Link to USGS home page
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

 
Fieldwork

Gravity Coring Offshore Puerto Rico and the U.S. Virgin Islands to Investigate the Timing of Submarine Landslides and Large Earthquakes


in this issue:
 previous story | next story

Recent analysis of the destructive 1918 tsunami that devastated western Puerto Rico has shown that the tsunami was likely caused by a large (10-km3 volume) earthquake-induced submarine landslide in the Mona Passage west of Puerto Rico. Many landslides have also been mapped along the edge of the submerged carbonate platform about 40 km seaward of the north shore of Puerto Rico. Volume analysis and hydrodynamic modeling indicate that at least eight of these submarine landslides could have caused damaging tsunamis; however, because the age of these landslides is unknown, their recurrence interval could not be estimated.

Caribbean region, showing approximate location of study area
Above: Caribbean region, showing approximate location of study area (shaded box). [larger version]

The goal of a recent USGS research cruise was to core and date submarine-landslide-related sediment north of Puerto Rico in order to determine the age of these landslides. Dating of these landslides is needed in order to calculate tsunami probability for the north coast of Puerto Rico. Another coring target of the cruise was the Virgin Islands Basin, the epicenter of the devastating 1867 earthquake and tsunami. There we focused on dating disturbances in the sedimentary layers caused by ground shaking, in hopes of extending the area's earthquake record backward in time. A long earthquake record is needed to adequately estimate the probability of additional earthquakes in the area in the near future.

Coring was carried out aboard the Harbor Branch Oceanographic Institution's research vessel (R/V) Seward Johnson during a 9-day cruise from March 16 to 24, 2008, leaving from and returning to San Juan, Puerto Rico. Cores were collected with the Woods Hole Oceanographic Institution (WHOI)'s Giant Gravity Corer, a 4-in.-diameter pipe, suspended from a cable, that penetrates the sea floor under its own weight and can collect cores as long as 6.5 m. In this cruise, many of the coring sites were expected to have a relatively hard sandy bottom, which is difficult to penetrate, and so we rigged the corer for a maximum core length of only 3 m.

Study area, showing locations of coring stations (yellow dots) occupied during the cruise.
Above: Study area, showing locations of coring stations (yellow dots) occupied during the cruise. Stations north of Puerto Rico are within and at the base of landslide scarps and deposits; stations southeast of Puerto Rico are within basins that may hold evidence of earthquake shaking. [larger version]

A total of 40 coring sites were occupied during the cruise—within Mona Canyon, on the south wall and floor of the Puerto Rico Trench, and in the Virgin Island, Vieques, and Whiting Basins south of the U.S. Virgin Islands—with site depths ranging from 1,350 m down to 8,000 m. Coring sites were chosen on the basis of multibeam bathymetry and seismic-reflection data collected by the USGS on several recent cruises in the northeastern Caribbean (for example, see "New Bathymetric Map of Mona Passage, Northeastern Caribbean, Aids in Earthquake and Tsunami-Hazard Mitigation," Sound Waves, May 2007), as well as GLORIA sidescan-sonar data (URL http://pubs.usgs.gov/dds/dds15/).

Just 2 days after we left port, the worst storm of Puerto Rico's winter arrived, generating 16-ft swells along the north side of the island, closing San Juan harbor for 3 days, and forcing the ship to seek shelter along the south side of the island. In spite of these conditions, the dedication and efforts of the science team and Captain George Gunther and the crew of the R/V Seward Johnson resulted in the recovery of more than 24 m of sediment from 21 of the 40 coring sites. The cores are now undergoing nondestructive testing, including multisensor core logging (MSCL), X-ray fluorescence (XRF), and lithologic logging, after which the sediment above and below submarine-landslide-debris deposits will be sampled for 14C radiometric dating.

