The Sea Floor Mapping Group (SFMG) is a core capability at the Woods Hole Coastal & Marine Science Center (WHCMSC) that provides support for coastal, lacustrine and marine geologic research. The staff has a wide-range of expertise and is responsible for geophysical and sampling data acquisition, processing, interpretation and publication, logistics, design, and research and development. SFMG has successfully supported Coastal/Marine Hazards and Resources Program research for more than 25 years.
Science Applications
SFMG uses acoustic and optical techniques to acquire detailed geologic information about the sea floor, such as seabed topography, sediment composition and distribution, and underlying geologic structure. This information defines the geologic framework and provides a base for a wide-range of USGS research.
Each year the SFMG supports dozens of research efforts, most recently including: gas hydrate and methane/carbon dioxide flux along the Atlantic margin; landslide and tsunami hazards along the mid-Atlantic and New England passive margin and the southeast Alaska active margin; characterization of mudflow hazards along the Mississippi River Delta Front; dive support for biological invasive species studies and benthic habitat studies; sediment characterization within the Stellwagen Bank National Marine Sanctuary; field observations in support of sea-level rise storm response studies along the east coast; and mapping lake floor topography and underlying stratigraphy in support of natural resource management within western reservoirs and Great Lakes.
Sea Floor Mapping Capabilities
SFMG maintains a suite of instruments used to map the seafloor surface and underlying structure in shallow to deep-water environments. These instruments include: multibeam, single-beam, and split beam echo sounders, sidescan-sonar, phase differencing bathymetric sonar, single- and multichannel seismic-reflection systems, and sample equipment designed to collect sediment samples, still photographs, and/or video images of the sea floor.
SFMG is a diverse team of marine electronics technicians, engineers, geologists, physical scientists, geographers, and visual and imaging specialists. This group has expertise in collecting, processing and interpreting geophysical and sample data in lacustrine, coastal and marine environments.
SFMG staff regularly collaborates with scientists at Universities, federal and state agencies, and the private sector to support collaborative research, and to help develop new software and hardware remote sensing techniques.
Below are publications associated with this project.
Change in morphology and modern sediment thickness on the inner continental shelf offshore of Fire Island, New York between 2011 and 2014: Analysis of hurricane impact
Assessing the impact of Hurricanes Irene and Sandy on the morphology and modern sediment thickness on the inner continental shelf offshore of Fire Island, New York
The impact of Hurricane Sandy on the shoreface and inner shelf of Fire Island, New York: large bedform migration but limited erosion
Maps showing the change in modern sediment thickness on the Inner Continental Shelf offshore of Fire Island, New York, between 1996-97 and 2011
Maps showing bathymetry and modern sediment thickness on the inner continental shelf offshore of Fire Island, New York, pre-Hurricane Sandy
Modification of the Quaternary stratigraphic framework of the inner-continental shelf by Holocene marine transgression: An example offshore of Fire Island, New York
High-resolution swath interferometric data collected within Muskeget Channel, Massachusetts
- Overview
The Sea Floor Mapping Group (SFMG) is a core capability at the Woods Hole Coastal & Marine Science Center (WHCMSC) that provides support for coastal, lacustrine and marine geologic research. The staff has a wide-range of expertise and is responsible for geophysical and sampling data acquisition, processing, interpretation and publication, logistics, design, and research and development. SFMG has successfully supported Coastal/Marine Hazards and Resources Program research for more than 25 years.
Graphic showing geophysical and sampling systems used to define the seafloor topography, surface sediments, and underlying geology. Sidescan-sonar systems acquire information about the surface of the seafloor, swath bathymetric systems measure the depth, or seafloor topography, seismic sources map the underlying geologic structure, single-beam echosounders map the depth at a point beneath the vessel, and sampling systems collect samples of the seafloor and can be equipped with digital camers and video systems to collect optical images of the seafloor. Wayne Baldwin, USGS, deploys a sound velocity profiler off the stern of the R/V Stephens in Lake Powell, UT-AZ as part of a collaborative program with the Utah Water Science Center to map the depth and sediments within Lake Powell, UT-AZ. Science Applications
SFMG uses acoustic and optical techniques to acquire detailed geologic information about the sea floor, such as seabed topography, sediment composition and distribution, and underlying geologic structure. This information defines the geologic framework and provides a base for a wide-range of USGS research.
Each year the SFMG supports dozens of research efforts, most recently including: gas hydrate and methane/carbon dioxide flux along the Atlantic margin; landslide and tsunami hazards along the mid-Atlantic and New England passive margin and the southeast Alaska active margin; characterization of mudflow hazards along the Mississippi River Delta Front; dive support for biological invasive species studies and benthic habitat studies; sediment characterization within the Stellwagen Bank National Marine Sanctuary; field observations in support of sea-level rise storm response studies along the east coast; and mapping lake floor topography and underlying stratigraphy in support of natural resource management within western reservoirs and Great Lakes.
Sea Floor Mapping Capabilities
SFMG maintains a suite of instruments used to map the seafloor surface and underlying structure in shallow to deep-water environments. These instruments include: multibeam, single-beam, and split beam echo sounders, sidescan-sonar, phase differencing bathymetric sonar, single- and multichannel seismic-reflection systems, and sample equipment designed to collect sediment samples, still photographs, and/or video images of the sea floor.
