Epicenter
•Download as PPT, PDF•
0 likes•1,711 views
The epicenter is defined as the point on the Earth's surface directly above the focus of an earthquake, where the focus is the location underground where the earthquake rupture initiates and energy begins radiating outward. The document cites two sources, a science courseware website and physical geography website, as well as a science textbook, for information on the definition of an epicenter and focus.
Report
Share
Report
Share
![Definition ,[object Object],[object Object]](data:image/gif;base64,R0lGODlhAQABAIAAAAAAAP///yH5BAEAAAAALAAAAAABAAEAAAIBRAA7)
Recommended
EARTHQUAKE
This document discusses seismic waves, earthquakes, and seismology. It begins by listing the objectives of describing seismic wave types, finding earthquake epicenters, earthquake magnitude scales, and challenges predicting earthquakes. It then defines earthquakes and seismology, the study of earthquakes. It describes how seismographs are used to record seismic waves from earthquakes. It discusses elastic rebound theory, earthquake focus and epicenter, where earthquakes occur, and the different types of seismic waves. The document concludes by covering earthquake classification, damage causes, challenges predicting earthquakes, earthquake prone areas, and safety tips before, during, and after an earthquake.
Seismic waves
1. Seismic waves are energy waves generated by earthquakes that travel through the earth. There are two main types of seismic waves: body waves and surface waves.
2. Body waves include P-waves and S-waves. P-waves are faster primary waves that can travel through solid and liquid materials. S-waves are slower secondary waves that only travel through solids.
3. Surface waves include Love waves and Rayleigh waves. Love waves cause side-to-side motions while Rayleigh waves cause up and down rolling motions. Surface waves do the most damage to structures during an earthquake.
Seismic waves
Seismic waves are the waves of energy caused by the sudden breaking of rock within the earth or an explosion.
Response of material to the arrival of energy fronts released by rupture.
Energy that travels through the earth and is recorded on seismographs.
Intensity
The document describes the Philippine Institute of Volcanology and Seismology (PHILVOLCS) earthquake intensity scale, which ranks earthquakes from intensity level 1 to 10 based on their observed effects on people, structures, and the earth's surface. Intensity 7 earthquakes are described as being destructive and causing cracks in structures, while an intensity 10 earthquake would be completely devastating and destroy virtually all human infrastructure. The intensity of an earthquake typically lessens as the distance from the earthquake's focus increases.
Earthquake Presentation
Earthquakes are caused by the movement of tectonic plates underneath the earth's surface. When the plates shift and release stress, seismic waves propagate outward from the epicenter. Scientists measure the intensity of earthquakes using the Richter scale. During an earthquake, it is important to drop, cover, and hold on underneath sturdy furniture to protect oneself from falling debris.
Earthquake
This presentation gives detailed information about earthquake , its types , waves , faults , especially in asian countries .A detailed case study of earthquake In NEPAL in 2015 is also covered in this with pictures . Also how it is measured and its warning system , vulnerability, deployment and future aspects has been covered .
HOPE YOU LIKE IT AND GET FULL INFORMATION!!!!!
Earthquakes ppt for class
This is the earthquake power point you saw in class. Feel free to take notes on it or view the animations again.
Earthquake ppt
1) Earthquakes are caused by the sudden release of energy from movement along geological faults in the earth's crust, generating seismic waves.
2) Larger earthquakes can trigger tsunamis if located offshore by displacing seabed, as well as landslides and volcanic eruptions.
3) Earthquake shaking causes loss of life and property destruction from building collapse and landslides burying infrastructure.
Recommended
EARTHQUAKE
This document discusses seismic waves, earthquakes, and seismology. It begins by listing the objectives of describing seismic wave types, finding earthquake epicenters, earthquake magnitude scales, and challenges predicting earthquakes. It then defines earthquakes and seismology, the study of earthquakes. It describes how seismographs are used to record seismic waves from earthquakes. It discusses elastic rebound theory, earthquake focus and epicenter, where earthquakes occur, and the different types of seismic waves. The document concludes by covering earthquake classification, damage causes, challenges predicting earthquakes, earthquake prone areas, and safety tips before, during, and after an earthquake.
Seismic waves
1. Seismic waves are energy waves generated by earthquakes that travel through the earth. There are two main types of seismic waves: body waves and surface waves.
2. Body waves include P-waves and S-waves. P-waves are faster primary waves that can travel through solid and liquid materials. S-waves are slower secondary waves that only travel through solids.
3. Surface waves include Love waves and Rayleigh waves. Love waves cause side-to-side motions while Rayleigh waves cause up and down rolling motions. Surface waves do the most damage to structures during an earthquake.
Seismic waves
Seismic waves are the waves of energy caused by the sudden breaking of rock within the earth or an explosion.
Response of material to the arrival of energy fronts released by rupture.
Energy that travels through the earth and is recorded on seismographs.
Intensity
The document describes the Philippine Institute of Volcanology and Seismology (PHILVOLCS) earthquake intensity scale, which ranks earthquakes from intensity level 1 to 10 based on their observed effects on people, structures, and the earth's surface. Intensity 7 earthquakes are described as being destructive and causing cracks in structures, while an intensity 10 earthquake would be completely devastating and destroy virtually all human infrastructure. The intensity of an earthquake typically lessens as the distance from the earthquake's focus increases.
