Uri ten Brink, PhD (Former Employee)
Science and Products
Filter Total Items: 150
Submarine landslide as the source for the October 11, 1918 Mona Passage tsunami: Observations and modeling Submarine landslide as the source for the October 11, 1918 Mona Passage tsunami: Observations and modeling
The October 11, 1918 ML 7.5 earthquake in the Mona Passage between Hispaniola and Puerto Rico generated a local tsunami that claimed approximately 100 lives along the western coast of Puerto Rico. The area affected by this tsunami is now significantly more populated. Newly acquired high-resolution bathymetry and seismic reflection lines in the Mona Passage show a fresh submarine...
Authors
A.M. López-Venegas, Uri S. ten Brink, Eric L. Geist
Preliminary results of the U.S. Nuclear Regulatory Commission collaborative research program to assess tsunami hazard for nuclear power plants on the Atlantic and gulf coasts Preliminary results of the U.S. Nuclear Regulatory Commission collaborative research program to assess tsunami hazard for nuclear power plants on the Atlantic and gulf coasts
In response to the 2004 Indian Ocean Tsunami, the United States Nuclear Regulatory Commission (US NRC) initiated a long-term research program to improve understanding of tsunami hazard levels for nuclear facilities in the United States. For this effort, the US NRC organized a collaborative research program with the United States Geological Survey (USGS) and other key researchers for the...
Authors
A.M. Kammerer, Uri S. ten Brink, David C. Twitchell, Eric L. Geist, Jason D. Chaytor, J. Locat, H. J. Lee, Brian J. Buczkowski, M. Sansoucy
Magnetic character of a large continental transform: an aeromagnetic survey of the Dead Sea Fault Magnetic character of a large continental transform: an aeromagnetic survey of the Dead Sea Fault
New high-resolution airborne magnetic (HRAM) data along a 120-km-long section of the Dead Sea Transform in southern Jordan and Israel shed light on the shallow structure of the fault zone and on the kinematics of the plate boundary. Despite infrequent seismic activity and only intermittent surface exposure, the fault is delineated clearly on a map of the first vertical derivative of the...
Authors
Uri S. ten Brink, Michael Rybakov, Abdallah S. Al-Zoubi, Yair Rotstein
Revisiting submarine mass movements along the U.S. Atlantic Continental Margin: Implications for tsunami hazards Revisiting submarine mass movements along the U.S. Atlantic Continental Margin: Implications for tsunami hazards
Interest in the generation of tsunamis by submarine mass movements has warranted a reassessment of their distribution and the nature of submarine landslides offshore of the eastern U.S. The recent acquisition and analysis of multibeam bathymetric data over most of this continental slope and rise provides clearer view into the extent and style of mass movements on this margin. Debris...
Authors
J.D. Chaytor, D.C. Twichell, Uri S. ten Brink, B.J. Buczkowski, B.D. Andrews
Sediment compaction rates and subsidence in deltaic plains: Numerical constraints and stratigraphic influences Sediment compaction rates and subsidence in deltaic plains: Numerical constraints and stratigraphic influences
Natural sediment compaction in deltaic plains influences subsidence rates and the evolution of deltaic morphology. Determining compaction rates requires detailed knowledge of subsurface geotechnical properties and depositional history, neither of which is often readily available. To overcome this lack of knowledge, we numerically forward model the incremental sedimentation and compaction...
Authors
T.A. Meckel, Uri S. ten Brink, S.J. Williams
The Northern end of the Dead Sea Basin: Geometry from reflection seismic evidence The Northern end of the Dead Sea Basin: Geometry from reflection seismic evidence
Recently released reflection seismic lines from the Eastern side of the Jordan River north of the Dead Sea were interpreted by using borehole data and incorporated with the previously published seismic lines of the eastern side of the Jordan River. For the first time, the lines from the eastern side of the Jordan River were combined with the published reflection seismic lines from the...
Authors
A. S. Al-Zoubi, T. Heinrichs, I. Qabbani, Uri S. ten Brink
Submarine slides north of Puerto Rico and their tsunami potential Submarine slides north of Puerto Rico and their tsunami potential
New 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 fail, at least in initial stages, as a coherent rock mass. This, combined with the fact that the edge of the carbonate platform is...
Authors
Uri S. ten Brink, Eric L. Geist, Patrick J. Lynett, Brian D. Andrews
A note on the correlation between geophysical observations and seismicity in the Arava/(Araba) Valley at the southern part of the Dead Sea fault A note on the correlation between geophysical observations and seismicity in the Arava/(Araba) Valley at the southern part of the Dead Sea fault
The spatial distribution of the earthquakes in the Arava Valley, a 150-km section of the Dead Sea Transform, is compared for the first time with the local subsurface geological features derived from geophysical and geological data. Gravity data suggested that the Gharandal, Timna, and Elat basins were filled by low-density young sediments. These features were confirmed by seismic...
