I work on a variety of marine geological and geohazard topics including sedimentary processes and geochronology of submarine slope failures, deep-sea sedimentary systems, submarine geomorphology, and neotectonics in marine and near-shore environments.
Dr. Jason Chaytor is a research geologist with the U.S. Geological Survey at the USGS Woods Hole Coastal and Marine Science Center. Jason conducts research on issues related to marine geohazards including submarine landslides, tsunamis, earthquakes, and plate tectonics and shallow- and deep-water sedimentary processes on Atlantic, Gulf of Mexico and Pacific margins of the U.S. and in the northeast Caribbean. He is the current principle scientist for the USGS Woods Hole Coastal and Marine Science Center Sediments Laboratory.
Research Interests
Marine Geohazards
Marine geohazards are sudden and extreme geologic events that affect coastal areas and seabed infrastructure on regional and transoceanic scales. The hazards include submarine earthquakes, submarine slope failures, and tsunami generation. The sediment record of past offshore and coastal hazardous events is generally more complete in the marine environment than on land and can be investigated with geological and geophysical tools. My research involves the identification and characterization of areas of the seafloor and subseafloor within and adjacent to the U.S. EEZ that record a history of fault movement or slope failure (or have the potential to be effected by these processes in the future). Included in this work is the development of conceptual models of seafloor movement and local/regional sedimentation patterns and supporting geochronological frameworks, formulation, planning and performance of field sampling and geophysical imaging activities and laboratory analyses, investigation of local and regional sedimentation processes, and communication of event characteristics to modelers and other stake holders to aid in developing hazard assessments.
Marine Sedimentation Processes and Framework Geology
I investigate dynamic shallow-water (< 200 m) and deep-water sedimentary environments to characterize physical properties affecting acoustic propagation (ONR Mud Patch Project), to evaluate the hazard of recurring seafloor motion to critical offshore infrastructure, and in the development of regional geologic analysis of surfical geologic processes across multiple potential areas of interest in to the U.S. Extended Continental Shelf Project.
Education and Certifications
2006-2009: Postdoctoral Scholar, Department of Geology and Geophysics, Woods Hole Oceanographic Institution, MA
2006: PhD, Geological Oceanography, Oregon State University, Corvallis, Oregon,
Science and Products
Puerto Rico Natural Hazards: Earthquakes | Peligros naturales de Puerto Rico: Terremotos
Puerto Rico Natural Hazards: Tsunamis | Peligros naturales de Puerto Rico: Maremotos
USGS Role in DEEP SEARCH: Deep Sea Exploration to Advance Research on Coral, Canyon, and Cold-seep Habitats
DISCOVRE: Diversity, Systematics and Connectivity of Vulnerable Reef Ecosystems
Sedimentological and geotechnical analyses of marine sediment cores from the Currituck Landslide Complex and upper slope adjacent to Baltimore Canyon collected on USGS Field Activity 2012-007-FA
Carbonate chemistry measurements of authigenic carbonates collected offshore the U.S. Mid- and South Atlantic in 2018 and 2019 as part of the DEEPSEARCH Project
Sedimentological and geotechnical analyses of marine sediment cores from the New England Mud Patch
Multichannel seismic-reflection and navigation data collected using SIG ELC1200 and Applied Acoustics Delta Sparkers and Geometrics GeoEel digital streamers during USGS field activity 2020-014-FA.
Acoustic ducting by shelf water streamers at the New England shelfbreak
Late Pleistocene-Holocene age and stratigraphy of the Currituck Slide Complex, U.S. mid-Atlantic continental slope: Implications for landslide triggering
Seafloor observations eliminate a landslide as the source of the 1918 Puerto Rico Tsunami
Climate change hotspots and implications for the global subsea telecommunications network
Measurements of Geologic Characteristics and Geophysical Properties of Sediments From the New England Mud Patch
Mature diffuse tectonic block boundary revealed by the 2020 southwestern Puerto Rico seismic sequence
Distributed faulting typically tends to coalesce into one or a few faults with repeated deformation. The progression of clustered medium-sized (≥Mw4.5) earthquakes during the 2020 seismic sequence in southwestern Puerto Rico (SWPR), modeling shoreline subsidence from InSAR, and sub-seafloor mapping by high-resolution seismic reflection profiles, suggest that the 2020 SWPR seismic sequence was dist
Subaqueous mass movements in the context of observations of contemporary slope failure
Mapping, exploration, and characterization of the California continental margin and associated features from the California-Oregon border to Ensenada, Mexico
Short and long-term movement of mudflows of the Mississippi River Delta Front and their known and potential impacts on oil and gas infrastructure
Geoacoustic inversion for a New England mud patch sediment using the silt-suspension theory of marine mud
Maximum entropy derived statistics of sound speed structure in a fine-grained sediment inferred from sparse broadband acoustic measurements on the New England continental shelf
