Online Links:
| Range of values | |
|---|---|
| Minimum: | 1972 |
| Maximum: | 2024 |
| Value | Definition |
|---|---|
| NA | Not referenced or assessed in the source material, or no interpretation available. |
| Y | Positively identified or inferred from supporting evidence in the source material. |
| Value | Definition |
|---|---|
| NA | Not referenced or assessed in the source material, or no interpretation available. |
| Y | Positively identified or inferred from supporting evidence in the source material. |
| Value | Definition |
|---|---|
| NA | Not referenced or assessed in the source material, or no interpretation available. |
| Y | Positively identified or inferred from supporting evidence in the source material. |
| Value | Definition |
|---|---|
| NA | Not referenced or assessed in the source material, or no interpretation available. |
| Y | Positively identified or inferred from supporting evidence in the source material. |
| Value | Definition |
|---|---|
| NA | Not referenced or assessed in the source material, or no interpretation available. |
| Y | Positively identified or inferred from supporting evidence in the source material. |
| Value | Definition |
|---|---|
| NA | Not referenced or assessed in the source material, or no interpretation available. |
| Y | Positively identified or inferred from supporting evidence in the source material. |
| Value | Definition |
|---|---|
| NA | Not referenced or assessed in the source material, or no interpretation available. |
| Y | Positively identified or inferred from supporting evidence in the source material. |
| Value | Definition |
|---|---|
| B | The domain was created by applying a buffer around a feature, such as a 10 km buffer around a coast. |
| DPR | The domain was derived, unaltered, from reputable and publicly accessible repositories, such as government, academic, or organizational data portals (e.g., USGS or NOAA) and only applies to vector format source data. The original geometry was preserved and reprojected into the Geographic Coordinate System (GCS) WGS 1984 to standardize spatial references. |
| GF | The domain was digitized after georeferencing a non-geospatial image into a spatial reference system. |
| MA | The domain was edited manually to refine boundaries or fix inconsistencies. |
| NAT | The domain was created, in part, using original geospatial data layers such as rasters, shapefiles, or other GIS data. The data type employed is specified by the second-order element which immediately follows, e.g., 'R' or 'V'. |
| R | The domain was created in part using the domain of original geospatial raster data such as bathymetry. |
| SG | The domain was created by simplifying complex geometries, for easier analysis or visualization. This may utilize simplification methods such as minimum bounding geometry (featuring geometry types such as convex hull and envelopes), simplify polygon, and smooth polygon. |
| V | The domain was created in part using the domain of native manual or automated interpretations of vector data, such as geological polygons or habitat boundaries. This element does not pertain to administrative or political boundaries from external sources. |
| VBD | The domain boundary was based on vector data of natural or artificial features, such as coastlines or administrative limits derived from sources external to the original study. |
| Value | Definition |
|---|---|
| B | The domain was created by applying a buffer around a feature, such as a 10 km buffer around a coast. |
| DC | The study domain was georeferenced and digitized to a point using coordinates provided in the source material. |
| DPR | The domain was derived, unaltered, from reputable and publicly accessible repositories, such as government, academic, or organizational data portals (e.g., USGS or NOAA) and applies to vector format source data. The original geometry was preserved and reprojected into the Geographic Coordinate System (GCS) WGS 1984 to standardize spatial references. |
| GF | The domain was digitized after georeferencing a non-geospatial image into a spatial reference system. |
| MA | The domain was edited manually to refine boundaries or fix inconsistencies. |
| NAT | The domain was created, in part, using original geospatial data layers such as rasters, shapefiles, or other GIS data. The data type employed is specified by the second-order element which immediately follows, e.g., 'R' or 'V'. |
| R | The domain was created in part using the domain of original geospatial raster data such as bathymetry. |
| SG | The domain was created by simplifying complex geometries, for easier analysis or visualization. This may utilize simplification methods such as minimum bounding geometry (featuring geometry types such as convex hull and envelopes), simplify polygon, and smooth polygon. |
| V | The domain was created in part using the domain of native manual or automated interpretations of vector data, such as geological polygons or habitat boundaries. This element does not pertain to administrative or political boundaries from external sources. |
| VBD | The domain boundary was based on vector data of natural or artificial features, such as coastlines or administrative limits derived from sources external to the original study. |
| Value | Definition |
|---|---|
| Anchorages, dumping grounds, disposal sites | (ANTHR) Human-made objects or designated use zones that that may present a physical or administrative boundary to offshore development activities. These specific items for this classification are anchorages, dumping grounds and disposals sites on the sea floor typically identified from sonar imagery, magnetometer data, seismic reflection profiles, or public inventories. |
| Areas Prone to scour | (MOBBED) Areas where sediment removal by hydrodynamic forces is likely to occur or has been observed. Scour processes may reduce sediment cover or undercut foundations. This classification includes both localized scour (e.g., around boulders, debris, or structures) and broader areas.
