CMECS geoform, substrate, and biotopes offshore of Tacoma, Washington

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Frequently anticipated questions:


What does this data set describe?

Title:
CMECS geoform, substrate, and biotopes offshore of Tacoma, Washington
Abstract:
This part of USGS Data Series 935 (Cochrane, 2014) presents substrate, geomorphic, and biotope data in the Offshore of Tacoma, Washington, map area, a part of the Southern Salish Sea Habitat Map Series. Given the variable bathymetric resolution, the complex geologic history of the region, and the lack of acoustic backscatter data, automated and semi-automated classification schemes of classifying seafloor substrate and geoform were deemed to have very low accuracy. Instead, classification of these properties was performed manually following the Coastal and Marine Ecological Classification Standard (CMECS; Federal Geographic Data Committee, 2012) using observations from underwater video footage. The best overall predictors of biotic assemblage were used to generate the CMECS biotopes. However, the nature of the biological data gathered makes it difficult to define clear biotopes. It was difficult to see or identify many organisms in the underwater video, and with an average of only 3-4 taxa identified per sampling unit, it is hard to characterize biotic assemblages. Some biological clusters of taxa were identified statistically for multiple map areas, and within each area, some of these groupings were found at consistent depths and/or with predictable substrates. The maps are not fine-grained enough to capture the physical variation seen within one-minute video units. Depth zones in the biotope map are based on Dethier (1992).
Supplemental_Information:
Additional information about the USGS field activities from which some of these data were derived is available online at https://cmgds.marine.usgs.gov/fan_info.php?fan=K109WO https://cmgds.marine.usgs.gov/fan_info.php?fan=K0111PS https://cmgds.marine.usgs.gov/fan_info.php?fan=M0111PS https://cmgds.marine.usgs.gov/fan_info.php?fan=M0112PS https://cmgds.marine.usgs.gov/fan_info.php?fan=M0212PS https://cmgds.marine.usgs.gov/fan_info.php?fan=G395PS https://cmgds.marine.usgs.gov/fan_info.php?fan=G297PS
Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government.
Although this Federal Geographic Data Committee-compliant metadata file is intended to document the data set in nonproprietary form, as well as in Esri format, this metadata file may include some Esri-specific terminology.
  1. How might this data set be cited?
    Hodson, Timothy O., Cochrane, Guy R., and Dethier, Megan N., 20230315, CMECS geoform, substrate, and biotopes offshore of Tacoma, Washington: data release DOI:10.5066/P9KA6GH2, U.S. Geological Survey, Pacific Coastal and Marine Science Center, Santa Cruz, CA.

    Online Links:

    This is part of the following larger work.

    Cochrane, Guy R., 2023, Bathymetry and topography, video observation, and derived benthic habitat data offshore of Tacoma, Washington: data release DOI:10.5066/P9KA6GH2, U.S. Geological Survey, Pacific Coastal and Marine Science Center, Santa Cruz, CA.

    Online Links:

