Newsgroup sci.geo.geology 36058

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Subject: Re: Einstein Equations Fail -- From: Dave Monroe
Subject: Re: Asteroid Hit at Deadly Oblique Angle 65 Million Years Ago -- From: davis@miphys.physics.lsa.umich.edu (Brian Davis)
Subject: Einstein Equations Fail -- From: jtbell@presby.edu (Jon Bell)
Subject: Re: Simulation of Plate Tectonics and Geological Time. -- From: stgprao@sugarland.unocal.COM (Richard Ottolini)
Subject: S or surface waves more damaging? -- From: dstierm@utnet.utoledo.edu (Donald J. Stierman)
Subject: Re: NEW GEOLOGY PIX ON WEB -- From: Joseph Zorzin
Subject: Re: Einstein Equations Fail -- From: "Todd K. Pedlar"
Subject: Re: Help me !!! -- From: Theresa Murison
Subject: Re: Three Mars Missions to Launch in Late 1996 -- From: jbartlo@ouchem.chem.oakland.edu (Joseph Bartlo)
Subject: Re: Creation VS Evolution -- From: vanomen
Subject: Re: NEW GEOLOGY PIX ON WEB -- From: DNations
Subject: Re: Einstein Equations Fail -- From: Survivor
Subject: Re: Asteroid Hit at Deadly Oblique Angle 65 Million Years Ago -- From: lream@comtch.iea.com (Lanny R. Ream)
Subject: Evidence of Life Found in 2nd Mars Meteorite -- From: baalke@kelvin.jpl.nasa.gov (Ron Baalke)
Subject: Re: Evidence of Life Found in 2nd Mars Meteorite -- From: Shelley
Subject: Re: Asteroid Hit at Deadly Oblique Angle 65 Million Years Ago -- From: davids@amsci.org (D. Schoonmaker)
Subject: Re: What is the source of geothermal energy?? -- From: Manley.Hubbell@hubert.rain.com (Manley Hubbell)
Subject: Re: Asteroid Hit at Deadly Oblique Angle 65 Million Years Ago -- From: ian@knowledge.co.uk (Ian Tresman)
Subject: Naturally Fractured Reservoirs Short Course -- From: aguilera@agt.net
Subject: Re: Asteroid Hit at Deadly Oblique Angle 65 Million Years Ago -- From: Phillip Bigelow
Subject: Re: Einstein Equations Fail -- From: braz
Subject: Surface geochemical information -- From: jamesF@geotech.org (James Fausnaugh)
Subject: Re: Evidence of Life Found in 2nd Mars Meteorite -- From: pollen@netcom.com (David Pollen)
Subject: Re: The science of Plate Tectonics, important for -- From: rlsmyth@aol.com (RLSmyth)
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)

Articles

Subject: Re: Einstein Equations Fail
From: Dave Monroe
Date: Fri, 01 Nov 1996 08:29:54 -0500
Johan Wevers wrote:
> My boss has probably never heard of the Einstein equations anyway :-)
Don't mean to outdo you but I'm not sure
if my boss even knows who Einstein is.
--
David S. Monroe                          David.Monroe@cdc.com
Software Engineer
Control Data Systems
2970 Presidential Drive, Suite 200
Fairborn, Ohio 45324
(937) 427-6385
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Subject: Re: Asteroid Hit at Deadly Oblique Angle 65 Million Years Ago
From: davis@miphys.physics.lsa.umich.edu (Brian Davis)
Date: Fri, 01 Nov 1996 08:34:06 -0400
In an article, Brian Pickrell wrote:
> I assume that the 20- to 30-degree angle referred to is the angle of the
> object's path relative to the ground.  But what was the object's orbital
> inclination (the angle of its path with respect to the plane of the
> equator)? A path leading from the Yucatan to the central United States
> (the article doesn't specify where in North America the blast debris
> supposedly went) would point more or less directly northward--an orbital
> inclination of roughly 40-140 degrees. 
