Newsgroup sci.geo.earthquakes 5993

Directory

Subject: S or surface waves more damaging? -- From: dstierm@utnet.utoledo.edu (Donald J. Stierman)
Subject: [lm 8/2/96] Frequently asked earthquake references, I -- From: eugene@amelia.nas.nasa.gov (Eugene N. Miya)
Subject: Home risk assessement -- From: Harold Asmis
Subject: Re: loma prieta -- From: mcfields@pacbell.net (Fields)
Subject: Re: Dew Point Theory Paper (Long) -- From: mroeder@macromedia.com (Michael Roeder)
Subject: Re: S or surface waves more damaging? -- From: Bill Oertell
Subject: San Francisco Bay USGS Quake Map 10/24-30/96 -- From: michael@garlock.wr.usgs.gov (Andy Michael)
Subject: Weekly USGS Quake Report 10/24-30/96 -- From: michael@garlock.wr.usgs.gov (Andy Michael)
Subject: N. California USGS Quake Map 10/24-30/96 -- From: michael@garlock.wr.usgs.gov (Andy Michael)
Subject: Long Valley USGS Quake Map 10/24-30/96 -- From: michael@garlock.wr.usgs.gov (Andy Michael)

Articles

Subject: S or surface waves more damaging?
From: dstierm@utnet.utoledo.edu (Donald J. Stierman)
Date: Fri, 1 Nov 1996 15:54:53 GMT
Many Physical Geology texts assert that surface waves are responsible for 
most damage and the strongest shaking.  I seem to recall from graduate 
school that shear waves do the job.
Those textbooks citing shear wave motion as most damaging are authored by 
scientists with closer ties to the seismological community that those 
blaming surface waves.  It is obvious that both points of view can not be 
correct.
How can fundamental contradictions persist for decades in those books used 
to teach introductory courses?
Don Stierman - Associate Professor - University of Toledo 
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Subject: [lm 8/2/96] Frequently asked earthquake references, I
From: eugene@amelia.nas.nasa.gov (Eugene N. Miya)
Date: 1 Nov 1996 13:56:12 GMT
Archive-name: ca-earthquakes
Cathy Smither (PhD, Caltech) asked that this post be dedicated to
Alfred Wegener.
The purpose of this FAQ is NOT to circumvent conventional media.
If it did, the FAQ would easily be as long as library text books.
If you are unwilling to look up information in a book,
this FAQ could easily be just as long as any book.
A source for most general questions about earthquakes is
THE classic reference work on the subject:
%A Charles F. Richter
%Z Caltech
%T Elementary Seismology
%I W. H. Freeman Publishers (try a library)
%C New York
%C San Francisco (it appears this office is now closed)
%D 1958
Why do we suggest THIS book?
Because most readers are familiar with Richter's name.  Other people will
question other authors (either authorities [whom the cranks question]
or cranks [who the authorities question], you are welcome to read anyone).
Although this text was published before the theory of plate tectonics,
it is quite readable by the general public (the extensive math being
in the Appendix).  It covers earthquake dynamics, questions like animals,
weather, etc.  And he is THE authority.  Also it's harder to question the dead.
For instance page 133:
"Earthquake weather," as commonly described, is merely a popular fable.
 . . .can be traced to classical writing.  The Greeks . . .
Visit a library to find this book to answer your questions before thinking
about posting to the net.  Do you really think an 100+ line net posting can
answer everything?  Richter's 1.5 inches thick and packed with information.
There are numerous other good books.  Bruce Bolt (UC Berkeley),
Norris (UCSB), and others.  Just check a library out.  Community
college classes are fun and useful (field trips!).  Additionally,
the Bay Area is especially fortunate to have the Menlo Park offices
of the US Geological Survey.  The USGS does work on cartography
(map making), seismology, volcanology, land slides, hydrology, etc.
They have tours, open house, and have speakers available on a wide
variety of subjects.  Just visit them.  They have maps, reports, etc.
IF YOU receive a prediction: earthquakes happen practically everyday
around the world.  Any GOOD prediction will have, epicenter:
	latitude
	longitude
	depth
	date (with time)
	magnitude
Insist on knowing these things and you will get ride of 80% of the cranks.
Simplying saying "A quake will happen" is like dowsing for water.
Richter specifically wrote:
  Amateur predictors are legion, and will continue to be, so long as claiming
  to predict earthquakes is an easy way to get one's name into the newspaper.
  Many of them are honestly self-deceived; they usually have
  (1) no concept of the frequency of small earthquakes (100,000 a year is
  a good figure to think of, although it needs definition in terms of the
  lower limit of the magnitude included),
  (2) no means of knowing what earthquakes have occured or how large they are,
  beyond mention in the press and the space allotted there, and
  (3) no effective training in scientific thinking.
  Some "predictors" select a large number of quakes through the year and then
  claim as predicted anything which happens within a few days of any such
  date -- so that the earthquakes of half the year or even more are called
  in as "verification."
   ...Predictions based on positions of the sun and moon have to be regarded
  a trifle more seriously, since there is evidence that tidal forces may
  occasionally act as triggers for earthquakes otherwise on the point of
  taking place; in this way the date and hours of occurence may show a
  slight statistical correlation with the tides.
Page 386
Chapter 24, Earthquake Risk and Protective Measures
Part I, Earthquake Nature and Observation
Charles Richter
The front of your California phone book, the Red Cross, Sunset Magazine,
your state and county offices of emergency services are
all good sources of information concerning earthquake preparedness.
Topics include:
+Preparing your home to prevent property damage and injury
 from falling objects (e.g. bolting houses to foundations,
 securing water heaters and bookcases, NOT having your bed under a window).
+Stocking a few days of food and water (albeit it could do you little good
 if you are not near your cache).
+Knowing what to do during (get under a doorway or desk, DO NOT run outside)
 and after an earthquake (Do you know how to turn off your utilities?).
+Try to stay off of the telephone except in EXTEREME emergencies.
 Emergency services personnel need the lines for disaster assistance.
 Temporarily disable UUCP connections as well.  If you need to make a
 call, wait patiently for a dial tone.  Clicking the receiver will
 prevent you from ever getting one.  To contact family, set up a contact
 person out of state whom everyone can call.  Calls out are given
 preference over calls into the damaged region.  Pay telephones (at
 least the ones run by Pacific Bell) are on priority service and should
 provide reliable service.
+LEARN FIRST AID.  SF 1989 showed that volunteer rescuers are critical.
 If you want to learn something useful, get a Red-Cross certification
 card, and even then, that's not a guarantee, it's First-Aid.  Any smart
 class will prepare you with pre-cautions.
