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Earthquake Liquefaction San Andreas Fault
Earthquake Liquefaction San Andreas Fault

... These liquefaction scenario maps are not intended to be site-specific. Rather, they depict the general risk within neighborhoods and the relative risk from community to community. ...
a testable five-year forecast of moderate and large earthquakes in
a testable five-year forecast of moderate and large earthquakes in

... from place to place only because the multiplicative regional density function f ( ,  ) does. Bird and Kagan (2004) found that this assumption was consistent with observed seismicity in ...
Resistivity structure across Itoigawa-Shizuoka tectonic line and its implications
Resistivity structure across Itoigawa-Shizuoka tectonic line and its implications

... by the Japan Meteorological Agency (Yuzo Ishikawa, personal communication). These hypocenters are generally located in resistive regions near the boundaries. Very few hypocenters are located within conductors. These may imply that the earthquakes are triggered by migration of fluid to less permeable ...
Slide 1
Slide 1

... output energies is estimated to be 10-5 – 10-6 • Large scale atmospheric pressure gradient (APG) can create the additional deformation deep enough in the earth’s crust • The ocean – land boundary can effectively transform homogeneous atmospheric pressure into its sharp gradient acting on the earth’s ...
Travel time curves
Travel time curves

... either through the earth’s interior (P and S waves; the fastest waves) or along or near the earth’s surface (Rayleigh and Love waves). Seismic waves travel at speeds of several kilometers per second. Seismicity—the geographic and historical distribution (the “where?” and “how often?”) of earthquakes ...
Lessons Learned from the Kobe Earthquake A Japanese
Lessons Learned from the Kobe Earthquake A Japanese

... prestressed concrete buildings during the Hyogoken-Nanbu earthquake (also known as the Great Hanshin earthquake) of January 17, 1995, situated in and around the city of Kobe, Japan. The performance of pile foundations is also examined. Highway bridges, rapid transit structures, and other special str ...
Effect of Diaphragm Discontinuity on Seismic Response
Effect of Diaphragm Discontinuity on Seismic Response

... They concluded that A summary of important seismic events from 1980 to 2008, where it is observed building damaged due to different irregularities causes. They conclude that constructions are more vulnerable when they are irregular are. The linear analyses provide important information for torsion b ...
o-47 inelastic finite element models to assess earthquake damage
o-47 inelastic finite element models to assess earthquake damage

... length toward the interior of the wall. Additionally, reinforcement buckling and fracture at wall boundaries, and in some cases, global inelastic wall buckling were observed. Research on the observed damage in RC walls has been mainly focused on analytical and experimental work on isolated RC wall s ...
Earthquakes, Plate Boundaries, and Depth Indiana Standard
Earthquakes, Plate Boundaries, and Depth Indiana Standard

... Students will use the world map with ocean floor age and plate tectonic overlays to assess and correlate earthquake data. Assignments and/or questions for Review: • Is there any relationship between earthquake depth and ocean floor age? If so explain the relationship. • Do any of the earthquakes doc ...
Zaliapin and Ben-Zion - University of Nevada, Reno
Zaliapin and Ben-Zion - University of Nevada, Reno

...  The figure below shows the 2D distribution of the time and space components of the nearest-neighbor earthquake distance for southern California  The bimodal structure is used to identify the cluster and background populations  This study explores in detail such 2D distributions for different loc ...
Term Project Exercise 1
Term Project Exercise 1

... Make a Bookmark for this map, and name it as “Mediterranean”. Examine the distribution of the earthquake locations around the Mediterranean Sea. Why do you think earthquakes occur lined up in some regions? Offer your explanation and illustrate it with a map. ...
Cost Modeling of Reinforced Concrete Buildings Designed for
Cost Modeling of Reinforced Concrete Buildings Designed for

... concrete and equivalent area of shuttering remain same but the quantum of reinforcement steel per square of floor area will generally gets reduced towards the upper floors due to the reduction in earthquake induced storey shears towards the upper storeys. BUILDINGS STUDIED The structural system with ...
Seismic Response Analysis Of Concrete Block Masonry Buildings
Seismic Response Analysis Of Concrete Block Masonry Buildings

... considerably the self-weight of the landing structure, representing also a very dangerous situation to the people nearby to the falling structure. Inspections to out-of-plane wall failures typically indicated poor or not anchorage of the wall to the supporting diaphragm. In-plane damage has been als ...
Temporal variation of seismic b-values beneath northeastern Japan
Temporal variation of seismic b-values beneath northeastern Japan

... the temporal variations of b-values has been used to explain bvalue changes prior to major earthquakes in Japan and elsewhere [Imoto, 1991]. Decrease in effective stress due to dehydration is thought to be the cause of the observed high b-values in the Alaska and New Zealand subduction zones at the ...
effects of distant and large magnitude earthquakes on the tallest
effects of distant and large magnitude earthquakes on the tallest

... the inhabitants of the higher floors of tall buildings. Other cities in Argentina were also shaken by this 1997 Chilean earthquake, different alarm levels being generated among their inhabitants. However, it caused no damage or casualties. In the Argentine provincial capital nearest to the epicentra ...
January 3 2013 - Hope`s Institutional Research Archive (HIRA)
January 3 2013 - Hope`s Institutional Research Archive (HIRA)