  2. What geographic area does the data set cover?
    West_Bounding_Coordinate: -122.788145
    East_Bounding_Coordinate: -122.394044
    North_Bounding_Coordinate: 47.349263
    South_Bounding_Coordinate: 47.077903
  3. What does it look like?
    CMECS_OffshoreTacoma.jpg (JPEG)
    Shaded-relief map of Offshore of Tacoma map area showing seafloor classified into CMECS substrate classes.
  4. Does the data set describe conditions during a particular time period?
    Calendar_Date: 2013
    Currentness_Reference:
    ground condition
  5. What is the general form of this data set?
    Geospatial_Data_Presentation_Form: vector digital data
  6. How does the data set represent geographic features?
    1. How are geographic features stored in the data set?
      This is a Vector data set. It contains the following vector data types (SDTS terminology):
      • GT-polygon composed of chains (3422)
    2. What coordinate system is used to represent geographic features?
      The map projection used is NAD 1983 UTM Zone 10N.
      Projection parameters:
      Scale_Factor_at_Central_Meridian: 0.9996
      Longitude_of_Central_Meridian: -123.0
      Latitude_of_Projection_Origin: 0.0
      False_Easting: 500000.0
      False_Northing: 0.0
      Planar coordinates are encoded using coordinate pair
      Abscissae (x-coordinates) are specified to the nearest 0.000000002220024164500956
      Ordinates (y-coordinates) are specified to the nearest 0.000000002220024164500956
      Planar coordinates are specified in meter
      The horizontal datum used is D North American 1983.
      The ellipsoid used is GRS 1980.
      The semi-major axis of the ellipsoid used is 6378137.0.
      The flattening of the ellipsoid used is 1/298.257222101.
  7. How does the data set describe geographic features?
    Polygon
    Polygons representing geologic/geomorphic map units (Source: This report)
    FID
    Internal feature number. (Source: Esri)
    Range of values
    Minimum:0
    Maximum:3819
    Shape
    feature type (Source: Esri) polygon type vector object
    geoform
    CMECS level 1 geoform structure, blank values indicate polygon was not assigned a geoform (Source: CMECS)
    ValueDefinition
    apronextensive blanket-like deposit of alluvial unconsolidated material derived from an identifiable source and deposited at the base of a high standing area
    basinlow relief area that lies below the surrounding bottom/terrain elevation
    boulder fieldan area dominated by large (boulder-sized) stones or pieces of rock
    channela linear or sinuous depression on an otherwise more flat area, for example, a small or large valley-like or groove-like feature through which rivers or tidal creeks flow
    deltathe low, nearly flat, alluvial tract of land at or near the mouth of a river, commonly forming a triangular or fan-shaped plain of considerable area
    depressiona low-lying area surrounded by higher ground often having no natural outlet.
    dredge depositfan or mound deposit of sediment from dredging
    dredged channelanthropogenic dredging for navigation
    drumlinmound or ridge formed beneath flowing glacier
    fana low, outspread, relatively flat to gently sloping mass of loose material, shaped like an open fan or a segment of a cone, deposited by a flow of water at the place where it issues from a narrower or steeper gradiant area into a broader area, valley, flat, or other feature
    gullya ravine formed by the action of water
    jettyanthropogenic structure to protect coastal feature from wave erosion
    lagoona shallow, highly enclosed, body of water with reduced exchange with the ocean, often experiencing high evaporation, and quiescent in terms of wind, current, and wave energy
    marinaanthropogenic structure for docking boats and ships
    morainemound, ridge, or other distinct accumulation of unsorted, unstratified glacial drift, predominantly till, deposited chiefly by direct action of glacier ice
    pieranthropogenic near sea-level structure for access to the water
    platforma level or nearly level surface, ranging in size from a terrace or bench to a plateau
    relic shore complexsubmerged archeo-shoreline
    relic tidal flatsubmerged archeo-tidal flat
    scarpa relatively straight, cliff-like face or slope of considerable linear extent, breaking the general continuity of the land by separating surfaces lying at different levels, as along the margin of a plateau or mesa
    sediment wave fieldarea of coarse sediment worked into waves by bottom currents
    shoreintersection of a specified plane of water with the beach
    sillrise at the mouth of a fjord caused by reduced erosion and added to by the glacier's terminal moraine
    slopecontiguous sloping area between shelf and basin
    submarine slide depositloose mass of angular rock fragments created by mass-movement downslope of soil and rock material en masse
    tidal channelchannel formed by erosion from tidal currents
    tidalite driftan area of sediment deposited by tidal activity
    tect_setti
    tectonic setting of the polygon (Source: CMECS)
    ValueDefinition
    Convergent Active Continental Marginarea is located on an active continental margin
