Volcanic Seismology:
For many centuries people living on volcanoes have known that the outset of seismic activity is often a forerunner of a volcanic eruption. This understand ing allowed people living close to the sites of the Mt. Nuovo 1538 eruption at Campi Flegrei, Italy, and of the Mt. Usu 1663 eruption, in Hokkaid...
Gespeichert in:
| Weitere Verfasser: | , , |
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| Format: | Elektronisch E-Book |
| Sprache: | English |
| Veröffentlicht: |
Berlin, Heidelberg
Springer Berlin Heidelberg
1992
|
| Schriftenreihe: | IAVCEI Proceedings in Volcanology
3 |
| Schlagworte: | |
| Online-Zugang: | BTU01 URL des Erstveröffentlichers |
| Zusammenfassung: | For many centuries people living on volcanoes have known that the outset of seismic activity is often a forerunner of a volcanic eruption. This understand ing allowed people living close to the sites of the Mt. Nuovo 1538 eruption at Campi Flegrei, Italy, and of the Mt. Usu 1663 eruption, in Hokkaido, Japan (to quote only two examples) to flee before the eruptions started. During the second half of the 19th century seismographs were installed on some volcanoes, and the link between seismic and eruptive activity started to be assessed on a firmer scientific basis. The first systematic observations of the correlations existing between seismic activity and volcanic eruptions were probably those carried out at Mt. Vesuvius by Luigi Palmieri in 1856. Palmieri was the Director of Osservatorio Vesuviano and built an electromagnetic seismograph with the aim of "making visible the smallest ground motions by recording them on paper and indicating direction, intensity and duration". He was able to show the relationship between earthquakes and the different phases of volcanic activity. He identified the harmonic tremor which he indicated was a precursor of volcanic activity: "the characteristic feature of the ground mo tions preceding eruption is its continuity . . . (before the eruption of 1861) the electromagnetic seismograph began to show a continuous tremor". The Palmieri seismograph was also utilized in Japan until 1883, when it was replaced by the new Gray-Milne seismographs, and, later, by the Omori in struments |
| Beschreibung: | 1 Online-Ressource (XVIII, 572 p) |
| ISBN: | 9783642770081 |
| DOI: | 10.1007/978-3-642-77008-1 |
Internformat
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| 520 | |a For many centuries people living on volcanoes have known that the outset of seismic activity is often a forerunner of a volcanic eruption. This understand ing allowed people living close to the sites of the Mt. Nuovo 1538 eruption at Campi Flegrei, Italy, and of the Mt. Usu 1663 eruption, in Hokkaido, Japan (to quote only two examples) to flee before the eruptions started. During the second half of the 19th century seismographs were installed on some volcanoes, and the link between seismic and eruptive activity started to be assessed on a firmer scientific basis. The first systematic observations of the correlations existing between seismic activity and volcanic eruptions were probably those carried out at Mt. Vesuvius by Luigi Palmieri in 1856. Palmieri was the Director of Osservatorio Vesuviano and built an electromagnetic seismograph with the aim of "making visible the smallest ground motions by recording them on paper and indicating direction, intensity and duration". He was able to show the relationship between earthquakes and the different phases of volcanic activity. He identified the harmonic tremor which he indicated was a precursor of volcanic activity: "the characteristic feature of the ground mo tions preceding eruption is its continuity . . . (before the eruption of 1861) the electromagnetic seismograph began to show a continuous tremor". The Palmieri seismograph was also utilized in Japan until 1883, when it was replaced by the new Gray-Milne seismographs, and, later, by the Omori in struments | ||
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Datensatz im Suchindex
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| dewey-full | 550 526.1 |
| dewey-hundreds | 500 - Natural sciences and mathematics |
| dewey-ones | 550 - Earth sciences 526 - Mathematical geography |
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| dewey-sort | 3550 |
| dewey-tens | 550 - Earth sciences 520 - Astronomy and allied sciences |
| discipline | Geologie / Paläontologie Physik |
| doi_str_mv | 10.1007/978-3-642-77008-1 |
| format | Electronic eBook |
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| id | DE-604.BV045177996 |
| illustrated | Not Illustrated |
| indexdate | 2024-07-10T08:10:48Z |
| institution | BVB |
| isbn | 9783642770081 |
| language | English |
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| publishDate | 1992 |
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| publisher | Springer Berlin Heidelberg |
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| series2 | IAVCEI Proceedings in Volcanology |
| spelling | Volcanic Seismology edited by Paolo Gasparini, Roberto Scarpa, Keiiti Aki Berlin, Heidelberg Springer Berlin Heidelberg 1992 1 Online-Ressource (XVIII, 572 p) txt rdacontent c rdamedia cr rdacarrier IAVCEI Proceedings in Volcanology 3 For many centuries people living on volcanoes have known that the outset of seismic activity is often a forerunner of a volcanic eruption. This understand ing allowed people living close to the sites of the Mt. Nuovo 1538 eruption at Campi Flegrei, Italy, and of the Mt. Usu 1663 eruption, in Hokkaido, Japan (to quote only two examples) to flee before the eruptions started. During the second half of the 19th century seismographs were installed on some volcanoes, and the link between seismic and eruptive activity started to be assessed on a firmer scientific basis. The first systematic observations of the correlations existing between seismic activity and volcanic eruptions were probably those carried out at Mt. Vesuvius by Luigi Palmieri in 1856. Palmieri was the Director of Osservatorio Vesuviano and built an electromagnetic seismograph with the aim of "making visible the smallest ground motions by recording them on paper and indicating direction, intensity and duration". He was able to show the relationship between earthquakes and the different phases of volcanic activity. He identified the harmonic tremor which he indicated was a precursor of volcanic activity: "the characteristic feature of the ground mo tions preceding eruption is its continuity . . . (before the eruption of 1861) the electromagnetic seismograph began to show a continuous tremor". The Palmieri seismograph was also utilized in Japan until 1883, when it was replaced by the new Gray-Milne seismographs, and, later, by the Omori in struments Earth Sciences Geophysics/Geodesy Geology Earth sciences Geophysics Gasparini, Paolo edt Scarpa, Roberto edt Aki, Keiiti edt Erscheint auch als Druck-Ausgabe 9783642770104 https://doi.org/10.1007/978-3-642-77008-1 Verlag URL des Erstveröffentlichers Volltext |
| spellingShingle | Volcanic Seismology Earth Sciences Geophysics/Geodesy Geology Earth sciences Geophysics |
| title | Volcanic Seismology |
| title_auth | Volcanic Seismology |
| title_exact_search | Volcanic Seismology |
| title_full | Volcanic Seismology edited by Paolo Gasparini, Roberto Scarpa, Keiiti Aki |
| title_fullStr | Volcanic Seismology edited by Paolo Gasparini, Roberto Scarpa, Keiiti Aki |
| title_full_unstemmed | Volcanic Seismology edited by Paolo Gasparini, Roberto Scarpa, Keiiti Aki |
| title_short | Volcanic Seismology |
| title_sort | volcanic seismology |
| topic | Earth Sciences Geophysics/Geodesy Geology Earth sciences Geophysics |
| topic_facet | Earth Sciences Geophysics/Geodesy Geology Earth sciences Geophysics |
| url | https://doi.org/10.1007/978-3-642-77008-1 |
| work_keys_str_mv | AT gasparinipaolo volcanicseismology AT scarparoberto volcanicseismology AT akikeiiti volcanicseismology |