 Remember STOP!
	  Think
	  Observe
	  Plan
+One previous net.thread involves fire-arms.  Guns have no use in this
 natural disaster.  That silly discussion belongs in other newsgroups.
USGS BBS  1(800) 358-2663	1200 baud.
Lastly, on a frequently mentioned topic peripheral to earthquakes:
The following message comes from a former Vice-President of Caltech:
As for "Caltech" vs. "Cal Tech," it is DEFINITELY supposed to be CALTECH,
one word, not Cal Tech.  Linda is a stickler on this, and woe unto him
who makes this mistake! She frequently finds the error in written stuff,
often stuff coming from Caltech itself.  She blasts the miscreant.
Best wishes  -----Barclay
As far as I know, it was always one word.  Supposedly, the powers that
be (or were) -- Millikan, Hale, and Noyes -- decided at the beginning that
Caltech would be different from Georgia Tech etc.  -----Barclay
This is a useful first order check of outgoing Tech material.
Return to Top
Subject: Home risk assessement
From: Harold Asmis
Date: Fri, 01 Nov 1996 14:03:09 -0500
Somebody gave me access to a Newsedge wire system, which is great, and I
sure hope nobody sues me for this, which seems to be a simple news
release, that everybody would want to get around.
********
SAN FRANCISCO--(BUSINESS WIRE)--Nov. 1, 1996--EQE International, a
leading authority on seismic risk assessment,
introduces today a free Internet application that allows California
homeowners and homebuyers to obtain an analysis of their
home's seismic risk during the next "big quake."
EQE hopes the HomeRisk program will provide sufficient knowledge to
homeowners and homebuyers to preserve life and property
and avert an adverse impact on the state economy during the next
catastrophic quake. Site-specific information can be used to
ascertain a preliminary risk rating for insurance.
"EQE believes HomeRisk can clarify seismic risk on an individual basis
for homeowners sufficiently, so that California's earthquake
preparedness will increase dramatically by the end of the century," says
Peter I. Yanev, EQE President and author of the
best-selling "Peace of Mind in Earthquake Country."
"EQE is making technology, previously restricted to use by financial
institutions, available to the public -- plus, referrals to
resources that can help them improve the seismic safety of their homes."
EQE's "plain English" HomeRisk blends residential real estate with the
San Francisco-based corporation's more than 15-years'
experience in structural engineering, earthquake retrofitting, and its
research into the effects of more than 65 earthquakes
worldwide. JCP Geologists, Inc., California's leading source of geologic
disclosure information, joins EQE in providing information
and expertise for this venture.
HomeRisk, obtainable on the World Wide Web by anyone at home or in
libraries and city halls throughout the state, consists of
three modules, each with increasing specificity of seismic risk, says
Tom K. Chan, EQE Senior Vice President, who heads EQE's
development team for HomeRisk. The uniform resource locator (URL) for
HomeRisk is: http://www.homerisk.com/.
Option A -- The Neighborhood: This is EQE's free program that explains
to homeowners and homebuyers how strongly their
neighborhood is expected to shake in the next big earthquake, which
fault is expected to cause the shaking, and how individual
housing designs, from bungalows to Victorians, will fare.
Option B -- The Snapshot: For $50, Option B provides an on-line seismic
risk profile and gives a preliminary risk rating for a house.
Option B produces the HomeRisk Internet Report. This summarizes the
description of the site and its potential hazards and
"damageability." It also proposes a preliminary risk rating and then
provides extended reports on: quake hazards, damageability,
risk rating, and reduction of risk.
Option C -- The Verified Report: Option C, costing $99, is called the
JCP-EQE Home Seismic Report. The Home Seismic Report is an
easy-to-read document that provides a homebuyer or homeowner with a
measure of earthquake-shaking fitness (seismic
resistances) of a home. The report combines the best available resources
for the job of home earthquake risk assessment, including
an inspection, a home checklist, a computerized hazard analysis, and a
verified risk determination.
-- 
Harold W. Asmis        harold.w.asmis@hydro.on.ca
tel 416.592.7379  fax 416.592.5322
Standard Disclaimers Apply
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Subject: Re: loma prieta
From: mcfields@pacbell.net (Fields)
Date: Fri, 01 Nov 1996 11:58:38 -0700
In article <553ppp$ns9@newsbf02.news.aol.com>, bjarcia@aol.com (Bjarcia) wrote:
> I wonder why it didnt cause as much damage here ( near where the loma
> prieta hit) than the kobe quake did to kobe when the official mag. is
> lower in kobe than in loma prieta?
Mainly because Kobe was *directly* under an extremely dense
population/urban center.
Ironically, the major damage in Kobe was to smaller residential homes
where everyone
was sleeping or getting ready to go to work.  With Norhridge, it was quite
the opposite--
small home faired very well.  There was some commerial failures but
luckily due to
the hour very few were around.   
Loma Prieta was under the mountains east of Santa Cruz.  Some of the intensity
was focused Northwest, however, and you saw waht happened in Oakland
and the Marina district.  And they were *many* miles from the quakes
origin.  Slip thgat coin and put and major 6.9 size rupture on the Haward
Fault and the results *will* be sickening:-(.
Matt Fields
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Subject: Re: Dew Point Theory Paper (Long)
From: mroeder@macromedia.com (Michael Roeder)
Date: Fri, 01 Nov 1996 10:23:26 -0800
In article <55b4uv$kmc@bashir.peak.org>, kellyt@PEAK.ORG (Tim Kelly) wrote:
> To Those Interested:
 I've posted this paper several times in the past two years on this 
 newsgroup. I decided that rather than modifying the original content to 
 clean up the bibliography, I would leave the body of the paper in it's 
 original form.  Since the original publication, I've added to the theory 

>     This paper introduces a set of hypotheses which incorporates many 
 unexplained events surrounding what shall be defined as Type II 
 earthquakes (EQ).  I propose that rather than only one type of EQ, there 
 are actually several types of EQs occurring on the planet.  Fault-free 
 EQs are not confined to fault lines, but occur in many diverse locations. 
 This assertion is based on the inference that Type II EQs are 
 electromagnetic in nature.

> CONCLUSION
    Though no Type II data has been presented, I have presented ideas that 
 incorporate many factors related to Type II earthquakes.  Type II 
 earthquakes: 
 1. Are generally 3.5 Richter or greater. 
 2. Caused from static charge buildup in the atmosphere.
 3. Discharge similar to a capacitor discharge.
 4. Have several fuzzy elements that affect occurrences.
 5. Discharge through sea water.
 6. Are able to generate tsunamis.
>     In conclusion, the raw data is easily accessible from a multitude of 
 sources to those willing to investigate. I am confident that, after an 
 unbiased examination of this hypothesis, the same conclusions will be 
 reached.  My request is that the hypothesis be known as the Timothy 
 Hypothesis.
