Uri ten Brink, PhD
My research focuses on quantifying tectonic and morphological processes and their impacts on the assessments of tsunami, landslide, and earthquake hazards. I am also interested in bridging gaps between disciplines in earth sciences. I am the Project Chief of the USGS Marine Geohazards Sources and Probability Project and in charge of the USGS Ocean Bottom Seismometers.
FIELD EXPERIENCE
41 cruises (26 as chief scientist)
3 over-ice land traverses, Antarctica (co-chief scientist)
4 Airborne magnetic, land gravity, and land seismic surveys (co-chief scientist)
Professional Experience
1991-present Research geophysicist, USGS, Woods Hole Coastal and Marine Science Center
2015-2019 Editor in Chief, Journal of Geophysical Research-Solid Earth
1999-present Adjunct Scientist, The Woods Hole Oceanographic Institution
2013-2016 Professor and Chairman, Department of Marine Geosciences, University of Haifa
2016-present Affiliate Professor, University of Haifa
Education and Certifications
1981-1986 Ph.D. Geological Sciences Lamont-Doherty Earth Observatory of Columbia University
1977-1980 B.Sc. Geology and Physics, The Hebrew University, Israel
1991-1996 Consulting Associate Professor, Stanford University
1987-1991 Post-doctoral scholar, Stanford University
1986-1987 Post-doctoral scholar, Tel Aviv University
Affiliations and Memberships*
Chairman, U.S.-Israel Bi-National Science Foundation panel for Earth and Atmospheric sciences, 2015
Member - Netherlands Science Foundation panel on Caribbean natural and social sciences, 2014
Member, ITU-WMO-UNESCO/IOC Joint Task Force on Submarine Cables for Tsunami Warnings and Scientific Research, 2013
Co-convenor, Workshop on landslide tsunami probability, 2011
Member, NSF panel evaluating the management structure of the ocean bottom seismometer facilities, 2011
Guest editor- Marine Geology "Assessment of tsunami hazards to the U.S. Atlantic coast", 2009
Honors and Awards
2016 – Fellow, American Geophysical Union
2010 – Senior Scientist (ST), Federal government
2007/8 – Distinguished Lecturer – Seismological Society of America/ IRIS
1996 - Fellow, Geological Society of America
1990 - Royal Society of New Zealand annual prize for Geophysics
Science and Products
RayGUI 2.0: a graphical user interface for interactive forward and inversion ray-tracing
Stress interaction between subduction earthquakes and forearc strike-slip faults: Modeling and application to the northern Caribbean plate boundary
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 three-dimensional models of static Coulomb stress change. Model results reveal that subduction earthquakes with sli
Archive of datasonics SIS-1000 chirp subbottom data collected during USGS cruise K-1-95-PS Puget Sound, State of Washington, 1995
Real-time seismic data from the coastal ocean
The Hula Valley subsurface structure inferred from gravity data
Corrigendum to "Lower crustal flow and the role of shear in basin subsidence: An example from the Dead Sea Basin"
Subsurface geometry and evolution of the Seattle fault zone and the Seattle Basin, Washington
The nature of the crust under Cayman Trough from gravity
Considerable crustal thickness variations are inferred along Cayman Trough, a slow-spreading ocean basin in the Caribbean Sea, from modeling of the gravity field. The crust to a distance of 50 km from the spreading center is only 2–3 km thick in agreement with dredge and dive results. Crustal thickness increases to ∼5.5 km at distances between 100 and 430 km west of the spreading center and to 3.5
Lower crustal flow and the role of shear in basin subsidence: An example from the Dead Sea basin
Crustal structure of central Lake Baikal: Insights into intracontinental rifting
Joint Israeli-Palestinian gravity survey in the Dead Sea Rift valley
Project PROBES (Puerto Rico Ocean Bottom Earthquake Survey)
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
RayGUI 2.0: a graphical user interface for interactive forward and inversion ray-tracing
Stress interaction between subduction earthquakes and forearc strike-slip faults: Modeling and application to the northern Caribbean plate boundary
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 three-dimensional models of static Coulomb stress change. Model results reveal that subduction earthquakes with sli
Archive of datasonics SIS-1000 chirp subbottom data collected during USGS cruise K-1-95-PS Puget Sound, State of Washington, 1995
Real-time seismic data from the coastal ocean
The Hula Valley subsurface structure inferred from gravity data
Corrigendum to "Lower crustal flow and the role of shear in basin subsidence: An example from the Dead Sea Basin"
Subsurface geometry and evolution of the Seattle fault zone and the Seattle Basin, Washington
The nature of the crust under Cayman Trough from gravity
Considerable crustal thickness variations are inferred along Cayman Trough, a slow-spreading ocean basin in the Caribbean Sea, from modeling of the gravity field. The crust to a distance of 50 km from the spreading center is only 2–3 km thick in agreement with dredge and dive results. Crustal thickness increases to ∼5.5 km at distances between 100 and 430 km west of the spreading center and to 3.5
Lower crustal flow and the role of shear in basin subsidence: An example from the Dead Sea basin
Crustal structure of central Lake Baikal: Insights into intracontinental rifting
Joint Israeli-Palestinian gravity survey in the Dead Sea Rift valley
Project PROBES (Puerto Rico Ocean Bottom Earthquake Survey)
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