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Soft Soil Effect on Soft Storey Response
Soft Soil Effect on Soft Storey Response

... Multi-storied reinforced concrete frame (RCF) buildings with open first storey to provide parking space is common in Dhaka city, the capital of Bangladesh. Such buildings are likely to produce soft storey action when subjected to earthquake loadings. Bangladesh building code places Dhaka in a modera ...
Causes of Tsunami - Tsunami: Magnitude of Terror
Causes of Tsunami - Tsunami: Magnitude of Terror

... When they occur beneath the sea, the water above the deformed area is displaced from its equilibrium position. Waves are formed as the displaced water mass, acting under the force of gravity, tries to regain equilibrium. When large areas of the sea floor elevate or subside, a tsunami can be created. ...
An____________is a movement of Earth’s lithosphere shift, releasing stored energy.
An____________is a movement of Earth’s lithosphere shift, releasing stored energy.

... • Folds form where rocks are squeezed together but do not break. • Rocks tend to fold rather than break when they are under high temperature or pressure. Stress can squeeze rock together, producing folds in layers of rock. ...
federal emergency
federal emergency

... [FEMA-88] Guidebook for Developing a School Earthquake Safety Program. Revised Edition. FEMA. Washington, DC, 1990. 52 pages. This Guidebook is designed to assist the school community of principal, teachers, staff, parents, and students in developing an earthquake safety program for their school. To ...
Malaysian Journal of Civil Engineering 28(1):108
Malaysian Journal of Civil Engineering 28(1):108

Basics of the modelling of the ground deformations produced by an
Basics of the modelling of the ground deformations produced by an

... Between major earthquakes: • the active faults are « locked » • the surrounding region deforms in a continuous manner, measurable until a distance of ~50km • velocity gradient looks like a sigmoid ...
Concurrent density dependence and independence in
Concurrent density dependence and independence in

... high (Fig. 3a). At the time of the shallow intrusion, the rift opened about 2 m (refs 11, 15, 21), an eruptive ®ssure formed (Fig. 1), and seismicity within this region of the south ¯ank immediately increased by more than a factor of ten (Fig. 2a). The intrusion also resulted in changes in the patte ...
Modified True/False - Indicate whether the
Modified True/False - Indicate whether the

... a. the mass c. the rotating drum b. the spring d. the frame ____ 19. The stress which causes a material to twist is known as ____. a. Tension ...
Case study of a 40-storey buckling-restrained braced frame building
Case study of a 40-storey buckling-restrained braced frame building

... behalf of the Pacific Earthquake Engineering Research Center (PEER) under its Tall Buildings Initiative (TBI). The objective of the TBI is to develop recommended performance-based design criteria for tall buildings as an alternative to the criteria contained in present building codes and standards. ...
Paper 42 - New Zealand Society for Earthquake Engineering Inc.
Paper 42 - New Zealand Society for Earthquake Engineering Inc.

... The seismic performance of a large variety of civil engineering structures has been investigated in the Department of Civil and Natural Resources Engineering at the University of Canterbury for many years. For that purpose several shake table experiments have been conducted using different models of ...
V - Uni Kassel
V - Uni Kassel

Earthquakes
Earthquakes

... • Seismic waves travel at different speeds. – P waves travel faster than S waves – To tell how far the epicenter is from the seismograph, scientists measure the difference between the arrival times of the P waves and S waves. – The longer the time difference, the further the epicenter is from the se ...
Earthquakes
Earthquakes

... • Seismic waves travel at different speeds. – P waves travel faster than S waves – To tell how far the epicenter is from the seismograph, scientists measure the difference between the arrival times of the P waves and S waves. – The longer the time difference, the further the epicenter is from the se ...
Earthquakes
Earthquakes

... • Seismic waves travel at different speeds. – P waves travel faster than S waves – To tell how far the epicenter is from the seismograph, scientists measure the difference between the arrival times of the P waves and S waves. – The longer the time difference, the further the epicenter is from the se ...
Lecture 2
Lecture 2

... 9. Faults can have relative movements which consist of: (1) dip slip, (2) strike slip, and (3) oblique. ...
3D Imaging of the Earth`s Lithosphere Using Noise from Ocean Waves
3D Imaging of the Earth`s Lithosphere Using Noise from Ocean Waves

