I support technical staff on various projects that need expertise in earthquake seismology, active source seismic processing both on land and marine and general geophysics such as gravity and magnetics. I have also done some work as a protected species observer (PPO). Finally, I provide Spanish translation for project support when needed.
Science and Products
Significant Earthquakes on a major fault system in Hispaniola, Puerto Rico, the Virgin Islands, and the Lesser Antilles, 1500–2010: Implications for Seismic Hazard
Caribbean Tsunami and Earthquake Hazards Studies- Models
Caribbean Tsunami and Earthquake Hazards Studies- Stress Changes and Earthquake Hazard
Caribbean Tsunami and Earthquake Hazards Studies-Tsunami Potential
Caribbean Tsunami and Earthquake Hazards Studies- Seafloor Map
Caribbean Tsunami and Earthquake Hazards Studies
Crustal structure across the central Dead Sea Transform and surrounding areas: Insights into tectonic processes in continental transforms
Seafloor observations eliminate a landslide as the source of the 1918 Puerto Rico Tsunami
Observations of seismicity and ground motion in the northeast U.S. Atlantic margin from ocean bottom seismometer data
Significant earthquakes on the Enriquillo fault system, Hispaniola, 1500-2010: Implications for seismic hazard
Historical records indicate frequent seismic activity along the north-east Caribbean plate boundary over the past 500 years, particularly on the island of Hispaniola. We use accounts of historical earthquakes to assign intensities and the intensity assignments for the 2010 Haiti earthquakes to derive an intensity attenuation relation for Hispaniola. The intensity assignments and the attenuation re
Accounts of damage from historical earthquakes in the northeastern Caribbean to aid in the determination of their location and intensity magnitudes
Earthquakes have been documented in the northeastern Caribbean since the arrival of Columbus to the Americas; written accounts of these felt earthquakes exist in various parts of the world. To better understand the earthquake cycle in the Caribbean, the records of earthquakes in earlier catalogs and historical documents from various archives, which are now available online, were critically examine
Geometry and subsidence history of the Dead Sea basin: A case for fluid-induced mid-crustal shear zone?
Historical perspective on seismic hazard to Hispaniola and the northeast Caribbean region
We evaluate the long-term seismic activity of the North-American/Caribbean plate boundary from 500 years of historical earthquake damage reports. The 2010 Haiti earthquakes and other earthquakes were used to derive regional attenuation relationships between earthquake intensity, magnitude, and distance from the reported damage to the epicenter, for Hispaniola and for Puerto Rico and the Virgin Isl
Science and Products
- Science
Significant Earthquakes on a major fault system in Hispaniola, Puerto Rico, the Virgin Islands, and the Lesser Antilles, 1500–2010: Implications for Seismic Hazard
Earthquakes have been documented in the northeastern Caribbean since the arrival of Columbus to the Americas; written accounts of these felt earthquakes exist in various parts of the world. To better understand the earthquake cycle in the Caribbean, the records of earthquakes in earlier catalogs and historical documents from various archives, which are now available online, were critically...Caribbean Tsunami and Earthquake Hazards Studies- Models
The Puerto Rico trench exhibits great water depth, extremely low gravity anomaly, and a tilted carbonate platform between (reconstructed) elevations of +1300 m and -4000 m. we suggest that these features are manifestations of large vertical movements of a segment of the Puerto Rico Trench, its forearc, and the island of Puerto Rico that took place 3.3 m.y. ago over a time period as short as 14-40...Caribbean Tsunami and Earthquake Hazards Studies- Stress Changes and Earthquake Hazard
Strike-slip faults in the forearc region of a subduction zone often present significant seismic hazard because of their proximity to population centers. We explore the interaction between thrust events on the subduction interface and strike-slip faults within the forearc region using 3-D models of static Coulomb stress change.Caribbean Tsunami and Earthquake Hazards Studies-Tsunami Potential
Newly-acquired multibeam bathymetry of the entire Puerto Rico trench reveals numerous retrograde slope failures at various scales at the edge of the carbonate platform north of Puerto Rico and the Virgin Islands. The slumped material comprises carbonate blocks, which are cohesive and the edge of the carbonate platform is steeper than most continental slopes, resulting in a higher potential runup...Caribbean Tsunami and Earthquake Hazards Studies- Seafloor Map
