An earthquake is caused by the sudden release of energy along fault lines, generating seismic waves. Major earthquakes can trigger hazardous events like tsunamis, which are massive sea waves that cause extensive damage and loss of life when they reach coastal areas. Living in earthquake and tsunami prone zones presents many risks such as property destruction, disruption of basic services, fires, landslides, and loss of lives.
This document discusses liquefaction, a phenomenon where soil loses strength and behaves like liquid during earthquakes. It defines liquefaction as when a mass of soil loses shear resistance and flows like a liquid under loading. The document explores causes of liquefaction like high pore water pressure reducing effective stress. It describes common effects like sand boils, lateral spreads, loss of bearing capacity. The document then outlines various liquefaction mitigation techniques including soil improvement methods like dewatering, stone columns, densification. It notes the selection of mitigation method depends on site conditions and structure. Deep foundations can also help liquefy resistant structures.
This document discusses liquefaction of soil during earthquakes and its effects based on case studies. It covers:
1) Examples of liquefaction and its effects observed during earthquakes in Chile 1960, Japan 1964, Alaska 1964, and Caracas 1967 including settlements, tilting of structures, and damage depending on soil thickness.
2) Factors influencing liquefaction potential such as soil type, density, water content, and depth to water table based on a case study of the 1964 Niigata earthquake in Japan.
3) Options for mitigating liquefaction including soil densification, stabilization, drainage, and structural measures like reinforcement and foundation modification.
This document provides information about natural hazards caused by tectonic plate movements. It discusses the three main types of plate boundaries: divergent where plates move apart, convergent where they move together, and transform where they move past each other. At divergent boundaries, mid-ocean ridges and volcanic islands form through sea floor spreading. Rift valleys and block mountains form when continents split apart. At convergent boundaries, denser plates subduct under lighter ones, creating ocean trenches, volcanic island arcs, and fold mountains through compression. Transform boundaries cause earthquakes along tear faults as plates grind past each other.
This document discusses earthquakes, including their definition, causes, effects, and precautions. Some key points:
- An earthquake is caused by vibrations beneath the earth's surface due to shifting tectonic plates or other disturbances. They can be measured using seismographs.
- The Richter scale measures an earthquake's magnitude - larger quakes over 8.0 occur about once per year globally.
- Earthquakes generate seismic waves that travel through the earth, including P-waves, S-waves, and L-waves.
- Major effects of earthquakes include damage to buildings and infrastructure, tsunamis, landslides, and cracks in the ground.
- Precautions
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.
earth is being cover with the blanket of gases called atmosphere which is further divided into 4 layers troposphere, stratosphere, mesosphere and thermospere
each layer is made up of some chemical constituents which could be water molecule traces of gases etc, Japan has done research and send a satellite in space to observe it as describe in this presentation
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.
This technical seminar presentation summarizes soil liquefaction. It defines liquefaction as when a saturated or partially saturated soil loses strength and stiffness during earthquakes or sudden stress changes, behaving like a liquid. The document outlines the process of liquefaction, criteria for evaluating liquefaction-susceptible soils, effects of liquefaction like loss of foundation support, and methods to mitigate liquefaction hazards such as improving drainage or increasing soil density. It concludes that liquefaction can cause devastating damage but methods exist to reduce its impacts.
This document discusses liquefaction, a phenomenon where soil loses strength and behaves like liquid during earthquakes. It defines liquefaction as when a mass of soil loses shear resistance and flows like a liquid under loading. The document explores causes of liquefaction like high pore water pressure reducing effective stress. It describes common effects like sand boils, lateral spreads, loss of bearing capacity. The document then outlines various liquefaction mitigation techniques including soil improvement methods like dewatering, stone columns, densification. It notes the selection of mitigation method depends on site conditions and structure. Deep foundations can also help liquefy resistant structures.
