Geometry.Net - the online learning center
Home  - Basic_E - Earthquake Measurement
e99.com Bookstore
  
Images 
Newsgroups
Page 2     21-40 of 47    Back | 1  | 2  | 3  | Next 20
A  B  C  D  E  F  G  H  I  J  K  L  M  N  O  P  Q  R  S  T  U  V  W  X  Y  Z  

         Earthquake Measurement:     more books (100)
  1. The development of the Seafloor Earthquake Measurement System by David E Ryerson, 1978
  2. Concerning the perceptibility of weak earthquakes and their dynamical measurement by Harry O Wood, 1914
  3. Earthquake measurement at Miyako, by Fusakichi Omori, 1899
  4. Seismic Source Signature Estimation and Measurement (Geophysics Reprint Series)
  5. In situ measurements of damping ratio using surface waves by Glenn J Rix, 1996
  6. A study on the duration of strong earthquake ground motion by Mihailo D Trifunac, 1976
  7. Micropulsation measurements during the Puget Sound earthquake of April 29, 1965 by James F Kenney, 1966
  8. Simple models for the estimation and measurement of frictional heating by an earthquake (Open-file report / United States Department of the Interior, Geological Survey) by Arthur H Lachenbruch, 1986
  9. Source and path effects for northeastern U.S. earthquakes: Implications for earthquake hazards : final report to the U.S. Geological Survey by M. N Toksöz, 1987
  10. Study of ground motions at soil sites during two California earthquakes: Final report (Miscellaneous paper - U.S. Army Engineer Waterways Experiment Station) by Ricardo Dobry, 1979
  11. A study of the engineering characteristics of the 1971 San Fernando earthquake records using time domain techniques by William Bond, 1980
  12. Crustal deformation measurements in Alaska seismic gap: Yakataga and the Shumagin Islands : final technical report by R Bilham, 1984
  13. Earthquake hazards in the New York City region: Deployment of a portable network of digitally recording seismographs : final technical report by A. L Kafka, 1983
  14. Seismic velocities and geological conditions at twelve sites subjected to strong ground motion in the 1994 Northridge, California, earthquake (SuDoc I 19.76:96-740) by James F. Gibbs, 1996

21. StudyWeb MathematicsWeights MeasurementEarthquake Measurement
Background Briefing Earthquake Richter Scale Gives step by step info on how to measure an earthquake with the Richter Scale.
http://seismo.um.ac.ir/education/StudyWeb MathematicsWeights & MeasurementEa

22. 227 Earthquake Measurement Lesson Plans Reviewed By Teachers
Search earthquake measurement lesson plans to find teacher approved lesson plans. Quickly find lesson plans that inspire student learning.
http://www.lessonplanet.com/search?keywords=earthquake measurement&media=les

23. Earthquake Magnitude
EARTHQUAKE MAGNITUDE SCALES Richter Magnitude Charles F. Richter introduced the Richter scale in 1935. The Richter magnitude is denoted as ML. It is also called the local magnitude.
http://www.vibrationdata.com/earthquakes/magnitude.html
EARTHQUAKE MAGNITUDE SCALES
Richter Magnitude Charles F. Richter introduced the Richter scale in 1935.
The Richter magnitude is denoted as ML. It is also called the "local magnitude." It is based on the maximum excursion of the needle on the "Wood-Anderson seismograph." The Richter scale was intended for southern California earthquakes only.
The Richter scale is a logarithmic scale. The earthquake wave displacement amplitude increases by a factor of 10 for every 1 unit increase of the Richter magnitude.
The same 1 unit increase in magnitude, however, corresponds to an increase of approximately 32 times the earthquakes energy. The magnitude calculation depends on two parameters:
1. The maximum displacement indicated on the Wood-Anderson seismograph
2. The distance from the focus to the seismograph For example, a 23 millimeter displacement measured at a station 210 kilometers from the focus would have a value of ML = 5.0. A maximum displacement of 2.3 millimeters at this same station and distance would correspond to ML = 4.0. Finally, note that the displacement indicated on the Wood-Anderson seismograph is proportional to, but not equal to, the ground displacement. The sensitivity of the Wood-Anderson instrument must be known in order to calculate the true ground displacement. A typical amplification factor is 2080. The ground displacement is thus much smaller than the displacement indicated on the seismograph.

