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= Broadband characteristics of earthquakes recorded during a dome-building eruption at Mount St. Helens, Washington, between October 2004 and May 2005 =
{"@context": "https://schema.org", "@type": "CreativeWork", "additionalType": "USGS Numbered Series", "name": "Broadband characteristics of earthquakes recorded during a dome-building eruption at Mount St. Helens, Washington, between October 2004 and May 2005", "identifier": [{"@type": "PropertyValue", "propertyID": "USGS Publications Warehouse IndexID", "value": "pp17505", "url": "https://pubs.usgs.gov/publication/pp17505"}, {"@type": "PropertyValue", "propertyID": "USGS Publications Warehouse Internal ID", "value": 70047344}, {"@type": "PropertyValue", "propertyID": "DOI", "value": "10.3133/pp17505", "url": "https://doi.org/10.3133/pp17505"}], "inLanguage": "en", "isPartOf": [{"@type": "CreativeWorkSeries", "name": "Professional Paper"}], "datePublished": "2008", "dateModified": "2019-05-31", "abstract": "From October 2004 to May 2005, the Center for Earthquake Research and Information of the University of Memphis \noperated two to six broadband seismometers within 5 to 20 \nkm of Mount St. Helens to help monitor recent seismic and \nvolcanic activity. Approximately 57,000 earthquakes identified during the 7-month deployment had a normal magnitude \ndistribution with a mean magnitude of 1.78 and a standard \ndeviation of 0.24 magnitude units. Both the mode and range \nof earthquake magnitude and the rate of activity varied during \nthe deployment. We examined the time domain and spectral \ncharacteristics of two classes of events seen during dome \nbuilding. These include volcano-tectonic earthquakes and \nlower-frequency events. Lower-frequency events are further \nclassified into hybrid earthquakes, low-frequency earthquakes, \nand long-duration volcanic tremor. Hybrid and low-frequency \nearthquakes showed a continuum of characteristics that varied \nsystematically with time. A progressive loss of high-frequency \nseismic energy occurred in earthquakes as magma approached \nand eventually reached the surface. The spectral shape of large \nand small earthquakes occurring within days of each other did \nnot vary with magnitude. Volcanic tremor events and lower-frequency earthquakes displayed consistent spectral peaks, \nalthough higher frequencies were more favorably excited during tremor than earthquakes.", "description": "14 p.", "publisher": {"@type": "Organization", "name": "U.S. Geological Survey"}, "editor": [{"@type": "Person", "name": "Sherrod, David R. dsherrod@usgs.gov", "givenName": "David R.", "familyName": "Sherrod", "email": "dsherrod@usgs.gov", "identifier": {"@type": "PropertyValue", "propertyID": "ORCID", "value": "0000-0001-9460-0434", "url": "https://orcid.org/0000-0001-9460-0434"}, "affiliation": [{"@type": "Organization", "name": "Volcano Science Center", "url": "https://www.usgs.gov/centers/volcano-science-center"}]}, {"@type": "Person", "name": "Stauffer, Peter H. pstauffe@usgs.gov", "givenName": "Peter H.", "familyName": "Stauffer", "email": "pstauffe@usgs.gov"}, {"@type": "Person", "name": "Scott, William E. wescott@usgs.gov", "givenName": "William E.", "familyName": "Scott", "email": "wescott@usgs.gov", "identifier": {"@type": "PropertyValue", "propertyID": "ORCID", "value": "0000-0001-8156-979X", "url": "https://orcid.org/0000-0001-8156-979X"}, "affiliation": [{"@type": "Organization", "name": "Volcano Science Center", "url": "https://www.usgs.gov/centers/volcano-science-center"}]}], "author": [{"@type": "Person", "name": "Moran, Seth C. smoran@usgs.gov", "givenName": "Seth C.", "familyName": "Moran", "email": "smoran@usgs.gov", "identifier": {"@type": "PropertyValue", "propertyID": "ORCID", "value": "0000-0001-7308-9649", "url": "https://orcid.org/0000-0001-7308-9649"}, "affiliation": [{"@type": "Organization", "name": "Volcano Hazards Program", "url": "https://www.usgs.gov/programs/VHP"}, {"@type": "Organization", "name": "Volcano Science Center", "url": "https://www.usgs.gov/centers/volcano-science-center"}]}, {"@type": "Person", "name": "Norris, Robert D.", "givenName": "Robert D.", "familyName": "Norris"}, {"@type": "Person", "name": "Horton, Stephen P.", "givenName": "Stephen P.", "familyName": "Horton"}], "funder": [{"@type": "Organization", "name": "Volcano Hazards