    physgrphc_
    physiograpinc setting of the area (Source: CMECS)
    ValueDefinition
    fjorda long, narrow, winding glacially eroded inlet or arm of the sea
    geoform_or
    Geoform Origin (Source: CMECS)
    ValueDefinition
    anthropogenicbuilt by or created by human activity
    geologicformed by abiotic processes
    geoform_ty
    Geoform Type, level 2 CMECS geoforms, blank values indicate polygon was not assigned a value for this attribute (Source: CMECS)
    ValueDefinition
    basin floor fangravity flow sediment deposit in a basin from the surrounding higher terrain
    breakwater/jettystructures extending more or less perpendicularly from the shore into a body of water and designed to direct and confine the current or tide, to protect a harbor, or to prevent shoaling of a navigable inlet aby littoral materials
    ebb tide deltaa largely subaqueous (sometimes intertidal) crudely fan-shaped deposit of sand-sized sediment formed on the seaward side of a tidal inlet
    erosion scarprelatively straight, cliff-like face or slope of considerable linear extent, breaking the general continuity of the topography by separating surfaces lying at different levels, as along the margin of an erosional channel
    relic wave-cut platforma level area formed by wave erosion during a time of lower sea level
    scour depressiona sedimented area deepened and winnowed by the action of bottom currents
    slopecontiguous sloping area between shelf and basin
    slope gullysmall, discontinuous submarine valley, usually formed by slumping along a fault scarp or the slope of a basin, canyon, or valley
    tidal channelchannel formed by erosion from tidal currents
    geoform_DI
    Combination of level 1 or level 2 (if exists) CMECS geoforms for map symbolization, blank values indicate polygon was not assigned a value for this attribute (Source: CMECS)
    ValueDefinition
    apronextensive blanket-like deposit of alluvial unconsolidated material derived from an identifiable source and deposited at the base of a high standing area
    basinlow relief area that lies below the surrounding bottom/terrain elevation
    basin floor fangravity flow sediment deposit in a basin from the surrounding higher terrain
    boulder fieldan area dominated by large (boulder-sized) stones or pieces of rock
    breakwater/jettyanthropogenic structure to protect coastal feature from wave erosion
    deltathe low, nearly flat, alluvial tract of land at or near the mouth of a river, commonly forming a triangular or fan-shaped plain of considerable area
    depressiona low-lying area surrounded by higher ground often having no natural outlet.
    dredge depositfan or mound deposit of sediment from dredging
    dredged channelanthropogenic dredging for navigation
    drumlinmound or ridge formed beneath flowing glacier
    ebb tide deltaa largely subaqueous (sometimes intertidal) crudely fan-shaped deposit of sand-sized sediment formed on the seaward side of a tidal inlet
    erosion scarprelatively straight, cliff-like face or slope of considerable linear extent, breaking the general continuity of the topography by separating surfaces lying at different levels, as along the margin of an erosional channel
    lagoona shallow, highly enclosed, body of water with reduced exchange with the ocean, often experiencing high evaporation, and quiescent in terms of wind, current, and wave energy
    marinaanthropogenic structure for docking boats and ships
    morainemound, ridge, or other distinct accumulation of unsorted, unstratified glacial drift, predominantly till, deposited chiefly by direct action of glacier ice
    pieranthropogenic near sea-level structure for access to the water
    relic shore complexsubmerged archeo-shoreline
    relic tidal flatsubmerged archeo-tidal flat
    relic wave-cut platforma level area formed by wave erosion during a time of lower sea level
    scour depressiona sedimented area deepened and winnowed by the action of bottom currents
    sediment wave fieldarea of coarse sediment worked into waves by bottom currents
    shoreintersection of a specified plane of water with the beach
    sillrise at the mouth of a fjord caused by reduced erosion and added to by the glacier's terminal moraine
    slopecontiguous sloping area between shelf and basin
    slope gullysmall, discontinuous submarine valley, usually formed by slumping along a fault scarp or the slope of a basin, canyon, or valley
    submarine slide depositloose mass of angular rock fragments created by mass-movement downslope of soil and rock material en masse
    tidal channelchannel formed by erosion from tidal currents
    tidalite driftan area of sediment deposited by tidal activity
    Shape_Area
    area of the polygon in square meters (Source: ESRI)
    Range of values
    Minimum:80.935
    Maximum:186910915.995
    Units:square meters
    Resolution:0.001
    substr_cls
    Substrate Class, grain size classes within CMECS, blank values indicate polygon was not assigned a value for this attribute (Source: CMECS)
    ValueDefinition
    anthropogenic rocksubstrate that is composed of natural mineral materials that were deposited by humans