Earthquake Presentation
Earthquakes are caused by the movement of tectonic plates underneath the earth's surface. When the plates shift and release stress, seismic waves propagate outward from the epicenter. Scientists measure the intensity of earthquakes using the Richter scale. During an earthquake, it is important to drop, cover, and hold on underneath sturdy furniture to protect oneself from falling debris.
Earthquake
This presentation gives detailed information about earthquake , its types , waves , faults , especially in asian countries .A detailed case study of earthquake In NEPAL in 2015 is also covered in this with pictures . Also how it is measured and its warning system , vulnerability, deployment and future aspects has been covered .
HOPE YOU LIKE IT AND GET FULL INFORMATION!!!!!
Earthquakes ppt for class
This is the earthquake power point you saw in class. Feel free to take notes on it or view the animations again.
Earthquake ppt
1) Earthquakes are caused by the sudden release of energy from movement along geological faults in the earth's crust, generating seismic waves.
2) Larger earthquakes can trigger tsunamis if located offshore by displacing seabed, as well as landslides and volcanic eruptions.
3) Earthquake shaking causes loss of life and property destruction from building collapse and landslides burying infrastructure.
Earthquake
The document discusses earthquakes, including their causes, types of seismic waves produced, measurement on the Richter scale, potential hazards caused by earthquakes like landslides, fires, liquefaction, tsunamis and floods. It also discusses methods of earthquake prediction and safety precautions to take during an earthquake based on one's location.
Magnitude and intensity of earthquake
Magnitude measures the energy released at the earthquake's source, while intensity measures the strength of shaking at a given location. Magnitude is determined seismographically, while intensity considers effects on people, structures and the environment. A table shows typical maximum intensities observed near epicenters of different magnitude quakes: magnitude 1.0-3.0 often sees intensity I; 3.0-3.9 sees intensity II-III; 4.0-4.9 sees intensity IV-V; 5.0-5.9 sees intensity VI-VII; 6.0-6.9 sees intensity VII-IX; and 7.0+ often sees intensity VIII or higher. The Modified Mercalli intensity scale further
Earthquake Intensity
This document discusses earthquake intensity and magnitude. It defines an earthquake as the sudden release of energy in the Earth's crust that creates seismic waves. Earthquake intensity is a measure of the effects on the Earth's surface based on the Mercalli scale, while magnitude measures the energy released using seismograph recordings. The document provides details on what causes earthquakes, the relationship between intensity and magnitude, and examples of intensity scales like the Modified Mercalli scale. Tables show the correlation between typical intensities and magnitudes.
Earthquake and its hazards
PHIVOLCS monitors earthquakes in the Philippines using a network of over 100 seismic stations. Earthquakes are natural occurrences caused by the slow motion of tectonic plates. The Philippines is located in a seismically active area between several plates. PHIVOLCS provides information to the public on earthquake locations, intensities, and issues advisories. Larger earthquakes are inevitable given the Philippines' position between plates and presence of faults.
Volcano ppt
Volcanoes form when tectonic plates collide and magma rises up through the crust. The document discusses the Ring of Fire around the Pacific Ocean which has many active volcanoes. It also defines key volcanic terms and describes the three main types of volcanoes: shield, composite, and cinder cone volcanoes. The effects of volcanic eruptions on humans and the environment are also summarized.
Liquefaction
An earthquake is caused by the sudden displacement of rock in the Earth's crust due to crustal strain, volcanoes, landslides, or collapsing caverns. Earthquakes can cause ground shaking, landslides, fires, soil liquefaction, tsunamis, floods, and damage human infrastructure. Soil liquefaction occurs when saturated granular soils like silty sands or sandy gravels lose strength during an earthquake or sudden stress change and behave like liquid, which can damage buildings and cause them to sink or tilt.
Earthquacke Elastic Rebound Theory Types of Waves
1) The document discusses the causes and types of earthquakes. It explains that earthquakes are caused by the sudden release of built-up energy between tectonic plates, which generates seismic waves.
2) It describes the elastic rebound theory of earthquakes, which states that stress gradually builds up along faults until it is suddenly released, causing the plates to snap back in an earthquake.
3) There are different types of seismic waves generated - P waves, S waves, and surface waves including Rayleigh and Love waves. P and S waves travel through the earth's interior as body waves, while surface waves travel along the surface.
Earthquake plate tectonic- Geomorphology Chapter
An earthquake is caused by a sudden release of energy stored in rocks below the earth's surface. Most earthquakes occur along existing faults in the earth's crust. There are two key terms used to describe the location of earthquakes - the focus, which is the location below the surface where fault movement begins, and the epicenter, which is the point directly above the focus on the surface.
Volcanoes
This document defines volcanoes as openings in the Earth's crust that allow molten rock and gases to escape. It notes that over half of the world's active volcanoes above sea level are located along the Ring of Fire. Volcanoes form when tectonic plates collide, spread apart, or interact under a plate. The parts of a volcano include the crater, pipe, cone, and vent. There are three main types of volcanoes: composite/strato volcanoes, shield volcanoes, and cinder cone volcanoes. Volcanic eruptions can have both beneficial effects like adding nutrients to soil or creating new islands, and harmful effects like releasing aerosols or abandoning land.
Earthquake and tsunami
1) An earthquake is intense ground shaking caused by a sudden release of energy, often due to movement along faults within the Earth.
2) Earthquake magnitude is measured by the Richter Scale, where each whole number increase means the amplitude of shaking is 10 times greater. Magnitude 2.5 or less quakes are usually not felt, while anything above 8 can totally destroy communities near the epicenter.