Incredible! 
Have you considered submitting the article for publication in the JIR?
-- 
Michael Roeder
Please to accept apologies, for English my third language is. 
Unsolicited commercial e-mail including advertising and not-for-profit
contribution solicitation to this private, paid-for, electronic mailbox
will be billed for advertising space at the rate $500 per message for the
first 100k, with a $25 charge for each additional 10k.
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Subject: Re: S or surface waves more damaging?
From: Bill Oertell
Date: Fri, 01 Nov 1996 21:51:03 -0800
Donald J. Stierman wrote:
> 
> Many Physical Geology texts assert that surface waves are responsible for
> most damage and the strongest shaking.  I seem to recall from graduate
> school that shear waves do the job.
> 
> Those textbooks citing shear wave motion as most damaging are authored by
> scientists with closer ties to the seismological community that those
> blaming surface waves.  It is obvious that both points of view can not be
> correct.
> 
> How can fundamental contradictions persist for decades in those books used
> to teach introductory courses?
> 
> Don Stierman - Associate Professor - University of Toledo 
   As a layman I've often wondered the same thing.  Both the Pressure
and Shear waves are body waves, which is why deep focii earthquakes
cause considerably less damage than those whose epicenters are shallow.
   I've seen seismographs supposedly showing the different P, S, and L
waves, and by far the L waves are both the strongest and longest
wavelength.
   In the Loma Preita earthquake I am fairly certain that I felt the
separate arrival of the P, S, and L waves.
                                    Bill
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Subject: San Francisco Bay USGS Quake Map 10/24-30/96
From: michael@garlock.wr.usgs.gov (Andy Michael)
Date: Fri, 1 Nov 1996 01:21:57 GMT
Thu Oct 31 17:41:48 PST 1996
The most recent version of this plot can be found
 here on the WWW
This map is associated with the USGS weekly seismicity report for
Northern California, the US, and the World.  Disclaimers in that report
apply to this map.  The format is GIF (GIF 87a, I believe) converted to
ascii by uuencode.  For more info contact michael@andreas.wr.usgs.gov.
DO NOT SEND EMAIL TO weekly@garlock.wr.usgs.gov  It will not be read.
UUENCODED FILE BEGINS BELOW THIS LINE
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`
end
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Subject: Weekly USGS Quake Report 10/24-30/96
From: michael@garlock.wr.usgs.gov (Andy Michael)
Date: Fri, 1 Nov 1996 01:21:46 GMT
NOTE: 5 or more maps will follow this post.
If you don't want to read them all the subjects include
the phrase "USGS Quake Map" for your killing convenience.
DISCLAIMER -- THIS IS NOT AN EARTHQUAKE PREDICTION OR WARNING!
  The commentary provided with these map(s) is for INFORMATIONAL
USE ONLY, and SHOULD NOT be construed as an earthquake prediction,
warning, or advisory.  Responsibility for such warnings rests with
the Office of Emergency Services of the State of California.
PLEASE REMEMBER -- THESE ARE PRELIMINARY DATA
  Releasing these summaries on a timely basis requires that the
data, analysis, and interpretations presented are PRELIMINARY. Of
necessity they can only reflect the views of the seismologists who
prepared them, and DO NOT carry the endorsement of the U.S.G.S.
Thus while every effort is made to ensure that the information is
accurate, nothing contained in this report is to be construed as
and earthquake prediction, warning, advisory, or official policy
statement of any kind, of the U.S. Geological Survey, or the
U.S. Government.
FOR QUESTIONS CONCERNING THIS REPORT
  Send e-mail to michael@andreas.wr.usgs.gov
  DO NOT SEND EMAIL TO weekly@garlock.wr.usgs.gov  It will not be read.
Seismicity Report for Northern California,
the Nation, and the World for the week of
October 24 - 30, 1996
 Stephen R. Walter
U.S. Geological Survey
345 Middlefield Rd.  MS-977, Menlo Park, CA  94025
San Francisco Bay Area   
 Seismicity continues at low ebb in the Bay Area.  During the seven-day
period ending at midnight on October 30, 1996 the U.S. Geological Survey
office in Menlo Park recorded 18 earthquakes of magnitude one (M1) and
greater within the San Francisco Bay area shown in Figure 1.  Only two
were as large as M2.  This total compares to 21 earthquakes during the
previous seven-day period (October 17 - 23), three of which were as large
as M2.
  The two M2 earthquakes included a M2.2 last Thursday afternoon at the
south end of the Concord fault six miles northeast of Danville (#1/1) and
a M2.1 early Sunday morning on the creeping San Andreas about two miles
southeast of San Juan Bautista (#2/1).   
Northern & Central California
   The region was relatively quiet during the past week.  Leading the list
was a pair of M3.0 events on the Mendocino fracture zone about 35 miles
west of Cape Mendocino (#1/2).  Neither was large enough to have been felt
onshore.  Closer to shore were a pair of M2.0 earthquakes (#4/2), the
second of which occurred beneath the coastal area about six miles
northeast of Petrolia.  To the north, a M2.3 earthquake occurred southeast
of Eureka (#6/2).  With a focal depth of about 27 kilometers, it was
clearly within the seismogenic zone that defines the upper part of the
subducting Gorda Plate.  
  Activity in the Coast Range was limited to a M3.1 event at the Geysers
geothermal area last Thursday evening, followed by a pair of M2 shocks in
the same location over the next two days (#3/2). 
   In central California the only notable earthquake along the San Andreas
was a M2.1 on the southern creeping segment about 13 miles northwest of
Parkfield (#2/2).   Two M2.0  earthquakes occurred along the Big Sur
coast, the first on Saturday morning about 18 miles west of San Simeon
(#7/2), the second early Monday afternoon about nine miles southeast of
Sur Point (#9/2).
   Activity in the eastern Sierra Nevada was equally light with the only
earthquake as large as M2 a M2.8 about nine miles northeast of
Markleeville (#8/2). 
Long Valley Caldera
    A small cluster of M1 events occurred early in the week along the
southwest edge of the resurgent dome just east of Mammoth Lakes (#1/3).  A
M2.1 Wednesday morning two miles southeast of Mammoth Lakes was too small
to have been felt (#2/3). 