>  If the angle was this much greater than the Earth's axial tilt, this and
> the fact that the Earth's gravity wouldn't change the direction of the
> object's motion much as it approached, would imply that the object's orbit
> lay outside the plane of the ecliptic.  This would be highly unlikely
> unless it was an extrasolar object.  Does anyone know how large the
> orbital inclinations of comets get? 
   If the object hit at a 20-30 degree angle to the ground, while going S
to N, this could be accounted for be the Earth's axial tilt of about 23
degrees. No need to have something coming in from wildly out of the plane
of the ecliptic. And the Earth's gravity would have some effect, *and*
something could come in from above or below the ecliptic while still
orbiting very close to the ecliptic. Some asteroids have large
inclinations too - Daedalus (an Appollo-type Earth-crosser) has an
inclination of 22 degrees. 1973 NA (another in the same group) has an
inclination of 68 degrees, well out of the ecliptic. But once again, I
don't think you *need* large inclinations to generate this type of impact.
> My understanding was that an impact at hypersonic velocities would form a
> roughly symmetrical fireball, regardless of the angle of impact.  This
> based on very little experimental evidence, since no available gun (at the
> time I was looking into this) could achieve anywhere near the requisite
> velocities.
   True about the fireball, the idea being that the expanssion of the
fireball is much faster than other dynamical processes that could effect
it. And the guns can't fire fast enough to make a fireball - but then
again they fire in vacuum also, a very different case than for any impact
on Earth.
> However, it's worth noting that all impact craters on Earth,
> the Moon, Mars and Mercury that I've ever seen are roughly round.  Could
> an impact form a round crater but still shoot all the debris off to one
> side? 
   Yes. There are at least a few craters on the Moon that do this. There's
one picture of a round crater from Apollo 15 whose ejecta surrounds it by
270 degrees - not 360. The missing sector is uprange from the impact. The
crater is still circular. These happen for impacts between 20-40 degrees.
The crater rim remains circular (from gun studies) down to impact angles
of 10 degrees or less.
> Does the fossil record support this?
[snip]
> ...the article states that plant extinction rates were higher in North
> America than anywhere else.  Is this right?
[snip]
   Your reasoning sounds Ok, although *many* dinosaur discoveries are made
outside N. America. I'm not a palentologist or paleobotanist.
> The Yucatan is part of North America.  I assume they mean the present
> United States and points north.
   Well, sort of - I'd call it part of central america currently, and at
the time of the impact it may not even have been connected to the main
mass of the North American plate.
> Would an effect that is (sort of) observed on Venus, with its dense
> atmosphere and high surface pressure, apply on Earth?  At the minimum, an
> Earth blast wave would be much less massive and pop up above the top of
> the atmosphere much more easily.
   A blast the size of the K-T Event would probably produce an atmospheric
blowout, but it might get downrange a ways first. From conservation of
momentum, a fireball produced from the dregs of the impact (at a
cross-range velocity of 20 km/sec * Cos(25 degrees) = 22.6 km/sec),
incorperating 10 times as much material from the target as from the
projectile, (convervation of momentum, Vfinal = 22.6 / 11), would be
moving north at 2 km/sec. That would rapidly move it downrange, out of the
near-vacuum wake channel, and thus it would have to expand against the
whole (intact) atmosphere, delaying breakout. Could happen - too little
has been done on this.
> Does anybody know how high-powered his gun was?  Could it achieve
> hypersonic velocities similar to meteoric impact velocities?
   The Vertical Gun Range, at Ames, can fire a projectile into a target at
a variety of angles and velocities of up to 6 km/sec. Hypervelocity, but
not fast enough for a lot of things. However, by properly choosing the
target and projectile materials, you can (in a limited way) scale these up
to higher effective velocities. But 6 km/sec is certainly hypersonic.
                                          -Brian Davis
Ref: Melosh, "Impact Cratering, a geologic process", Oxford press, 1989
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Subject: Einstein Equations Fail
From: jtbell@presby.edu (Jon Bell)
Date: Fri, 1 Nov 1996 13:45:37 GMT
 Paul B.Andersen  wrote:
>At the html page above I found:
>>
>> v3 = (v1 + v2)/(v1*v2/c^2)
>> 
>> The supporters of the theory don't
>> know that, in fact, the velocity sum
>> equation doesn't conserve energy and
>> momentum, when compared with the
>> calculation using SR's KE and
>> momentum equations.