3) Intensity refers to the amount of damage at a location and is measured by scales like Modified Mercalli, depending on factors like distance from the quake and duration of shaking.
Earthquakes 101
The document summarizes information about earthquakes, including:
1. It discusses major historical earthquakes like the 1877 Nebraska quake and the 1906 San Francisco earthquake.
2. It provides details on measuring earthquake magnitude, such as the largest quakes on record being the 1960 Chile quake at M9.5 and the 1964 Alaska quake at M9.2.
3. It describes the different types of plate boundaries like divergent, convergent and transform, and gives examples of each.
Study of earthquake hazards or disaster
Earthquake Hazards
Definition of Hazard
Liquefaction
Ground Shaking
Ground Displacement
Flooding
Tsunami
Fire
Types of Hazard
Natural Hazards as Earthquakes
What Are Earthquake Hazards?
Ground Shaking:
Folds and faults ppt
The document provides information about folds and faults. It defines folds as bent or curved rock layers, and describes common fold types like anticlines and synclines. It also defines various fault types including normal faults, thrust faults, strike-slip faults, and oblique faults. Specific structures are described like the San Andreas Fault, which is a major strike-slip fault in California. Dip, strike, heave and throw are also defined in relation to describing the orientation and movement of geological structures.
Earthquake Scales - Mercalli scale vs Richter scale
The document compares the Mercalli Intensity Scale and Richter Magnitude Scale. The Mercalli Scale describes earthquake intensity based on observed effects, ranging from I (detected only by instruments) to XII (total destruction). The Richter Scale uses seismograph measurements to describe an earthquake's magnitude on a logarithmic scale. Both scales were developed in the early 20th century - the Mercalli by Mercalli and the Richter by Charles Richter to study California quakes. While the Mercalli Scale relies on observations, the Richter Scale provides a more scientific measure of an earthquake's energy release.
natural and geological hazards
This document discusses different types of natural hazards including geological hazards such as earthquakes, tsunamis, landslides, and volcanic eruptions. It provides details on the impact of specific past events in the Philippines and recommends preparedness, response, and rehabilitation strategies. These include evaluating building safety, developing evacuation plans, staying away from damaged areas, and obtaining disaster information from radio after an event occurs. The goal is to minimize harm and casualties from natural hazards through preparedness before, appropriate response during, and rehabilitation after such events.
How rocks behave under different types of stress
This document discusses how rocks behave under different types of stress. It explains that rocks undergo deformation and strain when subjected to tensional, compressional, or shear stresses. The document outlines the different stages of rock deformation, from elastic to ductile to fracture, and factors like temperature, confining pressure, and composition that influence the deformation process. It also describes geological structures like joints, faults, folds, anticlines and synclines that form from rock deformation.
Faults
This document discusses faults, beginning with definitions and terminology. Faults occur due to brittle deformation from differential stresses and cause displacement of rock blocks. There are two types of movement: translational and rotational. Faults are classified based on their geometry, such as dip, pattern, and apparent movement. They are also classified based on the forces causing them, such as tensional, compressional, or shear stresses. Faults form important structures as ore deposits can be associated with them.
Study of an earthquake
WHAT IS AN EARTHQUAKE?
Where Do Earthquakes Happen?
Why Do Earthquakes Happen?
How Are Earthquakes Studied?
How To Locate The Earthquake's Epicenter?
SCALES FOR EARTHQUAKE MEASUREMENT
What Are Earthquake Hazards?
DRRR - Earthquake Hazards
Contents:
1. Concept of Earthquake
2. Hazards Associated to Earthquake
- Ground Shaking
- Ground Rapture
- Tsunami
- Earthquake induced landslide
3. What do to BEFORE, DURING, AFTER Earthquake
THUNDERSTORMS
A document tackling about the basis of Thunderstorms:
-What is Thunderstorm?
-How do the Thunderstorms form?
-What is the difference between thunder and lightning?
Between a water spout and a tornado?
-What are the types of Lightning? of a Thunderstorm?
-What are some signs of an approaching thunderstorm?
-What are some precautionary measures to do before and during a thunderstorm?
-Case of Thunderstorms in the Philippines and on Planes
Focus and Epicenter:
Focus and Epicenter:
The focus of an earthquake is the point where the rocks start to fracture. It is the origin of the earthquake.
The epicenter is the point on land directly above the focus.
Epicentre and Focus
The document explains the difference between an epicentre and focus of an earthquake. The epicentre is the point on the surface directly above where the earthquake starts, while the focus is the location below ground where the earthquake occurs. It provides the example of the 1995 Kobe earthquake, where the epicentre was marked on a map as a star, and it had a shallow focus close to the surface, causing significant damage to the city.
More Related Content
What's hot
Earthquake
The document discusses earthquakes, including their causes, types of seismic waves produced, measurement on the Richter scale, potential hazards caused by earthquakes like landslides, fires, liquefaction, tsunamis and floods. It also discusses methods of earthquake prediction and safety precautions to take during an earthquake based on one's location.