USA Seismicity (October 20 - 22)
   According to data provided by the National Earthquake Information
Center there were no notable earthquakes in the lower 48 states outside of
California.  Southern California experienced a pair of felt events in the
Santa Barbara area.  The first and largest was a M4.3 last Wednesday
afternoon  near Ojai that was felt throughout the area (#1/4).  It was
followed about an hour later by a M3.5 aftershock that was felt at Ojai
and The following evening by a M3.6 aftershock that also was probably felt
at Ojai.  Early Friday morning a M3.3 occurred about two miles northeast
of Yucca Valley, an aftershock to the Landers earthquake (June 28, 1992,
M7.3)(#2/4).    
The Planet Earth  (October 20 - 22)
   The largest earthquake on the planet was a M6.0 near the north Coast of
eastern Siberia that was felt on the Chukotka Peninsula towns of Egvekinot
and Provideniya (#4/5).   Slightly smaller was a M5.7 near the coast of
Peru that was strongly felt at Moquegua and Ilo, Peru (#5/5).   Other
events of note include a pair of Mt's along the southern East Pacific Rise
(#1/5), a M5.5 east of the southern Kurils (#2/5), and an ongoing sequence
in the Andreanof Islands of the central Aleutians that was capped this
week by a M5.1 last Thursday (#3/5).
Table 1. Northern & Central California Seismicity (M>1.0)
--ORIGIN TIME (UT)-- -LAT N-- --LON W-- DEPTH  N N RMS ERH ERZ       DUR
YR MON DA HRMN  SEC  DEG MIN  DEG  MIN    KM  RD S SEC  KM  KM REMKS MAG
96 OCT 24  906 34.71 39  8.26 123  3.36  4.34 20   .07  .2  .7 MAA   1.8
96 OCT 24  915 27.74 36 57.91 121 27.17  3.74 34   .08  .2  .3 CYS   1.4
96 OCT 24 1107 25.36 39 25.35 123 15.66 13.91  8   .18  .7 4.5 MAA   1.6
96 OCT 24 1417 53.00 37 32.14 118 52.10  1.90  7   .02 1.0 6.3 MOR - 1.3
96 OCT 24 1632 50.83 40 25.21 125  2.53  1.90 24   .09 1.7 5.0 MEN   3.0
96 OCT 24 1815 34.13 36 57.72 121 26.99  2.99 30   .08  .2  .5 CYS#  1.6
96 OCT 24 2208 30.13 37 21.12 121 43.06  5.81 11 2 .03  .3 1.0 ALU   1.0
96 OCT 24 2213  3.80 36  2.16 120 35.25  8.32 35 1 .08  .2  .3 SLA   2.1
96 OCT 24 2355 28.81 37 53.53 121 55.82 17.82 41   .08  .2  .3 CON   2.2
96 OCT 25   13 20.04 38 46.34 122 43.06  2.49 12   .06  .4  .6 GEY   1.3
96 OCT 25   16 41.09 37 53.43 121 56.00 17.28 28   .08  .4  .6 CON   1.7
96 OCT 25   48 51.95 38 46.80 122 44.71  4.99  8   .03  .4 1.2 GEY   1.4
96 OCT 25  126 31.25 38 47.62 122 44.91  2.52 45 1 .07  .1  .3 GEY   3.1
96 OCT 25  128 51.99 38 47.85 122 45.02  0.21  8   .08  .3 1.4 GEY   1.4
96 OCT 25  301 36.54 36 28.31 121  2.66  5.53 33   .07  .2  .5 BIT   1.8
96 OCT 25  531 13.83 38 49.17 122 48.52  3.83  8   .02  .3  .6 GEY   1.4
96 OCT 25  700 47.17 36  2.21 121 33.74 11.59 21 1 .04  .4 1.3 SUR   1.9
96 OCT 25  813 49.46 36 41.91 121 20.13  4.99 12   .03  .3  .7 STN    .9
96 OCT 25 1020 41.23 40 22.74 124 31.20 18.15 10   .07 2.0  .4 MEN   2.0
96 OCT 25 1116 15.40 35 59.69 120 33.15  5.20 13 1 .04  .4  .6 MID   1.3
96 OCT 25 1219 48.34 36 45.15 121 24.69  5.63 22 3 .07  .2  .5 SJB   1.3
96 OCT 25 1516 58.45 37 30.85 118 48.59  6.38 19 1 .05  .2  .6 MOR   1.4
96 OCT 25 1544 43.74 37 30.82 118 48.50  7.37 21 2 .04  .2  .5 MOR   1.4
96 OCT 25 1712 15.61 38 46.19 122 43.94  1.76 31   .11  .2  .3 GEY   2.4
96 OCT 25 1727 38.72 35 43.28 118  4.38  7.50 10   .05  .5 1.2 WWF   2.1
96 OCT 25 1740 41.74 37 31.18 118 48.57  5.23 19   .06  .3  .5 MOR   1.2
96 OCT 25 1745 23.03 37 38.19 118 53.44 10.85 15   .07  .8 1.2 SMO   1.4
96 OCT 25 1809 20.18 36 57.91 121 27.24  0.14  7   .09  .9 7.5 CYS # 1.0
96 OCT 25 2106 10.18 36 54.48 121 37.72  2.01 37   .13  .2  .7 SJB   1.8
96 OCT 25 2253 26.86 37 39.24 118 56.67  5.50 13   .05  .3  .6 SMO   1.4
96 OCT 26  109 58.82 37 39.30 118 56.50  6.44 15   .08  .4  .8 SMO   1.5
96 OCT 26  146 21.55 37 39.22 118 56.64  5.01 12   .02  .3  .6 SMO   1.3
96 OCT 26  219 35.23 37 39.60 118 56.79  6.91  8   .05  .8  .9 SMO   1.2
96 OCT 26  312 52.53 37 39.14 118 56.43  6.55 17   .08  .3  .7 SMO   1.4
96 OCT 26  431 25.32 37 39.76 118 55.60  6.20  7   .01  .8 1.2 DOM   1.0
96 OCT 26  627 43.74 37 38.89 118 56.52  6.39 19   .08  .3  .6 SMO   1.8