In situ measurements of compressional wave speed during gravity coring operations in the New England mud patch
Science and Products
- Science
Puerto Rico Natural Hazards: Earthquakes | Peligros naturales de Puerto Rico: Terremotos
USGS provides real-time earthquake data, information on historic earthquakes, resources for the most significant earthquakes, and seismicity and ground motions to support future updates to the seismic hazard models for Puerto Rico and the U.S. Virgin Islands. Our seismic research can help establish better building regulations that mitigate earthquake risks and improve public safety. The USGS...Puerto Rico Natural Hazards: Tsunamis | Peligros naturales de Puerto Rico: Maremotos
Tsunamis are long waves formed from a sudden displacement of the sea floor due to a fault rupture, landslide, or volcanic activity. Given that Puerto Rico lies above a subduction zone in the Caribbean Sea, it is especially susceptible to large earthquakes and tsunamis. The greatest tsunami ever recorded in Puerto Rico occurred from an earthquake off the Mona Passage in 1918. The USGS Earthquake...USGS Role in DEEP SEARCH: Deep Sea Exploration to Advance Research on Coral, Canyon, and Cold-seep Habitats
USGS scientists are collaborating with multiple agencies to provide the esssential foundation for understanding these deep-sea environments.DISCOVRE: Diversity, Systematics and Connectivity of Vulnerable Reef Ecosystems
DISCOVRE (DIversity, Systematics and COnnectivity of Vulnerable Reef Ecosystems) is an integrated, multidisciplinary, international effort investigating the unique and fragile deep-sea coral environments from the microscopic level to the ecosystem level. - Data
Sedimentological and geotechnical analyses of marine sediment cores from the Currituck Landslide Complex and upper slope adjacent to Baltimore Canyon collected on USGS Field Activity 2012-007-FA
Twenty-four piston cores (and associated trigger cores) were collected from the source zone of the Currituck Landslide Complex and upper slope adjacent to Baltimore Canyon by the U.S. Geological Survey and the University of Rhode Island Department of Ocean Engineering during an eight-day cruise aboard the R/V Hugh R. Sharp in September/October of 2012. These cores were analyzed for evidence of seaCarbonate chemistry measurements of authigenic carbonates collected offshore the U.S. Mid- and South Atlantic in 2018 and 2019 as part of the DEEPSEARCH Project
Geochemical analysis of carbonate rock samples collected from seep fields on the RB1903 and AT41 research expeditions in the U.S. Mid- and South Atlantic. Samples were collected as a fingerprint to past hydrocarbon seep activity, fluid source, and depositional environment.Sedimentological and geotechnical analyses of marine sediment cores from the New England Mud Patch
Variability in sediment properties with depth and the thickness of individual sedimentary layers are critical determinants of seabed acoustic response. The New England Mud Patch, located south of Cape Cod, is an unusual feature on the U.S. Continental Shelf in that it is composed of fine-grained sediment layers containing a relatively-homogeneous mix of sand, silt, and clay-sized particles boundedMultichannel seismic-reflection and navigation data collected using SIG ELC1200 and Applied Acoustics Delta Sparkers and Geometrics GeoEel digital streamers during USGS field activity 2020-014-FA.
In March 2020, the U.S. Geological Survey and the University of Puerto Rico Mayaguez (UPRM) Department of Marine Sciences conducted a marine seismic-reflection experiment focused on observing geophysical evidence of submarine faulting and mass wasting related to the southwestern Puerto Rico seismic sequence of 2019-20. The seismic sequence culminated with a magnitude 6.4 earthquake centered beneat - Multimedia
- Publications
Filter Total Items: 40
Acoustic ducting by shelf water streamers at the New England shelfbreak
Greater sound speed variability has been observed at the New England shelfbreak due to a greater influence from the Gulf Stream with increased meander amplitudes and frequency of Warm Core Ring (WCR) generation. Consequently, underwater sound propagation in the area also becomes more variable. This paper presents field observations of an acoustic near-surface ducting condition induced by shelf watAuthorsJennifer J. Johnson, Ying-Tsong Lin, Arthur E. Newhall, Glen G. Gawarkiewicz, David P. Knobles, Jason Chaytor, William S.. HodgkissLate Pleistocene-Holocene age and stratigraphy of the Currituck Slide Complex, U.S. mid-Atlantic continental slope: Implications for landslide triggering
Considerable effort has been made to link submarine slope failures to changes in local and global-scale environmental conditions, in order to assess landslide hazard probability. Here we provide the first radiocarbon dates of hemipelagic sediment overlying mass transport deposits and inferred failure surfaces of the Currituck Slide Complex (CSC), a prominent landslide scar on the U.S. mid-AtlanticAuthorsJason Chaytor, Uri S. ten Brink, Christopher D. P. BaxterSeafloor 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 GeorgiopoulouClimate change hotspots and implications for the global subsea telecommunications network