To help understand the origin of the unusual bathymetry, gravity, and vertical tectonics of the plate boundary and to provide constraints for hazard assessment, the morphology of the entire 770-km-long trench from the Dominican Republic in the west to Anguilla in the east was mapped with multibeam echosounder during three cruises in 2002 and 2003. Parts of the Puerto Rico Trench were previously...Caribbean Tsunami and Earthquake Hazards Studies
Puerto Rico and the Virgin Islands are located at an active plate boundary between the North American plate and the northeast corner of the Caribbean plate. Plate movements have caused large magnitude earthquakes and devastating tsunamis. The USGS has an ongoing program to identify and map the faults in this region using various geophysical and geological methods in order to estimate the location... - Publications
Crustal structure across the central Dead Sea Transform and surrounding areas: Insights into tectonic processes in continental transforms
New geophysical profiles across the central Dead Sea Transform (DST) near the Sea of Galilee, Israel, and surrounding highlands, augmented by static stress modeling, allow us to study continental transform plate deformation. The DST separates a ∼10 km thick sedimentary column above a thinned (16–23 km) crust to the west from a ∼7 km column above a ∼30-km thick crust to the east. Crustal thinning sAuthorsUri S. ten Brink, Eldad Levi, Claudia Flores, Ivan Koulakov, Nadav Bronshtein, Zvi Ben-AvrahamSeafloor observations eliminate a landslide as the source of the 1918 Puerto Rico Tsunami
The 11 October 1918 devastating tsunami in northwest Puerto Rico had been used as an example for earthquake‐induced landslide tsunami hazard. Three pieces of evidence pointed to a landslide as the origin of the tsunami: the discovery of a large submarine landslide scar from bathymetry data collected by shipboard high‐resolution multibeam sonar, reported breaks of submarine cable within the scar, aAuthorsUri S. ten Brink, Jason Chaytor, Claudia Flores, Yong Wei, Simon Detmer, Lilian Lucas, Brian D. Andrews, Aggeliki GeorgiopoulouObservations of seismicity and ground motion in the northeast U.S. Atlantic margin from ocean bottom seismometer data
Earthquake data from two short-period ocean-bottom seismometer (OBS) networks deployed for over a year on the continental slope off New York and southern New England were used to evaluate seismicity and ground motions along the continental margin. Our OBS networks located only one earthquake of Mc∼1.5 near the shelf edge during six months of recording, suggesting that seismic activity (MLg>3.0) ofAuthorsClaudia Flores, Uri S. ten Brink, Jeffrey J. McGuire, John A. CollinsSignificant earthquakes on the Enriquillo fault system, Hispaniola, 1500-2010: Implications for seismic hazard
Historical records indicate frequent seismic activity along the north-east Caribbean plate boundary over the past 500 years, particularly on the island of Hispaniola. We use accounts of historical earthquakes to assign intensities and the intensity assignments for the 2010 Haiti earthquakes to derive an intensity attenuation relation for Hispaniola. The intensity assignments and the attenuation re
AuthorsWilliam H. Bakun, Claudia H. Flores, Uri S. ten BrinkAccounts of damage from historical earthquakes in the northeastern Caribbean to aid in the determination of their location and intensity magnitudes
Earthquakes have been documented in the northeastern Caribbean since the arrival of Columbus to the Americas; written accounts of these felt earthquakes exist in various parts of the world. To better understand the earthquake cycle in the Caribbean, the records of earthquakes in earlier catalogs and historical documents from various archives, which are now available online, were critically examine
AuthorsClaudia H. Flores, Uri S. ten Brink, William H. BakunGeometry and subsidence history of the Dead Sea basin: A case for fluid-induced mid-crustal shear zone?
Pull‐apart basins are narrow zones of crustal extension bounded by strike‐slip faults that can serve as analogs to the early stages of crustal rifting. We use seismic tomography, 2‐D ray tracing, gravity modeling, and subsidence analysis to study crustal extension of the Dead Sea basin (DSB), a large and long‐lived pull‐apart basin along the Dead Sea transform (DST). The basin gradually shallows sAuthorsUri S. ten Brink, C.H. FloresHistorical perspective on seismic hazard to Hispaniola and the northeast Caribbean region
We evaluate the long-term seismic activity of the North-American/Caribbean plate boundary from 500 years of historical earthquake damage reports. The 2010 Haiti earthquakes and other earthquakes were used to derive regional attenuation relationships between earthquake intensity, magnitude, and distance from the reported damage to the epicenter, for Hispaniola and for Puerto Rico and the Virgin Isl
AuthorsUri S. ten Brink, W. H. Bakun, C.H. Flores