This document discusses liquefaction of soil during earthquakes and its effects based on case studies. It covers:
1) Examples of liquefaction and its effects observed during earthquakes in Chile 1960, Japan 1964, Alaska 1964, and Caracas 1967 including settlements, tilting of structures, and damage depending on soil thickness.
2) Factors influencing liquefaction potential such as soil type, density, water content, and depth to water table based on a case study of the 1964 Niigata earthquake in Japan.
3) Options for mitigating liquefaction including soil densification, stabilization, drainage, and structural measures like reinforcement and foundation modification.
This document provides information about natural hazards caused by tectonic plate movements. It discusses the three main types of plate boundaries: divergent where plates move apart, convergent where they move together, and transform where they move past each other. At divergent boundaries, mid-ocean ridges and volcanic islands form through sea floor spreading. Rift valleys and block mountains form when continents split apart. At convergent boundaries, denser plates subduct under lighter ones, creating ocean trenches, volcanic island arcs, and fold mountains through compression. Transform boundaries cause earthquakes along tear faults as plates grind past each other.
This document discusses earthquakes, including their definition, causes, effects, and precautions. Some key points:
- An earthquake is caused by vibrations beneath the earth's surface due to shifting tectonic plates or other disturbances. They can be measured using seismographs.
- The Richter scale measures an earthquake's magnitude - larger quakes over 8.0 occur about once per year globally.
- Earthquakes generate seismic waves that travel through the earth, including P-waves, S-waves, and L-waves.
- Major effects of earthquakes include damage to buildings and infrastructure, tsunamis, landslides, and cracks in the ground.
- Precautions
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.
earth is being cover with the blanket of gases called atmosphere which is further divided into 4 layers troposphere, stratosphere, mesosphere and thermospere
each layer is made up of some chemical constituents which could be water molecule traces of gases etc, Japan has done research and send a satellite in space to observe it as describe in this presentation
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.
This technical seminar presentation summarizes soil liquefaction. It defines liquefaction as when a saturated or partially saturated soil loses strength and stiffness during earthquakes or sudden stress changes, behaving like a liquid. The document outlines the process of liquefaction, criteria for evaluating liquefaction-susceptible soils, effects of liquefaction like loss of foundation support, and methods to mitigate liquefaction hazards such as improving drainage or increasing soil density. It concludes that liquefaction can cause devastating damage but methods exist to reduce its impacts.
soil liquefaction and quicksand conditionazlan ahmad
Soil liquefaction occurs when water-saturated soils lose strength during earthquakes or other vibrations, causing the soil particles to separate and behave like a liquid. This happens because earthquake shaking increases water pressure between soil particles. Buildings and structures can sink or collapse into liquefied soils. Techniques to prevent liquefaction include compacting soils or setting deep foundations below unstable layers. Quick sand conditions occur when upward seepage flow reduces effective stress in loose soils like sand, causing a floating effect with little weight-bearing capacity.
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.
Geotechnical Engineering-II [Lec #19: General Bearing Capacity Equation]Muhammad Irfan
Class notes of Geotechnical Engineering course I used to teach at UET Lahore. Feel free to download the slide show.
Anyone looking to modify these files and use them for their own teaching purposes can contact me directly to get hold of editable version.
Volcanic eruptions have both primary and secondary impacts. The primary impacts are the immediate destruction caused by lava flows, pyroclastic flows, ash falls, and gases. Secondary impacts occur later and include mudflows that cause additional destruction, fires started by the primary impacts, and shortages of food, water and other resources as crops are damaged and infrastructure is impacted.
The key factors that influence how hazardous an earthquake can be are:
1. The magnitude of the earthquake, with larger earthquakes causing more damage.
2. The distance from the earthquake's epicenter, with those closer experiencing greater shaking.
3. The population density of the affected area, increasing risks to human life and infrastructure in more populated locations.