Authors
M. Rybakov, A. Shapira, A. Al-Zoubi, Uri S. ten Brink, R. Hofstetter, N. Kraeva, L. Feldman
Seismic imaging of deep low-velocity zone beneath the Dead Sea basin and transform fault: Implications for strain localization and crustal rigidity Seismic imaging of deep low-velocity zone beneath the Dead Sea basin and transform fault: Implications for strain localization and crustal rigidity
New seismic observations from the Dead Sea basin (DSB), a large pull-apart basin along the Dead Sea transform (DST) plate boundary, show a low velocity zone extending to a depth of 18 km under the basin. The lower crust and Moho are not perturbed. These observations are incompatible with the current view of mid-crustal strength at low temperatures and with support of the basin's negative...
Authors
Uri S. ten Brink, A. S. Al-Zoubi, C.H. Flores, Y. Rotstein, I. Qabbani, S.H. Harder, Gordon R. Keller
Rupture models for the A.D. 900-930 Seattle fault earthquake from uplifted shorelines Rupture models for the A.D. 900-930 Seattle fault earthquake from uplifted shorelines
A major earthquake on the Seattle fault, Washington, ca. A.D. 900-930 was first inferred from uplifted shorelines and tsunami deposits. Despite follow-up geophysical and geological investigations, the rupture parameters of the earthquake and the geometry of the fault are uncertain. Here we estimate the fault geometry, slip direction, and magnitude of the earthquake by modeling shoreline...
Authors
Uri S. ten Brink, J. Song, R.C. Bucknam
Size distribution of submarine landslides and its implication to tsunami hazard in Puerto Rico Size distribution of submarine landslides and its implication to tsunami hazard in Puerto Rico
We have established for the first time a size frequency distribution for carbonate submarine slope failures. Using detailed bathymetry along the northern edge of the carbonate platform north of Puerto Rico, we show that the cumulative distribution of slope failure volumes follows a power-law distribution. The power-law exponent of this distribution is similar to those for rock falls on...
Authors
Uri S. ten Brink, E.L. Geist, B.D. Andrews
Current subsidence rates due to compaction of Holocene sediments in southern Louisiana Current subsidence rates due to compaction of Holocene sediments in southern Louisiana
Relative contributions of geologic and anthropogenic processes to subsidence of southern Louisiana are vigorously debated. Of these, shallow sediment compaction is often considered dominant, although this has never been directly observed or effectively demonstrated. Quantitative understanding of subsidence is important for predicting relative sea level rise, storm surge flooding due to...
Authors
T.A. Meckel, Uri S. ten Brink, S.J. Williams
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
Submarine landslide as the source for the October 11, 1918 Mona Passage tsunami: Observations and modeling Submarine landslide as the source for the October 11, 1918 Mona Passage tsunami: Observations and modeling
The October 11, 1918 ML 7.5 earthquake in the Mona Passage between Hispaniola and Puerto Rico generated a local tsunami that claimed approximately 100 lives along the western coast of Puerto Rico. The area affected by this tsunami is now significantly more populated. Newly acquired high-resolution bathymetry and seismic reflection lines in the Mona Passage show a fresh submarine...
Authors
A.M. López-Venegas, Uri S. ten Brink, Eric L. Geist
Preliminary results of the U.S. Nuclear Regulatory Commission collaborative research program to assess tsunami hazard for nuclear power plants on the Atlantic and gulf coasts Preliminary results of the U.S. Nuclear Regulatory Commission collaborative research program to assess tsunami hazard for nuclear power plants on the Atlantic and gulf coasts
In response to the 2004 Indian Ocean Tsunami, the United States Nuclear Regulatory Commission (US NRC) initiated a long-term research program to improve understanding of tsunami hazard levels for nuclear facilities in the United States. For this effort, the US NRC organized a collaborative research program with the United States Geological Survey (USGS) and other key researchers for the...
Authors
A.M. Kammerer, Uri S. ten Brink, David C. Twitchell, Eric L. Geist, Jason D. Chaytor, J. Locat, H. J. Lee, Brian J. Buczkowski, M. Sansoucy
Magnetic character of a large continental transform: an aeromagnetic survey of the Dead Sea Fault Magnetic character of a large continental transform: an aeromagnetic survey of the Dead Sea Fault
New high-resolution airborne magnetic (HRAM) data along a 120-km-long section of the Dead Sea Transform in southern Jordan and Israel shed light on the shallow structure of the fault zone and on the kinematics of the plate boundary. Despite infrequent seismic activity and only intermittent surface exposure, the fault is delineated clearly on a map of the first vertical derivative of the...
Authors
Uri S. ten Brink, Michael Rybakov, Abdallah S. Al-Zoubi, Yair Rotstein
Revisiting submarine mass movements along the U.S. Atlantic Continental Margin: Implications for tsunami hazards Revisiting submarine mass movements along the U.S. Atlantic Continental Margin: Implications for tsunami hazards
Interest in the generation of tsunamis by submarine mass movements has warranted a reassessment of their distribution and the nature of submarine landslides offshore of the eastern U.S. The recent acquisition and analysis of multibeam bathymetric data over most of this continental slope and rise provides clearer view into the extent and style of mass movements on this margin. Debris...