24. Earthquake Measurement : Abstract : Nature
Nature is the international weekly journal of science a magazine style journal that publishes fulllength research papers in all disciplines of science, as well as News and Views
http://www.nature.com/nature/journal/v31/n784/abs/031004b0.html
Login Search this journal all of nature.com Advanced search Journal home Archive Letters to Editor Abstract
Letters to Editor
nature doi
Earthquake Measurement
J. A. EWING Top of page
Abstract
IN an article on “Earthquakes” in last week's NATURE (p. 608), Dr. H. J. Johnston-Lavis takes exception to the records of earthquake motion which I have published, on the ground of their complexity, and pronounces the Plain of Yedo unsuitable for earthquake observations. Top of page
Main navigation
Journal content
Journal information

25. Totally Cats: The Cat As Earthquake Measurement Device
We had a minor (4.3) quake this morning, around 522 AM. The event was about 20 miles from the house, according to the USGS report that showed up in my emailbox a few minutes
http://totallycats.blogspot.com/2007/10/cat-as-earthquake-measurement-device.htm
Totally Cats
Wednesday, October 24, 2007
The Cat as Earthquake Measurement Device
purring about... cat humor cats earthquakes We had a minor (4.3) quake this morning, around 5:22 AM. The event was about 20 miles from the house, according to the USGS report that showed up in my email-box a few minutes afterward. So, according to the USGS this was a minor event.
According to The Cat, the sky is falling, the world as we know it is coming to an end, and let the Rapture begin.
According to the USGS report, the epicenter was about 15 miles north and 3.2 miles underground. According to The Cat, the epicenter was in the front yard and just slightly below the caliche level that stunts the growth of the trees around the property (about 15 inches down).
According to what I felt, the quake lasted just under 30 seconds. According to The Cat, it lasted just over four hours, and is probably still be going on.
As soon as the event is over for The Cat, I will coax her down off the ceiling with a plate of tuna. With my luck, however, we'll have a goodly aftershock just as I open the can, and we'll never hear the end of it.
California has had its share of natural and manmade disasters over the past few days. At this writing, our home turf is not in danger. We're keeping The Cat away from the tv set, though. She does tend to blow things out of proportion, and she'd probably figure out how to dial 9-1-1 whilst laboring under the delusion that the garage is ablaze.

26. Pioneers Of Earthquake Measurement: Giuseppe Mercalli | Earthquakes Today
Most of us know practically nothing about the way earthquakes are measured. We have this mental image of weird little guys in lab coats scrutinizing mysterious
http://earthquakes-today.com/earthquakes/earthquake-measurement/
Learn the latest information
Skip to content
Skip to content
Pioneers of Earthquake Measurement: Giuseppe Mercalli
Posted on September 8, 2010 by admin Of course, the number While there are various scales used by scientists to study earthquakes, there are two that have held a prominent place in our culture for some time, contributing much to our understanding of these phenomena called earthquakes. While neither of these scales is still used in its original form, modernized versions of them underlie our basic understanding of earthquakes and the way we talk about them. These two scales are the Mercalli Scale and the Richter Scale. When discussing the modern science of earthquake measurement, a good place to start is Giuseppe Mercalli. Here was an interesting character, a Roman Catholic priest who got thrown out of the Natural Sciences department at the Milan Seminary because he openly voiced his liberal political views, only to rise to prominence again and become the director of the Vesuvius Observatory. Unfortunately, the purpose of this article is not biography, and we are only interested in Mercalli because of his crucial contribution to the field of earthquake science. I. Very mild movement, only detectable by instruments.