4. The level of preparedness, as damage is reduced when populations have taken measures to prepare for earthquakes.
This document provides information on bearing capacity of soil and foundations. It defines key foundation terms like contact pressure, foundation depth, shallow and deep foundations. It describes different types of shallow foundations like spread footing, continuous footing, combined footing, strap footing, and mat or raft footing. Factors for selecting a foundation type and comparing shallow vs deep foundations are also discussed. Design criteria of safety against bearing capacity failure and limiting settlement are covered.
1. The document discusses key concepts about Earth's atmosphere including how solar radiation drives global climate and local weather patterns.
2. It explains different climate types based on factors like latitude, proximity to bodies of water, and elevation. Humid climates receive more precipitation than potential evapotranspiration while arid climates experience the opposite.
3. Atmospheric circulation patterns like global wind belts and ocean currents play an important role in moderating Earth's climate by transporting heat energy from the tropics to poles and distributing it around the globe over long time periods.
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.
This document discusses the theories of continental drift, folding, faulting, and seafloor spreading. It describes Alfred Wegener's theory of continental drift, including the idea of a supercontinent called Pangaea. It also discusses how Harry Hess theorized that seafloor is younger than continents. Finally, it explains that seafloor spreading occurs as new crust is formed at mid-ocean ridges and pushes the plates apart over time.
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.
Detailed content on shear strength of soils, principles of effective stresses, tests conducted to determine the shear strength of soils and its applications, dilatancy, thixotropy and sensitivity.
This document provides an overview of the Year 12 HSC Geography unit on ecosystems at risk. It defines key terms like ecology, ecosystems, biotic and abiotic factors. It explains how ecosystems vary naturally or through human intervention. It also describes ecosystem productivity, energy flows through food chains and nutrient cycling. Nutrient cycling involves elements like carbon, oxygen, water, phosphorus and nitrogen passing between living and non-living aspects of the environment. The document also notes how bioaccumulation can occur as toxic substances collect in animal tissues at higher rates than they are lost.
The document discusses global wind patterns that develop due to temperature differences between the equator and poles. Warm air rises at the equator, creating low pressure, while cold air sinks at the poles, creating high pressure. Air moves from high to low pressure areas, resulting in global wind currents called the prevailing westerlies, easterly trade winds, and polar easterlies in both hemispheres. The Coriolis effect causes these winds to curve right in the northern hemisphere and left in the southern hemisphere as they travel.
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.
ORIGIN OF EARTH AND IT’S PLACE IN UNIVERSEShahid Hussain
The document discusses the origin and evolution of the universe, Earth, and life. It describes evidence that supports the Big Bang theory of the origin of the universe approximately 13.8 billion years ago. It explains that galaxies, stars, and planets formed over time through evolutionary processes. The document also discusses different views on the origin and age of the universe, from both religious and scientific perspectives, including the idea of theistic evolution. It provides examples of the immense distances in the universe and compares the age of the Earth and the development of life to timescales in a hypothetical "cosmic calendar" representing the universe's age in one year.
This document discusses various concepts related to atmospheric humidity and cloud formation. It defines specific humidity, relative humidity, dew point, and how temperature affects the air's capacity to hold moisture. It explains the different types of atmospheric stability and instability, including stable, conditionally unstable, and absolutely unstable air. The document also covers cloud development processes like convection, collision and coalescence, ice crystal growth, and precipitation formation. Finally, it describes the characteristics and formation of different cloud types like cirrus, cumulus, stratus and nimbostratus clouds.
The document defines and provides examples of different types of geological folds including anticlines, synclines, monoclines, recumbent folds, overturned folds, plunging folds, ptygmatic folds, chevron folds, and drag folds. Examples show the folded rock strata, describing the plate tectonics settings and rock types involved. Different terminology is introduced for upwardly arched anticlines versus downwardly arched synclines and other specialized fold patterns.