SFMG is a diverse team of marine electronics technicians, engineers, geologists, physical scientists, geographers, and visual and imaging specialists. This group has expertise in collecting, processing and interpreting geophysical and sample data in lacustrine, coastal and marine environments.
USGS staff are preparing to deploy the Edgetech 512i sub-bottom profiling system from the stern of a research vessel. The sub-bottom profiling system was used to map the geologic structure and sediments beneath the seafloor. SFMG staff regularly collaborates with scientists at Universities, federal and state agencies, and the private sector to support collaborative research, and to help develop new software and hardware remote sensing techniques.
Sources/Usage: Public Domain. Visit Media to see details.This animation takes the viewer down the Glen Canyon from Bullfrog Bay to the Rincon, in the Glen Canyon National Recreation Area. New high resolution multibeam bathymetry collected by the USGS in 2018 shows the submerged portions of Glen Canyon. Brian Andrews, USGS Woods Hole Coast and Marine Science Center - Multimedia
- Publications
Below are publications associated with this project.
Change in morphology and modern sediment thickness on the inner continental shelf offshore of Fire Island, New York between 2011 and 2014: Analysis of hurricane impact
Seafloor mapping investigations conducted on the lower shoreface and inner continental shelf offshore of Fire Island, New York in 2011 and 2014, the period encompassing the impacts of Hurricanes Irene and Sandy, provide an unprecedented perspective regarding regional inner continental shelf sediment dynamics during large storm events. Analyses of these studies demonstrate that storm-induced eroAuthorsWilliam C. Schwab, Wayne E. Baldwin, John C. Warner, Jeffrey H. List, Jane F. Denny, Maria Liste Munoz, Ilgar SafakAssessing the impact of Hurricanes Irene and Sandy on the morphology and modern sediment thickness on the inner continental shelf offshore of Fire Island, New York
This report documents the changes in seabed morphology and modern sediment thickness detected on the inner continental shelf offshore of Fire Island, New York, before and after Hurricanes Irene and Sandy made landfall. Comparison of acoustic backscatter imagery, seismic-reflection profiles, and bathymetry collected in 2011 and in 2014 show that sedimentary structures and depositional patterns moveAuthorsWilliam C. Schwab, Wayne E. Baldwin, Jane F. DennyThe impact of Hurricane Sandy on the shoreface and inner shelf of Fire Island, New York: large bedform migration but limited erosion
We investigate the impact of superstorm Sandy on the lower shoreface and inner shelf offshore the barrier island system of Fire Island, NY using before-and-after surveys involving swath bathymetry, backscatter and CHIRP acoustic reflection data. As sea level rises over the long term, the shoreface and inner shelf are eroded as barrier islands migrate landward; large storms like Sandy are thought tAuthorsJohn A. Goff, Roger D. Flood, James A. Austin, William C. Schwab, Beth A. Christensen, Cassandra M. Browne, Jane F. Denny, Wayne E. BaldwinMaps showing the change in modern sediment thickness on the Inner Continental Shelf offshore of Fire Island, New York, between 1996-97 and 2011
The U.S. Geological Survey mapped approximately 336 square kilometers of the lower shoreface and inner continental shelf offshore of Fire Island, New York, in 1996 and 1997, using high-resolution sidescan-sonar and seismic-reflection systems, and again in 2011, using interferometric sonar and high-resolution chirp seismic-reflection systems. This report presents a comparison of sediment thicknessAuthorsWilliam C. Schwab, Wayne E. Baldwin, Jane F. DennyMaps showing bathymetry and modern sediment thickness on the inner continental shelf offshore of Fire Island, New York, pre-Hurricane Sandy
The U.S. Geological Survey mapped approximately 336 square kilometers of the lower shoreface and inner continental shelf offshore of Fire Island, New York, in 2011 by using interferometric sonar and high-resolution chirp seismic-reflection systems. This report presents maps of bathymetry, acoustic backscatter, the coastal plain unconformity, the Holocene marine transgressive surface, and modern seAuthorsWilliam C. Schwab, Jane F. Denny, Wayne E. BaldwinModification of the Quaternary stratigraphic framework of the inner-continental shelf by Holocene marine transgression: An example offshore of Fire Island, New York
The inner-continental shelf off Fire Island, New York was mapped in 2011 using interferometric sonar and high-resolution chirp seismic-reflection systems. The area mapped is approximately 50 km long by 8 km wide, extending from Moriches Inlet to Fire Island Inlet in water depths ranging from 8 to 32 m. The morphology of this inner-continental shelf region and modern sediment distribution patternsAuthorsWilliam C. Schwab, Wayne E. Baldwin, Jane F. Denny, Cheryl J. Hapke, Paul T. Gayes, Jeffrey H. List, John C. WarnerHigh-resolution swath interferometric data collected within Muskeget Channel, Massachusetts
Swath interferometric bathymetery data were collected within and around Muskeget Channel and along select nearshore areas south and east of Martha's Vineyard, Massachusetts. Data were collected aboard the U.S. Geological Survey research vessel Rafael in October and November 2010 in a collaborative effort between the U.S. Geological Survey and the Woods Hole Oceanographic Institution. This report dAuthorsElizabeth A. Pendleton, Jane F. Denny, William W. Danforth, Wayne E. Baldwin, Barry J. Irwin