>>                                                        
>> Example: 
>> 
>>      m_v = 600 MeV 
>> 
>>      KE1 = 50 MeV 
>> 
>>       v1 = 0.399 652*c
>> 
>>       v2 = 0.75*c
>> 
>>       v3 = 0.916059*c
>> 
>>      Velocity SUM: vs = 0.884525*c 
>> 
>> The velocities are different. Energy
>> and momentum are not conserved.
If this is truly representative of how the autodynamics people think of 
energy and momentum conservation, then they don't know what it *means* to 
say that energy and momentum conservation work under special relativity.
Conservation of momentum means that in any process that is not subject to 
"external forces", the total momentum of all objects in the system at the 
end of the process equals the total momentum at the beginning of the 
process.  Similarly for energy.  In relativity, one must use the "total" 
energy of an object, as given by the equation E = m0c^2 + K (where K is 
the kinetic energy) = sqrt((m0c^2)^2 + (pc)^2).
When we say that conservation of energy and momentum "work" under special
relativity, we mean that the statement above is true, regardless of which
inertial frame we analyze the process in, even though the energy and
momentum of each object depends on the frame.  To demonstrate this: 
    1.  Pick a collision or decay process, and work out the velocity, 
momentum and energy of each object, before and after.  I like to use a 
decay process such as lambda-zero --> proton + pi-minus and first assume 
that the lambda-zero is at rest in order to simplify the math.  Of 
course, in this step, you have to assume that energy and momentum are 
conserved in this frame.
    2. Switch to another inertial reference frame.  Use the velocity
addition equation to calculate the velocities of all the objects in the
new reference frame, based on their velocities on the original frame, and 
the relative velocity of the two frames.
    3.  Using the new velocities, and the basic formulas for energy and
momentum, calculate the new energy and momentum of each object.  Of
course, these values will be different from the energy and momentum in 
the original frame.
    4.  Add up the total energy and total momentum, both before and after 
the process, in the new frame.  If you have done all your math correctly, 
the total momentum before should equal the total momentum after, and the 
total energy before should equal the total energy after.
-- 
Jon Bell                         Presbyterian College
Dept. of Physics and Computer Science        Clinton, South Carolina USA
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Subject: Re: Simulation of Plate Tectonics and Geological Time.
From: stgprao@sugarland.unocal.COM (Richard Ottolini)
Date: 1 Nov 1996 14:30:10 GMT
In article <55ceeo$9u8@news.manawatu.gen.nz>,   wrote:
>I am looking for any simulation of the change in the position of the
>continents that has taken place throughout geological time. If it goes
>further and indicates mountain building, climate variation through
>time and the variation in the distribution of plant and animal
>species, this would be even better. Can anyone help?
A typical base system will give the outlines of the major tectonic
plates in the last 200 million years, their pole-path motions,
and constraints that obey the algorithms of spherical geometry.
Users than can attach their own geographic information such as
you describe and prescribe their own pole-path motions.
I've seen attachments for volcanic activity and petroleum basin location
done.   You can go back more than 200 million years, but scientists
have more divergent opinions of what happened then.
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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: Re: NEW GEOLOGY PIX ON WEB
From: Joseph Zorzin
Date: Fri, 01 Nov 1996 11:51:55 -0500
Douglas R. Grant wrote:
> 
> Announcing a web page that offers a wide selection of colour photos of
> Canadian landscapes and landforms with explanatory description in simple
> terms.
> 
> http://sts.gsc.nrcan.gc.ca/landf
> 
> The site is maintained by the Terrain Sciences Division of the Geological
> Survey of Canada.
> 
> Eventually 1000 photos will be available; at present about 100
> in Newfoundland are accessible for browsing.
> 
> THE AUTHOR
> --
> drgrant@gsc.emr.ca
That webb page is unavailable as of Saturday morning. Did it move or is
it temporarily down?
