science, Evolution, Fluid Mechanics