The New Encyclopædia BritannicaEncyclopædia Britannica, 1983 - Encyclopedias and dictionaries |
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Page 280
... material holdings are not great , and differences in life style from one person to another are very small . Where there is lack of continuous accumulation , there is often a lack of durable capital objects that can be passed on from ...
... material holdings are not great , and differences in life style from one person to another are very small . Where there is lack of continuous accumulation , there is often a lack of durable capital objects that can be passed on from ...
Page 579
... material flow into the p - type material and fill a few of the holes . This charges the p - material negatively and raises the potential energy of all the electrons in the material . Ac- cording to statistical mechanics the process ...
... material flow into the p - type material and fill a few of the holes . This charges the p - material negatively and raises the potential energy of all the electrons in the material . Ac- cording to statistical mechanics the process ...
Page 713
... material Figure 6 : The geochemical cycle . hydrosphere centration is usually compared , in the case of land organ- isms , with the content of the soil or of the Earth's crust in general and , in the case of aquatic organisms , with the ...
... material Figure 6 : The geochemical cycle . hydrosphere centration is usually compared , in the case of land organ- isms , with the content of the soil or of the Earth's crust in general and , in the case of aquatic organisms , with the ...
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activity Africa 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 feet field Figure flow force groups growth important income increase industry internal investment Italy kilometres known labour Lake land later less living magnetic major mantle material means measurements ment metres 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 River rocks social society South species structure surface theory tion trade traditional United West Western