96 OCT 26  738 15.22 37 39.02 118 56.71  6.84 16   .07  .4  .5 SMO   1.6
96 OCT 26  828 46.43 37 39.10 118 56.72  4.62  9   .02  .4  .8 SMO   1.3
96 OCT 26  847 32.53 38 46.48 122 45.03  0.04  9   .08  .3  .7 GEY##  .9
96 OCT 26  847 39.47 38 46.97 122 45.79  0.08 21 1 .23  .3 1.1 GEY # 1.8
96 OCT 26 1031 27.38 37 39.16 118 56.67  5.06  8   .04  .8  .7 SMO   1.2
96 OCT 26 1050 35.26 40 44.65 124  2.46 26.91 11   .02  .7  .6 EUR   2.3
96 OCT 26 1147 27.25 37 32.61 118 27.77  6.74 14   .01  .3 1.7 CHV   1.7
96 OCT 26 1249  5.72 36  7.33 120  4.57  3.22 27   .08  .5 1.5 COA   2.1
96 OCT 26 1403 52.94 37 36.64 118 49.22  7.68 12   .08  .6  .5 HCF   1.3
--ORIGIN TIME (UT)-- -LAT N-- --LON W-- DEPTH  N N RMS ERH ERZ       DUR
YR MON DA HRMN  SEC  DEG MIN  DEG  MIN    KM  RD S SEC  KM  KM REMKS MAG
96 OCT 26 1528 49.56 40 36.01 124 14.08 21.40 10 2 .02  .5  .6 EUR   1.8
96 OCT 26 1528 50.08 38 26.40 118 32.24 18.31 12 1 .07 1.6 2.8 MOL   2.4
96 OCT 26 1625 31.38 38 48.93 122 48.62  3.61 15   .02  .2  .4 GEY   1.7
96 OCT 26 1646 56.49 35 42.91 121 30.28  0.08 27 1 .15  .7 1.2 SSM # 2.0
96 OCT 26 1649  1.89 37 25.04 118 19.19  6.08 19 1 .05  .6  .8 CHV   2.1
96 OCT 26 2022 22.10 38 48.75 122 46.90  1.55 32   .06  .1  .2 GEY   2.3
96 OCT 26 2034 20.39 38 47.68 122 48.46  4.88  7   .03  .4 1.0 GEY   1.3
96 OCT 26 2056 21.72 36 32.07 121  7.12  2.68 22   .06  .3  .4 PIN   1.7
96 OCT 26 2115 31.58 36 47.18 121 24.14  5.17 12 1 .12  .6  .9 HOL   1.3
96 OCT 26 2147 30.37 38 45.66 119 38.05  4.63 19   .07  .3 1.3 WAK   2.8
96 OCT 27  145 25.45 36 18.99 120 12.43  0.03  8   .45  .9 9.2 COA## 1.8
96 OCT 27  316 33.82 37 38.69 118 52.33  6.42 10   .07  .6  .9 SMO   1.2
96 OCT 27  405 12.27 37 54.60 118 37.36  9.70 14 1 .02 1.0  .6 MOL   1.7
96 OCT 27  919  3.06 40 24.04 125  4.17  4.25 43   .15 1.9 2.1 MEN   3.0
96 OCT 27  929 53.59 36 48.95 121 31.58  3.72 55   .16  .2  .3 SJB   2.1
96 OCT 27  951 30.27 37 11.47 122  3.15 14.39 18   .07  .3 1.4 BLM   1.2
96 OCT 27  951 44.69 37 11.53 122  3.09 13.36 18   .07  .3 1.3 BLM   1.2
96 OCT 27 1121  0.69 37 39.07 118 56.52  6.51 21 2 .08  .3  .4 SMO   1.8
96 OCT 27 1304 25.66 36 35.69 120 49.54  3.21 11   .06 1.0 7.2 CRV - 1.0
96 OCT 27 1435 59.06 37 31.19 118 48.64  4.30 10   .03 1.0 1.0 MOR   1.1
96 OCT 27 1624 17.23 38 51.06 122 47.50  1.31  9   .05  .3  .9 GEY   1.6
96 OCT 27 1624 42.82 38 51.17 122 47.44  1.71  7   .03  .3 1.1 GEY   1.4
96 OCT 27 2025  8.38 38 47.64 122 46.13  4.48  7   .02  .4 1.1 GEY   1.2
96 OCT 27 2036 43.29 38 47.67 122 46.15  4.47  8   .03  .3 1.0 GEY   1.3
96 OCT 27 2120 20.72 38 47.70 122 46.20  4.73 10   .02  .3  .7 GEY   1.5
96 OCT 27 2307  0.02 37 35.64 118 49.66  1.94 14   .02  .3  .1 MOR   1.7
96 OCT 28   17 49.32 36 18.13 120 52.74  5.24 29   .12  .2  .5 BIT   2.0
96 OCT 28  120 49.53 37 34.27 118 48.49  3.66  8 2 .05 1.3  .6 MOR   1.1
96 OCT 28  427 56.64 35 57.63 120 30.37 10.70 32 3 .06  .3  .2 MID   1.7
96 OCT 28  504  0.33 38 46.44 122 35.03  5.51 13   .04  .3 1.1 GVL   1.6
96 OCT 28  516 35.72 37 38.87 118 56.89  5.90 18   .11  .4  .5 SMO   1.5
96 OCT 28  534 17.61 37 39.11 118 56.90  5.45 18 1 .07  .3  .5 SMO   1.2
96 OCT 28  554 36.43 38 22.98 122 35.36  2.12  7   .04  .4 1.8 ROG   1.7
96 OCT 28  820 40.66 36 14.70 120 48.37  5.63 18 1 .10  .4  .3 BIT   1.2
96 OCT 28  839 59.76 40 21.37 124 10.92 22.99 11 1 .08  .4  .6 MEN   2.0
96 OCT 28 1136 29.74 37 39.12 118 56.68  5.65 22 3 .06  .3  .4 SMO   1.8
96 OCT 28 1424 43.32 37  4.31 121 47.45  4.28 15 1 .05  .3  .7 LOM   1.0
96 OCT 28 1535  1.36 36 33.41 121  7.24  4.21 14 1 .06  .3 1.2 PIN   1.1
96 OCT 28 1731 22.88 38 46.96 122 43.81  2.54  7   .02  .9  .5 GEY   2.2
96 OCT 28 1731 25.76 38 47.67 122 44.49  4.69 17   .15  .4 1.1 GEY   1.8
96 OCT 28 1845 12.23 37 37.57 118 52.39  4.66 16   .07  .4  .6 SMO   1.5
96 OCT 28 1944 45.32 37 53.45 122 12.20  5.33 16   .16  .3  .6 CON   1.4
96 OCT 28 2022 41.16 37 25.87 118 36.72 10.44 14   .05  .6 1.7 RVL   1.9
96 OCT 28 2114 54.84 36 14.72 121 45.39  1.93 15   .04  .8 1.1 SUR   1.8
96 OCT 28 2151 38.03 36 12.99 121 46.68  4.46 18   .07 1.0  .3 SUR   1.8