Magnitude and intensity of earthquake
Magnitude measures the energy released at the earthquake's source, while intensity measures the strength of shaking at a given location. Magnitude is determined seismographically, while intensity considers effects on people, structures and the environment. A table shows typical maximum intensities observed near epicenters of different magnitude quakes: magnitude 1.0-3.0 often sees intensity I; 3.0-3.9 sees intensity II-III; 4.0-4.9 sees intensity IV-V; 5.0-5.9 sees intensity VI-VII; 6.0-6.9 sees intensity VII-IX; and 7.0+ often sees intensity VIII or higher. The Modified Mercalli intensity scale further
Earthquake Intensity
This document discusses earthquake intensity and magnitude. It defines an earthquake as the sudden release of energy in the Earth's crust that creates seismic waves. Earthquake intensity is a measure of the effects on the Earth's surface based on the Mercalli scale, while magnitude measures the energy released using seismograph recordings. The document provides details on what causes earthquakes, the relationship between intensity and magnitude, and examples of intensity scales like the Modified Mercalli scale. Tables show the correlation between typical intensities and magnitudes.
Earthquake and its hazards
PHIVOLCS monitors earthquakes in the Philippines using a network of over 100 seismic stations. Earthquakes are natural occurrences caused by the slow motion of tectonic plates. The Philippines is located in a seismically active area between several plates. PHIVOLCS provides information to the public on earthquake locations, intensities, and issues advisories. Larger earthquakes are inevitable given the Philippines' position between plates and presence of faults.
Volcano ppt
Volcanoes form when tectonic plates collide and magma rises up through the crust. The document discusses the Ring of Fire around the Pacific Ocean which has many active volcanoes. It also defines key volcanic terms and describes the three main types of volcanoes: shield, composite, and cinder cone volcanoes. The effects of volcanic eruptions on humans and the environment are also summarized.
Liquefaction
An earthquake is caused by the sudden displacement of rock in the Earth's crust due to crustal strain, volcanoes, landslides, or collapsing caverns. Earthquakes can cause ground shaking, landslides, fires, soil liquefaction, tsunamis, floods, and damage human infrastructure. Soil liquefaction occurs when saturated granular soils like silty sands or sandy gravels lose strength during an earthquake or sudden stress change and behave like liquid, which can damage buildings and cause them to sink or tilt.
Earthquacke Elastic Rebound Theory Types of Waves
1) The document discusses the causes and types of earthquakes. It explains that earthquakes are caused by the sudden release of built-up energy between tectonic plates, which generates seismic waves.
2) It describes the elastic rebound theory of earthquakes, which states that stress gradually builds up along faults until it is suddenly released, causing the plates to snap back in an earthquake.
3) There are different types of seismic waves generated - P waves, S waves, and surface waves including Rayleigh and Love waves. P and S waves travel through the earth's interior as body waves, while surface waves travel along the surface.
Earthquake plate tectonic- Geomorphology Chapter
An earthquake is caused by a sudden release of energy stored in rocks below the earth's surface. Most earthquakes occur along existing faults in the earth's crust. There are two key terms used to describe the location of earthquakes - the focus, which is the location below the surface where fault movement begins, and the epicenter, which is the point directly above the focus on the surface.
Volcanoes
This document defines volcanoes as openings in the Earth's crust that allow molten rock and gases to escape. It notes that over half of the world's active volcanoes above sea level are located along the Ring of Fire. Volcanoes form when tectonic plates collide, spread apart, or interact under a plate. The parts of a volcano include the crater, pipe, cone, and vent. There are three main types of volcanoes: composite/strato volcanoes, shield volcanoes, and cinder cone volcanoes. Volcanic eruptions can have both beneficial effects like adding nutrients to soil or creating new islands, and harmful effects like releasing aerosols or abandoning land.
Earthquake and tsunami
1) An earthquake is intense ground shaking caused by a sudden release of energy, often due to movement along faults within the Earth.
2) Earthquake magnitude is measured by the Richter Scale, where each whole number increase means the amplitude of shaking is 10 times greater. Magnitude 2.5 or less quakes are usually not felt, while anything above 8 can totally destroy communities near the epicenter.
3) Intensity refers to the amount of damage at a location and is measured by scales like Modified Mercalli, depending on factors like distance from the quake and duration of shaking.
Earthquakes 101
The document summarizes information about earthquakes, including:
1. It discusses major historical earthquakes like the 1877 Nebraska quake and the 1906 San Francisco earthquake.
2. It provides details on measuring earthquake magnitude, such as the largest quakes on record being the 1960 Chile quake at M9.5 and the 1964 Alaska quake at M9.2.
3. It describes the different types of plate boundaries like divergent, convergent and transform, and gives examples of each.
Study of earthquake hazards or disaster
Earthquake Hazards
Definition of Hazard
Liquefaction
Ground Shaking
Ground Displacement
Flooding
Tsunami
Fire
Types of Hazard
Natural Hazards as Earthquakes
What Are Earthquake Hazards?
Ground Shaking:
Folds and faults ppt
The document provides information about folds and faults. It defines folds as bent or curved rock layers, and describes common fold types like anticlines and synclines. It also defines various fault types including normal faults, thrust faults, strike-slip faults, and oblique faults. Specific structures are described like the San Andreas Fault, which is a major strike-slip fault in California. Dip, strike, heave and throw are also defined in relation to describing the orientation and movement of geological structures.
