Item talk:Q300641
From geokb
{
"USGS Publications Warehouse": { "@context": "https://schema.org", "@type": "Article", "additionalType": "Journal Article", "name": "Three-dimensional geophysical mapping of shallow water saturated altered rocks at Mount Baker, Washington: Implications for slope stability", "identifier": [ { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse IndexID", "value": "70197121", "url": "https://pubs.usgs.gov/publication/70197121" }, { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse Internal ID", "value": 70197121 }, { "@type": "PropertyValue", "propertyID": "DOI", "value": "10.1016/j.jvolgeores.2018.04.013", "url": "https://doi.org/10.1016/j.jvolgeores.2018.04.013" } ], "journal": { "@type": "Periodical", "name": "Journal of Volcanology and Geothermal Research", "volumeNumber": "357", "issueNumber": null }, "inLanguage": "en", "isPartOf": [ { "@type": "CreativeWorkSeries", "name": "Journal of Volcanology and Geothermal Research" } ], "datePublished": "2018", "dateModified": "2018-05-17", "abstract": "Water-saturated hydrothermal alteration reduces the strength of volcanic edifices, increasing the potential for catastrophic sector collapses that can lead to far traveled and destructive debris flows.\u00a0Intense hydrothermal alteration significantly lowers the resistivity and magnetization of volcanic rock\u00a0and therefore hydrothermally altered rocks can be identified with helicopter electromagnetic and magnetic measurements. Geophysical models constrained by rock properties and geologic mapping show that intensely altered rock is restricted to two small (500\u202fm diameter), >150\u202fm thick regions around Sherman Crater and Dorr Fumarole Field at Mount Baker, Washington. This distribution of alteration contrasts with much thicker and widespread alteration encompassing the summits of Mounts Adams and Rainier prior to the 5600\u202fyear old Osceola collapse, which is most likely due to extreme erosion and the limited duration of summit magmatism\u00a0at Mount Baker. In addition, the models suggest that the upper ~300\u202fm of rock contains water which could help to lubricate potential debris flows. Slope stability\u00a0modeling incorporating the geophysically modeled distribution of alteration and water indicates that the most likely and largest (~0.1\u202fkm3) collapses are from the east side of Sherman Crater. Alteration at Dorr Fumarole Field raises the collapse hazard there, but not significantly because of its lower slope angles. Geochemistry and analogs from other volcanoes suggest a model for the edifice hydrothermal system.", "description": "15 p.", "publisher": { "@type": "Organization", "name": "Elsevier" }, "author": [ { "@type": "Person", "name": "Finn, Carol A.", "givenName": "Carol A.", "familyName": "Finn", "identifier": { "@type": "PropertyValue", "propertyID": "ORCID", "value": "0000-0002-6178-0405", "url": "https://orcid.org/0000-0002-6178-0405" }, "affiliation": [ { "@type": "Organization", "name": "Crustal Geophysics and Geochemistry Science Center", "url": "https://www.usgs.gov/centers/geology-energy-and-minerals-science-center" } ] }, { "@type": "Person", "name": "Deszcz-Pan, Maria", "givenName": "Maria", "familyName": "Deszcz-Pan", "identifier": { "@type": "PropertyValue", "propertyID": "ORCID", "value": "0000-0002-6298-5314", "url": "https://orcid.org/0000-0002-6298-5314" }, "affiliation": [ { "@type": "Organization", "name": "Crustal Geophysics and Geochemistry Science Center", "url": 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