Authors
J.D. Chaytor, D.C. Twichell, Uri S. ten Brink, B.J. Buczkowski, B.D. Andrews
Sediment compaction rates and subsidence in deltaic plains: Numerical constraints and stratigraphic influences Sediment compaction rates and subsidence in deltaic plains: Numerical constraints and stratigraphic influences
Natural sediment compaction in deltaic plains influences subsidence rates and the evolution of deltaic morphology. Determining compaction rates requires detailed knowledge of subsurface geotechnical properties and depositional history, neither of which is often readily available. To overcome this lack of knowledge, we numerically forward model the incremental sedimentation and compaction...
Authors
T.A. Meckel, Uri S. ten Brink, S.J. Williams
The Northern end of the Dead Sea Basin: Geometry from reflection seismic evidence The Northern end of the Dead Sea Basin: Geometry from reflection seismic evidence
Recently released reflection seismic lines from the Eastern side of the Jordan River north of the Dead Sea were interpreted by using borehole data and incorporated with the previously published seismic lines of the eastern side of the Jordan River. For the first time, the lines from the eastern side of the Jordan River were combined with the published reflection seismic lines from the...
Authors
A. S. Al-Zoubi, T. Heinrichs, I. Qabbani, Uri S. ten Brink
Submarine slides north of Puerto Rico and their tsunami potential Submarine slides north of Puerto Rico and their tsunami potential
New 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 fail, at least in initial stages, as a coherent rock mass. This, combined with the fact that the edge of the carbonate platform is...
Authors
Uri S. ten Brink, Eric L. Geist, Patrick J. Lynett, Brian D. Andrews
A note on the correlation between geophysical observations and seismicity in the Arava/(Araba) Valley at the southern part of the Dead Sea fault A note on the correlation between geophysical observations and seismicity in the Arava/(Araba) Valley at the southern part of the Dead Sea fault
The spatial distribution of the earthquakes in the Arava Valley, a 150-km section of the Dead Sea Transform, is compared for the first time with the local subsurface geological features derived from geophysical and geological data. Gravity data suggested that the Gharandal, Timna, and Elat basins were filled by low-density young sediments. These features were confirmed by seismic...
Authors
M. Rybakov, A. Shapira, A. Al-Zoubi, Uri S. ten Brink, R. Hofstetter, N. Kraeva, L. Feldman
Seismic imaging of deep low-velocity zone beneath the Dead Sea basin and transform fault: Implications for strain localization and crustal rigidity Seismic imaging of deep low-velocity zone beneath the Dead Sea basin and transform fault: Implications for strain localization and crustal rigidity
New seismic observations from the Dead Sea basin (DSB), a large pull-apart basin along the Dead Sea transform (DST) plate boundary, show a low velocity zone extending to a depth of 18 km under the basin. The lower crust and Moho are not perturbed. These observations are incompatible with the current view of mid-crustal strength at low temperatures and with support of the basin's negative...
Authors
Uri S. ten Brink, A. S. Al-Zoubi, C.H. Flores, Y. Rotstein, I. Qabbani, S.H. Harder, Gordon R. Keller
Rupture models for the A.D. 900-930 Seattle fault earthquake from uplifted shorelines Rupture models for the A.D. 900-930 Seattle fault earthquake from uplifted shorelines
A major earthquake on the Seattle fault, Washington, ca. A.D. 900-930 was first inferred from uplifted shorelines and tsunami deposits. Despite follow-up geophysical and geological investigations, the rupture parameters of the earthquake and the geometry of the fault are uncertain. Here we estimate the fault geometry, slip direction, and magnitude of the earthquake by modeling shoreline...
Authors
Uri S. ten Brink, J. Song, R.C. Bucknam
Size distribution of submarine landslides and its implication to tsunami hazard in Puerto Rico Size distribution of submarine landslides and its implication to tsunami hazard in Puerto Rico
We have established for the first time a size frequency distribution for carbonate submarine slope failures. Using detailed bathymetry along the northern edge of the carbonate platform north of Puerto Rico, we show that the cumulative distribution of slope failure volumes follows a power-law distribution. The power-law exponent of this distribution is similar to those for rock falls on...
Authors
Uri S. ten Brink, E.L. Geist, B.D. Andrews
Current subsidence rates due to compaction of Holocene sediments in southern Louisiana Current subsidence rates due to compaction of Holocene sediments in southern Louisiana
Relative contributions of geologic and anthropogenic processes to subsidence of southern Louisiana are vigorously debated. Of these, shallow sediment compaction is often considered dominant, although this has never been directly observed or effectively demonstrated. Quantitative understanding of subsidence is important for predicting relative sea level rise, storm surge flooding due to...
Authors
T.A. Meckel, Uri S. ten Brink, S.J. Williams
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