Interpretations may be based on direct observation of scour features or inferred from environmental conditions such as high current velocity, exposed substrates, coarse-grained soils, or sparse sediment cover. Areas may be classified as prone to scour even when specific features are not resolved, if the hydrodynamic setting or sediment context suggests increased erosion potential based on information in the source material documentation. |
| Bedform migration | (MOBBED) Any sea floor where bedforms are observed to migrate on an engineering timescale. This classification is based on the interpreted or observed movement of bedforms across the sea floor, whether based on repeat survey comparison, sediment transport modeling, or direct mention in the source material. This classification may be used to document active migration or the absence of movement. Migration may involve isolated features or entire bedform fields and is often used to infer forcing activity, sediment availability, or stability of the seabed. |
| Buried channels | (SUBSURF) Paleochannels are complex stratigraphic features which typically contain a heterogeneous infill of soft muds, peats, organics, and coarse lag which fill ancient river or inlets that have been buried by the younger sediment. They present unique challenges in predicting subsurface conditions as their geometry, infill material, and internal stratigraphy often vary significantly over short distances. Seismic reflection profiling and geotechnical sampling are used to interpret these features within the broader geologic framework. |
| Cables | (ANTHR) This class is one of several which identify known or interpreted anthropogenic features or boundaries. This class identifies known or interpreted cables on or near the seafloor. These features are typically derived from sonar imagery, magnetometer data, or public inventories. Mitigation measures such as avoidance buffers or additional investigations may be specified by the source material. |
| Fault scarps | (STRUCT) Surficial expressions of faults, one of several classes part of the broader group of structural features. These features are characterized by linear breaks or steps and may mark the expressions of underlying fault structures and therefore may overlap with other hazard classes. These features are identified using sonar data, but their geometry, extent, and activity may be further characterized with seismic reflection profiles. |
| Faults | (STRUCT) Refers to a planar fracture or discontinuity in a volume of rock, indurated sediment or consolidated sediment across which there has been significant displacement as a result of mass movements.
These features are typically identified using seismic reflection profiles, which may reveal their geometry, extent, and activity. While sonar data may highlight surface expressions, such interpretations are more appropriately captured under the Fault Scarps class. Faults can deform overlying sediments and act as conduits for fluid migration, which may result in overlap with other hazard classes. In many cases, faults referenced in source material have been previously identified through legacy investigations or regional geologic studies. |
| Gas hydrates | (GAS) A naturally occurring, ice-like substance that forms when water and gas combine under high pressure and at moderate temperatures. Methane is the most common gas present in gas hydrate, although other gases may also be included in hydrate structures, particularly in areas close to conventional oil and gas reservoirs. Gas hydrate is widespread in ocean-bottom sediments at water depths greater than 300–500 meters and is also present in areas with permanently frozen ground (permafrost). Gas hydrates may contribute to soil instability when disturbed. Interpretations of gas hydrates are derived from seismic reflection profiling. |
| Glacial till | (HARDBOT) Poorly-sorted ice-contact sediments typically comprised of a dense mixture of clay, silt, sand, gravel, and cobble- to boulder-sized clasts. Till may exhibit high penetration resistance. It may also exhibit high soil heterogeneity due to complex depositional sequences and glacial reworking and deformation. The presence of till may be inferred using seismic reflection data, grab or core samples, and regional geologic framework context. It may occur on the sea floor or in the subsurface. Material which is characteristic of till is not always explicitly interpreted as such by the source. This class may overlap with other ice-contact classes such as moraines or boulder fields. |
| Glauconite | (SUBSURF) Iron-potassium micaceous clay of the illite family that occurs in both ancient and modern marine environments. In this geopackage 'Glauconite' encompasses glauconite, glauconitic sands and green sands. Glauconite is deposited in low-energy marine settings and its authigenic form is typically found in marine deposits at the base of transgressive system sequences. Glauconite-bearing sediments may resist penetration and result in monopile refusal. Interpretations of glauconite-rich sediment are typically verified by geotechnical sampling and complemented by seismic reflection profiling. |