Earthquake Scales - Mercalli scale vs Richter scale
The document compares the Mercalli Intensity Scale and Richter Magnitude Scale. The Mercalli Scale describes earthquake intensity based on observed effects, ranging from I (detected only by instruments) to XII (total destruction). The Richter Scale uses seismograph measurements to describe an earthquake's magnitude on a logarithmic scale. Both scales were developed in the early 20th century - the Mercalli by Mercalli and the Richter by Charles Richter to study California quakes. While the Mercalli Scale relies on observations, the Richter Scale provides a more scientific measure of an earthquake's energy release.
natural and geological hazards
This document discusses different types of natural hazards including geological hazards such as earthquakes, tsunamis, landslides, and volcanic eruptions. It provides details on the impact of specific past events in the Philippines and recommends preparedness, response, and rehabilitation strategies. These include evaluating building safety, developing evacuation plans, staying away from damaged areas, and obtaining disaster information from radio after an event occurs. The goal is to minimize harm and casualties from natural hazards through preparedness before, appropriate response during, and rehabilitation after such events.
How rocks behave under different types of stress
This document discusses how rocks behave under different types of stress. It explains that rocks undergo deformation and strain when subjected to tensional, compressional, or shear stresses. The document outlines the different stages of rock deformation, from elastic to ductile to fracture, and factors like temperature, confining pressure, and composition that influence the deformation process. It also describes geological structures like joints, faults, folds, anticlines and synclines that form from rock deformation.
Faults
This document discusses faults, beginning with definitions and terminology. Faults occur due to brittle deformation from differential stresses and cause displacement of rock blocks. There are two types of movement: translational and rotational. Faults are classified based on their geometry, such as dip, pattern, and apparent movement. They are also classified based on the forces causing them, such as tensional, compressional, or shear stresses. Faults form important structures as ore deposits can be associated with them.
Study of an earthquake
WHAT IS AN EARTHQUAKE?
Where Do Earthquakes Happen?
Why Do Earthquakes Happen?
How Are Earthquakes Studied?
How To Locate The Earthquake's Epicenter?
SCALES FOR EARTHQUAKE MEASUREMENT
What Are Earthquake Hazards?
DRRR - Earthquake Hazards
Contents:
1. Concept of Earthquake
2. Hazards Associated to Earthquake
- Ground Shaking
- Ground Rapture
- Tsunami
- Earthquake induced landslide
3. What do to BEFORE, DURING, AFTER Earthquake
THUNDERSTORMS
A document tackling about the basis of Thunderstorms:
-What is Thunderstorm?
-How do the Thunderstorms form?
-What is the difference between thunder and lightning?
Between a water spout and a tornado?
-What are the types of Lightning? of a Thunderstorm?
-What are some signs of an approaching thunderstorm?
-What are some precautionary measures to do before and during a thunderstorm?
-Case of Thunderstorms in the Philippines and on Planes
What's hot (20)
Earthquake Scales - Mercalli scale vs Richter scale
Earthquake Scales - Mercalli scale vs Richter scale
Viewers also liked
Focus and Epicenter:
Focus and Epicenter:
The focus of an earthquake is the point where the rocks start to fracture. It is the origin of the earthquake.
The epicenter is the point on land directly above the focus.
Epicentre and Focus
The document explains the difference between an epicentre and focus of an earthquake. The epicentre is the point on the surface directly above where the earthquake starts, while the focus is the location below ground where the earthquake occurs. It provides the example of the 1995 Kobe earthquake, where the epicentre was marked on a map as a star, and it had a shallow focus close to the surface, causing significant damage to the city.
Focus and epicenter
The focus of an earthquake is the point where the rocks start to fracture and is the origin of the earthquake. The epicenter is the point directly above the focus on the Earth's surface. Earthquake waves travel outward in all directions from the focus. Shallow earthquakes between 0-40 miles deep are more common and dangerous than deep earthquakes over 180 miles below the surface, as shallow quakes release more energy and plates moving together often cause them.
Port of Singapore Final !!
Singapore has established itself as a major global logistics hub due to its strategic location and world-class port infrastructure. It began as a British trading post in 1819 and now has a population over 5.5 million people. Singapore's port is the world's busiest in terms of cargo tonnage and containers handled annually. The port has over 50 container berths and over 190 quay cranes across its terminals. While Singapore faces challenges from rising costs and nearby competing ports, it continues to invest in expanding its port capacity and improving operations to maintain its status as a key international logistics center.
Port of Singapore
The Port of Singapore is a major global shipping hub located in Singapore. Some key facts:
- It is the world's second busiest port in terms of shipping tonnage and busiest port in terms of container transshipments.
- In 2012, it handled over 538 million tons of cargo including over 31 million shipping containers.
- It has expanded significantly over time with new terminals added and now provides services like bunkering, ship repair, and logistics.
Final Presentation
Amazon, Business Strategy - reference for First 3 slides - SlideShare
If you want to download the file, please send me an email.
Earthquakes
Earthquakes occur along plate boundaries due to the buildup and sudden release of energy from shifting tectonic plates. When plates lock, potential energy builds until released as seismic waves that propagate outward from the earthquake focus. Most earthquakes occur along oceanic and continental plate edges or along faults like normal, reverse, and transform boundaries. P and S waves are the primary seismic waves, with P waves traveling faster and S waves causing the shaking felt during quakes. Earthquake magnitude measures the energy released using the Richter scale, while intensity qualitatively describes the shaking effects on a place using the Mercalli scale.
Earthquake ppt
This presentation contains the brief introduction to earthquake,its effect,causes etc..
And case study of kuchha(bhuj),Gujarat Earthquake on 26th january,2001
Viewers also liked (8)
Recently uploaded
Poland vs Netherlands UEFA Euro 2024 Poland Battles Injuries Without Lewandow...
