{"accessLevel": "public", "bureauCode": ["010:12"], "contactPoint": {"@type": "vcard:Contact", "fn": "Public Information Officer", "hasEmail": "mailto:gs-w-txpublic-info@usgs.gov"}, "description": "This dataset consists of polyline estimates of the thickness of basin-fill sediments at 200-foot contour intervals for the middle Carson River basin as published on figure 9 in the U.S. Geological Survey Scientific Investigations Report 2011-5055. The estimates were made using gravity data collected at 736 stations in the middle Carson River basin reduced to a residual complete Bouguer anomaly. A relation between residual gravity and depth to bedrock was developed from descriptions on drillers logs of 25 wells that encountered bedrock.", "distribution": [{"@type": "dcat:Distribution", "accessURL": "https://doi.org/10.5066/P9P5LJ3P", "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.5ebdbdf382ce476925e44771.xml", "format": "XML", "mediaType": "text/xml", "title": "Original Metadata"}], "identifier": "http://datainventory.doi.gov/id/dataset/USGS_5ebdbdf382ce476925e44771", "keyword": ["Basin 101", "Basin 102", "Basin 103", "Carson Desert", "Carson River", "Carson River Region", "Churchill Valley", "Dayton Valley", "Hydrographic Region 8", "Nevada", "USGS:5ebdbdf382ce476925e44771", "bedrock geologic units", "bouguer anomaly", "geophysics", "geoscientificInformation", "gravitational field (earth)", "groundwater", "inlandWaters", "middle Carson River basin", "permeability", "stratigraphic thickness"], "modified": "2020-08-26T00:00:00Z", "publisher": {"@type": "org:Organization", "name": "U.S. Geological Survey"}, "spatial": "-119.635892, 39.184015, -118.836462, 39.556526", "theme": ["geospatial"], "title": "Estimated thickness of unconsolidated basin-fill sediments, middle Carson River basin, Nevada (from U.S. Geological Survey Scientific Investigations Report 2011-5055, figure 9)"}