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Subject: Re: Einstein Equations Fail
From: "Todd K. Pedlar"
Date: Fri, 01 Nov 1996 09:35:08 -0600
Amnon Meyers wrote:
> 
> Einstein's velocity sum equation is inconsistent with the KE
> and momentum equations, as shown by plugging in values.
> 
> See
>    http://www.autodynamics.org/Professional/velocitysum.html
> 
First of all, if you wish that these pages be taken seriously, you 
might want to make them a bit more clear in presentation.  The 
"derivation" on this page in particular is quite hard to follow.
> Warning!  You may see that the Autodynamics equations are
> self-consistent, on the same page.
In your example, you state m_v = 600 MeV.  I suspect that means
gamma*m = 600 MeV, in which case your beta_1 is the correct velocity
for the mass (which is 550 MeV), and gamma = 1.0909.  
I suppose then that beta_2 is supposed to be the relative velocity
between two frames, and that beta1 and beta2 are supposed to be
collinear.  
Then, I understand the calculation of the velocity sum = .8845.  
This is correct, given beta1 = .3997 and beta2 = .75.  (however
the velocity sum equation as presented is incorrect.  The c^2 in 
the beta1beta2 term in the denominator isn't supposed to be there.
Can you explain how beta3 was calculated?  It's not readily apparent.
Todd
------------------------------------------------------------------
Todd K. Pedlar   -  Northwestern University - FNAL E835
Nuclear & Particle Physics Group
------------------------------------------------------------------
Phone:  (847) 491-8630  (708) 840-8048  Fax: (847) 491-8627
------------------------------------------------------------------
WWW:	http://numep1.phys.nwu.edu/tkp.html
------------------------------------------------------------------
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Subject: Re: Help me !!!
From: Theresa Murison
Date: Wed, 30 Oct 1996 19:17:06 +0000
In article , T Bruce Tober
 writes
>In a rather exuberant mood, Theresa Murison  writes
>>In article <326675E1.49A9@tam2000.tamu.edu>, "Dawn C."
>> writes
>>>When replying to one of these MASS newsgroup messages (LIKE HELP ME)
>>>please delete all irrelevant newsgroups.
>>>
>>>That will make a lot of people happy.
>>
>>
>>Y'know, *I'D* be happy if you'd tell me how to do it?!  Peace.
>
>Since you're using Turnpike, look above your message editing window to
>the small window that says Newsgroups and simply cursor over the
>inappropriate newsgroup names and hit delete
Got it before I saw your post - thanks anyway.
-- 
Theresa 
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Subject: Re: Three Mars Missions to Launch in Late 1996
From: jbartlo@ouchem.chem.oakland.edu (Joseph Bartlo)
Date: 1 Nov 1996 17:14:25 GMT
Triple Quadrophenic (Frank_Hollis-1@sbphrd.com.see-sig) wrote:
: In article <553qf1$c8o@news2.acs.oakland.edu>, 
: jbartlo@ouchem.chem.oakland.edu (Joseph Bartlo) says...
: Nope. I've never seen this definition, and I doubt that anybody uses it. 
: Apart, that is, from people who've erroneously stated that increased 
: planetary rotation decreases gravity and can't admit they made a boo-boo.
No, you cannot admit you are wrong.  Gravity includes both
gravitational attraction and centrifugal effects.  I can
provide many references showing that.  More importantly,
measurements confirm that.
Joseph
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Subject: Re: Creation VS Evolution
From: vanomen
Date: 1 Nov 1996 10:04:01 -0700
Wrong again
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Subject: Re: NEW GEOLOGY PIX ON WEB
From: DNations
Date: Fri, 01 Nov 1996 22:43:28 -0800
The correct URL is http://sts.gsc.emr.ca/page1/landf/.
Darrell Nations, R.G.
Nations Groundwater Associates
>Douglas R. Grant wrote:
> 
> Announcing a web page that offers a wide selection of colour photos of
> Canadian landscapes and landforms with explanatory description in simple
> terms.
