{
 "culture": "en-US",
 "name": "",
 "guid": "",
 "catalogPath": "",
 "snippet": "Salinity for the Glen Canyon Group",
 "description": "<DIV STYLE=\"text-align:Left;\"><P STYLE=\"font-size:16ptmargin:7 0 7 0;\"><SPAN><SPAN>Formation-water salinity in the Glen Canyon Group is greatest in northeastern Utah (more than 35,000 ppm) but low to moderate in southeastern Utah, where it is less than 3,000 ppm (Freethey and Cordy, 1991; U.S. Geological Survey, 1996). <\/SPAN><\/SPAN><\/P><DIV><P><SPAN /><\/P><\/DIV><\/DIV>",
 "summary": "Salinity for the Glen Canyon Group",
 "title": "Glen Canyon Salinity",
 "tags": [
  "Kaiparowitz Bench",
  "Glen Canyon",
  "Colorado",
  "Sevier Basin",
  "Utah"
 ],
 "type": "",
 "typeKeywords": [],
 "thumbnail": "",
 "url": "",
 "minScale": "NaN",
 "maxScale": "NaN",
 "spatialReference": "",
 "accessInformation": "Freethey, G. W., and Cordy, G. E., 1991, Geohydrology of Mesozoic rocks in the Upper Colorado River Basin\u2014excluding the San Juan Basin\u2014in Arizona, Colorado, New Mexico, Utah, and Wyoming: U.S. Geological Survey, Professional Paper 1411-C, 118 p.\n*\nU.S. Geological Survey, 1996, Ground water atlas of the United States: Segment 2: Arizona, Colorado, New Mexico, and Utah.",
 "licenseInfo": "See access and use constraints information.",
 "portalUrl": ""
}