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Seismic Raves: Tremor Observations from an Electronic Dance Music Festival

2008; Seismological Society of America; Volume: 79; Issue: 4 Linguagem: Inglês

10.1785/gssrl.79.4.546

1938-2057

D. N. Green, Dennis Bowers,

Seismology and Earthquake Studies

Research Article| July 01, 2008 Seismic Raves: Tremor Observations from an Electronic Dance Music Festival David N. Green; David N. Green AWE Blacknest Brimpton, Reading, United Kingdom dgreen@blacknest.gov.uk (D.N.G.) Search for other works by this author on: GSW Google Scholar David Bowers David Bowers AWE Blacknest Brimpton, Reading, United Kingdom dgreen@blacknest.gov.uk (D.N.G.) Search for other works by this author on: GSW Google Scholar Author and Article Information David N. Green AWE Blacknest Brimpton, Reading, United Kingdom dgreen@blacknest.gov.uk (D.N.G.) David Bowers AWE Blacknest Brimpton, Reading, United Kingdom dgreen@blacknest.gov.uk (D.N.G.) Publisher: Seismological Society of America First Online: 09 Mar 2017 Online ISSN: 1938-2057 Print ISSN: 0895-0695 © 2008 by the Seismological Society of America Seismological Research Letters (2008) 79 (4): 546–553. https://doi.org/10.1785/gssrl.79.4.546 Article history First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation David N. Green, David Bowers; Seismic Raves: Tremor Observations from an Electronic Dance Music Festival. Seismological Research Letters 2008;; 79 (4): 546–553. doi: https://doi.org/10.1785/gssrl.79.4.546 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietySeismological Research Letters Search Advanced Search Repetitive signals of sustained amplitude are observed both in music and seismology; in music this is often described as the rhythm, whereas in seismology such signals are often labeled as tremor (e.g., Chouet 1996). Tremor is generated by a variety of sources including volcanoes, glaciers, and hydroelectric plants (for examples, see Ferrick et al. 1982) and is often characterized by narrowband spectral features that maintain their amplitude, sometimes for periods of hours or days (so-called harmonic tremor). In this paper we present observations from an unusual anthropogenic source of seismic tremor, generated at an interface between... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.