UEFA Euro 2024 fans worldwide can book Poland vs Netherlands Tickets from our online platform www.eticketing.co. Fans can book Euro Cup Germany Tickets on our website at discounted prices.
Croatia's UEFA Euro 2024 Puzzle of Experience versus Youth.docx
The Netherlands kicked off their Euro Cup 2024 campaign on Sunday against Poland but will have to navigate the tournament without two pivotal players Frenkie de Jong and Teun Koopmeiners
Luciano Spalletti Leads Italy's Transition at UEFA Euro 2024.docx
Italy are the defending European champs, but after Luciano Spalletti swapped Roberto Mancini last September, they are still taking the cautious first steps of a new era
一比一原版(Curtin毕业证)科廷大学毕业证如何办理
Curtin硕士学位证成绩单【微信95270640】科廷大学没毕业>办理科廷大学毕业证成绩单【微信Curtin】Curtin毕业证成绩单Curtin学历证书Curtin文凭《Curtin毕业套号文凭网认证科廷大学毕业证成绩单》《哪里买科廷大学毕业证文凭Curtin成绩学校快递邮寄信封》《开版科廷大学文凭》Curtin留信认证本科硕士学历认证
【实体公司】办科廷大学科廷大学毕业证offer学历认证学位证文凭认证办留信网认证办留服认证办教育部认证（网上可查实体公司专业可靠）
— — — 留学归国服务中心 — — -
【主营项目】
一.科廷大学毕业证成绩单使馆认证教育部认证成绩单等！
二.真实使馆公证(即留学回国人员证明,不成功不收费)
三.真实教育部学历学位认证（教育部存档！教育部留服网站永久可查）
四.办理各国各大学文凭(一对一专业服务,可全程监控跟踪进度)
国外毕业证学位证成绩单办理流程：
1客户提供科廷大学科廷大学毕业证offer办理信息：姓名生日专业学位毕业时间等（如信息不确定可以咨询顾问：我们有专业老师帮你查询）；
2开始安排制作毕业证成绩单电子图；
3毕业证成绩单电子版做好以后发送给您确认；
4毕业证成绩单电子版您确认信息无误之后安排制作成品；
5成品做好拍照或者视频给您确认；
6快递给客户（国内顺丰国外DHLUPS等快读邮寄）。
专业服务请勿犹豫联系我！本公司是留学创业和海归创业者们的桥梁。一次办理终生受用一步到位高效服务。详情请在线咨询办理,欢迎有诚意办理的客户咨询!洽谈。
招聘代理：本公司诚聘英国加拿大澳洲新西兰美国法国德国新加坡各地代理人员如果你有业余时间有兴趣就请联系我们咨询顾问：+微信:95270640着接听一个劲地提醒父亲别忘了正月说的话电话那头总会传来父亲嘿嘿的笑连连说记得记得但别忘了拿奖状进城啊考试一结束山娃就迫不及待地给父亲挂电话：爸我拿奖了三好学生接我进城吧父亲果然没有食言第二天就请假回家接山娃离开爷爷奶奶的那一刻山娃又伤心得泪如雨下宛如军人奔赴前线般难舍和悲壮卧空调大巴挤长蛇列车山娃发现车上挤满了叽叽喳喳的同龄人皆一脸惊喜地四处瞅山娃不认识他们也无暇去套近乎一味地跟着父亲昼夜兼程第无
Euro 2024 Predictions - Group Stage Outcomes
Here are our Euro 2024 predictions for the group stages
Will England make it through the group stages?, Will Germany use the home advantage to full effect?
Follow our progress, see how many we get right
If you want to join in let us know before the first game kick off and we can invite you to our private league
or join in with our friends at DeeperThanBlue
https://www.linkedin.com/posts/activity-7204868572995538944-qejG
https://www.selectdistinct.co.uk/2024/06/13/euro-2024-match-predictions/
#EURO2024 #Germany2024 #England #EURO2024predictions
Matka BOSS Result | Satta Matka Tips | Kalyan Matka 143
Satta BOSS Matka | DpBoss Matka | Matka BOSS Result | Satta Matka Tips | Kalyan Matka 143 · SATTA KING · ➥ SATTA MATKA TIME TEBAL · SATTA KING · ➥ Weekly ...
Olympic 2024 Key Players and Teams to Watch in Men's and Women's Football at ...
Olympic 2024 fans worldwide can book Olympic Football Tickets from our online platforms e-ticketing. co. Fans can book Olympic Tickets on our website at discounted prices. Experience the thrill of the Games in Paris and support your favorites athletes as they compete for glory.
Croatia vs Italy Modric's Last Dance Croatia's UEFA Euro 2024 Journey and Ita...
UEFA Euro 2024 fans worldwide can book Croatia vs Italy Tickets from our online platform www.eticketing.co. Fans can book Euro Cup Germany Tickets on our website at discounted prices.
Italy FIFA World Cup Italy's Ambition for FIFA 2026.docx
Football World Cup enthusiasts worldwide can secure their FIFA World Cup 2026 Tickets through our online platform, eticketing.co. With a user-friendly interface and exclusive deals, fans can effortlessly book FIFA World Cup Tickets for thrilling matches, all at discounted prices.
Euro 2024 Key Tactics and Strategies of the Netherlands.docx
We offer Euro Cup Tickets to admirers who can get Netherlands vs Austria Tickets through our trusted online ticketing marketplace. Eticketing.co is the most reliable source for booking Euro Cup Final Tickets. Sign up for the latest Euro Cup Germany Ticket alert.
