 
									
								
									The California earthquake of April 18, 1906 ranks as one of the most
									
... Francisco earthquake". Shaking damage, however, was equally severe in many other places along the fault rupture. The frequently quoted value of 700 deaths caused by the earthquake and fire is now believed to underestimate the total loss of life by a factor of 3 or 4. Most of the fatalities occurred ...
                        	... Francisco earthquake". Shaking damage, however, was equally severe in many other places along the fault rupture. The frequently quoted value of 700 deaths caused by the earthquake and fire is now believed to underestimate the total loss of life by a factor of 3 or 4. Most of the fatalities occurred ...
									Managing data for seismic networks, Hanoi, 2015
									
...  Regional data are accessed via internet through seedlink protocol plug-ins, installed with SeisComP3 software at the central server  The network utilises SeisComP3 as the primary software for data acquisition, analysis and archival Managing data for seismic networks, Hanoi, 2015 ...
                        	...  Regional data are accessed via internet through seedlink protocol plug-ins, installed with SeisComP3 software at the central server  The network utilises SeisComP3 as the primary software for data acquisition, analysis and archival Managing data for seismic networks, Hanoi, 2015 ...
									implementing low-damage structural systems
									
... mismatch between societal expectations over the reality of seismic performance of modern buildings. In general, albeit with some unfortunate exceptions, modern multi-storey buildings performed as expected from a technical point of view, in particular when considering the intensity of the shaking (hi ...
                        	... mismatch between societal expectations over the reality of seismic performance of modern buildings. In general, albeit with some unfortunate exceptions, modern multi-storey buildings performed as expected from a technical point of view, in particular when considering the intensity of the shaking (hi ...
									Design and Construction of a Full-scale 5
									
... repairs. Likewise, the 2010 Chile earthquake imposed significant nonstructural damage to all types of buildings (Moehle et al., 2010). The closure of airports due to nonstructural damage cost the airline $25 million in downtime, while 62% of the hospitals in the affected regions of Chile suffered fr ...
                        	... repairs. Likewise, the 2010 Chile earthquake imposed significant nonstructural damage to all types of buildings (Moehle et al., 2010). The closure of airports due to nonstructural damage cost the airline $25 million in downtime, while 62% of the hospitals in the affected regions of Chile suffered fr ...
									Earthquakes - Our Lady of Grace School / Homepage
									
... • some shake buildings from side to side • move more slowly than P waves and S waves, but produce the most severe ground movement ...
                        	... • some shake buildings from side to side • move more slowly than P waves and S waves, but produce the most severe ground movement ...
									Meagan Rodman
									
... may also be at risk. Volcanoes and earthquakes have a very important relationship. For instance, an earthquake can trigger an active volcano, which would trigger cause an eruption. Or, it could be the exact opposite, meaning that a volcanic eruption could cause an earthquake. The earthquake followin ...
                        	... may also be at risk. Volcanoes and earthquakes have a very important relationship. For instance, an earthquake can trigger an active volcano, which would trigger cause an eruption. Or, it could be the exact opposite, meaning that a volcanic eruption could cause an earthquake. The earthquake followin ...
									Japan Earthquake and Tsunami
									
... The USGS PAGER map shows the population exposed to different Modified Mercalli Intensity (MMI) levels. MMI describes the severity of an earthquake in terms of its effect on humans and structures and is a rough measure of the amount of shaking at a given location. Overall, the population in this regi ...
                        	... The USGS PAGER map shows the population exposed to different Modified Mercalli Intensity (MMI) levels. MMI describes the severity of an earthquake in terms of its effect on humans and structures and is a rough measure of the amount of shaking at a given location. Overall, the population in this regi ...
									earthquake
									
