Beagle Expedition (1831-1836); Coral reefs and islands; Geology -- South America; Islands; Volcanoes
very few in number and of insignificant dimensions. Lastly, some reefs
are left uncoloured from the want of information respecting them, and
some because they are of an intermediate structure between the barrier
and fringing classes. The value of the map is lessened, in proportion
to the number of reefs which I have been obliged to leave uncoloured,
although, in a theoretical point of view, few of them present any great
difficulty: but their number is not very great, as will be found by
comparing the map with the statements in the Appendix. I have
experienced more difficulty in colouring fringing-reefs than in
colouring barrier-reefs, as the former, from their much less
dimensions, have less attracted the attention of navigators. As I have
had to seek my information from all kinds of sources, and often from
indirect ones, I do not venture to hope that the map is free from many
errors. Nevertheless, I trust it will give an approximately correct
view of the general distribution of the coral-reefs over the whole
world (with the exception of some fringing-reefs on the coast of
Brazil, not included within the limits of the map), and of their
arrangement into the three great classes, which, though necessarily
very imperfect from the nature of the objects classified, have been
adopted by most voyagers. I may further remark, that the dark blue
colour represents land entirely composed of coral-rock; the pale blue,
land with a wide and thick border of coral-rock; and the red, a mere
narrow fringe of coral-rock.
Public-domain text, read in full here on John Shaqi.
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