Euro 2024 Belgium's Rebirth the New Generation Match the Golden Era.docx
The Golden Group is over. Can a new group step up? Two years ago, Kevin De Bruyne plunged Belgium’s Euro 2024 plans into disorder when he claimed the team was “too old” to win in an interview with The Protector. That Belgian squad had 10 players over 30 and the maximum average age of any Euro Cup 2024 team at the competition. A group-stage exit and just one goal at the World Cup put Belgium on course for a restructure.
We offer Euro Cup Tickets to admirers who can get Belgium vs Romania Tickets through our trusted online ticketing marketplace. Eticketing.co is the most reliable source for booking Euro Cup Final Tickets. Sign up for the latest Euro Cup Germany Ticket alert.
Belgium vs Romania Tickets | Euro Cup Tickets | Euro Cup Final Tickets
Coach Domenico Tedesco has managed a tactical shakeup and a regular exit for some of the oldest players. Experienced bests remain, not least the 37-year-old Jan Vertonghen in defense, the 32-year-old De Bruyne himself in midfield, and 31-year-old Romelu Lukaku up visible.
Still, younger actors like De Bruyne’s Manchester City partner Jeremy Doku bring fresh vitality to the team. Euro Cup Germany Qualifying unbeaten with just four goals allowed from eight games was a welcome sign of accomplishment back on track under Tedesco.
The only other squad in Group E besides Belgium to UEFA Euro 2024 qualify unbeaten, Romania was awestruck by winning a group that also checked Switzerland and Israel. Still, Euro 2024 will test a squad sorely lacking in top-level skill.
Euro 2024: Belgium's Transition from Golden Generation to New Hope
Tottenham guardian Vlad Dragusin is the only Euro Cup 2024 squad member singing regularly for one of Europe’s top clubs this flavor. He even played only nine Premier League games since adoption in January. Goalkeeper Horatiu Moldovan is a stoppage at Atletico Madrid.
There’s a link to the beauty days of Romanian soccer with midfielder Ianis Hagi, son of Gheorghe Hagi, who assisted the team to the rounds of the 1994 World Cup and Euro 2000.
We are only a combine of days away from the UEFA Euro 2024 curtain raiser. The 24 squads are winding up their provisions and getting ready to give it their all to life the wanted Euro Cup Final trophy on July 14. Spread across six clusters, the first hurdle in the knockout phase will be the plump of 16.
Euro fans worldwide can book Euro 2024 Tickets from our online platform, www.eticketing.co. Fans can book Euro Cup 2024 Tickets on our website at discounted prices.
Germany and Scotland will take things off before we get into overdrive in two weeks. Meanwhile, Belgium will be longing to bounce back after a horrendous 2022 FIFA World Cup movement, which ended in the group stage.
Belgium vs Romania Tickets | Euro Cup 2024 Tickets | Euro Cup Tickets | Euro Cup Final Tickets
Roberto Martinez completed the way for Domenico Tedesco, who has overseen a compact start to his tenure. The 38-year-old will be assured heading into the group stage
快速制作加拿大西蒙菲莎大学毕业证（sfu毕业证书）硕士学位证书原版一模一样
原版一模一样【微信：741003700 】【加拿大西蒙菲莎大学毕业证（sfu毕业证书）硕士学位证书】【微信：741003700 】学位证，留信认证（真实可查，永久存档）offer、雅思、外壳等材料/诚信可靠,可直接看成品样本，帮您解决无法毕业带来的各种难题！外壳，原版制作，诚信可靠，可直接看成品样本。行业标杆！精益求精，诚心合作，真诚制作！多年品质 ,按需精细制作，24小时接单,全套进口原装设备。十五年致力于帮助留学生解决难题，包您满意。
本公司拥有海外各大学样板无数，能完美还原海外各大学 Bachelor Diploma degree, Master Degree Diploma
1:1完美还原海外各大学毕业材料上的工艺：水印，阴影底纹，钢印LOGO烫金烫银，LOGO烫金烫银复合重叠。文字图案浮雕、激光镭射、紫外荧光、温感、复印防伪等防伪工艺。材料咨询办理、认证咨询办理请加学历顾问Q/微741003700
留信网认证的作用:
1:该专业认证可证明留学生真实身份
2:同时对留学生所学专业登记给予评定
3:国家专业人才认证中心颁发入库证书
4:这个认证书并且可以归档倒地方
5:凡事获得留信网入网的信息将会逐步更新到个人身份内，将在公安局网内查询个人身份证信息后，同步读取人才网入库信息
6:个人职称评审加20分
7:个人信誉贷款加10分
8:在国家人才网主办的国家网络招聘大会中纳入资料，供国家高端企业选择人才
The most promising young Players to watch during Euro 2024.docx