| Mass transport scarps | (SLOPE) An abrupt change in relief related to a mass movement. These features are identified as surficial expressions of gravity-induced slope failure events, including landslides and debris flows. Sonar data may be used to identify steep escarpments and arcuate headwalls which are indicative of these features. Seismic reflection profiling may be used to further characterize their age, origin, extent, and the potential for future instability. |
| Megaripples | (MOBBED) Medium-scale bedforms that have a wavelength of 5-60 meters and a height between 0.5-1.5 meters. However, this classification may also apply to megaripple-like features described in source material that lack defined geometry. While often associated with active sediment transport, features may also represent relict (non-mobile) forms preserved from past depositional conditions. Megaripple fields may occur in isolation or as part of larger bedform complexes (e.g., sand waves and sand ridges). Interpretations may reflect the presence, type, geometry, and distribution of bedforms; evidence of migration or orientation; and indicators of sediment transport and supply. Interpretations may also incorporate observations of active scour, zones of high mobility, or sediment thickness conducive to ripple formation. |
| Moraines | (HARDBOT) The accumulation of unsorted sediments deposited by a glacier typically as ridges, mounds, or irregular terrain at the edges or extremity of the glacier position. This class identifies areas where glacial moraines are present or inferred on the sea floor or in the shallow subsurface.
Interpretations derived from the source material may be based on bathymetric and backscatter expression, sub-bottom reflectors, geologic mapping, or regional geologic context. This class may overlap with ice-contact classes such as glacial till or boulder fields. |
| Organic soil | (SUBSURF) Refers to substrates rich in organic material, typically fine-grained (e.g., soft clays, silts) and low in shear strength. They are associated with low-energy depositional settings such as estuaries and lagoons. They may be prone to compression, differential settlement, and exhibit low bearing capacity. They may also be associated with gaseous sediments. Interpretations of organic sediment are typically verified by geotechnical sampling and complemented by seismic reflection profiling. |
| Other seabed obstructions | (ANTHR) This class identifies anthropogenic features or boundaries not otherwise categorized—such as unidentified debris, anchors, or submerged infrastructure. These features may represent physical hazards, cultural resources, or administrative boundaries. Mitigation measures such as avoidance buffers or additional investigations may be specified by the source material. In some instances, these features or objects are identified in geophysical data and addressed in the source material. |
| Outcrops, reefs, or exposed rocky areas | (HARDBOT) This classification includes natural bedrock outcrops, reef structures (biotic or abiotic), and other zones of exposed hardbottom. Features may present as ridges, scarps, elevated rock platforms, or irregular (e.g., hummocky) terrain, and are typically identified through sonar imagery, seismic reflection profiling, or regional geologic characterization. If identified in the subsurface, the depth of these features is sometimes constrained. This class is distinct from “Shallow Bedrock” in that it identifies only surficial expressions. |
| Peat | (SUBSURF) This class identifies the presence of peat, which is a fibrous organic-rich sediment deposited in low-energy marsh or bog environments. Peats are highly compressible, exhibit low shear strength, and may present challenges to cable heat dissipation. Interpretations of peat are typically verified by geotechnical sampling and complemented by seismic reflection profiling. |
| Pipelines | (ANTHR) This class identifies known or interpreted pipelines on or near the seafloor. These features are typically derived from sonar imagery, magnetometer data, or public inventories. Mitigation measures such as avoidance buffers or additional investigations may be specified by the source material. |
| Pockmarks | (GAS) Sea floor craters usually associated with fluid or gas escape from seabed sediments. These features are typically identified through sonar data and may occur singly or in clusters. Due to their typically steep sidewalls, their presence can present both slope and gas-related hazards. |
| Ripples | (MOBBED) small-scale bedforms typically less than 5 meters in wavelength and 0.5 meters in height, however, this classification may also apply to ripple-like features described in source material that lack defined geometry. While often associated with active sediment transport, features may also represent relict (non-mobile) forms preserved from past depositional conditions. Ripple fields may occur in isolation or as part of larger bedform complexes (e.g., megaripples, sand waves).