    rock substrateigneous, metamorhic, or sedimentary rock with particle sizes greater than or equal to 4.0 meters (4096 mm) in any dimension covers greater than or equal to 50 percent of the geologic substrate surface
    unconsolidated mineral substrategeologic substrates with less than 50 percent cover of rock substrate; uses Folk (1954) terminology to describe any mix of loose mineral substrate occurring at any range of sizes, from boulders to clay
    sbstr_scls
    Substrate Subclass, grain size sub-classes within the CMECS Substrate Class, blank values indicate insufficient information to determine a Substrate Subcls (Source: CMECS)
    ValueDefinition
    anthropogenic rock rubblesubstrate that is dominated by anthropogenic rock with a median particle size of 64 mm to less than 4096 mm
    bedrocksubstrate with largely continuous formations of bedrock covering 50 percent or more of the surface
    coarse unconsolidated substratesubstrate surface layer containing any amount of gravel (particles greater than or equal to 2 mm), from a single grannule to 100 percent boulders.
    fine unconsolidated substratesubstrate surface layer containing no trace of gravel (particles greater than or equal to 2mm).
    substr_grp
    Substrate Group, grain size sub-classes within the Substrate Group, blank values indicate insufficient information to determine a Substrate Group (Source: CMECS or Hodson when the substrate value is not in the CMECS standard)
    ValueDefinition
    cobble mixsubstrate surface layer contains 30 percent to less than 80 percent cobble
    gravelsubstrate surface layer contains 80 percent or higher gravel
    gravel mixsubstrate surface layer contains 30 percent to less than 80 percent gravel
    gravellysubstrate surface layer contains 5 percent to less than 30 percent gravel
    mudsubstrate surface layer shows no trace of gravel and contains 90 percent or more mud
    muddy sandsubstrate surface layer shows no trace of gravel and contains 50 percent to less than 90 percent sand, with the remainder composed of mud
    sandsubstrate surface layer contains no trace of gravel and is composed of greater than or equal to 90 percent sand
    sandy mudsubstrate surface layer shows no trace of gravel and contains 10 percent to less than 50 percent sand, with the remainder composed of mud
    slightly gravellysubstrate surface layer contains a trace to < 5 percent gravel
    substr_sgr
    Substrate Subgroup narrower grain size classes than the CMECS Substrate Group, blank values indicate insufficient information to determine a Subgroup (Source: CMECS)
    ValueDefinition
    boulderboulders (256 mm to <4096 mm) constitute the median gravel size
    cobblecobbles constitute the median gravel size
    gravelly sandsubstrate is 5 percent to less than 30 percent gravel, with sand composing 90 percent or more of the remaining sand-mud mix
    sandy cobblesubstrate is 30 percent to < 80 percent cobble, with sand composing 90 percent or more of the remaining sand-mud mix
    sandy cobble mixsubstrate surface layer contains 30 percent to less than 80 percent cobble, with sand composing 90 percent or more of the remaining sand-mud mix
    sandy gravel mixsubstrate surface layer contains 30 percent to less than 80 percent gravel, with sand composing 90 percent or more of the remaining sand-mud mix
    slightly gravelly sandtrace to < 5 percent gravel, with sand composing 90 percent or more of the remaining sand-mud mix
    sbstr_orig
    Substrate Origin Federal Geographic Data Committee, 2012), blank values indicate insufficient information to determine a value (Source: CMECS)
    ValueDefinition
    anthropogenic substratedominant source of the substrate is man-made
    geologic substratedominant source of the substrate is either geologic or biogenic (but no longer living)
    substrate
    the value of the highest order substrate class attribute for the polygon for map symbolization (Source: CMECS)
    ValueDefinition
    anthropogenic rock rubblesubstrate that is dominated by anthropogenic rock with a median particle size of 64 mm to less than 4096 mm
    bedrocksubstrate with largely continuous formations of bedrock covering 50 percent or more of the surface
    boulderboulders (256 mm to <4096 mm) constitute the median gravel size
    coarse unconsolidated substratesubstrate surface layer containing any amount of gravel (particles greater than or equal to 2 mm), from a single grannule to 100 percent boulders.
    cobblecobbles constitute the median gravel size
    cobble mixsubstrate surface layer contains 30 percent to less than 80 percent cobble
    fine unconsolidated substratesubstrate surface layer containing no trace of gravel (particles greater than or equal to 2mm).
    gravelsubstrate surface layer contains 80 percent or higher gravel
    gravel mixsubstrate surface layer contains 30 percent to less than 80 percent gravel
    gravellysubstrate surface layer contains 5 percent to less than 30 percent gravel
    gravelly sandsubstrate is 5 percent to less than 30 percent gravel, with sand composing 90 percent or more of the remaining sand-mud mix
