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Article #8829

Re: Types of earthquake waves

#8829
From: Richard Stead
Date: Fri, 11 Feb 1994 07:14
26 lines
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In article <2j6b51$fo@elroy.jpl.nasa.gov> stephen@crank.jpl.nasa.gov (Stephen Watson) writes:
>In article <1994Feb5.194031.7607@texhrc.uucp>, gpcsjs@sjstat.NoSubdomain.NoDomain (Stanley J. Sramek) writes:
>|> Sheriff describes Rayleigh waves in these words:
>
>And the natural follow-on question:  what are Love waves?  (That is the right name,

Nobody else seems to have answered this yet...

Yes, Love waves are the other type of surface wave.  Specifically, they
are a special type of SH wave trapped in a crustal waveguide.

SH waves are that component of S waves that produce motion only parallel to
the surface - the motion is side to side.  They are trapped by the increase
in velocity with depth and the fact that they cannot convert to P waves
or Rayleigh waves like the SV component of S can.  The most readily observed
Love waves are the 20-second oceanic Love waves.  This is because the
ocean crust is such an excellent waveguide at that frequency.  These trains
can last for several minutes.  Different structures allow different
frequencies to be trapped, but they remain trapped only as far as the structure
persists with the same thickness.


-- 
Richard Stead
Arlington, VA
stead@seismo.css.gov
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From: stead@seismo.CSS.GOV (Richard Stead)
Newsgroups: sci.physics,ca.earthquakes
Subject: Re: Types of earthquake waves
Date: 11 Feb 1994 07:14:17 GMT
Organization: Center for Seismic Studies, Arlington, VA
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