... Since Shapiro et al. (2005) first showed that group velocity dispersion maps can be obtained from ambient noise, ANT has become popular for imaging crustal and uppermost mantle structure. Compared to earthquake-based surface wave tomography, ANT frees surface wave tomography from its dependence on e ...
`Thinking & Learning Toolbox` Example Lesson Four: Tectonic Plates
`Thinking & Learning Toolbox` Example Lesson Four: Tectonic Plates

... TASK: Name the three types of Tectonic Plate Margin, and give two pieces of information on each, such as typical features & characteristics that may be found at each type of margin. ...
Accelerating Seismicity and Stress Accumulation Before Large
Accelerating Seismicity and Stress Accumulation Before Large

... Simpson, 1996]. From these studies we can draw the conclusion that stress must accumulate not only on the fault itself, but also in a large region surrounding the fault prior to an earthquake. It is this stressed volume that we seek t o define. One approach to solving this problem is to combine the ...
The Continued Utility of Probabilistic Seismic
The Continued Utility of Probabilistic Seismic

... 1g in an area of formerly low seismicity where the New Zealand PSH model (Stirling et al., 2012) showed 500-year PGA motions of about 0.3g. As I have mentioned, the 500-year return period is one of the most frequently used portrayals of PSH, but in low seismicity areas, the 500-year motions will alm ...
Concrete Design Steel Design Masonry Design Timber/Wood
Concrete Design Steel Design Masonry Design Timber/Wood

... Sonoma State University Dormitory Remodel. Jeff was the structural design engineer responsible for the design and permitting of the Zinfandel Village Residential Community Remodel in 2007 and 2008. The project included the modernization and remodel of the multi-structure, on-campus dormitory facilit ...
Multi-station Seismograph Network
Multi-station Seismograph Network

... the maximum motion recorded by a seismograph. Several scales have been defined, but the most commonly used are (1) local magnitude (ML), commonly referred to as “Richter magnitude,” (2) surface-wave magnitude (Ms), (3) body-wave magnitude (Mb), and (4) moment magnitude (Mw). Scales 1-3 have limited ...
Earthquake Tips
Earthquake Tips

... have a timer device (i.e., the drum holding the chart paper does not rotate). Such instruments provide only the maximum extent (or scope) of motion during the earthquake; for this reason they are called seismoscopes. The analog instruments have evolved over time, ...
EARTHQUAKES
EARTHQUAKES

... • Is the total force acting on crustal rocks per unit of area • Movement occurs when stress overcomes the strength of the rocks • There are three kinds of stress – Compression is the stress that decreases the volume of a material – Tension is the stress that pulls a material ...
Tsunami waveform analyses of the 2006 underthrust and 2007 outer
Tsunami waveform analyses of the 2006 underthrust and 2007 outer

... Many large earthquakes have occurred along the KurileKamchatka subduction zone from Kamchatka, Russia, to Hokkaido, Japan, as shown in Fig. 1. The largest earthquake was the 1952 Kamchatka earthquake (Mw =9.2). However, no historical large shallow earthquakes were known in the central Kurile segment ...
Multi-Offset Seismic Acquisition Using Optical Fiber
Multi-Offset Seismic Acquisition Using Optical Fiber

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Earthquake engineering



Earthquake engineering or Seismic engineering is a branch of engineering that searches for ways to make structures, such as buildings and bridges, resistant to earthquake damage. Earthquake engineer, better known as a seismic engineer aim to develop building techniques that will prevent any damage in a minor quake and avoid serious damage or collapse in a major shake. It is the scientific field concerned with protecting society, the natural environment, and the man-made environment from earthquakes by limiting the seismic risk to socio-economically acceptable levels. Traditionally, it has been narrowly defined as the study of the behavior of structures and geo-structures subject to seismic loading; it is considered as a subset of both structural and geotechnical engineering. However, the tremendous costs experienced in recent earthquakes have led to an expansion of its scope to encompass disciplines from the wider field of civil engineering, mechanical engineering and from the social sciences, especially sociology, political science, economics and finance. The main objectives of earthquake engineering are: Foresee the potential consequences of strong earthquakes on urban areas and civil infrastructure. Design, construct and maintain structures to perform at earthquake exposure up to the expectations and in compliance with building codes.A properly engineered structure does not necessarily have to be extremely strong or expensive. It has to be properly designed to withstand the seismic effects while sustaining an acceptable level of damage.
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