{
  "type" : "Feature",
  "links" : [
    {
      "href" : "https://energy.usgs.gov/arcgis/rest/services/MRData/Asbestos/OGCFeatureServer/collections/0/items?f=application%2fjson",
      "rel" : "collection",
      "type" : "application/geo+json",
      "title" : "The collection document"
    },
    {
      "href" : "https://energy.usgs.gov/arcgis/rest/services/MRData/Asbestos/OGCFeatureServer/collections/0/items/1004?f=json",
      "rel" : "self",
      "type" : "application/geo+json",
      "title" : "This document as JSON"
    },
    {
      "href" : "https://energy.usgs.gov/arcgis/rest/services/MRData/Asbestos/OGCFeatureServer/collections/0/items/1004?f=text/html",
      "rel" : "alternate",
      "type" : "text/html",
      "title" : "This document as text/html"
    },
    {
      "href" : "https://energy.usgs.gov/arcgis/rest/services/MRData/Asbestos/OGCFeatureServer/collections/0/items/1004?f=application/geo+json",
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  "id" : "1004",
  "properties" : {
    "rec_id" : 1004,
    "site_name" : "Golden Horn batholith",
    "oremin" : "Single prismatic amphibole crystals are occasionally encountered with fibrous blue terminations resembling paint brushes or are totally covered with fibrous blue needles oriented parallel to the c-axis. According to analyses of the composite crystals, composition ranges from fluorine-rich riebeckite at the fibrous termination to ferrorichterite, then to riebeckite, ferrowinchite, ferrorichterite, and finally to katophorite at the base of the prism\"\" (Becker, 1991, p. 457).",
    "devel" : "outcrops",
    "json" : "{\"id\":\"http:\\/\\/mrdata.usgs.gov\\/asbestos\\/record\\/1004\",\"type\":\"Feature\",\"geometry\":{\"type\":\"Point\",\"coordinates\":[-120.66821426002,48.502859286304]},\"properties\":{\"state\":\"WA\",\"county\":\"Chelan\",\"site_name\":\"Golden Horn batholith\",\"devel\":\"outcrops\",\"latitude\":\"48.503\",\"longitude\":\"-120.667\",\"oremin\":\"Single prismatic amphibole crystals are occasionally encountered with fibrous blue terminations resembling paint brushes or are totally covered with fibrous blue needles oriented parallel to the c-axis. According to analyses of the composite crystals, composition ranges from fluorine-rich riebeckite at the fibrous termination to ferrorichterite, then to riebeckite, ferrowinchite, ferrorichterite, and finally to katophorite at the base of the prism\\\"\\\" (Becker, 1991, p. 457).\",\"assocmin\":\"numerous minerals reported--see Becker (1991)\",\"hostrock\":\"alkaline granite\",\"mineral\":[{\"role\":\"asbestos\",\"name\":\"winchite\"},{\"role\":\"asbestos\",\"name\":\"richterite\"},{\"role\":\"asbestos\",\"name\":\"riebeckite\"}],\"reference\":[{\"citation\":\"Boggs (1984)\",\"source\":\"ofr20101041\",\"reference\":\"Boggs, R.C., 1984, Mineralogy and geochemistry of the Golden Horn batholith, northern Cascades, Washington: University of California at Santa Barbara, Ph.D. dissertation, 211 p.\"},{\"citation\":\"Becker (1991)\",\"source\":\"ofr20101041\",\"reference\":\"Becker, Randy, 1991, Minerals of the Golden Horn batholith, Okanogan County, Washington: Rocks & Minerals, v. 66, no. 6, p. 450-459.\"}]}}",
    "url" : "https://mrdata.usgs.gov/asbestos/show-asbestos.php?rec_id=1004"
  }
}