{
  "accessLevel": "public",
  "bureauCode": [
    "010:12"
  ],
  "contactPoint": {
    "@type": "vcard:Contact",
    "fn": "Jeffrey Kennedy",
    "hasEmail": "mailto:jkennedy@usgs.gov"
  },
  "description": "Data are drift-corrected relative gravity differences between stations. Drift correction was carried out by modeling drift as a continuous function of time using polynomial or locally-weighted scatterplot smooth (lowess) curves. The process and software for carrying out drift correction is described in the USGS Arizona Water Science Center QA/QC plan for relative gravity data collection.",
  "distribution": [
    {
      "@type": "dcat:Distribution",
      "accessURL": "https://doi.org/10.5066/F7K935M8",
      "description": "Landing page for access to the data",
      "format": "XML",
      "mediaType": "application/http",
      "title": "Digital Data"
    },
    {
      "@type": "dcat:Distribution",
      "description": "The metadata original format",
      "downloadURL": "https://data.usgs.gov/datacatalog/metadata/USGS.56e9e4b7e4b0f59b85d81a70.xml",
      "format": "XML",
      "mediaType": "text/xml",
      "title": "Original Metadata"
    }
  ],
  "identifier": "http://datainventory.doi.gov/id/dataset/USGS_56e9e4b7e4b0f59b85d81a70",
  "keyword": [
    "Hydrology",
    "USGS:56e9e4b7e4b0f59b85d81a70"
  ],
  "modified": "2020-08-07T00:00:00Z",
  "publisher": {
    "@type": "org:Organization",
    "name": "U.S. Geological Survey"
  },
  "spatial": "-114.84558105371, 32.458421888315, -114.72473144435, 32.652882499534",
  "theme": [
    "geospatial"
  ],
  "title": "Relative-gravity differences from the 2014 Minute 319 Pulse Flow in the Colorado River Delta"
}