--ORIGIN TIME (UT)-- -LAT N-- --LON W-- DEPTH  N N RMS ERH ERZ       DUR
YR MON DA HRMN  SEC  DEG MIN  DEG  MIN    KM  RD S SEC  KM  KM REMKS MAG
96 OCT 28 2152 33.81 36 12.72 121 46.83  4.64 24 1 .09  .7  .2 SUR   2.0
96 OCT 29  139  4.79 37 36.65 118 54.76  4.54 23 4 .07  .3  .4 SHE   1.5
96 OCT 29  146 25.11 36  2.27 120 35.38  3.32  7   .01  .8 2.8 SLA   1.0
96 OCT 29  207  4.26 37 34.31 118 50.04  1.96 14 1 .05  .6  .3 MOR   1.6
96 OCT 29  234 18.88 38 49.09 122 48.17  4.24 16   .03  .2  .4 GEY   1.6
96 OCT 29  524 48.67 38 50.78 122 47.89  0.90 10   .03  .3  .9 GEY   1.7
96 OCT 29  607 41.07 37 34.55 118 50.47 12.45 17   .06  .5  .6 MOR   1.6
96 OCT 29  638 36.09 37 37.63 118 52.92  1.98  9   .04  .9 1.4 SMO   1.1
96 OCT 29  729 25.92 36 42.90 121  7.08  1.22  7   .36 2.0 6.3 PAN # 1.0
96 OCT 29 1051 39.24 38 47.04 122 45.50  1.21 18   .04  .2  .4 GEY   1.7
96 OCT 29 1204  6.37 37 27.33 119  0.40  3.33 20 1 .10  .8 2.6 SIL   1.5
96 OCT 29 1230 51.18 37  5.53 121 50.05  7.93 24 2 .06  .3  .4 LOM   1.2
96 OCT 29 1633  5.02 38 49.70 122 45.94  1.31 10   .06  .3  .8 GEY   1.7
96 OCT 29 1953 32.51 36 40.95 120 51.83  2.76 11 2 .05 1.3 3.4 ORT   1.2
96 OCT 29 2019 49.27 38 47.87 122 46.80  0.51  9   .18  .5 1.1 GEY   1.6
96 OCT 30  301  5.02 38 29.07 118 31.56  1.26 30   .06 1.2 7.8 MOL - 2.3
96 OCT 30  352 47.62 37 27.85 121 48.78  6.45 29 2 .05  .2  .3 ALU   1.3
96 OCT 30  451  4.35 37 10.20 121 34.27  3.57 44   .05  .1  .3 CYN   1.5
96 OCT 30 1040 21.40 38 47.63 122 44.45  1.47 14   .06  .2  .6 GEY   1.5
96 OCT 30 1042 25.05 38 47.60 122 44.70  0.84 15   .05  .2  .4 GEY   1.6
96 OCT 30 1429 13.41 38 46.31 122 43.75  2.84 21   .08  .2  .4 GEY   1.8
96 OCT 30 1517 34.11 37 35.44 118 52.93  4.74 10   .06  .4  .7 MOR   1.1
96 OCT 30 1534 44.59 37 35.79 118 52.88  4.89 20 1 .09  .3  .5 MOR   1.4
96 OCT 30 1720 18.02 37 37.80 118 55.97  5.61 17   .11  .4  .6 SMO   2.1
96 OCT 30 1720 52.64 38 49.54 122 48.18  3.63  7   .04  .4 1.3 GEY   1.3
96 OCT 30 1748 45.69 37 37.96 118 55.99  6.90  9   .09  .6 1.3 SMO   1.1
96 OCT 30 1942 41.65 38 48.84 122 48.28  3.38  7   .02  .3  .7 GEY   1.2
96 OCT 30 2312  0.24 38 47.92 122 44.62  1.52 15   .05  .2  .6 GEY   2.1
96 OCT 31  200 51.05 37 34.25 118 49.13  4.91  9   .02  .4  .6 MOR   1.2
96 OCT 31  206 24.11 37 35.40 118 48.95  7.32 14   .07  .3  .6 MOR   1.4
96 OCT 31  238 46.37 36 42.01 121  5.21  8.77  9   .14 1.2 3.3 PAN   1.1
TABLE 2.
Data from National Earthquake Information Center (NEIC)
UTC TIME    LAT     LONG    DEP GS MAGS  SD STA  REGION AND COMMENTS
HRMNSEC                         MB  Msz     USED
------------------------------------------------------------------------------
OCT 20
042912.4* 55.933N 160.772E  33N 4.5     1.8  24 KAMCHATKA
093937.9* 48.032S  31.840E  10G 4.7     1.0  13 SOUTH OF AFRICA
141032.6?  9.73 N 126.28 E  33N 4.3     1.2  10 MINDANAO, PHILIPPINE ISLANDS
142026.8   4.914S 129.153E 254  4.7     1.0  22 BANDA SEA
150002.5  42.816N  17.875E  10G         1.5 124 ADRIATIC SEA. ML 4.6 
170024.4*  8.063N 126.824E  33N 4.2     1.2  17 MINDANAO, PHILIPPINE ISLANDS
170243.8  36.796N  21.583E  33N 4.0     0.7  16 SOUTHERN GREECE
182012.0? 17.39 S 179.00 W 550G 4.4     0.8  13 FIJI ISLANDS REGION
190655.1  42.617N  13.329E   5G 4.1     1.4  46 CENTRAL ITALY. 
191738.9  36.828N  21.570E  33N 4.0     0.7  28 SOUTHERN GREECE
192047.3*  0.340N 126.479E  63* 4.8     0.8  22 NORTHERN MOLUCCA SEA
205544.6% 10.523N  60.902W  33N         0.6   6 TRINIDAD. MD 3.6 (TRN).
OCT 21
025913.0*  8.026N 126.884E  33N 4.6     1.2  22 MINDANAO, PHILIPPINE ISLANDS
032021.6  12.684N  40.443E  33N 4.8 4.3 0.9  87 ETHIOPIA
115351.3?  5.32 S 154.37 E 100G 4.4     0.7   9 SOLOMON ISLANDS
193301.9  19.200S 177.477W 500G 5.0     1.0  38 FIJI ISLANDS REGION
200434.0* 12.621S 114.833E  10G 4.5     1.5  11 NORTHWEST OF AUSTRALIA
222330.9* 20.815S 179.113W 600G 4.4     0.9  34 FIJI ISLANDS REGION
224619.6* 13.141N 144.997E  49* 4.5     0.6  12 MARIANA ISLANDS
OCT 22
005928.7? 37.83 S 176.91 E 150G 4.9     1.0   7 NORTH ISLAND, NEW ZEALAND
041022.4* 51.524N 177.330W  33N 4.7     1.6  32 ANDREANOF ISLANDS, ALEUTIAN IS.