A global network of subsea telecommunications cables underpins our daily lives, enabling >95% of global digital data transfer, $trillions/day in financial trading, and providing critical communications links, particularly to remote, low-income countries. Despite their importance, subsea cables and their landing stations are vulnerable to damage by natural hazards, including storm surges, waves, cyAuthorsM.A. Clare, I.A. Yeo, L. Bricheno, Y Askenov, J. Browning, I.D. Haigh, T. Wahl, J. A. Hunter, C. Sams, Jason Chaytor, B.J. Bett, L. CarterMeasurements of Geologic Characteristics and Geophysical Properties of Sediments From the New England Mud Patch
The characterization of physical, geological, and geophysical properties of sediments within the New England Mud Patch (NEMP) was undertaken to provide a physical basis for acoustic inversions associated with the SeaBed Characterization EXperiment 2017 (SBCEX17). Using a suite of 89 sediment cores (piston/trigger, gravity [acoustic], and vibracore), a comprehensive database of laboratory-based sedAuthorsJason Chaytor, Meagan Ballard, Brian J. Buczkowski, John A. Goff, Kevin M. Lee, Allen Reed, Allyson Anne BoggessMature diffuse tectonic block boundary revealed by the 2020 southwestern Puerto Rico seismic sequence
Distributed faulting typically tends to coalesce into one or a few faults with repeated deformation. The progression of clustered medium-sized (≥Mw4.5) earthquakes during the 2020 seismic sequence in southwestern Puerto Rico (SWPR), modeling shoreline subsidence from InSAR, and sub-seafloor mapping by high-resolution seismic reflection profiles, suggest that the 2020 SWPR seismic sequence was dist
AuthorsUri S. ten Brink, L Vanacore, E. J. Fielding, Jason Chaytor, A.M. Lopez-Venegas, Wayne E. Baldwin, David S. Foster, Brian D. AndrewsSubaqueous mass movements in the context of observations of contemporary slope failure
The consequences of subaqueous landslides have been at the forefront of societal conscience more than ever in the last few years, with devastating and fatal events in the Indonesian Archipelago making global news. The new research presented in this volume demonstrates the breadth of ongoing investigation into subaqueous landslides, and shows that while events like the recent ones can be devastatinAuthorsJ.J. Mountjoy, Aggeliki Georgiopoulou, Jason Chaytor, M.A. Clare, D. Gamboa, J. MoernautMapping, exploration, and characterization of the California continental margin and associated features from the California-Oregon border to Ensenada, Mexico
Priority Geographic Area: Both within and outside US Exclusive Economic Zone (EEZ). California continental margin. This area includes and continues south of the geographic area captured in the Watt et al. white paper. Description of Priority Area: The California continental margin, from the narrow shelf to abyssal depths, contains diverse seafloor features that influence benthic community types, bAuthorsAmanda Demopoulos, Nancy G. Prouty, Daniel S. Brothers, Janet Watt, James E. Conrad, Jason Chaytor, Chris CaldowShort and long-term movement of mudflows of the Mississippi River Delta Front and their known and potential impacts on oil and gas infrastructure
Mudflows on the Mississippi River Delta Front (MRDF) are recognized hazards to oil and gas infrastructure in the shallow (20 – 300 m water depth) Gulf of Mexico. Preconditioning of the seafloor for failure results from high sedimentation rates coupled with slope over-steepening, under-consolidation, and abundant biogenic gas production. Catastrophic failure of production platforms and pipelines duAuthorsJason Chaytor, Wayne E. Baldwin, Samuel J. Bentley, Melanie Damour, Douglas Jones, Jillian Maloney, Michael Miner, Jeff Obelcz, Kehui XuGeoacoustic inversion for a New England mud patch sediment using the silt-suspension theory of marine mud
This article provides an application of the silt-suspension theory to a Bayesian-inference inversion for the geo-acoustic parameters in marine mud. The theory, with consequences that have been developed recently, postulates a suspension of water and clay mineral card-houses that supports moderately dilute concentrations of silt particles. The approach is an example of a physically based model inveAuthorsElisabeth M. Brown, Ying-Tsong Lin, Jason Chaytor, William L. SiegmannMaximum entropy derived statistics of sound speed structure in a fine-grained sediment inferred from sparse broadband acoustic measurements on the New England continental shelf
Marginal probability distributions for parameters representing an effective sound-speed structure of a fine-grained sediment are inferred from a data ensemble maximum entropy method that utilizes a sparse spatially distributed set of received pressure time series resulting from multiple explosive sources in a shallow-water ocean environment possessing significant spatial variability of the seabed.AuthorsDavid P. Knobles, Preston S. Wilson, J.A. Goff, L. Wan, M.J. Buckingham, Jason Chaytor, Mohsen BadieyIn situ measurements of compressional wave speed during gravity coring operations in the New England mud patch
This paper presents measurements of sediment sound-speed profiles measured in situ using the acoustic coring system (ACS). The reported measurements were obtained from seven gravity cores collected in the New England Mud Patch. The ACS uses two sets of transducers mounted below the penetrating tip of a sediment corer to make in situ measurements of geoacoustic properties as the corer penetrates thAuthorsMegan S. Ballard, Kevin M. Lee, Andrew R. McNeese, Preston S. Wilson, Jason Chaytor, John A. Goff, Allen H. Reed - News