Football writer Daniel Story highlights each nation's potential breakout star at this summer's UEFA Euro 2024 tournament
一比一原版(Columbia毕业证)哥伦比亚大学毕业证如何办理
Columbia毕业证假文凭【微信95270640】办文凭{哥伦比亚大学毕业证}Q微Q微信95270640Columbia毕业证书成绩单/学历认证Columbia Diploma未毕业、挂科怎么办？+QQ微信：Q微信95270640-大学Offer（申请大学）、成绩单（申请考研）、语言证书、在读证明、使馆公证、办真实留信网认证、真实大使馆认证、学历认证
(诚招代理)办理国外高校毕业证成绩单文凭学位证,真实使馆公证（留学回国人员证明）真实留信网认证国外学历学位认证雅思代考国外学校代申请名校保录开请假条改GPA改成绩ID卡
1.高仿业务:【本科硕士】毕业证,成绩单（GPA修改）,学历认证（教育部认证）,大学Offer,,ID,留信认证,使馆认证,雅思,语言证书等高仿类证书；
2.认证服务: 学历认证（教育部认证）,大使馆认证（回国人员证明）,留信认证（可查有编号证书）,大学保录取,雅思保分成绩单。
3.技术服务：钢印水印烫金激光防伪凹凸版设计印刷激凸温感光标底纹镭射速度快。
办理哥伦比亚大学哥伦比亚大学硕士学位证成绩单流程：
1客户提供办理信息：姓名生日专业学位毕业时间等（如信息不确定可以咨询顾问：我们有专业老师帮你查询）；
2开始安排制作毕业证成绩单电子图；
3毕业证成绩单电子版做好以后发送给您确认；
4毕业证成绩单电子版您确认信息无误之后安排制作成品；
5成品做好拍照或者视频给您确认；
6快递给客户（国内顺丰国外DHLUPS等快读邮寄）
-办理真实使馆公证（即留学回国人员证明）
-办理各国各大学文凭（世界名校一对一专业服务,可全程监控跟踪进度）
-全套服务：毕业证成绩单真实使馆公证真实教育部认证。让您回国发展信心十足！
（详情请加一下 文凭顾问+微信:95270640）欢迎咨询！将要跨出门槛的一刹那山娃突然抱紧父亲的大腿嚎啕大哭父亲吃力地掰开山娃的手哽咽道山娃好好听话好好念书到了暑假爸也接你进城爸的城好远好大好美山娃于是天天扳着手指算计着读书也格外刻苦无奈时间总过得太慢太慢每次父亲往家打电话山娃总抢着接听一个劲地提醒父亲别忘了正月说的话电话那头总会传来父亲嘿嘿的笑连连说记得记得但别忘了拿奖状进城啊考试一结束山娃就迫不及待地给父亲挂电话：爸我拿奖了三好学生接我进城吧父亲果不
Georgia vs Portugal Euro Cup 2024 Clash Unites a Nation Amid Turmoil.pdf
Euro 2024 fans worldwide can book Georgia vs Portugal Tickets from our online platform www.eticketing.co. Fans can book Euro Cup Germany Tickets on our website at discounted prices.
Belgium vs Romania Ultimate Guide to Euro Cup 2024 Tactics, Ticketing, and Qu...
Euro Cup 2024 fans worldwide can book Belgium vs Romania Tickets from our online platform www.eticketing.co. Fans can book Euro Cup Germany Tickets on our website at discounted prices.
Euro Cup Group E Preview, Team Strategies, Key Players, and Tactical Insights...
We offer Euro Cup Tickets to admirers who can get Belgium vs Romania Tickets through our trusted online ticketing marketplace. Eticketing.co is the most reliable source for booking Euro Cup Final Tickets. Sign up for the latest Euro Cup Germany Ticket alert.
Recently uploaded (20)
Poland vs Netherlands UEFA Euro 2024 Poland Battles Injuries Without Lewandow...
Poland vs Netherlands UEFA Euro 2024 Poland Battles Injuries Without Lewandow...
Croatia's UEFA Euro 2024 Puzzle of Experience versus Youth.docx
Croatia's UEFA Euro 2024 Puzzle of Experience versus Youth.docx
Luciano Spalletti Leads Italy's Transition at UEFA Euro 2024.docx
Luciano Spalletti Leads Italy's Transition at UEFA Euro 2024.docx
Matka BOSS Result | Satta Matka Tips | Kalyan Matka 143
Matka BOSS Result | Satta Matka Tips | Kalyan Matka 143
Olympic 2024 Key Players and Teams to Watch in Men's and Women's Football at ...
Olympic 2024 Key Players and Teams to Watch in Men's and Women's Football at ...
Croatia vs Italy Modric's Last Dance Croatia's UEFA Euro 2024 Journey and Ita...
Croatia vs Italy Modric's Last Dance Croatia's UEFA Euro 2024 Journey and Ita...
Italy FIFA World Cup Italy's Ambition for FIFA 2026.docx
Italy FIFA World Cup Italy's Ambition for FIFA 2026.docx
Euro 2024 Key Tactics and Strategies of the Netherlands.docx
Euro 2024 Key Tactics and Strategies of the Netherlands.docx
Euro 2024 Belgium's Rebirth the New Generation Match the Golden Era.docx
Euro 2024 Belgium's Rebirth the New Generation Match the Golden Era.docx
The most promising young Players to watch during Euro 2024.docx
The most promising young Players to watch during Euro 2024.docx
Georgia vs Portugal Euro Cup 2024 Clash Unites a Nation Amid Turmoil.pdf
Georgia vs Portugal Euro Cup 2024 Clash Unites a Nation Amid Turmoil.pdf
Belgium vs Romania Ultimate Guide to Euro Cup 2024 Tactics, Ticketing, and Qu...
Belgium vs Romania Ultimate Guide to Euro Cup 2024 Tactics, Ticketing, and Qu...
Euro Cup Group E Preview, Team Strategies, Key Players, and Tactical Insights...
Euro Cup Group E Preview, Team Strategies, Key Players, and Tactical Insights...