Interpretations may reflect the presence, type, geometry, and distribution of bedforms; evidence of migration or orientation; and indicators of sediment transport and supply. Interpretations may also incorporate observations of active scour, zones of high mobility, or sediment thickness conducive to ripple formation. |
| Sand resource areas | (ANTHR) Refers to areas identified by BOEM as having sand that may be mined, and areas hosting active or inactive borrow sites. These areas designated for sand extraction are typically used for beach nourishment or coastal restoration. These zones may be protected from conflicting activities and are often defined by federal or state sediment resource programs. In addition to the resource implications, these areas may be susceptible to significant morphological changes. Mitigation measures such as avoidance buffers or additional investigations may be specified by the source material. |
| Sand ridges | (MOBBED) Elongated sand bodies that are larger and geographically more stable than dunes or sand waves. These are large-scale features which far exceed the scale of sand wave bedforms and are not typically defined by specific height or wavelength parameters. They often appear as shore-oblique or shore-parallel features with a ridge-and-swale morphology. These features may reflect past depositional regimes and are often considered quasi-stable or relict, but their form is attributed to wave- and current-driven sediment transport. Sand ridges may occur independently or in association with smaller-scale bedforms (e.g., sand waves, ripples).
Interpretations may reflect the presence, type, geometry, and distribution of bedforms; evidence of migration or orientation; and indicators of sediment transport and supply. Interpretations may also incorporate observations of active scour, zones of high mobility, or sediment thickness conducive to bedform development. |
| Sand waves | (MOBBED)Large-scale bedforms typically exceeding 60 meters in wavelength and 1.5 meters in height, however, this classification may also apply to sand-wave-like features described in source material that lack defined geometry. While often associated with active sediment transport, features may also represent relict (non-mobile) forms preserved from past depositional conditions. Sand waves may occur in isolation or as part of bedform complexes (e.g., ripples, megaripples).
Interpretations may reflect the presence, type, geometry, and distribution of bedforms; evidence of migration or orientation; and indicators of sediment transport and supply. Interpretations may also incorporate observations of active scour, zones of high mobility, or sediment thickness conducive to ripple formation. |
| Shallow bedrock | (HARDBOT) Refers to features characterized by consolidated, semi-consolidated, or otherwise hard substrate buried by younger sediments that resides within tens of meters of the sea floor. |
| Shallow gas or gas seeps | (GAS) Refers to the gas trapped in shallow sediments that can be derived from biogenic activities or seeping upwards from a deeper gas reservoir source.
Shallow gas or gas seeps can be inferred from acoustic blanking, gas chimneys, or water column anomalies identified in seismic reflection and sonar data. Indications of gas may also be identified from geotechnical sampling. |
| Shipwrecks | (ANTHR) Remnants of a ship once it has sunk to the sea floor. These features are typically derived from sonar imagery, magnetometer data, or public inventories. Mitigation measures such as avoidance buffers or additional investigations may be specified by the source material. |
| Slides | (SLOPE) Refers to a mass movement where slide material is separated from more stable underlying material. Slides are identified as areas of mass movement where distinct blocks of sediments have been displaced along shear failure surfaces. Sonar data may identify morphological indicators of sliding and seismic reflection profiling may resolve disturbed stratigraphy. Both sources of data may be used to infer the age of sliding, its extent, and the potential for future instability. |
| Slumps | (SLOPE) Refers to a coherent mass of loosely consolidated material that moved down a slope. Slumps are identified as areas of rotational mass movement and deformation. Sonar data may identify morphological indicators of slumping and seismic reflection profiling may resolve deformed stratigraphy and concave upward reflectors. Both sources may be used to infer the age of slumping, its extent, and the potential for future instability. |
| Steep slopes | (SLOPE) A slope of 10 degrees or greater. However, this class may also include features or areas described as steep or potentially unstable without explicit slope measurements.