27. Magnitude 9.1 - OFF THE WEST COAST OF NORTHERN SUMATRA
USGS Earthquake Hazards Program, responsible for monitoring, reporting, and researching earthquakes and earthquake hazards
http://earthquake.usgs.gov/eqinthenews/2004/usslav/

28. Earthquakes - Energy
Earthquake Measurement. Geologists use seismographs to measure earthquake waves, and use the Mercalli and Richter scales to report the relative size of earthquakes.
http://www.iupui.edu/~g107cwt/10_earthquakes/energy/04.html
skip to the content
Environmental Geology - G107
by IUPUI Department of Earth Sciences
Earthquakes
Earth Processes Unit
Earthquake Measurement
Geologists use seismographs to measure earthquake waves, and use the Mercalli and Richter scales to report the relative size of earthquakes. Your textbook describes how these two scales function. Richter is based on analytical measurements, while Mercalli is based on historical and eyewitness accounts of shaking and damage.
Seismographs
An example of a seismograph recording the arrival of P-, S-, and R/L- waves from an earthquake. (Pearson/Prentice Hall) how seismographs work Sensitive seismographs can record earthquakes 1000s of miles away. Geologists use a method called triangulation to find the epicenter of earthquakes using seismographs. Using three seismograph stations, geologists can use the arrival time of the P- and S-waves to find the exact location of the epicenter
Scales
  • Richter Scale : Based on measurements from seismographs, these are always used in modern earthquakes. Reported as a magnitude (example: Magnitude 5 or M5 earthquake). The measurement is based on the largest amplitude(size) seismic wave measured for that earthquake.

29. Caltech Earthquake Engineering Research Laboratory Technical Reports - Strong-mo
This paper presents results of a study of some of the characteristics of the Kinemetrics PDR1 digital strong-motion accelerograph. The paper gives the results of laboratory
http://caltecheerl.library.caltech.edu/157/
Caltech Earthquake Engineering Research Laboratory Technical Reports Main About Browse Search ... Help
Strong-motion earthquake measurement using a digital accelerograph
Iwan, Wilfred D. and Moser, Michael Anthony and Peng, Chia-Yen Strong-motion earthquake measurement using a digital accelerograph. Technical Report CaltechEERL:1984.EERL-84-02 California Institute of Technology Full text available as: PDF Adobe PDF (3 MB) - Requires Adobe Acrobat Reader or other PDF viewer.
Abstract
This paper presents results of a study of some of the characteristics of the Kinemetrics PDR-1 digital strong-motion accelerograph. The paper gives the results of laboratory tests of the background noise level of the instrument and compares these results with previously reported observations for optical instruments. The determination of displacement from acceleration data is discussed and results of laboratory tests are presented. Certain instrument anomalies are identified, data correction algorithms proposed, and examples given. The paper also presents the results of a comparison of earthquake records obtained from side-by-side digital and optical analog instruments. Finally, some results obtained from a recent Chinese earthquake are discussed. EPrint Type: Monograph (Technical Report) Additional Information: PB-91-170191/AS Subjects: All Records Earthquake Engineering Research Laboratory ID Code: Deposited By: Jim O'Donnell Deposited On: 19 February 2008 Record Number: CaltechEERL:1984.EERL-84-02

