FREE BOOKS

Author's List




PREV.   NEXT  
|<   38   39   40   41   42   43   44   45   46   47   48   49   50   51   52   53   54   55   56   57   58   59   60   61   62  
63   64   65   66   67   68   69   70   71   72   73   74   75   76   77   78   79   80   81   82   83   84   85   86   87   >>   >|  
hich it was formed, is the foundation of Agricultural Geology. Geology may be briefly named the _science of rocks_. It would not be proper in an elementary work to introduce much of this study, and we will therefore simply state that the same kind of rock is of the same composition all over the world; consequently, if we find a soil in New England formed from any particular rock, and a soil from the same rock in Asia, their natural fertility will be the same in both localities. Some rocks consist of a mixture of different kinds of minerals; and some, consisting chiefly of one ingredient, are of different degrees of _hardness_. Both of these changes must affect the character of the soil, but it may be laid down as rule that, _when the rocks of two locations are exactly alike, the soils formed from them will be of the same natural fertility, and in proportion as the character of rocks changes, in the same proportion will the soils differ_. [What rule may be given in relation to soils formed from the same or different rocks? Are all soils formed from the rocks on which they lie? What instances can you give of this?] In most districts the soil is formed from the rock on which it lies; but this is not always the case. Soils are often formed by deposits of matter brought by water from other localities. Thus the alluvial banks of rivers consist of matters brought from the country through which the rivers have passed. The river Nile, in Egypt, yearly overflows its banks, and deposits large quantities of mud brought from the uninhabited upper countries. The prairies of the West owe a portion of their soil to deposits by water. Swamps often receive the washings of adjacent hills; and, in these cases, their soil is derived from a foreign source. We might continue to enumerate instances of the relations between soils and the sources whence they originated, thus demonstrating more fully the importance of geology to the farmer; but it would be beyond the scope of this work, and should be investigated by scholars more advanced than those who are studying merely the _elements_ of agricultural science. The mind, in its early application to any branch of study, should not be charged with intricate subjects. It should master well the _rudiments_, before investigating those matters which should _follow_ such understanding. [In what light will plants and soils be regarded by those who understand them?] By pursuing the prop
PREV.   NEXT  
|<   38   39   40   41   42   43   44   45   46   47   48   49   50   51   52   53   54   55   56   57   58   59   60   61   62  
63   64   65   66   67   68   69   70   71   72   73   74   75   76   77   78   79   80   81   82   83   84   85   86   87   >>   >|  



Top keywords:

formed

 

brought

 
deposits
 

localities

 

natural

 

consist

 

fertility

 

character

 

rivers

 

matters


proportion
 
instances
 
science
 

Geology

 

relations

 

enumerate

 
continue
 

Agricultural

 

demonstrating

 

sources


originated
 

prairies

 

countries

 

quantities

 

uninhabited

 

portion

 

Swamps

 

importance

 

derived

 

foreign


adjacent
 

receive

 

washings

 

source

 

investigating

 

follow

 

rudiments

 

intricate

 

subjects

 

master


understanding
 

pursuing

 

understand

 

regarded

 

plants

 
charged
 

scholars

 

advanced

 

investigated

 

foundation