050106.4  10.523S 165.943E  33N 5.1 4.8 0.9  58 SANTA CRUZ ISLANDS
070205.2  35.989N  70.957E 108D 4.6     0.9  50 HINDU KUSH REGION, AFGHANISTAN
082847.5* 54.121S   7.264E  10G 4.7     1.2  12 BOUVET ISLAND REGION
085955.8* 22.631S 174.905W  33N 5.0     0.2  14 TONGA ISLANDS REGION
102716.0   7.338N  34.946W  10G 5.0     1.0  28 CENTRAL MID-ATLANTIC RIDGE
105125.4* 60.937S 154.049E  10G 4.9     0.7  21 WEST OF MACQUARIE ISLAND
115503.0* 53.151N 159.955E  33N 4.6     1.0  25 NEAR EAST COAST OF KAMCHATKA
120911.3*  6.515S 147.703E  33N 4.7     0.7  16 EASTERN NEW GUINEA REG., P.N.G.
132451.9*  5.636S 130.608E  33N 4.0     1.0   6 BANDA SEA
143253.9* 34.091N 141.827E   0* 4.3     1.1  14 OFF EAST COAST OF HONSHU, JAPAN
165454.9?  0.22 N 119.79 E  33N 4.0     1.2   9 MINAHASSA PENINSULA, SULAWESI
200929.5*  7.103S 146.900E  33N 4.1     0.4   9 EASTERN NEW GUINEA REG., P.N.G.
203721.1* 50.261S 115.852W  10G 4.9 5.5 1.5  32 SOUTHERN EAST PACIFIC RISE
OCT 23
010157.3* 49.349S 116.523W  10G 4.8 5.1 1.3  22 SOUTHERN EAST PACIFIC RISE
015005.6* 49.404S 117.015W  10G 4.9 4.9 1.5  19 SOUTH PACIFIC OCEAN
020149.3  52.316N  31.828W  10G 4.2 3.9 0.7  18 NORTHERN MID-ATLANTIC RIDGE
025122.4*  7.132S 129.436E 167? 4.4     1.5  10 BANDA SEA
031340.9  37.613N 141.536E  85D 4.7     0.9  29 NEAR EAST COAST OF HONSHU, JAPAN
101854.9* 22.204S 170.789E  33N 4.9     1.6  31 LOYALTY ISLANDS REGION
112755.3   9.912N 126.081E  54? 5.2 5.0 1.2  59 MINDANAO, PHILIPPINE ISLANDS
112835.9*  4.216N 157.014E  33N 4.8     1.3   8 E. CAROLINE ISLANDS, MICRONESIA
113440.9*  9.944N 126.242E  33N 5.1     1.0  24 MINDANAO, PHILIPPINE ISLANDS
120549.4  44.630N 149.377E  33N 5.5 4.7 1.1 154 KURIL ISLANDS
120740.9  37.247N  20.948E  33N 3.8     0.8  17 IONIAN SEA
124326.2*  9.921N 126.039E  33N 4.7     0.8  21 MINDANAO, PHILIPPINE ISLANDS
142025.8? 16.84 S 178.82 W 400G 4.4     0.9  17 FIJI ISLANDS REGION
151805.8*  9.912N 126.047E  33N 4.5     1.0  31 MINDANAO, PHILIPPINE ISLANDS
161734.6  51.566N 177.231W  44D 4.7     1.1  47 ANDREANOF ISLANDS, ALEUTIAN IS.
163213.1  34.055N 139.261E   2  3.9     0.9  27 NEAR S. COAST OF HONSHU, JAPAN
165841.7*  4.434S 144.114E  33N 4.1     0.5   8 NEAR N COAST OF NEW GUINEA, PNG.
174048.6& 63.300N 145.250W   7               52 CENTRAL ALASKA. . ML 2.9
                                                (AEIC).
175350.7*  5.445S 147.095E 150G 4.8     0.8  14 EASTERN NEW GUINEA REG., P.N.G.
191356.1*  9.896N 126.154E  33N 5.0     1.1  14 MINDANAO, PHILIPPINE ISLANDS
192034.1* 40.434N  73.574E 100G 3.9     1.4  15 KYRGYZSTAN
203911.1*  1.713N 127.891E 100G 4.2     0.5   7 HALMAHERA, INDONESIA
204138.9* 77.117N 125.634E  30D 3.6     0.7   9 LAPTEV SEA
220927.6  34.388N 119.441W  15G         0.9  86 SOUTHERN CALIFORNIA. ML 4.3
                                                Felt in the Santa Barbara area.
222717.4  34.449N 119.355W  15G         0.7  30 SOUTHERN CALIFORNIA. ML 2.8
223307.7*  9.853N 125.940E  84? 4.5     1.1  25 MINDANAO, PHILIPPINE ISLANDS
231818.1  34.414N 119.352W  10G         0.9  51 SOUTHERN CALIFORNIA. ML 3.5
                                                Felt at Ojai.
OCT 24
014417.3* 55.375N 160.926E 100G 4.4     0.4  14 KAMCHATKA
021455.2  34.194N 139.085E  21  4.8     0.8  47 NEAR S. COAST OF HONSHU, JAPAN
024747.6  55.448N 142.589W  10G 4.1     0.7  44 GULF OF ALASKA
031859.4  36.859N  21.535E  10G 4.7     1.2  47 SOUTHERN GREECE.Felt at Messinia
031906.3* 25.733N 142.793E  33N 4.9     1.0  16 VOLCANO ISLANDS REGION
044641.0? 20.77 S 179.02 W 600G 4.9     1.2  26 FIJI ISLANDS REGION
083643.7* 39.623N 144.627E  33N 4.6     0.6   9 OFF EAST COAST OF HONSHU, JAPAN
095631.9*  6.871N  93.074E  33N 4.7     1.4  23 NICOBAR ISLANDS, INDIA
102358.8  51.384N 178.492W  53  5.1 4.4 1.0 116 ANDREANOF ISLANDS, ALEUTIAN IS.
102601.6* 21.834S 175.423W  33N 4.8     1.1  13 TONGA ISLANDS
134440.6  63.345N 145.289W   7          0.7  17 CENTRAL ALASKA. ML 3.0 (AEIC).
135829.7* 31.004S 179.961W 400G 4.3     1.1  37 KERMADEC ISLANDS REGION
193154.1  66.965N 173.159W  20G 6.0 5.9 1.0 288 NEAR N. COAST-EASTERN SIBERIA.
                                                Felt on the Chukotka Peninsula. 