The document provides information about the composition and structure of the atmosphere. It discusses that the atmosphere is composed of gases, water vapor, and dust particles. It also describes the different layers of the atmosphere including the troposphere, stratosphere, mesosphere, and ionosphere. Additionally, it covers various elements that determine weather and climate such as temperature, pressure, winds, humidity, and clouds/precipitation.
This document discusses deep foundation piles. It defines deep foundations as those where the depth is much larger than the width and are not constructed through ordinary open pit excavation. It then discusses different types of piles based on function and material, including bearing piles, friction piles, sheet piles, and timber, concrete, composite and steel piles. It provides details on pile construction procedures, including borehole drilling, reinforcement installation, concrete pouring using a tremie pipe, and casting the pile cap. It concludes by discussing potential causes of pile failure.
The document provides an overview of urban sprawl and the compact city model. It discusses how urban sprawl developed in the 20th century due to factors like increased car ownership and declining public transport. This caused the decentralization and low-density expansion of cities. Urban sprawl has negative environmental, social, and economic impacts. The compact city model is presented as a strategy to contain urban sprawl and create more sustainable cities by increasing density. The document then analyzes the case of Gothenburg, Sweden to understand how it applies compact city strategies and policies to achieve densification.
soil liquefaction and quicksand conditionazlan ahmad
Soil liquefaction occurs when water-saturated soils lose strength during earthquakes or other vibrations, causing the soil particles to separate and behave like a liquid. This happens because earthquake shaking increases water pressure between soil particles. Buildings and structures can sink or collapse into liquefied soils. Techniques to prevent liquefaction include compacting soils or setting deep foundations below unstable layers. Quick sand conditions occur when upward seepage flow reduces effective stress in loose soils like sand, causing a floating effect with little weight-bearing capacity.
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.
Geotechnical Engineering-II [Lec #19: General Bearing Capacity Equation]Muhammad Irfan
Class notes of Geotechnical Engineering course I used to teach at UET Lahore. Feel free to download the slide show.
Anyone looking to modify these files and use them for their own teaching purposes can contact me directly to get hold of editable version.
Volcanic eruptions have both primary and secondary impacts. The primary impacts are the immediate destruction caused by lava flows, pyroclastic flows, ash falls, and gases. Secondary impacts occur later and include mudflows that cause additional destruction, fires started by the primary impacts, and shortages of food, water and other resources as crops are damaged and infrastructure is impacted.
The key factors that influence how hazardous an earthquake can be are:
1. The magnitude of the earthquake, with larger earthquakes causing more damage.
2. The distance from the earthquake's epicenter, with those closer experiencing greater shaking.
3. The population density of the affected area, increasing risks to human life and infrastructure in more populated locations.
4. The level of preparedness, as damage is reduced when populations have taken measures to prepare for earthquakes.
This document provides information on bearing capacity of soil and foundations. It defines key foundation terms like contact pressure, foundation depth, shallow and deep foundations. It describes different types of shallow foundations like spread footing, continuous footing, combined footing, strap footing, and mat or raft footing. Factors for selecting a foundation type and comparing shallow vs deep foundations are also discussed. Design criteria of safety against bearing capacity failure and limiting settlement are covered.
1. The document discusses key concepts about Earth's atmosphere including how solar radiation drives global climate and local weather patterns.
2. It explains different climate types based on factors like latitude, proximity to bodies of water, and elevation. Humid climates receive more precipitation than potential evapotranspiration while arid climates experience the opposite.
3. Atmospheric circulation patterns like global wind belts and ocean currents play an important role in moderating Earth's climate by transporting heat energy from the tropics to poles and distributing it around the globe over long time periods.
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.
This document discusses the theories of continental drift, folding, faulting, and seafloor spreading. It describes Alfred Wegener's theory of continental drift, including the idea of a supercontinent called Pangaea. It also discusses how Harry Hess theorized that seafloor is younger than continents. Finally, it explains that seafloor spreading occurs as new crust is formed at mid-ocean ridges and pushes the plates apart over time.
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.
