Uri ten Brink, PhD (Former Employee)
Science and Products
Filter Total Items: 150
Event sedimentation in low-latitude deep-water carbonate basins, Anegada passage, northeast Caribbean Event sedimentation in low-latitude deep-water carbonate basins, Anegada passage, northeast Caribbean
The Virgin Islands and Whiting basins in the Northeast Caribbean are deep, structurally controlled depocentres partially bound by shallow-water carbonate platforms. Closed basins such as these are thought to document earthquake and hurricane events through the accumulation of event layers such as debris flow and turbidity current deposits and the internal deformation of deposited...
Authors
Jason D. Chaytor, Uri S. ten Brink
Assessment of tsunami hazard to the U.S. Atlantic margin Assessment of tsunami hazard to the U.S. Atlantic margin
Tsunami hazard is a very low-probability, but potentially high-risk natural hazard, posing unique challenges to scientists and policy makers trying to mitigate its impacts. These challenges are illustrated in this assessment of tsunami hazard to the U.S. Atlantic margin. Seismic activity along the U.S. Atlantic margin in general is low, and confirmed paleo-tsunami deposits have not yet...
Authors
Uri S. ten Brink, Jason Chaytor, Eric L. Geist, Daniel S. Brothers, Brian D. Andrews
A framework for the probabilistic analysis of meteotsunamis A framework for the probabilistic analysis of meteotsunamis
A probabilistic technique is developed to assess the hazard from meteotsunamis. Meteotsunamis are unusual sea-level events, generated when the speed of an atmospheric pressure or wind disturbance is comparable to the phase speed of long waves in the ocean. A general aggregation equation is proposed for the probabilistic analysis, based on previous frameworks established for both tsunamis...
Authors
Eric L. Geist, Uri S. ten Brink, Matthew D. Gove
Seabed fluid expulsion along the upper slope and outer shelf of the U.S. Atlantic continental margin Seabed fluid expulsion along the upper slope and outer shelf of the U.S. Atlantic continental margin
Identifying the spatial distribution of seabed fluid expulsion features is crucial for understanding the substrate plumbing system of any continental margin. A 1100 km stretch of the U.S. Atlantic margin contains more than 5000 pockmarks at water depths of 120 m (shelf edge) to 700 m (upper slope), mostly updip of the contemporary gas hydrate stability zone (GHSZ). Advanced attribute...
Authors
D.S. Brothers, C. Ruppel, J.W. Kluesner, Uri S. ten Brink, J.D. Chaytor, J. C. Hill, B.D. Andrews, C. Flores
Slope failures and timing of turbidity flows north of Puerto Rico Slope failures and timing of turbidity flows north of Puerto Rico
The submerged carbonate platform north of Puerto Rico terminates in a high (3,000–4,000 m) and in places steep (>45°) slope characterized by numerous landslide scarps including two 30–50 km-wide amphitheater-shaped features. The origin of the steep platform edge and the amphitheaters has been attributed to: (1) catastrophic failure, or (2) localized failures and progressive erosion...
Authors
Uri S. ten Brink, Jason D. Chaytor
Bathymetric Terrain Model of the Puerto Rico Trench and the Northeastern Caribbean Region for Marine Geological Investigations Bathymetric Terrain Model of the Puerto Rico Trench and the Northeastern Caribbean Region for Marine Geological Investigations
Multibeam bathymetry data collected in the Puerto Rico Trench and Northeast Caribbean region are compiled into a seamless bathymetric terrain model for broad-scale geological investigations of the trench system. These data, collected during eight separate surveys between 2002 and 2013, covering almost 180,000 square kilometers are published here in large format map sheet and digital...
Authors
Brian D. Andrews, Uri S. ten Brink, William W. Danforth, Jason D. Chaytor, J Granja-Bruna, A Carbo-Gorosabel
Seismic hazard from the Hispaniola subduction zone: correction to "Historical perspective on seismic hazard to Hispaniola and the northeast Caribbean region" Seismic hazard from the Hispaniola subduction zone: correction to "Historical perspective on seismic hazard to Hispaniola and the northeast Caribbean region"
No abstract available
Authors
Uri S. ten Brink, William H. Bakun, Claudia H. Flores
Slab tears and intermediate-depth seismicity Slab tears and intermediate-depth seismicity
Active tectonic regions where plate boundaries transition from subduction to strike slip can take several forms, such as triple junctions, acute, and obtuse corners. Well-documented slab tears that are associated with high rates of intermediate-depth seismicity are considered here: Gibraltar arc, the southern and northern ends of the Lesser Antilles arc, and the northern end of Tonga...
