Origin of the Belize Atolls
"Lighthouse Reef, Glover's Reef and the Turneffe Islands are all distinct
anomalies in the Caribbean. Nothing else in the Western Hemisphere resembles a
true coral atoll, except perhaps Chinchorro Reef, off Mexico's southern Yucatan
Peninsula (just above the Belize atolls). According to geologists they are even
more unusual in that the origin of their formation does not seem to mirror the
atolls of the Pacific Ocean, where rings of coral are better known.
The ancient
processes contributing to Belize atoll development may have begun as many as 70
million years ago and the atolls did not develop around subsiding volcanoes.
Instead, they originated atop giant fault blocks; limestone covered ridges that
settled in steps, providing a series of offshore platforms for coral growth.
After the last ice age, with the slow rise of sea level, coral growth continued
upward, creating the precipitous outer walls and the shallow inside lagoon that
typifies these distinct formations. Many drop-offs surrounding the Belize atolls
are thousands of feet deep, while depths in the shallow lagoons average 10 to 30
feet.