    mudsubstrate surface layer shows no trace of gravel and contains 90 percent or more mud
    muddy sandsubstrate surface layer shows no trace of gravel and contains 50 percent to less than 90 percent sand, with the remainder composed of mud
    sandsubstrate surface layer contains no trace of gravel and is composed of greater than or equal to 90 percent sand
    sandy cobblesubstrate is 30 percent to < 80 percent cobble, with sand composing 90 percent or more of the remaining sand-mud mix
    sandy cobble mixsubstrate surface layer contains 30 percent to less than 80 percent cobble, with sand composing 90 percent or more of the remaining sand-mud mix
    sandy gravel mixsubstrate surface layer contains 30 percent to less than 80 percent gravel, with sand composing 90 percent or more of the remaining sand-mud mix
    sandy mudsubstrate surface layer shows no trace of gravel and contains 10 percent to less than 50 percent sand, with the remainder composed of mud
    slightly gravelly sandtrace to < 5 percent gravel, with sand composing 90 percent or more of the remaining sand-mud mix
    unconsolidated mineral substrategeologic substrates with less than 50 percent cover of rock substrate; uses Folk (1954) terminology to describe any mix of loose mineral substrate occurring at any range of sizes, from boulders to clay
    depthzone
    Water depth classes from Dethier (1992) (Source: M.N. Dethier)
    ValueDefinition
    1water depths from 0 to less than 15 meters
    2water depths from 15 to less than 25 meters
    3water depths from 25 to less than 50 meters
    4water depths from 50 to less than 150 meters
    5water depths 150 meters or deeper
    group_a
    Biotic group characterized by any sea whip, bat, slime, sand, or leather sea stars, any species of surface-dwelling cucumber other than Parastichopus, and any flatfish on sand substrate in water depths greater than 50 meters (Source: M.N. Dethier)
    ValueDefinition
    0Biotic group is likely absent from area
    1Biotic group is likely present in area
    group_b
    Biotic group characterized by any rockfish on bedrock in water depths of 50 to 150 meters (Source: M.N. Dethier)
    ValueDefinition
    0Biotic group is likely absent from area
    1Biotic group is likely present in area
    group_c
    Biotic group characterized by any barnacle species, any encrusting invertebrate or corallines, colonial and solitary tube worms, and any Pisaster on coarse unconsolidated substrate, boulder, cobble, and megaclast substrate in water depths of 50 to 150 meters (Source: M.N. Dethier)
    ValueDefinition
    0Biotic group is likely absent from area
    1Biotic group is likely present in area
    group_d
    Biotic group characterized by any species of hydroid, any encrusting invertebrate or corallines, rock and swimming scallops, and sunflower star on cobble and gravel in water depths of 15 to 50 meters (Source: M.N. Dethier)
    ValueDefinition
    0Biotic group is likely absent from area
    1Biotic group is likely present in area
    group_e
    Biotic group characterized by any sculpins, crabs in the Cancer genus, and any sunstar on sand substrate in all water depths (Source: M.N. Dethier)
    ValueDefinition
    0Biotic group is likely absent from area
    1Biotic group is likely present in area
    group_f
    Biotic group characterized by any green algae, any bony fish not otherwise coded, and sunflower star on sand substrate in all water depths (Source: M.N. Dethier)
    ValueDefinition
    0Biotic group is likely absent from area
    1Biotic group is likely present in area
    group_g
    Biotic group characterized by any species of hydroid, any encrusting invertebrate or corallines, mottled, rainbow, black sea stars,orange sea pen, and colonial and solitary tube worms on gravel and cobble substrate in water depths of 50 to 150 meters (Source: M.N. Dethier)
    ValueDefinition
    0Biotic group is likely absent from area
    1Biotic group is likely present in area
    group_h
    Biotic group characterized by any species of hydroid, colonial and solitary tube worms, and metridium anemones on sand substrate in water depths of 25 to 150 meters (Source: M.N. Dethier)
    ValueDefinition
    0Biotic group is likely absent from area
    1Biotic group is likely present in area
    group_i
    Biotic group characterized by any species of hydroid, colonial and solitary tube worms, any burrowing anemone, and any Bryozoan, epilithic or epiphytic on sand and bedrock substrate in water depths of 25 to 150 meters (Source: M.N. Dethier)
    ValueDefinition
    0Biotic group is likely absent from area
    1Biotic group is likely present in area
    group_j
    Biotic group characterized by any species of hydroid, any burrowing anemone, and any sunstar on cobelly sand substrate in water depths of 25 to 150 meters (Source: M.N. Dethier)
    ValueDefinition
    0Biotic group is likely absent from area
    1Biotic group is likely present in area
    group_k
    Biotic group characterized by any Pisaster, any red algae, any encrusting invertebrate or corallines, and metridium anemones on sandb substrate in water depths of 15 to 150 meters (Source: M.N. Dethier)
    ValueDefinition
    0Biotic group is likely absent from area