Interpretations may indicate sea-floor morphology, adjacent geomorphic features (e.g., scarps, bedform faces), or areas inferred to have higher mass movement or erosional risk. Descriptions may vary depending on data resolution and whether slope instability is actively assessed. |
| Subsurface boulders | (HARDBOT) This class identifies buried features interpreted as boulders located beneath the sea-floor surface, typically within glacial or para-glacial sedimentary units. These features may pose hazards to foundation and cable installation.
Interpretations are derived from seismic reflection data. As with surface boulders, this classification is limited by the resolution and penetration of available data and is not based on strict grain-size definitions. Subsurface boulders are often inferred in areas underlain by till, moraine, or other heterogeneous glacial deposits. |
| Subsurface deformation | (SUBSURF) Refers to disrupted stratigraphy that has undergone deformation due mechanisms such as folding, shearing, and thrusting. These features are identified in seismic reflection profiles as warped reflectors, however they may not correspond to discrete fault planes. Many deformational features are glaciotectonic in origin, formed by ice loading or thrusting. |
| Surface boulders | (HARDBOT) This class identifies isolated or clustered features interpreted as boulders present at or near the sea floor surface. Classification is based primarily on data such as sonar, bathymetry, and backscatter. The ability to resolve individual boulder features is constrained by the resolution of the dataset. Consequently, this classification is not tied to a strict grain-size threshold. Instead, it includes clastic features that are visibly distinct in geophysical data and interpreted as potential obstructions.
Boulders may occur as isolated features or within mapped boulder fields and are often associated with glacial deposits or coarse lag surfaces. |
| Unclassified bedforms | (MOBBED) Any bedforms that are not classified as ripples, megaripples, sand waves or sand ridges. Unclassified bedforms are used where the term “bedform” is mentioned in source material without clear attribution to a specific type. This classification also applies when features are noted based on acoustic signature or generalized morphology but lack sufficient resolution or description to assign to a defined category. It may reflect uncertainty in scale, geometry, or process interpretation.
Interpretations may reflect the presence, type, geometry, and distribution of bedforms; evidence of migration or orientation; and indicators of sediment transport and supply. Interpretations may also incorporate observations of active scour, zones of high mobility, or sediment thickness conducive to bedform development. |
| UXO/MEC | (ANTHR) Identifies known or interpreted unexploded ordnance (UXO) or munitions of explosive concern (MEC) on or near the seafloor.
These features are typically derived from sonar imagery, magnetometer data, or public inventories. Mitigation measures such as avoidance buffers or additional investigations may be specified by the source material. |
| Value | Definition |
|---|---|
| NA | Not referenced or assessed in the source material, or no sufficient interpretation available. |
| N | Explicitly confirmed absent within the area of interest, to the extent permitted by the resolution, coverage, and quality of available data. |
| Y | Positively identified or inferred from supporting evidence in the source material. |
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| Access_Constraints | No access constraints. |
|---|---|
| Use_Constraints | No use constraints. |
| Data format: | information content in format geopackage (GPKG) (version Created in ArcGIS Pro v. 3.4, subsequent edits in QGIS 3.4 or Navicat Premium v. 16 database management tool.) Size: 70 |
|---|---|
| Network links: |
https://www.sciencebase.gov/catalog/file/get/67dacd32d34ef1653388702f https://www.sciencebase.gov/catalog/item/67dacd32d34ef1653388702f https://doi.org/10.5066/P1SLUTW9 |