Detailed content on shear strength of soils, principles of effective stresses, tests conducted to determine the shear strength of soils and its applications, dilatancy, thixotropy and sensitivity.
This document provides an overview of the Year 12 HSC Geography unit on ecosystems at risk. It defines key terms like ecology, ecosystems, biotic and abiotic factors. It explains how ecosystems vary naturally or through human intervention. It also describes ecosystem productivity, energy flows through food chains and nutrient cycling. Nutrient cycling involves elements like carbon, oxygen, water, phosphorus and nitrogen passing between living and non-living aspects of the environment. The document also notes how bioaccumulation can occur as toxic substances collect in animal tissues at higher rates than they are lost.
The document discusses global wind patterns that develop due to temperature differences between the equator and poles. Warm air rises at the equator, creating low pressure, while cold air sinks at the poles, creating high pressure. Air moves from high to low pressure areas, resulting in global wind currents called the prevailing westerlies, easterly trade winds, and polar easterlies in both hemispheres. The Coriolis effect causes these winds to curve right in the northern hemisphere and left in the southern hemisphere as they travel.
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.
ORIGIN OF EARTH AND IT’S PLACE IN UNIVERSEShahid Hussain
The document discusses the origin and evolution of the universe, Earth, and life. It describes evidence that supports the Big Bang theory of the origin of the universe approximately 13.8 billion years ago. It explains that galaxies, stars, and planets formed over time through evolutionary processes. The document also discusses different views on the origin and age of the universe, from both religious and scientific perspectives, including the idea of theistic evolution. It provides examples of the immense distances in the universe and compares the age of the Earth and the development of life to timescales in a hypothetical "cosmic calendar" representing the universe's age in one year.
This document discusses various concepts related to atmospheric humidity and cloud formation. It defines specific humidity, relative humidity, dew point, and how temperature affects the air's capacity to hold moisture. It explains the different types of atmospheric stability and instability, including stable, conditionally unstable, and absolutely unstable air. The document also covers cloud development processes like convection, collision and coalescence, ice crystal growth, and precipitation formation. Finally, it describes the characteristics and formation of different cloud types like cirrus, cumulus, stratus and nimbostratus clouds.
The document defines and provides examples of different types of geological folds including anticlines, synclines, monoclines, recumbent folds, overturned folds, plunging folds, ptygmatic folds, chevron folds, and drag folds. Examples show the folded rock strata, describing the plate tectonics settings and rock types involved. Different terminology is introduced for upwardly arched anticlines versus downwardly arched synclines and other specialized fold patterns.
The document provides information about the composition and structure of the atmosphere. It discusses that the atmosphere is composed of gases, water vapor, and dust particles. It also describes the different layers of the atmosphere including the troposphere, stratosphere, mesosphere, and ionosphere. Additionally, it covers various elements that determine weather and climate such as temperature, pressure, winds, humidity, and clouds/precipitation.
This document discusses deep foundation piles. It defines deep foundations as those where the depth is much larger than the width and are not constructed through ordinary open pit excavation. It then discusses different types of piles based on function and material, including bearing piles, friction piles, sheet piles, and timber, concrete, composite and steel piles. It provides details on pile construction procedures, including borehole drilling, reinforcement installation, concrete pouring using a tremie pipe, and casting the pile cap. It concludes by discussing potential causes of pile failure.
The document provides an overview of urban sprawl and the compact city model. It discusses how urban sprawl developed in the 20th century due to factors like increased car ownership and declining public transport. This caused the decentralization and low-density expansion of cities. Urban sprawl has negative environmental, social, and economic impacts. The compact city model is presented as a strategy to contain urban sprawl and create more sustainable cities by increasing density. The document then analyzes the case of Gothenburg, Sweden to understand how it applies compact city strategies and policies to achieve densification.
Here are the statements coloured as instructed:
Red: Volcanoes and earthquakes are most likely to occur in areas where the plates collide.
