The New Encyclopaedia Britannica, Volume 6 |
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Page 33
Any theoretical model of the main geomagnetic field must be able to account for
its frequent reversals in geologic times as well as its general behaviour at present
. No theory has ever been proposed to account quantitatively for the observed ...
Any theoretical model of the main geomagnetic field must be able to account for
its frequent reversals in geologic times as well as its general behaviour at present
. No theory has ever been proposed to account quantitatively for the observed ...
Page 34
Figure 5: Four-dynamo theory. (A) Chain reactions of dynamo model. (B)
Modified dynamo model. See text for explanation of symbols. chain of dynamo
processes starting from B0 and returning to Bo again through toroidal field Tu Tt,
Tt can be ...
Figure 5: Four-dynamo theory. (A) Chain reactions of dynamo model. (B)
Modified dynamo model. See text for explanation of symbols. chain of dynamo
processes starting from B0 and returning to Bo again through toroidal field Tu Tt,
Tt can be ...
Page 561
ionic charge in the field applied during solidification. The electret gives a useful
method of maintaining a static electric field over long periods. Electrostatic
microphones using plastic electrets are commercially available, and there has
been ...
ionic charge in the field applied during solidification. The electret gives a useful
method of maintaining a static electric field over long periods. Electrostatic
microphones using plastic electrets are commercially available, and there has
been ...
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activity African agriculture America became become body called capital caused central centre century changes Christian Church continued core countries cultural demand direction early Earth East Eastern eclipse economic effect established Europe example existence feet field Figure flow force groups growth important income increase industry influence internal investment Italy kilometres known labour Lake land later less living magnetic major mantle material means measurements ment miles mountains move movement nature North observed occur ocean organization origin Orthodox patriarch percent period planning Pleistocene political population position possible present problems production region relatively remained result rise rocks social society South species structure surface theory tion trade traditional United West Western