    1Biotic group is likely present in area
    group_l
    Biotic group characterized by sunflower star, any brown algae, and metridium anemones on sand substrate in water depths of 0 to 50 meters (Source: M.N. Dethier)
    ValueDefinition
    0Biotic group is likely absent from area
    1Biotic group is likely present in area
    group_m
    Biotic group characterized by any brown algae, and any attached kelp species on sand substrate in water depths of 0 to 15 meters (Source: M.N. Dethier)
    ValueDefinition
    0Biotic group is likely absent from area
    1Biotic group is likely present in area
    group_n
    Biotic group characterized by any brown algae, any species of hydroid, any bivalve species not scallops, mostly mussels, any eelpout, and any sunstar on sand substrate in water depths of 50 to 150 meters (Source: M.N. Dethier)
    ValueDefinition
    0Biotic group is likely absent from area
    1Biotic group is likely present in area
    group_o
    Biotic group characterized by any species of hydroid, any attached kelp species, any brown algae, any sunstar, any burrowing anemone, and colonial and solitary tube worms on sand substrate in water depths of 50 to 150 meters (Source: M.N. Dethier)
    ValueDefinition
    0Biotic group is likely absent from area
    1Biotic group is likely present in area
    group_p
    Biotic group characterized by any species of hydroid, any red algae, any brown algae, any attached kelp species, and any green algae on sand, gravel substrate in water depths of 0 to 150 meters (Source: M.N. Dethier)
    ValueDefinition
    0Biotic group is likely absent from area
    1Biotic group is likely present in area
    group_q
    Biotic group characterized by colonial and solitary tube worms, colonial and solitary tube worms, any burrowing anemone, and blood star on unconsolidated substrate in all water depths (Source: M.N. Dethier)
    ValueDefinition
    0Biotic group is likely absent from area
    1Biotic group is likely present in area
    group_r
    Biotic group characterized by colonial and solitary tube worms, any burrowing anemone, and any species of hydroid on unconsolidated substrate in water depths of 50 to 150 mete (Source: M.N. Dethier)
    ValueDefinition
    0Biotic group is likely absent from area
    1Biotic group is likely present in area
    group_s
    Biotic group characterized by giant sea cucumber, colonial and solitary tube worms, and any burrowing anemone on unconsolidated substrate in water depths of 50 to 150 meters (Source: M.N. Dethier)
    ValueDefinition
    0Biotic group is likely absent from area
    1Biotic group is likely present in area
    group_t
    Biotic group characterized by any burrowing anemone, colonial and solitary tube worms, any nudibranch, and any sea whip on sand substrate in water depths of 25 to 50 meters (Source: M.N. Dethier)
    ValueDefinition
    0Biotic group is likely absent from area
    1Biotic group is likely present in area
    group_u
    Biotic group characterized by any burrowing anemone, any shrimp, and any sea whip on sand substrate in water depths greater than 50 meters (Source: M.N. Dethier)
    ValueDefinition
    0Biotic group is likely absent from area
    1Biotic group is likely present in area
    group_v
    Biotic group characterized by any eelpout, any species of hydroid, any sea whip, any shrimp, and colonial and solitary tube worms on sand substrate in water depths of 50 to 150 meters (Source: M.N. Dethier)
    ValueDefinition
    0Biotic group is likely absent from area
    1Biotic group is likely present in area
    biotope
    Combination of Dethier depth class and CMECS substrate subclass. (Source: M.N. Dethier and CMECS)
    ValueDefinition
    11fine unconsolidated sediment in depth zone 1
    12coarse unconsolidated sediment in depth zone 1
    21fine unconsolidated sediment in depth zone 2
    22coarse unconsolidated sediment in depth zone 2
    31fine unconsolidated sediment in depth zone 3
    32coarse unconsolidated sediment in depth zone 3
    33bedrock substrate in depth zone 3
    40unknown grain size unconsolidated sediment in depth zone 4
    41fine unconsolidated sediment in depth zone 4
    42coarse unconsolidated sediment in depth zone 4
    43bedrock substrate in depth zone 4
    50unknown grain size unconsolidated sediment in depth zone 5
    51fine unconsolidated sediment in depth zone 5
    52coarse unconsolidated sediment in depth zone 5
    53bedrock substrate in depth zone 5
    Entity_and_Attribute_Overview:
    shapefile consisting of 3,819 polygons classified into CMECS geoforms and substrate classes, and M.N. Dethier depth zones
    Entity_and_Attribute_Detail_Citation:
    Federal Geographic Data Committee, 2012, Coastal and Marine Ecological Classification Standard, 343 p., accessed March 10, 2022, at https://www.fgdc.gov/standards/projects/cmecs-folder/CMECS_Version_06-2012_FINAL.pdf
    Entity_and_Attribute_Detail_Citation:
    Dethier, M.N., 1992, Classifying marine and estuarine natural communities: An alternative to the Cowardin system: Natural Areas Journal, v. 12, p. 90-100, accessed July 23, 2022 at https://www.jstor.org/stable/43911274

