{
 "culture": "en-US",
 "name": "",
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 "snippet": "This map's main purpose is to provide regional-scale guidance as to the thickness of target Cambrian sandstone units which may be suitable for deep geologic injection. The average thickness (vertical) accuracy of the map is approximately 100 feet (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 isopach map shows the thickness of the interval from the top of the Copper Ridge Dolomite to the top of the Mt. Simon Sandstone and latterly equivalent lower Cambrian confining units. It was created by computer interpolation (kriging) of borehole data for much of the map extent. In several places the computer generated contours were modified by hand to accommodate faults or where such modification was deemed necessary by other geologic information that was available. In Kentucky, the extensive faulting required that the data be interpolated by hand. The map displays the thickness from the top of the Trempealeau Formation to the top of the Mt. Simon formation in Michigan. In Indiana the units displayed are the top of the Potosi Dolostone to the top of the Mt. Simon. Within Ohio the top the Basal Sandstone transitions to top of the Mt. Simon from East to West. The top of the Copper Ridge Dolostone to the tops of these two formations show the thickness in Ohio. Within Kentucky the map conveys the top of the Copper Ridge to the tops of the Basal Sandstone, Rome formation, and the Mt. Simon, which trend East to West respectively. Eastern West Virginia is shown by the top of the Conococheague Group to the top of the Antietam. The thickness in western West Virginia is composed of the top of the Copper Ridge to the top of the Basal Sandstone. In western Pennsylvania the thickness extends from the top of the Middle Dolomite Member to the top of the Potsdam Sandstone. More detailed mapping of these units is planned for phase II of the project.<\/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 target Cambrian sandstone units which may be suitable for deep geologic injection. The average thickness (vertical) accuracy of the map is approximately 100 feet (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 Copper Ridge Dolomite to the top of the Basal Sandstone in Indiana, Kentucky, Maryland, Michigan, Ohio, Pennsylvania, and West Virginia",
 "tags": [
  "CCUS",
  "MRCI",
  "Thickness Grid",
  "Copper Ridge Dolomite",
  "Mount Simon Sandstone",
  "Conasauga Group",
  "Eau Claire Formation",
  "Cambrian",
  "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>",
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}