> 
> http://sts.gsc.nrcan.gc.ca/landf
> 
> The site is maintained by the Terrain Sciences Division of the Geological
> Survey of Canada.
> 
> Eventually 1000 photos will be available; at present about 100
> in Newfoundland are accessible for browsing.
> 
> THE AUTHOR
> --
> drgrant@gsc.emr.ca
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Subject: Re: Einstein Equations Fail
From: Survivor
Date: Fri, 01 Nov 1996 11:12:19 -0800
Todd K. Pedlar wrote:
> 
> Amnon Meyers wrote:
> >
> > Einstein's velocity sum equation is inconsistent with the KE
> > and momentum equations, as shown by plugging in values.
> >
To all people participating in this thread! Please remove 
alt.prophecies.nostradamas from the thread.
Thanks
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Subject: Re: Asteroid Hit at Deadly Oblique Angle 65 Million Years Ago
From: lream@comtch.iea.com (Lanny R. Ream)
Date: 1 Nov 96 19:19:03 GMT
In article , wa2ise@netcom.com (Robert Casey)
wrote:
> In article <31OCT199604304697@kelvin.jpl.nasa.gov>
baalke@kelvin.jpl.nasa.gov (Ron Baalke) writes:
> >
> >The asteroid that wiped out the dinosaurs was
> >particularly deadly because it hit the Yucatan peninsula
> >at an oblique angle, spreading a killing zone of matter
> >downrange, according to a new study. Color
> >transparencies are available.
> >
> (more plant extinctions in North America implys the astroid that hit Yucatan
> came in on an angle and scattered debres and stuff northward)
> 
> It should be fairly easy to confirm, or at least add more evidence,
> by looking to see if there is more asteroid debres (irridium) in
> North America than say South America, Europe, etc.  And that there be
> an intermediate amount in Siberia, and less in China.  
> 
> Or did the stuff hang in the atmosphere long enough that the distribution
> became even around the planet?
The original statement is that more material was sent "downrange" creating
a "killing zone." Which to me states that if true, there has to be more
iridium and other elements.
But, I see a big conflict in this hypotheses based on other information
posted in this newsgroup a few months ago. Someone asked a question about
impact craters being oval instead of round if a meteor impacted at an
angle. There were several answers that stated that it has been shown that
even at an angle, the crater is round. Wouldn't this mean that the debris
is thrown out relatively equally 360 deg.? If so, the idea of the oblique
impact throwing more debris towards North America is as questionable as
the entire idea that an impact wiped out the dinosaurs.
Lanny
-- 
*********************************************************
/  Lanny R. Ream     lream@comtch.iea.com               /
/  Publisher,                                           /
/    Mineral News--The Mineral Collector's Newsletter   /
/  Owner/Publisher   LR Ream Publishing                 /
/  Publisher  of gem & mineral references and guides    /
/  and The Mineral Database                             /
/  Visit our Web page at http://www.iea.com/~lream      /
*********************************************************
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Subject: Evidence of Life Found in 2nd Mars Meteorite
From: baalke@kelvin.jpl.nasa.gov (Ron Baalke)
Date: 1 Nov 1996 18:31 UT
EVIDENCE OF LIFE FOUND IN SECOND MARS METEORITE
Written by Ron Baalke
November 1, 1996
In a press conference yesterday, scientists in England claimed that they've
found traces of organic material in a second Mars meteorite, EETA 79001.  
The same team also reported that they've found organic matter in the ALH 84001
meteorite, the same meteorite that a NASA team reported last August as having 
possible microfossils.  A critical finding by the British team is that
EETA 79001 contains significant amounts of organic material, up to 
1,000 parts per million.  This organic material has yet to be identified.
The British team consists of Ian Wright and Colin Pillinger from Britain's 
The Open University, and Monica Grady from London's Natural History Museum. 
The EETA 79001 meteorite was found in Elephant Morraine in the Antarctic, and 
was the first meteorite found during the 1979-1980 collecting season.  
EETA 79001 is classified as a shergotite, the most common subgroup of the 
Mars meteorites.  EETA 79001 weights 7,900 grams (17.4 pounds), and is the 
second largest Mars meteorite ever found - only the Zagami meteorite is larger.
