FREE BOOKS

Author's List




PREV.   NEXT  
|<   352   353   354   355   356   357   358   359   360   361   362   363   364   365   366   367   368   369   370   371   372   373   374   375   376  
377   378   379   380   381   382   383   384   385   386   387   388   389   390   391   392   393   394   395   396   >>  
et below they die. But now suppose that the land sinks very gradually indeed. Let it subside by slow degrees, until the mountain peak, which we have in the middle of it, alone projects beyond the sea level. The fringing reef would be carried down also; but we suppose that the sinking is so slow that the coral polypes are able to grow up as fast as the land is carried down; consequently they will add layer upon layer until they form a deep cup, because the inner part of the reef grows much more slowly than the outer part. Thus you have the reef forming a bed thicker upon the flanks of the island; but the edge of the reef will be very much further out from the land, and the lagoon will be many times deeper; in short, your fringing reef will be converted into an encircling reef. And if, instead of this being an island, it were a great continent like Australia, then you will have the phenomenon of a barrier reef which I have described. The barrier reef of Australia was originally a fringing reef; the land has gone slowly down; the consequence is the lagoon has deepened until its depth is now 25 fathoms and the corals have grown up at the outer edge until you have that prodigious accumulation which forms the barrier reef at present. Now let this process go on further still; let us take the land a further step down, so as to submerge even the peak. The coral, still growing up, will cover the surface of the land, and you will have an atoll reef; that is to say, a more or less circular or oval ring of coral rock with a lagoon in the middle. Thus you see that every peculiarity and phenomenon of these different forms of coral reef was explained at once by the simplest of all possible suppositions, namely, by supposing that the land has gone down at a rate not greater than that at which the coral polypes have grown up. You explain a Fringing Reef as a reef which is formed round land comparatively stationary; an Encircling Reef as one which is formed round land going down; and an Atoll as a reef formed upon land gone down; and the thing is so simple that a child may understand it when it is once explained. But this would by no means satisfy the conditions of a scientific hypothesis. No man who is cautious would dream of trusting to an explanation of this kind simply because it explained one particular set of facts. Before you can possibly be safe in dealing with Nature--who is very properly made of the feminine gender, on account o
PREV.   NEXT  
|<   352   353   354   355   356   357   358   359   360   361   362   363   364   365   366   367   368   369   370   371   372   373   374   375   376  
377   378   379   380   381   382   383   384   385   386   387   388   389   390   391   392   393   394   395   396   >>  



Top keywords:

fringing

 

lagoon

 
barrier
 

explained

 

formed

 

island

 

slowly

 

Australia

 

phenomenon

 

suppose


middle

 
polypes
 
carried
 

simplest

 
properly
 
Nature
 

dealing

 

supposing

 

possibly

 

suppositions


peculiarity

 

circular

 

account

 

gender

 

feminine

 

explain

 

explanation

 

understand

 

trusting

 
conditions

scientific

 

satisfy

 
surface
 

cautious

 

simply

 
Before
 

Fringing

 
hypothesis
 

greater

 
comparatively

simple

 

stationary

 

Encircling

 
forming
 

flanks

 

thicker

 
subside
 

gradually

 

degrees

 
mountain