Article View: sci.physics
Article #8831Re: Types of earthquake waves
From: Stanley J. Sramek
Date: Sat, 05 Feb 1994 19:40
Date: Sat, 05 Feb 1994 19:40
39 lines
3153 bytes
3153 bytes
In article <2iv6lq$huj@crl.crl.com>, William H. Rowan originally wrote: >My understanding of it is that there are two types of waves: the P (pressure) >wave, which propagates by compression like sound waves, and the S (shear) >wave, which propagates by side-to-side motion, like waves in a fence when >you wiggle it. The P wave travels faster than the S wave. My memory of the >P wave in a quake in 1977 was as a sudden bang, after which there were some >seconds of quietness, and then the shaking started. That was the S waves, >which of course cause the destruction and bring buildings down. This quake >was a magnitude 4.5, I think, about 10 miles away. In article <CKrFIt.D0J@unocal.com>, Richard Ottolini replied: >There are many more than that, including those that propagate along interfaces >in rock. P and S propagate through the interior of bodies. Two interface modes- >called surface waves because they propgate at the rock-air interface- can have >higher amplitudes than P and S waves and cause destruction. At short distances >the S and surface waves are scrunched together and that is what people feel. >At medium distances, people experience the surface waves as strongest. My own comments: I believe that the surface waves important in earthquakes are "Rayleigh" waves. In his "Encyclopedic Dictionary of Exploration Geophysics," Robert Sheriff describes Rayleigh waves in these words: A type of seismic wave propagated along a free surface; the dominant wave involved in ground roll. ... Particle motion is elliptical and retrograde (i.e., the particle moves opposite to the direction of propagation at the top of its elliptical path) in the vertical plane containing the direction of propagation; ... Its amplitude decreases exponentially with depth, and the elastic properties to a depth of about one wavelength determine its velocity. ... ************************************************************************ * Stanley J. Sramek My posted statements * * Texaco Inc. do not reflect the * * Houston, Texas, U.S.A. views of my employer. * ************************************************************************
Technical Details
Message-ID:
<1994Feb5.194031.7607@texhrc.uucp>Path:
arc1-ca.pugleaf.net!gmd.de!xlink.net!howland.reston.ans.net!cs.utexas.edu!swrinde!menudo.uh.edu!nuchat!texhrc!sjstat!gpcsjsReferences:
<CARASSO.94Jan24112935@Quaestor.Inference.COM> <CARASSO.94Jan25100721@Quaestor.Inference.COM> <CKJ2C5.Dyu@umassd.edu> <2iv6lq$huj@crl.crl.com> <CKrFIt.D0J@unocal.com>Show Full Headers
Complete Article Headers
X-Google-Language: ENGLISH,ASCII-7-bit X-Google-Thread: 111c3f,7ca4767b95098142 X-Google-Attributes: gid111c3f,public X-Google-Thread: 10b271,7ca4767b95098142 X-Google-Attributes: gid10b271,public X-Google-ArrivalTime: 1994-02-06 09:21:51 PST Newsgroups: sci.physics,ca.earthquakes Path: arc1-ca.pugleaf.net!gmd.de!xlink.net!howland.reston.ans.net!cs.utexas.edu!swrinde!menudo.uh.edu!nuchat!texhrc!sjstat!gpcsjs From: gpcsjs@sjstat.NoSubdomain.NoDomain (Stanley J. Sramek) Subject: Re: Types of earthquake waves Message-ID: <1994Feb5.194031.7607@texhrc.uucp> Lines: 40 Sender: news@texhrc.uucp Nntp-Posting-Host: sjstat Organization: Texaco Inc. References: <CARASSO.94Jan24112935@Quaestor.Inference.COM> <CARASSO.94Jan25100721@Quaestor.Inference.COM> <CKJ2C5.Dyu@umassd.edu> <2iv6lq$huj@crl.crl.com> <CKrFIt.D0J@unocal.com> Date: Sat, 5 Feb 1994 19:40:31 GMT