{
 "culture": "en-US",
 "name": "",
 "guid": "",
 "catalogPath": "",
 "snippet": "This map's main purpose is to provide regional-scale guidance as to the thickness of the confining interval. The Knox represents the beginning of a large confining interval that continues up to the Lower Silurian Unconformity. The average vertical accuracy of the map is approximately 160 ft (RMSE). Local errors may be better or worse than this value, depending on the quality of data at the map location. This data should not be used as a substitute for detailed site investigations.",
 "description": "<DIV STYLE=\"text-align:Left;\"><DIV><DIV><P><SPAN>This is an isopach contour map representing the Knox Dolomite to Lower Silurian Unconformity Interval. The interval was mapped because of its potential function as a major confining interval. This interval is dominated by thick, relatively impermeable carbonates at the bottom and thick shale sequences at the top. It was created by computer interpolation (kriging) of borehole data, with minor manual editing of contour lines near the map edges.<\/SPAN><\/P><P><SPAN>Author/Originator: The Geological Surveys of Ohio, Kentucky, Maryland, Michigan, Pennsylvania and West Virginia<\/SPAN><\/P><P><SPAN>Date Created: 2005<\/SPAN><\/P><\/DIV><\/DIV><\/DIV>",
 "summary": "This map's main purpose is to provide regional-scale guidance as to the thickness of the confining interval. The Knox represents the beginning of a large confining interval that continues up to the Lower Silurian Unconformity. The average vertical accuracy of the map is approximately 160 ft (RMSE). Local errors may be better or worse than this value, depending on the quality of data at the map location. This data should not be used as a substitute for detailed site investigations.",
 "title": "Thickness Grid of the top of the Knox Dolomite to Lower Silurian Unconformity in Indiana, Kentucky, Maryland, Michigan, Ohio, Pennsylvania, and West Virginia",
 "tags": [
  "CCUS",
  "MRCI",
  "Thickness Grid",
  "Knox Dolomite",
  "Black River Group",
  "Trenton Limestone",
  "Utica Shale",
  "Point Pleasant Formation",
  "Cincinnati Group",
  "Queenston Shale",
  "Cambrian",
  "Ordovician",
  "Cambrian-Ordovician Carbon System",
  "Indiana",
  "Kentucky",
  "Maryland",
  "Michigan",
  "Ohio",
  "Pennsylvania",
  "West Virginia"
 ],
 "type": "",
 "typeKeywords": [],
 "thumbnail": "",
 "url": "",
 "minScale": 150000000,
 "maxScale": 5000,
 "spatialReference": "",
 "accessInformation": "Midwest Regional Carbon Sequestration Partnership (MRCSP) and the Midwest Regional Carbon Initiative (MRCI)",
 "licenseInfo": "<DIV STYLE=\"text-align:Left;\"><DIV><DIV><P><SPAN>This product of the Midwest Regional Carbon Initiative (MRCI) is intended to provide general geologic information only and should not be used for any other purpose. It is not intended for resale or to replace site-specific investigations. These data were compiled by MRCI, which reserves the publication rights to this material. If these data are used in the compilation of other data sets or maps for distribution or publication, this source must be referenced.<\/SPAN><\/P><P><SPAN>The information contained herein may be updated or edited in the future. Future releases of this material, if altered, will display a revision date. Users should check to ensure they have the latest version and reference the appropriate revision date if it is being used in other works. <\/SPAN><\/P><P><SPAN>This material was prepared as an account of work sponsored by an agency of the United States Government. Neither the United States Government, nor any agency thereof, nor any of their employees, nor Battelle, nor any member of the MRCI makes any warranty, express or implied, or assumes any liability or responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed, or represents that its use would not infringe privately owned rights. Reference herein to any specific commercial product, process, or service by trade name, trademark, manufacturer, or otherwise does not necessarily constitute or imply its endorsement, recommendations, or favoring by Battelle, members of the MRCI, the United States Government or any agency thereof. The views and the opinions of authors expressed herein do not necessarily state or reflect those of the members of the MRCI, the United States Government or any agency thereof.<\/SPAN><\/P><\/DIV><\/DIV><\/DIV>",
 "portalUrl": ""
}