{
  "export": {
    "source": "https://urth.darkrealm.vip/thread/urth/353",
    "note": "Exported from an unofficial mirror of a public mailing list. Copyright in each message remains with the person who wrote it.  Email addresses are obscured as `user at host`, the form the original archive published. This file was rebuilt from parsed fields rather than retained headers, so it is faithful in content but not byte-exact.",
    "addresses": "obscured as 'user at host'"
  },
  "archive": "urth",
  "thread": {
    "id": 353,
    "subject": "Geography of Urth",
    "messages": 1,
    "voices": 1,
    "first": "1998-02-06T15:12:00+00:00",
    "last": "1998-02-06T15:12:00+00:00"
  },
  "messages": [
    {
      "message_id": "<urth-v0007-0526@digest.urth.net>",
      "from": {
        "name": "m.driussi",
        "address": "m.driussi at genie.geis.com"
      },
      "date": "1998-02-06T15:12:00+00:00",
      "subject": "(urth) Geography of Urth",
      "in_reply_to": null,
      "reply_link": null,
      "blocks": [
        {
          "kind": "text",
          "depth": 0,
          "text": "Reply:  Item #7943209 from URTH at LISTS.BEST.COM@INET01#\n\nMountains of Urth, head and shoulders above the snowline.\n\nELEVATION\nAmbient temperature drops about 1 degree F for every 300 feet of\nelevation.\n\nLATITUDE\nAmbient temperature at the equator is nearly \"seasonless\"; seasons\nbecome more pronounced at latitudes beyond the tropics.\n\nTERRAIN\nHill: 100 to 200 feet rapid elevation.\nMountain: 1,000 feet to 6 miles rapid elevation.\n\nSNOWLINES (Earth)\nTropical Andes: 18,400 feet\nHimalayas     : 19,000 feet (30 degrees N)\nRocky Mts.    : 11,000 feet\nAlps          :  7,500 to 9,000 feet (45 degrees N)\nPatagonia     :  6,000 feet (40 to 50 degrees S)\nIceland       :  3,000 feet (65 degrees N)\n\n=mantis=\n\nP.S. Re Paul Park, I read the Starbridge Trilogy first and liked it a\nwhole lot.  I haven't re-read it yet, but I probably will.\n\n=m="
        }
      ]
    }
  ]
}