Green: These plates move at about the same rate as our fingernails grow!
The red statement with a fact about earthquakes and volcanoes is: "Volcanoes and earthquakes are most likely to occur in areas where the plates collide."
The green statement is: "These plates move at about the same rate as our fingernails grow!"
1. Geotechnical earthquake engineering is concerned with assessing how soil properties influence earthquake shaking and effects like liquefaction. Key soil properties include grain size, density, and water content.
2. Evaluating liquefaction risk involves determining the soil's standard penetration test value, grain size, water content, and comparing the expected earthquake shear stresses to the soil's shear resistance.
3. Methods to prevent liquefaction include deep foundations, compacting or replacing liquefiable soils, installing drains or stone columns, dewatering, and applying surcharges.
This document discusses densities and compactness in developing country cities. It finds that densities are much higher than in developed countries, facilitated by smaller dwelling sizes, mixed land uses, and higher densities near city centers. While central city densities are higher, overall city areas are larger in developing countries. Higher densities support more diverse transit options but congestion is also higher. Compactness provides some environmental and infrastructure benefits but does not necessarily correlate with better environmental quality. Lessons are that developing country transportation cannot be directly replicated and compactness results less from planning than from economic factors.
The document discusses rebuilding Kamaishi City after the 2011 earthquake and tsunami in the context of Japan's shrinking and aging population. It describes how the disaster devastated East Kamaishi and left main issues of depopulation and elderly needs. The thesis aims to propose a successful socio-economic recovery for East Kamaishi through a compact urban development formed by small independent communities, using a place-based participatory planning process led by a community-based organization similar to machizukuri groups in Kobe. This approach combines the benefits of planning models like "Urban Islands" and "Smart Shrinking" analyzed in the document.
The Historical City as the Sustainable Compact City Model_2001Joaquim Flores
2001 – “The Historical City as the Sustainable Compact City Model” – Comunicação apresentada no 6º Simpósio Internacional da Organização das Cidades Património Mundial “Risk Preparedness and Emergency Response in the context of the management of the World Heritage Cities” – Puebla (México), 3 a 7 de Outubro.
This document discusses some of the negative impacts of urban sprawl such as increased cost of living, resource consumption, water pollution from agriculture and waste, and air pollution from reliance on automobiles and industry. It notes that pollution can come from point sources like factories or non-point sources like runoff. Urban sprawl is also linked to health issues like respiratory illnesses that disproportionately impact the elderly and young. Some proposed solutions include promoting smart growth to reduce car dependency, creating sustainable cities that allow walking and transit, and educating communities to encourage sustainable development.
RV 2015: Sinking in a Sea of Green? Anti-Government Crusaders Get Their Way b...Rail~Volution
While other cities sprawled, expanding suburbs and highways, Metro Vancouver, BC, invested in transit, complete communities and compact development to create "Cities in a Sea of Green." After two decades of progress, voters rejected a referendum to expand the region's transit system. How was a community convinced to vote against a funding measure that supported the sustainable ethos they'd embraced for so long? Was it really the successful work of anti-government crusaders? Join in a discussion of the Vancouver experience and see what lessons you can take home.
Moderator: Ron Stewart, AIA, Principal, ZGF Architects, LLP, Portland, Oregon
Gordon Price, Program Director, The City Program, Simon Fraser University at Harbour Centre, Vancouver, British Columbia
liquefaction, its causes,mechanism and liquefaction potential mappings. Liquefaction analysis and measure of mitigation . along with susceptibility map of Kathmandu valley, Nepal and conclusion.
Urban sprawl is characterized by low-density, auto-dependent development outside of urban centers that consumes excessive land. It lacks diversity in transportation and housing options and results in fragmented open spaces between scattered development. Sprawl is driven by consumer preferences for large homes and yards, business preferences for highway access, and land use and tax policies that promote low-density development. The impacts of sprawl include increased auto dependency, pollution, and commuting times as well as isolation of populations. It also results in higher public costs, economic disinvestment in urban centers, and environmental impacts like loss of habitat and farmland.
