The New Encyclopædia BritannicaEncyclopædia Britannica, 1983 - Encyclopedias and dictionaries |
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Page 315
... atmospheric gases ( see ATMOSPHERE ) . Thus , the most probable explanation is that the Earth's atmosphere and the hydrosphere that condensed from it originally arose from within the Earth and thus most probably consisted of those gases ...
... atmospheric gases ( see ATMOSPHERE ) . Thus , the most probable explanation is that the Earth's atmosphere and the hydrosphere that condensed from it originally arose from within the Earth and thus most probably consisted of those gases ...
Page 316
... atmosphere for the first half of pre - Paleozoic time . 4. Carbonate rocks older than two aeons are uncom- mon , sedimentary carbon of this age being mainly in the form of ... atmospheric and combined O2 316 Atmosphere , Development of.
... atmosphere for the first half of pre - Paleozoic time . 4. Carbonate rocks older than two aeons are uncom- mon , sedimentary carbon of this age being mainly in the form of ... atmospheric and combined O2 316 Atmosphere , Development of.
Page 320
... Atmospheric Sciences The atmospheric sciences are concerned with under- standing the composition , structure , and behaviour of the atmosphere . Their role can be described in terms of the natural phenomena to be understood ...
... Atmospheric Sciences The atmospheric sciences are concerned with under- standing the composition , structure , and behaviour of the atmosphere . Their role can be described in terms of the natural phenomena to be understood ...
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