{
 "culture": "en-US",
 "name": "",
 "guid": "",
 "catalogPath": "",
 "snippet": "Permeability for Basin and Range (Arizona, Nevada, California",
 "description": "<DIV STYLE=\"text-align:Left;\"><P STYLE=\"font-size:16ptmargin:7 0 7 0;\"><SPAN><SPAN>Simulated transmissivity values, from which permeability is inferred, were presented for carbonate aquifers in Nevada by Prudic and others (1985). The distribution of low-permeability consolidated rock, including tuff layers and intrusive bodies was shown by Harrill and others (1988).<\/SPAN><\/SPAN><\/P><DIV><P><SPAN /><\/P><\/DIV><\/DIV>",
 "summary": "Permeability for Basin and Range (Arizona, Nevada, California",
 "title": "Basin Fill Sandstone and Carbonate Aquifers Permeability",
 "tags": [
  "Basin and Range"
 ],
 "type": "",
 "typeKeywords": [],
 "thumbnail": "",
 "url": "",
 "minScale": 0,
 "maxScale": 0,
 "spatialReference": "",
 "accessInformation": "Harrill, J. R., Gates, J. S., and Thomas, J. M., 1988, Major ground-water flow systems in the Great Basin region of Nevada, Utah, and adjacent states: U.S. Geological Survey Hydrologic Investigations Atlas HA-694-C, scale 1;1,000,000, 1 sheet.\n*\nPrudic, D. E., Harrill, J. R., Burbey, and Thomas J., 1995, Conceptual evaluation of regional ground-water flow in the carbonate-rock province of the Great Basin, Nevada, Utah, and adjacent states: U.S. Geological Survey Professional Paper P-1409-D, 102 p.",
 "licenseInfo": "See access and use constraints information."
}