{
  "type" : "Feature",
  "links" : [
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      "rel" : "collection",
      "type" : "application/geo+json",
      "title" : "The collection document"
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    {
      "href" : "https://energy.usgs.gov/arcgis/rest/services/MRData/Asbestos/OGCFeatureServer/collections/0/items/1106?f=json",
      "rel" : "self",
      "type" : "application/geo+json",
      "title" : "This document as JSON"
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    {
      "href" : "https://energy.usgs.gov/arcgis/rest/services/MRData/Asbestos/OGCFeatureServer/collections/0/items/1106?f=text/html",
      "rel" : "alternate",
      "type" : "text/html",
      "title" : "This document as text/html"
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  "id" : "1106",
  "properties" : {
    "rec_id" : 1106,
    "site_name" : "Ketcherside Gap deposit",
    "oremin" : "Actinolite exhibits colour-zoned prismatic to fibrous grains replacing clinopyroxene, garnet, and early scapolite\"\" (Lowell and Noll, 2001, p. 379). \"\"Colour-zoned prismatic to fibrous amphibole with colourless to pale green pleochroism is the dominant late skarn phase in both volcaniclastic and dolomite protoliths\"\" (Lowell and Noll, 2001, p. 388).",
    "devel" : "small former copper mine",
    "json" : "{\"id\":\"http:\\/\\/mrdata.usgs.gov\\/asbestos\\/record\\/1106\",\"type\":\"Feature\",\"geometry\":{\"type\":\"Point\",\"coordinates\":[-90.660120491735,37.513249845331]},\"properties\":{\"state\":\"MO\",\"county\":\"Iron\",\"site_name\":\"Ketcherside Gap deposit\",\"devel\":\"small former copper mine\",\"latitude\":\"37.5132\",\"longitude\":\"-90.66\",\"oremin\":\"Actinolite exhibits colour-zoned prismatic to fibrous grains replacing clinopyroxene, garnet, and early scapolite\\\"\\\" (Lowell and Noll, 2001, p. 379). \\\"\\\"Colour-zoned prismatic to fibrous amphibole with colourless to pale green pleochroism is the dominant late skarn phase in both volcaniclastic and dolomite protoliths\\\"\\\" (Lowell and Noll, 2001, p. 388).\",\"assocmin\":\"numerous minerals reported--see Lowell and Noll (2001)\",\"hostrock\":\"scapolite skarn\",\"reference\":[{\"citation\":\"Sides (1981)\",\"onlink\":\"http:\\/\\/gsabulletin.gsapubs.org\\/content\\/92\\/9\\/686.full.pdf+html\",\"source\":\"ofr20061211\",\"reference\":\"Sides, R.J., 1981, Geology of the Ketcherside Mountain area, southeastern Missouri, and the source of Grassy Mountain Ignimbrite: Geological Society of America Bulletin, v. 92, p. 686-693.\"},{\"citation\":\"Lowell and Noll (2001)\",\"source\":\"ofr20061211\",\"reference\":\"Lowell, G.R., and Noll, P.D., Jr., 2001, Fe-Cu-Au-bearing scapolite skarn in moat sediments of the Taum Sauk Caldera, southeastern Missouri, USA: Mineralogical Magazine, v. 65, no. 3, p. 373-396.\"}]}}",
    "url" : "https://mrdata.usgs.gov/asbestos/show-asbestos.php?rec_id=1106"
  }
}