470 BARRIEK-REEFS. [chaf. xx 



wall sometimes between two and three hundred feet under water 

 in height : externally the reef rises, like an atoll, with extreme 

 abruptness out of the profound depths of the ocean. What can 

 be more singular tlian these structures? We see an island, 

 which may be compared to a castle situated on the summit of a 

 lofty submarine mountain, protected by a great wall of coral - 

 rock, always steep externally and sometimes internally, with a 

 broad level summit, here and there breached by narrow gate- 

 ways, through which the largest ships can enter the wide and 

 deep encircling moat. 



As far as the actual reef of coral is concerned, there is not the 

 smallest difference, in general size, outline, grouping, and even 

 in quite trifling details of structure, between a barrier and an 

 atoll. The geographer Balbi has well remarked, that an encircled 

 island is an atoll with high land rising out of its lagoon ; remove 

 the land from within, and a perfect atoll is left. 



But what has caused these reefs to spring up at such great 

 distances from the shores of the included islands? It cannot be 

 that the corals will not grow close to the land ; for the shores 

 within the lagoon-channel, when not surrounded by alluvial soil, 

 are often fringed by living reefs ; and we shall presently see 

 that there is a whole class, which I have called Fringing Reefs 

 from their close attachment to the shores both of continents and 

 of islands. Again, on what have the reef-building corals, which 

 cannot live at great depths, based their encircling structures ? 

 This is a great apparent difficulty, analogous to that in the case 

 of atolls, which has generally been overlooked. It will be per- 

 ceived more clearly by inspecting the following sections, which 

 are real ones, taken in north and south lines, through the islands 

 with their barrier-reefs, of Vanikoro, Gambler, and Maurua ; 

 and they are laid down, both vertically and horizontally, on the 

 same scale of a quarter of an inch to a mile. 



It should be observed that the sections might have been taken 

 iii any direction through these islands, or through many other 

 encircled islands, and the general features would have been the 

 same. Now bearing in mind that reef-building coral cannot 

 live at a greater depth than from 20 to 30 fathoms, and that the 

 scale is so small that the plummets on the right hand sliow a 

 depth of 200 fathoms, on what are these barrier-reefs based? 



