Home Archived February 20, 2019

Link to USGS home page
125 years of science for America 1879-2004
Sound Waves Monthly Newsletter - Coastal Science and Research News from Across the USGS
Home || Sections: Spotlight on Sandy | Fieldwork | Research | Outreach | Meetings | Awards | Staff & Center News | Publications || Archives


The Great Blue Hole of Belize

in this issue:
next story

aerial photograph of Lighthouse Reef Atoll Blue Hole
Blue Hole: Aerial view of the 400-ft-deep oceanic blue hole (Lighthouse Reef Atoll Blue Hole) located east of Belize.
People in Belize think it should be one of the seven wonders of the world. Dive boats visit it every day. It is protected by the Belize Audubon Society and is a Belize National Monument. It became a World Heritage site in 1997. Jacques Cousteau took the Calypso and his one-man submarines into the hole in 1972 to examine stalactites suspended from overhanging walls. The Great Blue Hole is surrounded by shallow water of Lighthouse Reef Atoll, a nearly perfect circle in the middle of a shallow reef. The atoll is located ~96 km east of the Belize mainland. It is not an easy place to reach.

In 1997, geologist Robert F. Dill and divers from the Cambrian Foundation, an organization of mixed-gas divers (also called tech divers), visited the Great Blue Hole to collect stalactites for isotopic dating and sea-level studies. Two divers descended 407 ft and obtained two short push cores. The 2-ft long cores revealed outstanding sedimentary laminations. There is no oxygen near the bottom, and hydrogen sulfide prevents bottom dwellers from burrowing and disturbing the sediment. Preliminary analyses of the short cores showed fluctuating pollen, spores, mercury, and arsenic levels. Arsenic ranges between 15 and 21 ppm. That's right! ppm as in parts per million. Other events recorded in the short cores included hurricane or large storm layers. The storm layers are light-colored, beautifully laminated, and are distinct from the darker organic and clay-rich sediments representing slow deposition. Could these sediments provide a long-term record of climate, mercury, arsenic, and African dust flux? We think so!

the crew on the bow of the R/V Winning Ticket
At work: A small crew was needed to deploy and recover the Rossfelder vibracoring system to and from a depth of 400 ft. All work took place from the bowsprit aboard the R/V Winning Ticket. From left to right: Chris Reich, Elizabeth Williams, Don Hickey, and Randy Migdalski. Chuck Holmes is in the wheelhouse.
There were a few hurdles to get over before sampling could begin, not to mention the proposal-to-funding process. Permits had to be obtained from the Bureau of Fisheries in Belize City along with permission from Audubon, which had to consult with the Department of Forestry. Former USF student Melanie McField, who represents the World Wildlife Fund in Belize City, made the permitting process easier. There was also collaboration with the American Embassy in Belize City, and last but not least, a suitable vessel had to be located and chartered.

On May 8th, Gene Shinn, Chuck Holmes, Chris Reich, and Don Hickey entered the deep blue hole aboard Winning Ticket, a 55-ft boat out of Miami operated by Captain Barry Denton with Randy Migdalski as First Mate. Winning Ticket traveled to Belize with the coring equipment where the USGS crew boarded for the final run out to the blue hole. Along the way, we picked up student/volunteer Elizabeth Williams who served as observer for Audubon during the sampling. Our purpose was to obtain long cores and hopefully a several-thousand-year record of dust flux. Coring was done with a Rossfelder electro-vibracoring system using 20-ft-long core tubes. We lowered the 300 lbs. of equipment to the bottom on a 500-ft length of rope from the bow of the boat. Cores and equipment were retrieved with the boat's electric anchor windlass and divers removed the cores from the apparatus at the surface. By the third and last day, we had obtained two 18-ft cores. In all, seven cores were recovered. Sound easy? Fieldwork is seldom easy. On this trip, the electric vibracoring equipment failed. But as luck would have it, First Mate Randy's other job is running an electric motor rewinding shop. In a few hours he rewired components and we were back in business. Thanks to Randy, we got the 18 footers.

Why this blue hole? The Belize Great Blue Hole is located far from industrial sources of aerosols but is well within the area affected by silica- and clay-bearing African soil dust. African dust is deposited in the Caribbean mainly between June and October. The hole thus serves as a giant sediment trap where the overall sedimentation rate is slow and layering is preserved due to anoxic conditions. A high rate of atmospheric deposition relative to normal shallow-marine sedimentation should make it easier to identify and separate African soil dust from local carbonate mud. If all goes as planned, these cores will provide the centerpiece of a study aimed at determining the geologic history of dust deposition over the past few thousand years. Stay Tuned!

Related Web Sites
Coral Mortality and African Dust Project
U.S. Geological Survey (USGS)

in this issue:
next story


Mailing List:

in this issue: Fieldwork cover story:
Great Blue Hole of Belize

Channel Islands Cruise

Lake Mead Mapping

Research New Underwater Microscope System

Hurricane Display

Outreach Reston Open House

WHFC Outreach

Monterey Open House

School-to-Work Partnership

Acadiana Migratory Bird Day

Meetings SWICA-M³

Global Assessment of Geologically-Sourced Methane

Methane Hydrates

Metadata Workshop

Awards Sue Hunt—Recycling

Coastal Stewardship

GIS 2001: Logan

GIS 2001: Massachusetts Bay

Staff & Center News WHFC Visitors

Publications Northeast Earthquake Hazards Map

June Publications List

FirstGov.gov U. S. Department of the Interior | U.S. Geological Survey
Sound Waves Monthly Newsletter

email Feedback | USGS privacy statement | Disclaimer | Accessibility

This page is http://soundwaves.usgs.gov/2001/06/index.html
Updated December 02, 2016 @ 12:09 PM (THF)