What makes the findings from the British team particularly exciting, is that 
EETA 79001 is much younger than ALH 84001.  EETA 79001 is only 180 million years
old - very young on the solar system scale - and was launched into space 
from Mars 600,000 years ago.  The young age of this meteorite suggests that 
life existed on Mars much longer than what was previously thought, and that 
there is a possibility that life could still exist on Mars today. 
For more info on Mars meteorites, see the Mare Meteorite home page:
http://www.jpl.nasa.gov/snc/
     ___    _____     ___   
    /_ /|  /____/ \  /_ /|      Ron Baalke     | baalke@kelvin.jpl.nasa.gov
    | | | |  __ \ /| | | |  Jet Propulsion Lab |
 ___| | | | |__) |/  | | |__   Pasadena, CA    | Kindness is one thing you
/___| | | |  ___/    | |/__ /|                 | can't give away -- 
|_____|/  |_|/       |_____|/                  | it always comes back.
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Subject: Re: Evidence of Life Found in 2nd Mars Meteorite
From: Shelley
Date: Fri, 01 Nov 1996 16:47:58 -0800
We live in exciting times.. thanks for the update!
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Subject: Re: Asteroid Hit at Deadly Oblique Angle 65 Million Years Ago
From: davids@amsci.org (D. Schoonmaker)
Date: Fri, 01 Nov 1996 17:02:25 -0500
In article , lream@comtch.iea.com
(Lanny R. Ream) wrote:
> But, I see a big conflict in this hypotheses based on other information
> posted in this newsgroup a few months ago. Someone asked a question about
> impact craters being oval instead of round if a meteor impacted at an
> angle. There were several answers that stated that it has been shown that
> even at an angle, the crater is round. Wouldn't this mean that the debris
> is thrown out relatively equally 360 deg.? If so, the idea of the oblique
> impact throwing more debris towards North America is as questionable as
> the entire idea that an impact wiped out the dinosaurs.
At the annual meeting of the Geological Society of America this past
Tuesday, Dick Buffler of the University of Texas, Austin, discussed
preliminary seismic evidence that the Chicxulub crater does, indeed, appear
to be roughly round but that the ejecta rim seems to be absent to the north
in the Gulf of Mexico. He did not discuss any implications.
David Schoonmaker
amsci.org
David Schoonmaker
davids@amsci.org
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Subject: Re: What is the source of geothermal energy??
From: Manley.Hubbell@hubert.rain.com (Manley Hubbell)
Date: 01 Nov 96 15:15:01
bf>  no ways 
bf>  to increase the half-lives of elements, so they are going to take
bf>  thousands of 
   hmm? are you by any chance in Cummings Class ?
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Subject: Re: Asteroid Hit at Deadly Oblique Angle 65 Million Years Ago
From: ian@knowledge.co.uk (Ian Tresman)
Date: Fri, 01 Nov 1996 23:22:36 GMT
Readers of this thread may be interested in the following:
Natural Catastrophes during Bronze Age Civilisations:
Archaeological, Geological and Astronomical Perspectives.
A conference at Fitzwilliam College. Cambridge. 11th-13th July 1997
This SIS Cambridge conference will bring together historians,
archaeologists, climatologists and astronomers in order to discuss
whether the 'giant comet' hyopothesis brought forward by
neo-catastrophist astronomers such as Victor Clube, Bill Napier, Sir
Fred Hoyle, David Asher, Mark Bailey, Duncan Steel et al. can be
substantiated by the archaeological, climatological and historical
record.
Astronomy
Research in the field of astronomical neo-catastrophism and impact
cratering has quickened its pace since the early 1980s. An increasing
number of astronomers have suggested that a series of cosmic disasters
punctuated the Earth in prehistoric times. Scholars such as Victor
Clube, Bill Napier, Mark Bailey, Fred Hoyle, David Asher and Duncan
Steel claim that a more 'active' and threatening sky might have caused
major cultural changes of Bronze Age civilisations, belief systems and
religious rituals. Can the astronomical evidence brought forward by
these astronomers be substantiated by historical, archaeological and
climatological evidence? 