30. Earthquake Measurement Online - Sky’s Blog
This is more fun than any sporting event. The US Geological Survey long ago automated their earthquake reporting instruments and it has become somewhat of a sport to see how
http://blog.red7.com/earthquake-measurement-online/
Sky’s Blog
Spreading the word in a networked world
Earthquake Measurement Online
by Sky on Mar.30, 2009, under Entertainment and Places The Quantified Self Read more about what the USGS has available online for earthquake reporting. Here’s what the event looked like on the seismograph at Stanford Telescope in the hills west of Stanford University ( click this for full original recording of this quake Then a map is assembled (again, by computers) showing (with color) the intensity as felt by those who reported the quake. The map shows zip code area outlines and colors them to represent the reported intensity. ( Click the map to see an original .) If you look at the map for this particular quake you’ll see that the shock was felt mostly northwest and southeast along the major fault lines in our area. A friend in Santa Cruz on the coast reported to me that he didn’t feel the quake at all. In case you non-Californians are wondering, a quake this size may not even make the TV news. It’s strong enough to be felt, but causes no damage. They occur maybe several times a month if you consider the state as a whole. As I was out hiking yesterday I was thinking it has been just about 20 years now since the Loma Prieta quake of 1989. We have a quake that you can feel maybe once or twice a year, but so far nothing even alarming for 20 years.

31. Earthquakes In Japan
Earthquake measurement. The Japanese shindo scale for measuring earthquakes is more commonly used in Japan than the Richter scale to describe earthquakes.
http://www.japan-guide.com/e/e2116.html
document.write(spod.nickname); document.write(spod.quote); document.write(spod.nickname); document.write(spod.quote); document.write(spod.nickname); document.write(spod.quote); Meet new friends, find pen-pals and language learning partners, or meet your ideal match! Travel Living A-Z ... Questions Search this site Apartment Search Area:
All Areas (Tokyo) Minato-ku Shibuya-ku Chuo-ku Shinjuku-ku Bunkyo-ku Chiyoda-ku Meguro-ku Setagaya-ku Shinagawa-ku Oota-ku Suginami-ku Nakano-ku Koto-ku Taito-ku Sumida-ku Toshima-ku Nerima-ku
Monthly rent:
to no max. Yen
Bedrooms (multiple selections possible):
Studio
4BED or more
Related Pages Living in Japan
Travel

Geography
Great Kanto Earthquake 1923 ...
Kobe Earthquake Museum
Survey If you had a choice, through which airport would you prefer to enter Japan? Narita Airport (Tokyo) Haneda Airport (Tokyo) Kansai Airport (Osaka) Central Japan Airport (Nagoya) Fukuoka Airport New Chitose Airport (Sapporo) see results Other Surveys: Tsukiji Market Favorite hotel reservation website Favorite travel guide books How to improve tourism ... Have you recently entered Japan? japan-guide.com newsletter Keeping you up to date on Japan travel and living related issues and site updates.

32. Earthquake
Despite their slow speed, these waves are particularly destructive to human construction because they cause considerable ground movement. Earthquake Measurement
http://www.eoearth.org/article/Earthquake
@import url(/themes/newbase/css/print.css); Encyclopedia of Earth Articles Earthquake
  • Sign up ... SITE FEED
    Earthquake
    document.getElementById('lightbox').style.display = 'none';
    Earthquake
    Published: July 18, 2010, 2:05 pm
    Edited: July 18, 2010, 2:05 pm Lead Author: Michael Pidwirny Topics: Geology Rate: Content Source: USGS This article has been reviewed by the following Topic Editors: William Heins Galal Hassan Galal Hussein C Michael Hogan PhD.
    Introduction
    An earthquake is a sudden vibration or trembling in the Earth. More than 150,000 tremors strong enough to be felt by humans occur each year worldwide. Earthquake motion is caused by the quick release of stored potential energy into the kinetic energy of motion. Most earthquakes are produced along faults, tectonic plate boundary zones, or along the mid-oceanic ridges (Figures 1 and 2). At these areas, large masses of rock that are moving past each other can become locked due to friction. Friction is overcome when the accumulating stress has enough force to cause a sudden slippage of the rock masses. The magnitude of the shock wave released into the surrounding rocks is controlled by the quantity of stress built up because of friction, the distance the rock moved when the slippage occurred, and ability of the rock to transmit the energy contained in the seismic waves. The San Francisco earthquake of 1906 involved a 6