... Table 1 represents the results of this bibliographic research and summarises two catalogues compiled by the authors: one for major earthquakes dating from 1890; and the other for the principal volcanic eruptions that have occurred after 1856 and which have impacted Islamic countries or those with a ...
Souces and scenarios for tsunami hazard assessment in the
Souces and scenarios for tsunami hazard assessment in the

... tsunami history. Tsunami scenarios are computed for each grid cell and for different EQ magnitudes starting from “standard” tsunami initial conditions (practice by Global Disasters Alerts & Coordination System, JRC, Ulutas et al., 2012). ...
PDF - Geophysical Journal International
PDF - Geophysical Journal International

... of earthquakes since 1900. A break in Gutenberg–Richter scaling for large earthquakes in global seismicity has been observed, this break is also observed in our Taiwan study. The seismic data from the Central Weather Bureau Seismic Network are in good agreement with the Gutenberg–Richter relation ta ...
Tromp et al. 2010 - ShakeMovie Global
Tromp et al. 2010 - ShakeMovie Global

... calculates normal-mode synthetic seismograms for the Preliminary Reference Earth Model, and spectral-element synthetic seismograms for 3-D mantle model S362ANI in combination with crustal model Crust2.0. The 1-D and 3-D synthetics for more than 1800 seismographic stations operated by members of the ...
Coupled Simulation of Ground Shaking and Tsunami for Mega
Coupled Simulation of Ground Shaking and Tsunami for Mega

... results based on low-frequency data place large slip patches near the epicenter and along the Japan Trench at shallow depths. On the other hand, results based on high-frequency data suggest that multiple localized areas, which radiate intense high-frequency seismic energy, are required at relatively ...
General Committee 3 Chair Report-1
General Committee 3 Chair Report-1

... The 1990 Luzon earthquake happened on July 16 on the highly populated island Luzon in Philippines. The magnitude of this earthquake was 7.8. The shock effected 125km around the island Luzon. It included Dingalan to Cuyapo. The earthquake occurred due to the strike-slip movement on the Philippine Fau ...
Shayla
Shayla

... The parts of the earth most prone to earthquakes are around the ring of fire. The area with the most earthquakes is Indonesia and South Eastern Asia. We are able to predict where earthquakes are going to happen by knowing that most occur along faults or plate boundaries. The relationship between ear ...
Application of Neural Networks and Statistical Pattern Recognition
Application of Neural Networks and Statistical Pattern Recognition

... is crucial for seismic risk prevention strategies in urban systems, as well as for the safe design of major structures. However, the largest seismic events of the last decade have demonstrated that the observed ground shaking can be much more severe than expected and its spatial distribution poorly ...
SERVO-CCE
SERVO-CCE

... 0.0 6.0 7 0.07 3358386 1932-01-01 23:52:07.87 ...
Lithosphere
Lithosphere

... mantle. This corresponds to mantle material at or near its melting point (1300 C). This shows that the mantle material at this depth behaves differently compared with mantle above and below. The low velocity zone is ductile, while the mantle around it is rigid. So it makes sense to group the rigid m ...
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1988 Armenian earthquake



The 1988 Armenian earthquake, also known as the Spitak earthquake (Armenian: Սպիտակի երկրաշարժ Spitaki yerkrašarž) occurred in the northern region of Armenia (then part of the Soviet Union) on Wednesday, December 7, 1988 at 11:41 local time (07:41 UTC). The earthquake measured 6.8 on the surface wave magnitude scale and had a maximum perceived intensity of X (Devastating) on the Medvedev–Sponheuer–Karnik scale. The region that the earthquake occurred is vulnerable to occasional large and destructive earthquakes and is part of a larger active seismic belt that stretches from the Alps to the Himalayas. Activity in the area is associated with tectonic plate boundary interaction and the source of the event was a slip of a thrust fault just to the north of Spitak.Seismologists thoroughly studied the effects of the Spitak event, including the mainshock and aftershock fault rupture mechanisms and were on site setting up temporary seismometers before the end of 1988. Earthquake engineering experts scrutinized building construction styles and found fault in the poorly constructed apartments and other buildings that were built during the Era of Stagnation under the rule of Leonid Brezhnev. The cities of Spitak, Leninakan (Gyumri), and Kirovakan (Vanadzor) were greatly affected with large losses of life and devastating effects to buildings and other structures. A number of the smaller outlying villages away from the larger population centers were also severely affected.Despite the tensions of the Cold War, Soviet leader Mikhail Gorbachev formally asked the United States for humanitarian help within a few days of the earthquake, the first such request since World War II. One hundred and thirteen countries sent substantial amounts of humanitarian aid to the Soviet Union in the form of rescue equipment, search teams and medical supplies, but private donations and assistance from non-governmental organizations also had a large part of the international effort. While transporting some of these supplies to the region, a Soviet aircraft carrying 78 relief workers from Azerbaijan and a transport plane from Yugoslavia were both destroyed in separate incidents. In support of the relief effort, recording artists united to produce several music-related contributions for the victims of the quake. A song was produced by a duo of French composers (including Charles Aznavour) and a studio album that featured songs donated by mainstream rock bands was released from the Rock Aid Armenia effort by the British music industry.
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