Culture
In light of new astronomical and archaeological theories and the
emergence of scientific neo-catastrophism, it seems necessary to
re-assess the origins and cultural implications of apocalyptic
religions and catastrophe traditions in ancient mythologies and
rituals. In particular, the significant cultural and religious changes
at the beginning of the Bronze Age and those which occurred after its
final collapse will be re-evaluated. 
Details at http://www.knowledge.co.uk/xxx/cat/sis/cambconf.htm
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Subject: Naturally Fractured Reservoirs Short Course
From: aguilera@agt.net
Date: 2 Nov 1996 01:04:01 GMT
Servipetrol's last course during 1996 will held in Denver,
Colorado on November 18-22. Course contents follow:
Geologic Aspects, log interpretation, well testing, completion
methods, fractured shales, horizontal wells, primary and
secondary recovery, case histories, economic
considerations and reserves.
Attendees will receive a copy of the book "Naturally
Fractured Reservoirs" written by the Instructor and
a supplemental manual. For further information please
contact Roberto Aguilera or visit our web site at
the location shown below and click on "Trainining
Services".
*******************************************************
Roberto Aguilera,Ph.D.,P.Eng.  e-mail: aguilera@agt.net
Servipetrol Ltd.                       Ph: (403)2662535
736 - 6th Avenue SW, Suite 1640       Fax: (403)2648297
Calgary, Canada T2P 3T7             Telex: 03-821172CGY
   http://www.agt.net/public/aguilera/servipetrol.htm   
*******************************************************

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Subject: Re: Asteroid Hit at Deadly Oblique Angle 65 Million Years Ago
From: Phillip Bigelow
Date: Fri, 01 Nov 1996 19:09:32 +0800
D. Schoonmaker wrote:
> 
> At the annual meeting of the Geological Society of America this past
> Tuesday, Dick Buffler of the University of Texas, Austin, discussed
> preliminary seismic evidence that the Chicxulub crater does, indeed, appear
> to be roughly round but that the ejecta rim seems to be absent to the north
> in the Gulf of Mexico. He did not discuss any implications.
> 
> David Schoonmaker
> amsci.org
I seem to remember recently reading a journal article by 
a team of geologists, who reported a meteoritic fragment in
a deep see core sample from the central Pacific Basin.
This in itself is unremarkable news, but it happens that
the meteoritic fragment they found was positioned *exactly* within
the K-T boundary layer of the core sample...within the
zone with the iridium spike.    The researchers postulated
that perhaps the impactor hit at an oblique angle, comming
in from the east, and that the meteoritic fragment was part of
the down-range ejecta blanket. This latest news that Baalke posted 
seems to support these guys' earlier hypothesis. Unfortunately, I 
forgot where I read this research paper.  Does anyone 
know, and could they post the complete citation?
Return to Top
Subject: Re: Einstein Equations Fail
From: braz
Date: Fri, 01 Nov 1996 21:58:06 -0800
Todd K. Pedlar wrote:
> 
> Amnon Meyers wrote:
> >
> > Einstein's velocity sum equation is inconsistent with the KE
> > and momentum equations, as shown by plugging in values.
> >
> > See
> >    http://www.autodynamics.org/Professional/velocitysum.html
> >
> 
> First of all, if you wish that these pages be taken seriously, you
> might want to make them a bit more clear in presentation.  The
> "derivation" on this page in particular is quite hard to follow.
> 
> > Warning!  You may see that the Autodynamics equations are
> > self-consistent, on the same page.
> 
> In your example, you state m_v = 600 MeV.  I suspect that means
> gamma*m = 600 MeV, in which case your beta_1 is the correct velocity
> for the mass (which is 550 MeV), and gamma = 1.0909.
> 
> I suppose then that beta_2 is supposed to be the relative velocity
> between two frames, and that beta1 and beta2 are supposed to be
> collinear.
> 
> Then, I understand the calculation of the velocity sum = .8845.
