Elementary Lessons in the Science of Agricultural Practice |
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Page 11
... rock into a soft or a gritty powder . This change on the surface of this stonework is very similar in character to the decay of our rocks , whereby they are made to yield portions of their surface in that , more or less CHAP . III ...
... rock into a soft or a gritty powder . This change on the surface of this stonework is very similar in character to the decay of our rocks , whereby they are made to yield portions of their surface in that , more or less CHAP . III ...
Page 12
... rocks which are now known as the primitive rocks , or , plainly speaking , the first rocks . We have large masses of these rocks still remaining , so that we can form a very accurate opinion of their nature and character . But a period ...
... rocks which are now known as the primitive rocks , or , plainly speaking , the first rocks . We have large masses of these rocks still remaining , so that we can form a very accurate opinion of their nature and character . But a period ...
Page 13
... rocks in like manner has become rock and then soil , and again rock and then soil , very many times . In the periods during which it was existing as soil , it may have been intermingled with the soils produced from other primitive rocks ...
... rocks in like manner has become rock and then soil , and again rock and then soil , very many times . In the periods during which it was existing as soil , it may have been intermingled with the soils produced from other primitive rocks ...
Page 14
... rocks which were found at latter periods of time were little more than recon- structions of the original materials of the primitive rocks . As a matter of fact we do find in the primi- tive rocks just those mineral matters which now ...
... rocks which were found at latter periods of time were little more than recon- structions of the original materials of the primitive rocks . As a matter of fact we do find in the primi- tive rocks just those mineral matters which now ...
Page 15
... rocks modified . So also in the soils which were produced by their decay equally marked variations were to be found ... rocks into earthy matter is accomplished . We have seen that ordinary stone buildings bear signs of the same decay ...
... rocks modified . So also in the soils which were produced by their decay equally marked variations were to be found ... rocks into earthy matter is accomplished . We have seen that ordinary stone buildings bear signs of the same decay ...
Contents
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Elementary Lessons in the Science of Agricultural Practice (1881) Henry Tanner No preview available - 2008 |
Common terms and phrases
acre advantages Agricultural Science alumina ammonia animal arising atmosphere become Cambridge carbonic acid chalk CHAPTER character chemical clay climate clover composition contain corn Crown 8vo cultivation decay desirable dormant matter double silicates duty ELEMENTARY TREATISE English Eton College Extra fcap fact farm farm-yard manure farmer favourable feeding fermentation fertilising matter fertility flesh-forming frost Greek green manures growing crop grown growth Hence herbage HISTORY important influence irrigation J. P. MAHAFFY John's College land late Fellow LATIN LESSONS marl materials mechanical condition mineral matter moisture necessary nitrogenous nitrogenous matter numerous Illustrations oats organic matter Owens College phosphate phosphoric acid plant plant-food ploughed portion potash practice preparation produced Professor quantity R. C. JEBB rendered revised rocks roots sand School secure seed silicates soil soluble straw substances success superphosphate supply surface takes place tillage tion Trinity College turnips valuable wheat whilst wurzel
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