Matt Arsenault and Jim Broda recover the Giant Gravity Corer Emily Himmelstoss, Kate McMullen, Brian Buczkowski, and Jason Chaytor prepare a recovered core for transport and storage Brown Boobies accompanying the Research Vessel Seward Johnson
Above left: Matt Arsenault (USGS, left) and Jim Broda (WHOI) recover the Giant Gravity Corer aboard the R/V Seward Johnson after deployment of the corer into the Mona Canyon. Photograph by Uri ten Brink (USGS). [larger version]

Above center: Emily Himmelstoss (USGS, right), Kate McMullen (USGS, bottom), Brian Buczkowski (USGS, middle), and Jason Chaytor (WHOI, top) prepare a recovered core for transport and storage by cutting the core liner at the top of the sediment. Inset, dark gray mud at the bottom of one core. Photographs by Sandy Baldwin (USGS). [larger version]

Above right: Brown Boobies (Sula leucogaster) accompanying the R/V Seward Johnson during transit between Vieques and St. John on the way to coring stations on the north side of Puerto Rico. Photograph by Sandy Baldwin (USGS). [larger version]

Participants in the cruise included Matt Arsenault, Sandy Baldwin, Brian Buczkowski, Michael Casso, Claudia Flores, Emily Himmelstoss, Kate McMullen, and Uri ten Brink from the USGS Woods Hole Science Center, Jason Chaytor (chief scientist, WHOI-USGS Postdoctoral Scholar), and Jim Broda (coring specialist, WHOI).

For additional information about submarine landslides and tsunamis in the Caribbean region, see:

  • López-Venegas, A.M., ten Brink, U.S., and Geist, E.L., in press, Submarine landslide as the source for the October 11, 1918 Mona Passage tsunami; observations and modeling: Marine Geology, doi:10.1016/j.margeo.2008.05.001 [URL http://www.sciencedirect.com/science/journal/00253227].

  • ten Brink, U.S., Geist, E.L., Lynett, P., and Andrews, B.D., 2006, Submarine slides north of Puerto Rico and their tsunami potential, in Mercado-Irizarry, A., and Liu, P., eds., Caribbean tsunami hazard: Singapore, World Scientific Publishers, p. 67-90 [URL http://www.worldscibooks.com/engineering/5969.html].

  • ten Brink, U.S., Geist, E.L., and Andrews, B.D., 2006, Size distribution of submarine landslides and its implication to tsunami hazard in Puerto Rico: Geophysical Research Letters, v. 33, L11307, doi:10.1029/2006GL026125 [URL http://www.agu.org/pubs/crossref/2006/2006GL026125.shtml].


Related Sound Waves Stories
New Bathymetric Map of Mona Passage, Northeastern Caribbean, Aids in Earthquake and Tsunami-Hazard Mitigation
May 2007
Joint Spanish-United States Cruise Investigates Tsunami and Earthquake Hazards in the Northeastern Caribbean
June 2005
Workshop Addresses Tsunami Hazard to Puerto Rico, the Virgin Islands, and Other Caribbean Islands
June 2004

Related Web Sites
CD-ROM Atlas of the Deepwater Parts of the U.S. Exclusive Economic Zone in the Atlantic Ocean, the Gulf of Mexico, and the Eastern Caribbean Sea - USGS Digital Data Series 15
USGS (U.S. Geological Survey)

in this issue:
 previous story | next story

 

Mailing List:


print this issue print this issue

in this issue:

Fieldwork
cover story:
Palos Verdes Shelf Experiment: Contaminated Mud

Palos Verdes Shelf Experiment: Whatever Can Go Wrong

Submarine Landslides and Large Earthquakes

Research
Whitings Possible Explanation for Middle East Oil Deposits

Outreach
USGS Participates in Marine Quest 2008

Law of the Sea Studies

Meetings USGS/DOI Santa Barbara Channel Workshop

USGS Part of Law of the Sea Delegation

Carolinas Coastal Change Processes Project

Awards USGS Circular Wins Blue Pencil Award

Publications

July 2008 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/2008/07/fieldwork3.html
Updated April 15, 2014 @ 01:53 PM (JSS)