{
 "culture": "en-US",
 "name": "",
 "guid": "",
 "catalogPath": "",
 "snippet": "Continuity for Basin and Range (Arizona, Nevada, California",
 "description": "<DIV STYLE=\"text-align:Left;\"><P STYLE=\"font-size:16ptmargin:7 0 7 0;\"><SPAN><SPAN>Sand-body continuity of the Tertiary basin-fill aquifers is inferred from data in Planert (1996), and Robson (1996). Sand-body continuity in these aquifers is typically very high within each fault-bounded basin, but poor between basins because of the complex structure.<\/SPAN><\/SPAN><\/P><DIV><P><SPAN /><\/P><\/DIV><\/DIV>",
 "summary": "Continuity for Basin and Range (Arizona, Nevada, California",
 "title": "Continuity for Basin Fill Sandstone and Carbonate Aquifers",
 "tags": [
  "Basin and Range"
 ],
 "type": "",
 "typeKeywords": [],
 "thumbnail": "",
 "url": "",
 "minScale": "NaN",
 "maxScale": "NaN",
 "spatialReference": "",
 "accessInformation": "Planert, M., 1996, Ground water atlas of the United States, Segment 1: California and Nevada: U.S. Geological Survey Atlas.\n*\nRobson, S. G., 1996, Ground water atlas of the United States, Segment 2: Colorado, Nevada, and New Mexico: U.S. Geological Survey Atlas.",
 "licenseInfo": "See access and use constraints information.",
 "portalUrl": ""
}