> This is correct, given beta1 = .3997 and beta2 = .75.  (however
> the velocity sum equation as presented is incorrect.  The c^2 in
> the beta1beta2 term in the denominator isn't supposed to be there.
> 
> Can you explain how beta3 was calculated?  It's not readily apparent.
> 
> Todd
> 
> ------------------------------------------------------------------
> Todd K. Pedlar   -  Northwestern University - FNAL E835
> Nuclear & Particle Physics Group
> ------------------------------------------------------------------
> Phone:  (847) 491-8630  (708) 840-8048  Fax: (847) 491-8627
> ------------------------------------------------------------------
> WWW:    http://numep1.phys.nwu.edu/tkp.html
> ------------------------------------------------------------------
I'm absolutely SURE that Nostradams did NOT know who EINSTEIN was. Now, 
please take this elsewhere.
-- 
mailto:braz@mnw.net
mailto:braz@usa.systar-corp.com
http://www.mnw.net/brazil
Assembler is not for the meek...
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Subject: Surface geochemical information
From: jamesF@geotech.org (James Fausnaugh)
Date: Sat, 02 Nov 96 03:55:52 GMT
Information regarding the use of Surface Exploration Techniques for hydrocarbon
exploration can be found on the Surface Survey Information Web at
http://www.geotech.org/survey/ssiweb/ssiweb.html.
The current list of companies includes:
Gallagher Research and Development Co. - surface geochemical services
geoScout - surveys in the northeast and midcontinent
Geolog Geochemical Services - surveys in the northwest
GrayStone Exploration Lab - iodine analysis and surveys
GeoTechnica BBS - bibliographies and general information about SET's
Association of Petroleum Geochemical Explorationists - professional organization
Information regarding radiometrics, iodine, and hydrocarbon sampling can be
found at anyone of the pages listed above.
===================================
         GeoTechnica BBS
http://www.geotech.org/geotech.htm
    webmaster: Jim Fausnaugh
===================================
===================================
         GeoTechnica BBS
http://www.geotech.org/geotech.htm
    webmaster: Jim Fausnaugh
===================================
Return to Top
Subject: Re: Evidence of Life Found in 2nd Mars Meteorite
From: pollen@netcom.com (David Pollen)
Date: Sat, 2 Nov 1996 03:46:12 GMT
In article <327A9A3E.51B3@oeonline.com> Shelley  writes:
>We live in exciting times.. thanks for the update!
So do the Martians!
-- 
David Pollen                                             pollen@netcom.com
=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=
Free A. Square!                                   Long Live Byron the Bulb!
=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=
                         See you at the Omega Point!
=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=-=
Return to Top
Subject: Re: The science of Plate Tectonics, important for
From: rlsmyth@aol.com (RLSmyth)
Date: 1 Nov 1996 23:17:57 -0500
You certainly have jumped into the deep end of the pool. The questions you
pose have not all been satisfactorily answered yet. Rather than attempt to
give my understanding of the current theories and hypotheses surrounding
plate tectonics (the name is here to stay I'm afraid), I would advise you
to expand your thinking beyond the present and consider the past as well.
The continents are now certainly clustered more in the north than south.
It has not always been so. Same with the avoidance of equatorial
latitudes. Pick up a good historical geology text. It should give you an
indication of past plate positions. 
As far as what drives the plate tectonic machine, several ideas have been
put forward. Some say that a single zone of convection exists in the
mantle while others suggest a segregation between upper mantle and lower
mantle convection cells with plumes rising from the core/mantle boundary
that penetrate both regions. Other ideas are out there.
Your observation that the land masses appear roughly triangular is
interesting. If significant, I wonder if it has anything to do with the
fact that the continents tend to rift at triple junctions? Also, please
remember that plates are composed of oceanic as well as continental crust
and move as a unit. For instance, the continent of Australia is on the
same plate as India, with much oceanic crust in between. This plate is
nowhere near triangular.
Return to Top
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
Return to Top
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.
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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
</PRE>
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<HR>Downloaded by WWW Programs<BR>Byron Palmer