{
  "$type": "site.standard.document",
  "bskyPostRef": {
    "cid": "bafyreihzviuuzbdiavfbc6czqrj4toy4cegoifkq6mns7bcidhkg4h4pqm",
    "uri": "at://did:plc:3smsdppscbbmgh33ttbch2od/app.bsky.feed.post/3mklcoxnrags2"
  },
  "coverImage": {
    "$type": "blob",
    "ref": {
      "$link": "bafkreiadotes42f7g5s3zn2uydkm5fjuniesqv7etczhrjlxx2g3g3ugqa"
    },
    "mimeType": "image/png",
    "size": 759386
  },
  "path": "/editors-vox/hydrothermal-heat-flow-as-a-window-into-subsurface-arc-magmas",
  "publishedAt": "2026-04-28T18:47:27.000Z",
  "site": "https://eos.org",
  "tags": [
    "Editors' Vox",
    "Earth science",
    "Earth's mantle",
    "Earth's crust",
    "hydrothermal systems",
    "lava & magma",
    "Reviews of Geophysics",
    "subduction",
    "Ingebritsen et al. [2026]"
  ],
  "textContent": "U.S. Geological Survey work party in a fumarolic area near Crater Rock, Mount Hood, Oregon. Credit:  Ingebritsen et al. [2026], Figure 4c",
  "title": "Hydrothermal Heat Flow as a Window into Subsurface Arc Magmas"
}