The Great Bahama Bank, from which rise the low coral-built Andros
Islands and a large number of crags and rocks, measures about 360
geographical miles from southeast to northwest, and has a width of
approximately 200 geographical miles. Throughout its entire submerged
portion the water is less than 100, and over much of the area less than
10 fathoms deep. It is invaded and given an irregular shape, however, by
a "tongue of the ocean" which curves in from the northward, in which
soundings of from 700 to 1,000 fathoms have been obtained. To the north
of the Great Bahama Bank, and separated from it by water nearly 2,000
fathoms deep, is the Little Bahama Bank, measuring 50 by 150
geographical miles, from which rises the low islands known as Great
Bahama, Great Abaco, and a multitude of islets and crags, while beneath
the water, as is the case also on the greater submarine plateau to the
south, there are numerous shoals. Southeast from the Great Bahama Bank,
and in a general view to be classed with it, are several other shallow
areas in the sea, of similar character, and with numerous islands and
reefs rising from them. The southeastern terminus of this series of
plateaus, the surfaces of which have been built up practically to the
level of the surface of the sea, is the Navidad Bank, situated about 50
miles to the north of the eastern end of the island of Santo Domingo
(Haiti) and forms the west border of Brownson Deep. The length of the
series of banks to the north of the Greater Antilles is about 800, and
its average width 120 geographical miles.
Public-domain text, read in full here on John Shaqi.
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