... • Identified as P waves or S waves • P waves (a.k.a. primary or pressure) - Are push-pull waves that push (compress) and pull (expand) in the direction that the waves travel. (Physics: Longitudinal waves) - Travel through solids, liquids, and gases - Have the greatest velocity of all earthquake wave ...
                        	... • Identified as P waves or S waves • P waves (a.k.a. primary or pressure) - Are push-pull waves that push (compress) and pull (expand) in the direction that the waves travel. (Physics: Longitudinal waves) - Travel through solids, liquids, and gases - Have the greatest velocity of all earthquake wave ...
									earthquake
									
... Figure 8 Locating an Earthquake A A travel-time graph is used to determine the distance to the epicenter. The difference in arrival times of the first P wave and the first S wave in the graph is 5 minutes. So the epicenter is roughly 3800 kilometers away. B The epicenter is located using the distanc ...
                        	... Figure 8 Locating an Earthquake A A travel-time graph is used to determine the distance to the epicenter. The difference in arrival times of the first P wave and the first S wave in the graph is 5 minutes. So the epicenter is roughly 3800 kilometers away. B The epicenter is located using the distanc ...
									Earthquakes - Siemens Science Day
									
... – Reality: An earthquake is not caused by a volcanic erup?on. Faults are cracks in the Earth’s crust that form along plate boundaries. When the plates move, pressure builds and energy is relea ...
                        	... – Reality: An earthquake is not caused by a volcanic erup?on. Faults are cracks in the Earth’s crust that form along plate boundaries. When the plates move, pressure builds and energy is relea ...
									Revelation of 5.12 Quake, Sichuan, ChinaPart I Background of
									
... constructed of concrete or mixed materials were three times more likely to sustain injuries (odds ratio [OR] = 3.4; 95% confidence interval [CI],1.1-13.5)than were those inside wooden buildings (76). ...
                        	... constructed of concrete or mixed materials were three times more likely to sustain injuries (odds ratio [OR] = 3.4; 95% confidence interval [CI],1.1-13.5)than were those inside wooden buildings (76). ...
									Seismic velocity and crustal thickness inversions: Moon and Mars
									
... impact sites. A full 3-D model of the lunar crustal thickness is then obtained using the GRAIL gravimetric data, anchored by the crustal thicknesses under each Apollo station and impact site. To avoid the use of any seismic reference model, a Bayesian inversion technique is implemented. The advantag ...
                        	... impact sites. A full 3-D model of the lunar crustal thickness is then obtained using the GRAIL gravimetric data, anchored by the crustal thicknesses under each Apollo station and impact site. To avoid the use of any seismic reference model, a Bayesian inversion technique is implemented. The advantag ...
									Earthquakes
									
... stationery whilst the surrounding apparatus moves with the vibrations caused by the tremor. The spring amplifies the movement so that it can be recorded directly on the chart attached to the revolving drum. Modern Seismometers work on a similar principle but instead of using a pen the signal is conv ...
                        	... stationery whilst the surrounding apparatus moves with the vibrations caused by the tremor. The spring amplifies the movement so that it can be recorded directly on the chart attached to the revolving drum. Modern Seismometers work on a similar principle but instead of using a pen the signal is conv ...
									Seismic Response Analysis Of Concrete Block Masonry Buildings
									
... concrete block masonry building with a constructive system recently proposed at University of Minho and compared with the performance of an unreinforced concrete block masonry building with an identical configuration. The seismic behavior of the masonry buildings is acquired by experimental shaking ...
                        	... concrete block masonry building with a constructive system recently proposed at University of Minho and compared with the performance of an unreinforced concrete block masonry building with an identical configuration. The seismic behavior of the masonry buildings is acquired by experimental shaking ...
									Seismic Refraction / Reflection
									
... and layer geometry (folds). The Seismic Refraction & Reflection (SRR) system is designed to allow for either seismic refraction or seismic reflection data acquisition. The SRR system, which is designed for shallow surveys, can also be used for detecting voids in large civil structures such as dams ( ...
                        	... and layer geometry (folds). The Seismic Refraction & Reflection (SRR) system is designed to allow for either seismic refraction or seismic reflection data acquisition. The SRR system, which is designed for shallow surveys, can also be used for detecting voids in large civil structures such as dams ( ...
									EARTHQUAKE DIRECTED READING – DUACSEK EARTH SCIENCE
									