Authors
Hallie E. Meighan, Uri S. ten Brink, Jay Pulliam
Seismic evidence for a slab tear at the Puerto Rico Trench Seismic evidence for a slab tear at the Puerto Rico Trench
The fore-arc region of the northeast Caribbean plate north of Puerto Rico and the Virgin Islands has been the site of numerous seismic swarms since at least 1976. A 6 month deployment of five ocean bottom seismographs recorded two such tightly clustered swarms, along with additional events. Joint analyses of the ocean bottom seismographs and land-based seismic data reveal that the swarms...
Authors
Hallie E. Meighan, Jay Pulliam, Uri S. ten Brink, Alberto M. Lopez-Venegas
Geomorphic process fingerprints in submarine canyons Geomorphic process fingerprints in submarine canyons
Submarine canyons are common features of continental margins worldwide. They are conduits that funnel vast quantities of sediment from the continents to the deep sea. Though it is known that submarine canyons form primarily from erosion induced by submarine sediment flows, we currently lack quantitative, empirically based expressions that describe the morphology of submarine canyon...
Authors
Daniel S. Brothers, Uri S. ten Brink, Brian D. Andrews, Jason D. Chaytor, David C. Twichell
Geomorphic characterization of the U.S. Atlantic continental margin Geomorphic characterization of the U.S. Atlantic continental margin
The increasing volume of multibeam bathymetry data collected along continental margins is providing new opportunities to study the feedbacks between sedimentary and oceanographic processes and seafloor morphology. Attempts to develop simple guidelines that describe the relationships between form and process often overlook the importance of inherited physiography in slope depositional...
Authors
Daniel S. Brothers, Uri S. ten Brink, Brian D. Andrews, Jason D. Chaytor
Reply to a comment by Carol S. Prentice, Paul Mann, and Luis R. Peña on: "Historical perspective on seismic hazard to Hispaniola and the northeast Caribbean region" by U. ten Brink et al. (2011) Reply to a comment by Carol S. Prentice, Paul Mann, and Luis R. Peña on: "Historical perspective on seismic hazard to Hispaniola and the northeast Caribbean region" by U. ten Brink et al. (2011)
No abstract available.
Authors
Uri S. ten Brink, William H. Bakun, Claudia H. Flores
Non-USGS Publications**
**Disclaimer: The views expressed in Non-USGS publications are those of the author and do not represent the views of the USGS, Department of the Interior, or the U.S. Government.
Science and Products
Filter Total Items: 150
Event sedimentation in low-latitude deep-water carbonate basins, Anegada passage, northeast Caribbean Event sedimentation in low-latitude deep-water carbonate basins, Anegada passage, northeast Caribbean
The Virgin Islands and Whiting basins in the Northeast Caribbean are deep, structurally controlled depocentres partially bound by shallow-water carbonate platforms. Closed basins such as these are thought to document earthquake and hurricane events through the accumulation of event layers such as debris flow and turbidity current deposits and the internal deformation of deposited...
Authors
Jason D. Chaytor, Uri S. ten Brink
Assessment of tsunami hazard to the U.S. Atlantic margin Assessment of tsunami hazard to the U.S. Atlantic margin
Tsunami hazard is a very low-probability, but potentially high-risk natural hazard, posing unique challenges to scientists and policy makers trying to mitigate its impacts. These challenges are illustrated in this assessment of tsunami hazard to the U.S. Atlantic margin. Seismic activity along the U.S. Atlantic margin in general is low, and confirmed paleo-tsunami deposits have not yet...
Authors
Uri S. ten Brink, Jason Chaytor, Eric L. Geist, Daniel S. Brothers, Brian D. Andrews
A framework for the probabilistic analysis of meteotsunamis A framework for the probabilistic analysis of meteotsunamis
A probabilistic technique is developed to assess the hazard from meteotsunamis. Meteotsunamis are unusual sea-level events, generated when the speed of an atmospheric pressure or wind disturbance is comparable to the phase speed of long waves in the ocean. A general aggregation equation is proposed for the probabilistic analysis, based on previous frameworks established for both tsunamis...
Authors
Eric L. Geist, Uri S. ten Brink, Matthew D. Gove
Seabed fluid expulsion along the upper slope and outer shelf of the U.S. Atlantic continental margin Seabed fluid expulsion along the upper slope and outer shelf of the U.S. Atlantic continental margin
Identifying the spatial distribution of seabed fluid expulsion features is crucial for understanding the substrate plumbing system of any continental margin. A 1100 km stretch of the U.S. Atlantic margin contains more than 5000 pockmarks at water depths of 120 m (shelf edge) to 700 m (upper slope), mostly updip of the contemporary gas hydrate stability zone (GHSZ). Advanced attribute...