Who produced the data set?

  1. Who are the originators of the data set? (may include formal authors, digital compilers, and editors)
    • Timothy O. Hodson
    • Guy R. Cochrane
    • Megan N. Dethier
  2. Who also contributed to the data set?
  3. To whom should users address questions about the data?
    U.S. Geological Survey, Pacific Coastal and Marine Science Center
    Attn: PCMSC Science Data Coordinator
    2885 Mission Street
    Santa Cruz, CA

    831-427-4747 (voice)
    pcmsc_data@usgs.gov

Why was the data set created?

To expand geologic mapping to the seafloor within Washington's State Waters, to update coastal habitat mapping, and to contribute to a uniform regional habitat database. Additionally, to provide a habitat map for the public and ecoscience community to aid in land-use and land-management decisions both onshore and offshore.

How was the data set created?

  1. From what previous works were the data drawn?
  2. How were the data generated, processed, and modified?
    Date: 2012 (process 1 of 3)
    Map unit Geoform polygons were digitized over underlying 2-meter base layers developed from multibeam bathymetry data, available elsewhere in this data release (BathyTopo_OffshoreTacoma data). The specificity of our CMECS geoform interpretations reflects the resolution of the underlying NOS bathymetry. Where there was sufficient resolution to attribute a particular genetic process to a geoform, we ascribed an appropriately specific geoform type. Where bathymetric resolution was low and the genetic interpretation equivocal, our geoform classifications were more generic. Seafloor geoforms were classified based on their physical attributes as observed in the NOS bathymetric surveys and USGS seismic reflection profiles from field activities G395PS and G297PS (Triezenberg and others, 2016) in combination with knowledge of common glacial and estuarine processes and interpretations from the regional geologic literature (Ballantyne, 2002; Booth, 1994; Burns, 1985).
    Date: 2012 (process 2 of 3)
    Areas near USGS seafloor video transects were classified with more specificity, down to Substrate Group or Substrate Subgroup, depending on proximity to ground-truthed transects and the local heterogeneity of the seafloor. Our classification of substrates in areas outside the primary study region was based primarily upon geomorphological interpretations drawn from historical NOS surveys and historical NOS seabed descriptions. Consequently, these interpretations are less specific; substrate classifications in these areas are typically limited to the Substrate Class or Substrate Subclass. The CMECS Substrate Component values are described in Federal Geographic Data Committee (2012).
    Date: 2012 (process 3 of 3)
    Depth zones classes in the biotope map are based on Dethier (1992). The biotope polygons were derived by merging (using the ArcGIS union tool) depth zone polygons with the CMECS geoform-substrate polygons and creating an integer code to represent the substrate class and depth zone of each polygon. A depthzone attribute was created that has Dethier (1992) attribute values.
  3. What similar or related data should the user be aware of?
    Folk, R.L., 1954, The Distinction between Grain Size and Mineral Composition in Sedimentary Rock Nomenclature.

    Other_Citation_Details:
    Folk, R.L., The Distinction between Grain Size and Mineral Composition in Sedimentary Rock Nomenclature: J. Geol., v. 62, p. 344-359.
    Cochrane, Guy R., 2014, Southern Salish Sea Habitat Map Series Data Catalog.

    Online Links:

    Other_Citation_Details:
    Cochrane, G.R., compiler, 2014, Southern Salish Sea Habitat Map Series Data Catalog: U.S. Geological Survey Data Series 935
    Dethier, Megan N., 1992, Classifying marine and estuarine natural communities: An alternative to the Cowardin system.

    Online Links:

    Other_Citation_Details:
    Dethier, M.N., 1992, Classifying marine and estuarine natural communities: An alternative to the Cowardin system: Natural Areas Journal, v. 12, p. 90-100.
    Federal Geographic Data Committee, 2012, Coastal and Marine Ecological Classification Standard.

    Online Links:

    Other_Citation_Details:
    Federal Geographic Data Committee, 2012, Coastal and Marine Ecological Classification Standard, 343 p.
    Triezenberg, P.J., Hart, P.E., and Childs, J.R., 2016, National Archive of Marine Seismic Surveys (NAMSS): A USGS data website of marine seismic reflection data within the U.S. Exclusive Economic Zone (EEZ).

    Online Links:

    Other_Citation_Details:
    Triezenberg, P.J., Hart, P.E., and Childs, J.R., 2016, National Archive of Marine Seismic Surveys (NAMSS): A USGS data website of marine seismic reflection data within the U.S. Exclusive Economic Zone (EEZ): U.S. Geological Survey data release
    Reid, J.A., Jenkins, C.J., Zimmermann, M., Williams, S. Jeffress, and Field, M.E., 2006, usSEABED: Pacific Coast (California, Oregon, Washington) Offshore Surficial-Sediment Data Release, version 1.