... c. the type of force exerted on each unit of area d. the amount of force exerted on each unit of area 2. The type of stress that squeezes and shortens a body is called a. collision. b. tension. c. compression. d. convergence. 3. In addition to reducing the amount of space that rock occupies, compres ...
                        	... c. the type of force exerted on each unit of area d. the amount of force exerted on each unit of area 2. The type of stress that squeezes and shortens a body is called a. collision. b. tension. c. compression. d. convergence. 3. In addition to reducing the amount of space that rock occupies, compres ...
									Vulnerability evaluation and seismic rehabilitation of steel building
									
... The 14 World Conference on Earthquake Engineering October 12-17, 2008, Beijing, China ...
                        	... The 14 World Conference on Earthquake Engineering October 12-17, 2008, Beijing, China ...
									COUNTRY REPORT ON Jordan seismological Observatory
									
... Earthquake hazard assessment no longer refers to single parameters such as the horizontal peak ground acceleration (PGA) as a quantifier of the hazard. The modern construction engineer requires information about the expected acceleration at frequencies similar to the natural frequencies of the build ...
                        	... Earthquake hazard assessment no longer refers to single parameters such as the horizontal peak ground acceleration (PGA) as a quantifier of the hazard. The modern construction engineer requires information about the expected acceleration at frequencies similar to the natural frequencies of the build ...
									12.2 Note Outline key.jnt
									
... Earth is composed of layers, including the lithosphere (surface) and asthenosphere (just below the surface) The asthenosphere is partly molten, and allows the tectonic plates of the lithosphere to “float” on the convection currents of hot magma. When tectonic plates meet (converge), one plate may sl ...
                        	... Earth is composed of layers, including the lithosphere (surface) and asthenosphere (just below the surface) The asthenosphere is partly molten, and allows the tectonic plates of the lithosphere to “float” on the convection currents of hot magma. When tectonic plates meet (converge), one plate may sl ...
									12.2 Note Outline
									
... Earth is composed of layers, including the lithosphere (surface) and asthenosphere (just below the surface) The asthenosphere is partly molten, and allows the tectonic plates of the lithosphere to “float” on the convection currents of hot magma. When tectonic plates meet (converge), one plate may sl ...
                        	... Earth is composed of layers, including the lithosphere (surface) and asthenosphere (just below the surface) The asthenosphere is partly molten, and allows the tectonic plates of the lithosphere to “float” on the convection currents of hot magma. When tectonic plates meet (converge), one plate may sl ...
									comparison on the effect of earthquake and wind loads on the
									
... high-rise reinforced concrete buildings were generally deemed satisfactory under the low intensity earthquake level (0.20g). The Inter-storey Drift Index (IDI) level shows that HKB had reached the fourth level, while KK, KM and PPJ buildings had reached the third level of the damaging potential. Bas ...
                        	... high-rise reinforced concrete buildings were generally deemed satisfactory under the low intensity earthquake level (0.20g). The Inter-storey Drift Index (IDI) level shows that HKB had reached the fourth level, while KK, KM and PPJ buildings had reached the third level of the damaging potential. Bas ...
									S waves - PHS GEOGRAPHY
									
... Plate boundaries and faults (= cracks where plate sections are moving in different directions) cause friction as plates move ...
                        	... Plate boundaries and faults (= cracks where plate sections are moving in different directions) cause friction as plates move ...
									S waves
									
... Plate boundaries and faults (= cracks where plate sections are moving in different directions) cause friction as plates move ...
                        	... Plate boundaries and faults (= cracks where plate sections are moving in different directions) cause friction as plates move ...
									Chapter 5
									
...  Lose soil shakes more than solid rock – house built on sandy soil will shake more than the one built on solid rock ...
                        	...  Lose soil shakes more than solid rock – house built on sandy soil will shake more than the one built on solid rock ...
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.
 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									