Authors
D.S. Brothers, C. Ruppel, J.W. Kluesner, Uri S. ten Brink, J.D. Chaytor, J. C. Hill, B.D. Andrews, C. Flores
Slope failures and timing of turbidity flows north of Puerto Rico Slope failures and timing of turbidity flows north of Puerto Rico
The submerged carbonate platform north of Puerto Rico terminates in a high (3,000–4,000 m) and in places steep (>45°) slope characterized by numerous landslide scarps including two 30–50 km-wide amphitheater-shaped features. The origin of the steep platform edge and the amphitheaters has been attributed to: (1) catastrophic failure, or (2) localized failures and progressive erosion...
Authors
Uri S. ten Brink, Jason D. Chaytor
Bathymetric Terrain Model of the Puerto Rico Trench and the Northeastern Caribbean Region for Marine Geological Investigations Bathymetric Terrain Model of the Puerto Rico Trench and the Northeastern Caribbean Region for Marine Geological Investigations
Multibeam bathymetry data collected in the Puerto Rico Trench and Northeast Caribbean region are compiled into a seamless bathymetric terrain model for broad-scale geological investigations of the trench system. These data, collected during eight separate surveys between 2002 and 2013, covering almost 180,000 square kilometers are published here in large format map sheet and digital...
Authors
Brian D. Andrews, Uri S. ten Brink, William W. Danforth, Jason D. Chaytor, J Granja-Bruna, A Carbo-Gorosabel
Seismic hazard from the Hispaniola subduction zone: correction to "Historical perspective on seismic hazard to Hispaniola and the northeast Caribbean region" Seismic hazard from the Hispaniola subduction zone: correction to "Historical perspective on seismic hazard to Hispaniola and the northeast Caribbean region"
No abstract available
Authors
Uri S. ten Brink, William H. Bakun, Claudia H. Flores
Slab tears and intermediate-depth seismicity Slab tears and intermediate-depth seismicity
Active tectonic regions where plate boundaries transition from subduction to strike slip can take several forms, such as triple junctions, acute, and obtuse corners. Well-documented slab tears that are associated with high rates of intermediate-depth seismicity are considered here: Gibraltar arc, the southern and northern ends of the Lesser Antilles arc, and the northern end of Tonga...
Authors
Hallie E. Meighan, Uri S. ten Brink, Jay Pulliam
Seismic evidence for a slab tear at the Puerto Rico Trench Seismic evidence for a slab tear at the Puerto Rico Trench
The fore-arc region of the northeast Caribbean plate north of Puerto Rico and the Virgin Islands has been the site of numerous seismic swarms since at least 1976. A 6 month deployment of five ocean bottom seismographs recorded two such tightly clustered swarms, along with additional events. Joint analyses of the ocean bottom seismographs and land-based seismic data reveal that the swarms...
Authors
Hallie E. Meighan, Jay Pulliam, Uri S. ten Brink, Alberto M. Lopez-Venegas
Geomorphic process fingerprints in submarine canyons Geomorphic process fingerprints in submarine canyons
Submarine canyons are common features of continental margins worldwide. They are conduits that funnel vast quantities of sediment from the continents to the deep sea. Though it is known that submarine canyons form primarily from erosion induced by submarine sediment flows, we currently lack quantitative, empirically based expressions that describe the morphology of submarine canyon...
Authors
Daniel S. Brothers, Uri S. ten Brink, Brian D. Andrews, Jason D. Chaytor, David C. Twichell
Geomorphic characterization of the U.S. Atlantic continental margin Geomorphic characterization of the U.S. Atlantic continental margin
The increasing volume of multibeam bathymetry data collected along continental margins is providing new opportunities to study the feedbacks between sedimentary and oceanographic processes and seafloor morphology. Attempts to develop simple guidelines that describe the relationships between form and process often overlook the importance of inherited physiography in slope depositional...
Authors
Daniel S. Brothers, Uri S. ten Brink, Brian D. Andrews, Jason D. Chaytor
Reply to a comment by Carol S. Prentice, Paul Mann, and Luis R. Peña on: "Historical perspective on seismic hazard to Hispaniola and the northeast Caribbean region" by U. ten Brink et al. (2011) Reply to a comment by Carol S. Prentice, Paul Mann, and Luis R. Peña on: "Historical perspective on seismic hazard to Hispaniola and the northeast Caribbean region" by U. ten Brink et al. (2011)
No abstract available.
Authors
Uri S. ten Brink, William H. Bakun, Claudia H. Flores
Non-USGS Publications**
**Disclaimer: The views expressed in Non-USGS publications are those of the author and do not represent the views of the USGS, Department of the Interior, or the U.S. Government.
*Disclaimer: Listing outside positions with professional scientific organizations on this Staff Profile are for informational purposes only and do not constitute an endorsement of those professional scientific organizations or their activities by the USGS, Department of the Interior, or U.S. Government