FREE BOOKS

Author's List




PREV.   NEXT  
|<   185   186   187   188   189   190   191   192   193   194   195   196   197   198   199   200   201   202   203   204   205   206   207   208   209  
210   211   212   213   214   215   216   217   218   219   220   221   222   223   224   225   226   227   228   229   230   231   232   233   234   >>   >|  
and is sustained by the largest number of scientific men is that which traces volcanic effects back to the old accepted cause of internal fires in the center of the earth. Only in this way can the molten streams of lava emitted by volcanoes be accounted for. The youngest student of familiar science knows that heat generates an upward and outward force, and like all other forces that it follows the path of least resistance. This force is always present in the internal regions of the earth, which for ages upon ages has been gradually cooling from its poles toward its center. When conditions occur by which it can outwardly manifest itself, it follows the natural law and escapes where the crust of the earth is thinnest. But something more than the mere presence of internal fire is necessary to account for volcanic action, although it may in a large degree account for minor seismic convulsions in the form of an earthquake. The elements which enter into the source of volcanic eruption are fire and water. The characteristic phenomenon of a volcanic eruption is the steam which issues from the crater before the appearance of the molten lava, dust, ashes and scoria. This accepted theory is plainly illustrated in the eruption of a geyser, which is merely a small water volcano. The water basin of a geyser is connected by a natural bore with a region of great internal heat, and as fast as the heat turns the water into steam, columns of steam and hot water are thrown up from the crater. One form of volcanic eruption, and its simplest form, is likewise illustrated in a boiler explosion. Observations of the most violent volcanic eruptions show them to be only tremendous boiler explosions at a great depth beneath the earth's surface, where a great quantity of water has been temporarily imprisoned and suddenly converted into steam. In minor eruptions the presence of steam is not noticeable in such quantities, which is simply because the amount of imprisoned water was small and the amount of steam generated was only sufficient to expel the volcanic dust and ashes which formed between the earth's surface and the internal fires of the volcano. The flow of lava which follows violent eruptions is expelled by the outward and upward force of the great internal heat, through the opening made by the steam which precedes it. The two lines of volcanoes, one north and south, the other east and west, which intersect in the neighborhood of t
PREV.   NEXT  
|<   185   186   187   188   189   190   191   192   193   194   195   196   197   198   199   200   201   202   203   204   205   206   207   208   209  
210   211   212   213   214   215   216   217   218   219   220   221   222   223   224   225   226   227   228   229   230   231   232   233   234   >>   >|  



Top keywords:

volcanic

 

internal

 

eruption

 

eruptions

 

natural

 

presence

 

account

 

violent

 

surface

 
imprisoned

amount

 
boiler
 
crater
 

illustrated

 
geyser
 

volcano

 

upward

 

outward

 
accepted
 

volcanoes


molten

 

center

 

traces

 
sustained
 
tremendous
 

explosions

 

Observations

 

effects

 

beneath

 

likewise


region

 
columns
 

simplest

 

quantity

 

thrown

 

explosion

 

suddenly

 

precedes

 
opening
 

expelled


intersect
 
neighborhood
 

formed

 

noticeable

 

converted

 

quantities

 

simply

 
sufficient
 

generated

 
number