FREE BOOKS

Author's List




PREV.   NEXT  
|<   13   14   15   16   17   18   19   20   21   22   23   24   25   26   27   28   29   30   31   32   33   34   35   36   37  
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   >>   >|  
he foundations of the great mountains, in this way are gigantic beyond measurement. This folding of the earth's crust is caused by the fact that the "crust," or skin of the earth, has ceased to cool, being warmed by the sun, and therefore does not shrink, whilst the great white-hot mass within (in comparison with which the twenty-mile-thick crust is a mere film) continually loses heat, and shrinks definitely in volume as its temperature sinks. The crust or jacket of stratified rock deposited by the action of the waters on the surface of the globe has been compelled--at whatever cost, so to speak--to fit itself to the diminishing "core" on which it lies. Slowly, but steadily, this "settlement" has gone on, and is going on. The horizontal rock layers, being now too great in length and breadth, adjust themselves by "buckling"--just as a too large, ill-fitting dress does--and the Alps, the Himalayas, and other great mountain ranges, are regions where this "buckling" process has for countless ages proceeded, slowly but surely. Probably the "buckling" has proceeded to a large extent without sudden movement, but with a lateral pressure of such power as ultimately to throw a crust of thousands of feet thickness into deep folds a mile or so in vertical measurement from crest to hollow, protruding from the general level both upwards and downwards, whilst often the folds are rolled over on to each other. [Illustration: Fig. 3.--Diagrams to show the "folding" of rock strata. A. Normal horizontal position of the strata, _a_, _b_, _c_, _d_; _xy_, horizontal line. B. Folding due to a shortening of the horizontal _xy_ by lateral pressure, acting in the direction of the arrow and due to shrinkage. C. More extreme case of folding, in which a raised ridge is made to fall over so as to bring the lowest layer _d_ above _a_, _b_ and _c_.] This crumbling and folding has gone on at great depths--that is to say, some miles below the surface (a mere nothing compared with the 8,000 miles diameter of the globe itself), though we now see the results exposed, like the pastry folded by a cook. Immense time has been taken in the process. A folding movement involving a vertical rise of an inch in ten years would not be noticed by human onlookers, but in 600,000 years this would give you a vertical displacement of more than 5,000 ft. (nearly a mile!). It has been shown that in Switzerland, along a line of country extending from Basle to Milan, stra
PREV.   NEXT  
|<   13   14   15   16   17   18   19   20   21   22   23   24   25   26   27   28   29   30   31   32   33   34   35   36   37  
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   >>   >|  



Top keywords:

folding

 

horizontal

 

vertical

 
buckling
 

surface

 

proceeded

 

pressure

 

lateral

 

strata

 
movement

process

 

whilst

 

measurement

 
Folding
 

Immense

 

shortening

 

acting

 

extreme

 

shrinkage

 

direction


Switzerland

 

Illustration

 
rolled
 

extending

 

position

 

Normal

 

Diagrams

 
country
 

raised

 
noticed

diameter
 

compared

 
results
 

exposed

 
folded
 

pastry

 

onlookers

 

lowest

 

involving

 

displacement


depths

 

crumbling

 

slowly

 

volume

 

temperature

 

shrinks

 

continually

 

jacket

 
stratified
 

diminishing