{
 "currentVersion": 11.1,
 "cimVersion": "3.1.0",
 "serviceDescription": "This map provides a summary of bottom types and bottom habitats in the Gulf of Mexico. The sediment characteristics are described as follows: if the most abundant of the seabed-sized fractions of rock, gravel, sand, or mud is >66%, then it is said to be dominant. If the most abundant of these is >33%, then it is subdominant.\nIf one of the four\u2014rock, gravel, sand, or mud\u2014is the more dominant in an area, then strong control is exerted over the types of organisms (benthos) that live on the ocean floor. Rock and gravel provide microhabitats for organisms and favor attached epibenthos (e.g., suspension feeders). However, rock is more stable. Sand is the most mobile of substrates and encourages vagrant and active burrowing forms. Mud is usually stable on the scale of burrows because of its cohesiveness and favors infauna. It also tends to have the highest organic carbon contents.\nThe data for this analysis comes from USGS's usSEABED.",
 "mapName": "Seafloor Substrates - Dominant Sediments",
 "description": "This map provides a summary of bottom types and bottom habitats in the Gulf of Mexico. The sediment characteristics are described as follows: if the most abundant of the seabed-sized fractions of rock, gravel, sand, or mud is >66%, then it is said to be dominant. If the most abundant of these is >33%, then it is subdominant.\nIf one of the four\u2014rock, gravel, sand, or mud\u2014is the more dominant in an area, then strong control is exerted over the types of organisms (benthos) that live on the ocean floor. Rock and gravel provide microhabitats for organisms and favor attached epibenthos (e.g., suspension feeders). However, rock is more stable. Sand is the most mobile of substrates and encourages vagrant and active burrowing forms. Mud is usually stable on the scale of burrows because of its cohesiveness and favors infauna. It also tends to have the highest organic carbon contents.",
 "copyrightText": "Chris Jenkins, Institute of Arctic and Alpine Research, University of Colorado at Boulder",
 "supportsDynamicLayers": true,
 "layers": [
  {
   "id": 0,
   "name": "Dominant Sediments - Mud Sand Gravel Rock",
   "parentLayerId": -1,
   "defaultVisibility": true,
   "subLayerIds": null,
   "minScale": 0,
   "maxScale": 0,
   "type": "Feature Layer",
   "geometryType": "esriGeometryPolygon",
   "supportsDynamicLegends": true
  }
 ],
 "tables": [],
 "spatialReference": {
  "wkid": 102100,
  "latestWkid": 3857,
  "xyTolerance": 0.001,
  "zTolerance": 0.001,
  "mTolerance": 0.001,
  "falseX": -20037700,
  "falseY": -30241100,
  "xyUnits": 1.4892314192838538E8,
  "falseZ": -100000,
  "zUnits": 10000,
  "falseM": -100000,
  "mUnits": 10000
 },
 "singleFusedMapCache": false,
 "initialExtent": {
  "xmin": -1.1919741073816266E7,
  "ymin": 1143101.2401004757,
  "xmax": -8006447.778179678,
  "ymax": 4297301.742431762,
  "spatialReference": {
   "wkid": 102100,
   "latestWkid": 3857,
   "xyTolerance": 0.001,
   "zTolerance": 0.001,
   "mTolerance": 0.001,
   "falseX": -20037700,
   "falseY": -30241100,
   "xyUnits": 1.4892314192838538E8,
   "falseZ": -100000,
   "zUnits": 10000,
   "falseM": -100000,
   "mUnits": 10000
  }
 },
 "fullExtent": {
  "xmin": -1.1131949079293922E7,
  "ymin": 1860376.9812916156,
  "xmax": -8794239.772701908,
  "ymax": 3697855.3303508624,
  "spatialReference": {
   "wkid": 102100,
   "latestWkid": 3857,
   "xyTolerance": 0.001,
   "zTolerance": 0.001,
   "mTolerance": 0.001,
   "falseX": -20037700,
   "falseY": -30241100,
   "xyUnits": 1.4892314192838538E8,
   "falseZ": -100000,
   "zUnits": 10000,
   "falseM": -100000,
   "mUnits": 10000
  }
 },
 "datesInUnknownTimezone": false,
 "minScale": 0,
 "maxScale": 0,
 "units": "esriMeters",
 "supportedImageFormatTypes": "PNG32,PNG24,PNG,JPG,DIB,TIFF,EMF,PS,PDF,GIF,SVG,SVGZ,BMP",
 "documentInfo": {
  "Title": "Seafloor Substrates - Dominant Sediments",
  "Author": "National Centers for Environmental Information, NESDIS, NOAA, U.S. Department of Commerce",
  "Comments": "This map provides a summary of bottom types and bottom habitats in the Gulf of Mexico. The sediment characteristics are described as follows: if the most abundant of the seabed-sized fractions of rock, gravel, sand, or mud is >66%, then it is said to be dominant. If the most abundant of these is >33%, then it is subdominant.\nIf one of the four\u2014rock, gravel, sand, or mud\u2014is the more dominant in an area, then strong control is exerted over the types of organisms (benthos) that live on the ocean floor. Rock and gravel provide microhabitats for organisms and favor attached epibenthos (e.g., suspension feeders). However, rock is more stable. Sand is the most mobile of substrates and encourages vagrant and active burrowing forms. Mud is usually stable on the scale of burrows because of its cohesiveness and favors infauna. It also tends to have the highest organic carbon contents.\nThe data for this analysis comes from USGS's usSEABED.",
  "Subject": "",
  "Category": "",
  "Version": "10.1",
  "AntialiasingMode": "Fastest",
  "TextAntialiasingMode": "Force",
  "Keywords": "dbSEABED,benthic,marine,habitat,grain size,seabed,seafloor,sediment data,texture,INSTAAR"
 },
 "capabilities": "Map,Query,Data",
 "supportedQueryFormats": "JSON, geoJSON, PBF",
 "exportTilesAllowed": false,
 "referenceScale": 0.0,
 "datumTransformations": [
  {
   "geoTransforms": [
    {
     "wkid": 108001,
     "latestWkid": 1241,
     "transformForward": true,
     "name": "NAD_1927_To_NAD_1983_NADCON"
    }
   ]
  },
  {
   "geoTransforms": [
    {
     "wkid": 108001,
     "latestWkid": 1241,
     "transformForward": false,
     "name": "NAD_1927_To_NAD_1983_NADCON"
    }
   ]
  }
 ],
 "supportsDatumTransformation": true,
 "archivingInfo": {"supportsHistoricMoment": false},
 "supportsClipping": true,
 "supportsSpatialFilter": true,
 "supportsTimeRelation": true,
 "supportsQueryDataElements": true,
 "mapUnits": {"uwkid": 9001},
 "maxRecordCount": 1000,
 "maxImageHeight": 4096,
 "maxImageWidth": 4096,
 "supportedExtensions": "KmlServer, WMSServer"
}