215739.5* 67.222N 174.438W  20G 5.1 4.5 0.7  18 NEAR N. COAST OF EASTERN SIBERIA
OCT 25
000416.3* 67.054N 173.037W  20G 4.9     1.0  26 NEAR N. COAST OF EASTERN SIBERIA
012631.4  38.777N 122.731W   5G         0.8  29 NORTHERN CALIFORNIA. ML 3.3
013705.6% 34.305S  70.292W  10G         0.4  10 CHILE-ARGENTINA BORDER. MD 3.0
032516.8  35.367N 139.087E  33N 4.6     0.9  24 NEAR S. COAST OF HONSHU, JAPAN.
                                                Felt at Yokohama.
034117.8* 10.397N 126.349E  33N 4.8     0.7  12 PHILIPPINE ISLANDS REGION
054823.7  34.416N 119.385W  10G         0.9  51 SOUTHERN CALIFORNIA. ML 3.6
071458.2* 21.863S 173.970W  33N 5.2 4.6 0.6  33 TONGA ISLANDS
113901.4? 11.85 N 126.11 E  33N 4.8     1.4  12 PHILIPPINE ISLANDS REGION
115131.3  34.122N 116.409W   5G         1.0  27 SOUTHERN CALIFORNIA. ML 3.3
195941.7  17.288S  70.084W 116D 5.7     1.0  92 NEAR COAST OF PERU. Mw 5.7 
        Felt (V) at Moquegua and Ilo, Peru; (IV) at Tacna, Peru and Iquique,
        Chile; (III) at Tarata and Arequipa, Peru; and (II) at Mollendo, Peru. 
212336.5* 63.470N 145.232W   5G         1.7  12 CENTRAL ALASKA. ML 4.1 (PMR).
OCT 26
102549.9  32.787S  68.848W  33N 4.4     1.0  18 MENDOZA PROVINCE, ARGENTINA. MD
        5.0 (SAN). Felt (V) in Maipu Department. Also felt in the Mendoza area.
122536.2* 42.561N   0.195E  10G         0.4   6 PYRENEES. mbLg 3.5 (MDD).
200535.9* 63.766N 130.259W  10G 4.3     1.7   8 SOUTHERN YUKON TERRITORY, CANADA
OCT 27
091857.1* 40.408N 125.550W  10G         0.8  25 OFFSHORE-NORTHERN. CALIF. ML 3.1
130714.0* 51.121N 177.137W  33N 4.6     1.1  13 ANDREANOF ISLANDS, ALEUTIAN IS.
162918.4? 11.87 N 142.85 E  33N 5.0     0.4   7 SOUTH OF MARIANA ISLANDS
165109.7* 34.188N 139.151E  33N 5.1     0.8  28 NEAR S. COAST OF HONSHU, JAPAN
205755.6?  1.52 N 122.74 E  83? 5.1     1.0   7 MINAHASSA PENINSULA, SULAWESI
224128.7* 44.216N 149.898E  33N 5.0     1.1  23 KURIL ISLANDS
OCT 28
065938.4* 40.208N  76.256W   5G         1.4   6 PENNSYLVANIA
090556.2* 51.863N 178.281W  58* 5.0     1.0  24 ANDREANOF ISLANDS, ALEUTIAN IS.
093318.1* 51.664N 173.317W  33N 4.9     0.8  25 ANDREANOF ISLANDS, ALEUTIAN IS.
200144.2* 51.423N 175.307W  33N 5.0     1.2  37 ANDREANOF ISLANDS, ALEUTIAN IS.
224357.5? 19.01 N 104.78 W  33N 4.2     0.6  11 NEAR COAST OF JALISCO, MEXICO
OCT 29
020021.7  34.500N  32.223E  33N 4.1     0.6  16 CYPRUS REGION
045051.0? 45.36 N 149.50 E  52D 4.6     0.5  12 KURIL ISLANDS
103113.8* 45.113N 152.015E  33N 5.0 4.6 1.0  45 EAST OF KURIL ISLANDS
Note:  Computer users can get faster access to the Weekly Seismicity      
 Reports in any of three ways:
       1. World-Wide-Web (WWW) access:    http://quake.wr.usgs.gov
       2. Anonymous FTP access:           quake.wr.usgs.gov 
                                          (in pub/www/QUAKES/WEEKREPS)
       3. Email Access:    (send email to michael@andreas.wr.usgs.gov)
Notes for Table 1:
       Origin time in the list is in GMT, in the text and on maps
       it is in local time.
       N RD: is the number of readings used to locate the event.
       N S: is the number of S waves in N RD.
       RMS SEC: is the root mean squared residual misfit for the
                location is seconds, the lower the better, over 0.3
                to 0.5 seconds is getting bad, but this is machine,
                not hand timed, data.
       ERH: is the estimated horizontal error in kilometers.
       ERZ: is the estimated vertical error in kilometers.
       N FM: is the number of readings used to compute the magnitude.
       REMKS: obtuse region codes that denote the velocity model
              used to locate the event.
       DUR MAG: is the magnitude as determined from the duration of
                the seismograms, not the amplitude.  Sort of like
                going to echo canyon and measuring how loud your
                yell is by counting echos.
       FIG: denotes the figure/event number in the maps posted separately.
Return to Top
Subject: N. California USGS Quake Map 10/24-30/96
From: michael@garlock.wr.usgs.gov (Andy Michael)
Date: Fri, 1 Nov 1996 01:22:06 GMT
Thu Oct 31 17:41:49 PST 1996
The most recent version of this plot can be found
 here on the WWW
This map is associated with the USGS weekly seismicity report for
Northern California, the US, and the World.  Disclaimers in that report
apply to this map.  The format is GIF (GIF 87a, I believe) converted to
ascii by uuencode.  For more info contact michael@andreas.wr.usgs.gov.
DO NOT SEND EMAIL TO weekly@garlock.wr.usgs.gov  It will not be read.
UUENCODED FILE BEGINS BELOW THIS LINE
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`
end
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Subject: Long Valley USGS Quake Map 10/24-30/96
From: michael@garlock.wr.usgs.gov (Andy Michael)
Date: Fri, 1 Nov 1996 01:22:14 GMT
Thu Oct 31 17:41:49 PST 1996
The most recent version of this plot can be found
 here on the WWW
This map is associated with the USGS weekly seismicity report for
Northern California, the US, and the World.  Disclaimers in that report
apply to this map.  The format is GIF (GIF 87a, I believe) converted to
ascii by uuencode.  For more info contact michael@andreas.wr.usgs.gov.
DO NOT SEND EMAIL TO weekly@garlock.wr.usgs.gov  It will not be read.
UUENCODED FILE BEGINS BELOW THIS LINE
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end
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Byron Palmer