    Online Links:

    Other_Citation_Details:
    Reid, J.A., Reid, J.M., Jenkins, C.J., Zimmermann, M., Williams, S.J., and Field, M.E., 2006, usSEABED: Pacific Coast (California, Oregon, Washington) offshore surficial-sediment data release: U.S. Geological Survey Data Series 182, version 1.0
    Ballantyne, C.K., 2002, Paraglacial geomorphology.

    Other_Citation_Details:
    Ballantyne, C.K., 2002, Paraglacial geomorphology: Quaternary Science Reviews, v. 21, p. 1935�2017
    Booth, D.B., 1994, Glaciofluvial infilling and scour of the Puget Lowland, Washington, during ice-sheet glaciations.

    Other_Citation_Details:
    Booth, D.B., 1994, Glaciofluvial infilling and scour of the Puget Lowland, Washington, during ice-sheet glaciations: Geology, v. 22, p. 695�698
    Burns, R., 1985, The shape and form of Puget Sound.

    Other_Citation_Details:
    Burns, R., 1985, The shape and form of Puget Sound: Seattle, Wash., University of Washington Press, Washington Sea Grant.

How reliable are the data; what problems remain in the data set?

  1. How well have the observations been checked?
    Polygons were hand delineated; the accuracy of substrate and biota observations cannot be quantified. Polygons were visually checked for overshoots, undershoots, duplicate features, polygon closure, and other errors by the lead author and by the GIS technician who created the digital database.
  2. How accurate are the geographic locations?
    Polygons were primarily mapped by interpretation of 2-meter-resolution hillshaded bathymetry data interpreted from bathymetric lidar and sonar surveys (see BathyTopo data available in this data release), from visual observations of underwater sea floor video (also available in this data release), and from sediment samples (Reid and others, 2006). Sea floor video and sediment sample information positions are highly variable, on the order of 10 meters. Horizontal position given is ship position. Towed camera can be on the order of 10 meters distance from the ship during deployment. Map Unit contact locations were interpreted typically at a scale of 1:2,000 using the above base data. Bathymetric sonar and LiDAR data have a horizontal accuracy greater than the resolution of the base data. Map unit contacts were digitized by heads-up screen digitization of line data on 2-meter-resolution DEMs described above. Horizontal accuracy is estimated to be between 2 and 5 meters depending on how clearly contacts can be resolved. Most digitized positions on the map are estimated to have better than 5 m horizontal accuracy.
  3. How accurate are the heights or depths?
  4. Where are the gaps in the data? What is missing?
    Data are complete, no offshore features that could be accurately identified and represented at the compilation scale of 1:30,000 were eliminated or generalized. All geospatial database elements are attributed.
  5. How consistent are the relationships among the observations, including topology?
    No checks for consistency were performed on this data.

How can someone get a copy of the data set?

Are there legal restrictions on access or use of the data?
Access_Constraints None
Use_Constraints USGS-authored or produced data and information are in the public domain from the U.S. Government and are freely redistributable with proper metadata and source attribution. Please recognize and acknowledge the U.S. Geological Survey as the originator of the dataset and in products derived from these data.
  1. Who distributes the data set? (Distributor 1 of 1)
    U.S. Geological Survey - CMGDS
    2885 Mission Street
    Santa Cruz, CA

    831-427-4747 (voice)
    pcmsc_data@usgs.gov
  2. What's the catalog number I need to order this data set? These data are available in shapefile format (CMECS_OffshoreTacoma.shp and associated files) contained in a single zip file (CMECS_OffshoreTacoma.zip).
  3. What legal disclaimers am I supposed to read?
    Unless otherwise stated, all data, metadata and related materials are considered to satisfy the quality standards relative to the purpose for which the data were collected. Although these data and associated metadata have been reviewed for accuracy and completeness and approved for release by the U.S. Geological Survey (USGS), no warranty expressed or implied is made regarding the display or utility of the data on any other system or for general or scientific purposes, nor shall the act of distribution constitute any such warranty.
  4. How can I download or order the data?
  5. What hardware or software do I need in order to use the data set?
    These data can be viewed with GIS software.

Who wrote the metadata?

Dates:
Last modified: 15-Mar-2023
Metadata author:
U.S. Geological Survey, Pacific Coastal and Marine Science Center
Attn: PCMSC Science Data Coordinator
2885 Mission Street
Santa Cruz, CA

831-427-4747 (voice)
pcmsc_data@usgs.gov
Metadata standard:
Content Standard for Digital Geospatial Metadata (FGDC-STD-001-1998)

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