Program", "url": "https://www.usgs.gov/programs/VHP"}], "spatialCoverage": [{"@type": "Place", "additionalType": "country", "name": "United States", "url": "https://geonames.org/6252001"}, {"@type": "Place", "additionalType": "state", "name": "Washington", "url": "https://geonames.org/5815135"}, {"@type": "Place", "additionalType": "unknown", "name": "Mount St. Helens"}, {"@type": "Place", "geo": [{"@type": "GeoShape", "additionalProperty": {"@type": "PropertyValue", "name": "GeoJSON", "value": {"type": "FeatureCollection", "features": [{"type": "Feature", "properties": {}, "geometry": {"type": "Polygon", "coordinates": [[[-122.238678, 46.161175], [-122.238678, 46.233792], [-122.131489, 46.233792], [-122.131489, 46.161175], [-122.238678, 46.161175]]]}}]}}}, {"@type": "GeoCoordinates", "latitude": 46.197483500000004, "longitude": -122.18508349999999}]}]}
From October 2004 to May 2005, the Center for Earthquake Research and Information of the University of Memphis operated two to six broadband seismometers within 5 to 20 km of Mount St. Helens to help monitor recent seismic and volcanic activity. Approximately 57,000 earthquakes identified during the 7-month deployment had a normal magnitude distribution with a mean magnitude of 1.78 and a standard deviation of 0.24 magnitude units. Both the mode and range of earthquake magnitude and the rate of activity varied during the deployment. We examined the time domain and spectral characteristics of two classes of events seen during dome building. These include volcano-tectonic earthquakes and lower-frequency events. Lower-frequency events are further classified into hybrid earthquakes, low-frequency earthquakes, and long-duration volcanic tremor. Hybrid and low-frequency earthquakes showed a continuum of characteristics that varied systematically with time. A progressive loss of high-frequency seismic energy occurred in earthquakes as magma approached and eventually reached the surface. The spectral shape of large and small earthquakes occurring within days of each other did not vary with magnitude. Volcanic tremor events and lower-frequency earthquakes displayed consistent spectral peaks, although higher frequencies were more favorably excited during tremor than earthquakes.

Revision as of 01:07, 16 July 2024

{"@context": "https://schema.org", "@type": "CreativeWork", "additionalType": "USGS Numbered Series", "name": "Broadband characteristics of earthquakes recorded during a dome-building eruption at Mount St. Helens, Washington, between October 2004 and May 2005", "identifier": [{"@type": "PropertyValue", "propertyID": "USGS Publications Warehouse IndexID", "value": "pp17505", "url": "https://pubs.usgs.gov/publication/pp17505"}, {"@type": "PropertyValue", "propertyID": "USGS Publications Warehouse Internal ID", "value": 70047344}, {"@type": "PropertyValue", "propertyID": "DOI", "value": "10.3133/pp17505", "url": "https://doi.org/10.3133/pp17505"}], "inLanguage": "en", "isPartOf": [{"@type": "CreativeWorkSeries", "name": "Professional Paper"}], "datePublished": "2008", "dateModified": "2019-05-31", "abstract": "From October 2004 to May 2005, the Center for Earthquake Research and Information of the University of Memphis \noperated two to six broadband seismometers within 5 to 20 \nkm of Mount St. Helens to help monitor recent seismic and \nvolcanic activity. Approximately 57,000 earthquakes identified during the 7-month deployment had a normal magnitude \ndistribution with a mean magnitude of 1.78 and a standard \ndeviation of 0.24 magnitude units. Both the mode and range \nof earthquake magnitude and the rate of activity varied during \nthe deployment. We examined the time domain and spectral \ncharacteristics of two classes of events seen during dome \nbuilding. These include volcano-tectonic earthquakes and \nlower-frequency events. Lower-frequency events are further \nclassified into hybrid earthquakes, low-frequency earthquakes, \nand long-duration volcanic tremor. Hybrid and low-frequency \nearthquakes showed a continuum of characteristics that varied \nsystematically with time. A progressive loss of high-frequency \nseismic energy occurred in earthquakes as magma approached \nand eventually reached the surface. The spectral shape of large \nand small earthquakes occurring within days of each other did \nnot vary with magnitude. 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