33. Facts About Modified Mercalli Intensity Scale: Earthquakes, As Discussed In Brit
Facts about Modified Mercalli Intensity Scale earthquakes, as discussed in Britannica Compton's Encyclopedia earthquake Measurement
http://www.britannica.com/facts/11/827757/Modified-Mercalli-Intensity-Scale-as-d
document.write(''); Search Site: With all of these words With the exact phrase With any of these words Without these words Home

34. Analysis Of Earthquake Recordings Obtained From The Seafloor Earthquake Measurem
Analysis of earthquake recordings obtained from the Seafloor Earthquake Measurement System (SEMS) instruments deployed off the coast of southern California
http://www.bssaonline.org/cgi/content/abstract/89/1/260

35. Buy.com - Earthquake Measurement (1883) Ewing, James Alfred : ISBN 33094
Find, shop, and buy computers, laptops, books, dvd, videos, games, video games, music, sporting goods, software, electronics, digital cameras, camcorders, toys, luggage, and
http://www.buy.com/prod/earthquake-measurement-1883/q/loc/106/212678445.html

36. Earthquakes
The California Geological Survey studies earthquakes to help Californians plan and build earthquake resistant communities. We record the strong ground motion from earthquakes
http://www.consrv.ca.gov/cgs/geologic_hazards/earthquakes/Pages/index.aspx

37. Earthquake Measurement: Question Preview
Preview questions found in the review game data set titled Earthquake Measurement Chapter 5 , Section 2
http://reviewgamezone.com/preview.php?id=208

38. Himselp.Net.In - Home Page
The Himalayan School Earthquake Laboratory Programme (HIMSELP) is one of the important components of the Mission Mode Project of Department of Science Technology, Govt. of India.
http://www.himselp.net.in/earthquakemeasurement.html
Menu:
Student's Corner Himalayan Earthquakes Kangra(1905)
Bihar-Nepal(1934)

Bihar-Nepal(1988)
Uttarkashi(1991) ...
Chamoli(1999)

EarthQuake Sites ASC-INDIA.ORG
USGS.GOV

FEMA.GOV

BGS.AC.UK
Earthquake Measurement
HOW TO MEASURE THE SIZE OF EARTHQUAKE? The severity of an earthquake can be expressed in terms of both magnitude and intensity . However, the two terms are quite different, and they are often confused. INTENSITY Intensity is defined as the degree of damage.It is based on the observed effects of ground shaking on people, buildings, and natural features. It varies from place to place within the disturbed region depending on the location of the observer with respect to the earthquake epicenter.
Intensity scale:
  • Rossi Forrels scale Modified Mercalli Scale MSK Scale EMS Scale
  • (**********add link for reference) MAGNITUDE Magnitude is related to the amount of seismic energy released at the hypocenter of the earthquake. It is based on the amplitude of the earthquake waves recorded on instruments which have a common calibration. The magnitude of an earthquake is thus represented by a single, instrumentally determined value. Richter developed a scale using the amplitudes recorded during earthquake with standard Wood Anderson seismograph in California .Richter magnitude scale is a logarithamic scale .An increase in magnitude by 1 means 10 times higher wave amplitude and about 30 times higher energy release .Earthquake magnitude can be expressed in terms of energy of TNT.

    39. Earthquake Measurement Games (ID: 208)
    Review Games Chapter 5 , Section 2 Chapter 5 , Section 2. Linked to NJ state standards at the 6th 7th grade level.
    http://reviewgamezone.com/game.php?id=208

    40. USGS Science Topics: Real-time Monitoring And Reporting
    Provides links to USGS information about realtime monitoring and reporting and earthquakes. Provides a topical browse interface into USGS information utilizing controlled
    http://www.usgs.gov/science/combine.php?term=1351&with=304

    A  B  C  D  E  F  G  H  I  J  K  L  M  N  O  P  Q  R  S  T  U  V  W  X  Y  Z  

    Page 2     21-40 of 47    Back | 1  | 2  | 3  | Next 20

    free hit counter