FREE BOOKS

Author's List




PREV.   NEXT  
|<   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   >>  
feet. Those of the second class are of crystallised limestone, and vary in height from one hundred to five hundred feet. The hills on these are not so wild or broken as those of the first class, but are richly clothed with vegetation, and very beautiful. I have no doubt that the Coral Island on which you were wrecked was one of this class. They are supposed to have been upheaved from the bottom of the sea by volcanic agency; but they are not themselves volcanic in their nature, neither are they of coral formation. Those of the third class are the low coralline islands, usually having lagoons of water in their midst. They are very numerous. "As to the manner in which coral islands and reefs are formed, there are various opinions on this point. I will give you what seems to me the most probable theory--a theory, I may add, which is held by some of the good and scientific missionaries. It is well known that there is much lime in salt water; it is also known that coral is composed of lime. It is supposed that the polypes, or coral insects, have the power of attracting this lime to their bodies, and with this material they build their little cells or habitations. They choose the summit of a volcano, or the top of a submarine mountain, as a foundation on which to build, for it is found that they never work at any great depth below the surface. On this they work. The polypes on the mountain-top, of course, reach the surface first; then those at the outer edges reach the top sooner than the others between them and the centre, thus forming the coral reef surrounding the lagoon of water and the central island. After that, the insects within the lagoon cease working. When the surface of the water is reached, these myriads of wonderful creatures die. Then birds visit the spot, and seeds are thus conveyed thither, which take root and spring up and flourish. Thus are commenced those coralline islets of which you have seen so many in these seas. The reefs round the large islands are formed in a similar manner. When we consider," added the missionary, "the smallness of the architects used by our heavenly Father in order to form those lovely and innumerable islands, we are filled with much of that feeling which induced the ancient king to exclaim, `How manifold, O Lord, are Thy works! in wisdom hast Thou made them all.'" We all heartily agreed with the missionary in this sentiment, and felt not a little gratified to
PREV.   NEXT  
|<   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   >>  



Top keywords:
islands
 

surface

 

theory

 
manner
 
volcanic
 
coralline
 

formed

 

lagoon

 

missionary

 

insects


mountain
 
polypes
 

supposed

 

hundred

 

commenced

 

conveyed

 

thither

 

spring

 

flourish

 

myriads


surrounding
 

limestone

 

forming

 
height
 

centre

 
central
 
island
 

reached

 

islets

 

wonderful


crystallised

 

working

 
creatures
 
manifold
 

ancient

 
exclaim
 

wisdom

 

sentiment

 

gratified

 

agreed


heartily

 

induced

 
feeling
 

smallness

 
similar
 
architects
 

lovely

 

innumerable

 
filled
 

heavenly