Urban sprawl occurs when cities expand outward into rural areas, consuming land. This document summarizes some key causes and impacts of urban sprawl in the United States. Population growth is a major driver, as people seek more affordable housing and space in the suburbs. However, urban sprawl leads to increased pollution, traffic, and loss of agricultural land. It also strains infrastructure and finances as governments must expand services further out. The document recommends controlling population growth and changing attitudes about development to limit unsustainable urban sprawl.
Contribution of compact city to urban sustainabilityNaina Gupta
This document discusses the relevance of compact cities in today's context. Compact cities are characterized by dense and proximate development patterns, urban areas linked by public transportation systems, and accessibility to local services and jobs. Compact city development can contribute to urban sustainability through environmental, social, and economic benefits such as reduced CO2 emissions from less automobile dependency, greater accessibility, and higher productivity due to shorter travel times. The document outlines indicators for measuring the compactness and impact of compact city policies and discusses how compact cities can help address challenges of continuing urbanization, global warming, rising energy prices, changing demographics, and local government finances.
This document discusses compact cities and urban sprawl. It defines a compact city as having high residential density, mixed land uses, and an efficient transportation system to reduce energy consumption and pollution. Benefits include lower costs, less resource use, and more social interaction. Examples given are Melbourne, Toyama, Vancouver, and Curitiba. Urban sprawl is defined as uncontrolled urban growth into rural areas, characterized by low densities and car dependency, which increases infrastructure costs. The document suggests limiting sprawl to better manage expenses and control population growth.
Tsunamis occur due to undersea earthquakes, volcanic eruptions, or landslides. As the wave enters shallow coastal waters, it slows down and grows dramatically in height. When the tsunami reaches land, it can cause devastating flooding and destruction from its immense power. The 2004 Indian Ocean tsunami showed that while earthquakes cannot be predicted, tsunamis can be detected with sensors and their impact assessed using computer modeling - however most nations around the Indian Ocean lacked a proper warning system, costing many lives.
Why Were So Many People Killed In The In The Haiti Earthquake Of 2010Mr Cornish
Many people were killed in the 2010 Haiti earthquake due to a combination of geographical, political, economic, and infrastructure factors that exacerbated the effects of the natural disaster. Located near a fault line that had not seen a major quake in over 200 years, the 7.3 magnitude earthquake struck close to the densely populated capital of Port-au-Prince. Years of poverty, political instability, and lack of enforcement of building codes led to unsafe housing in crowded slums. When the earthquake hit, thousands of poorly constructed homes collapsed, and the country lacked emergency response capabilities due to underinvestment in infrastructure and relief systems. These human factors amplified the death and destruction from what would otherwise have been a damaging but less deadly seismic
This document discusses liquefaction of soil. It begins by defining liquefaction as the loss of strength in saturated, cohesionless soils due to increased pore water pressure during dynamic loading. This causes the soil particles to lose contact with one another and behave like a liquid. The document then discusses two types of liquefaction - flow liquefaction, which occurs when static shear stresses exceed residual strength, and cyclic mobility, which occurs due to lower static stresses and develops incrementally. Several effects of liquefaction are also described, such as loss of bearing strength, lateral spreading, sand boils, flow failures, and ground oscillations. Finally, methods to reduce liquefaction risk are presented, including avoiding susceptible soils, using deep foundations, soil improvement techniques
This document provides an overview of the concept of a compact city presented by a group of students. It begins with listing the group members and structure of the presentation. It then discusses the origin of compact cities, defines what a compact city is, and outlines the compact city model. Key characteristics of compact cities are presented for both developed and developing countries. The document contrasts compact cities with urban sprawl and defines an eco-compact city model. It lists indicators to measure compact cities and discusses both positive and negative impacts. Finally, it provides examples of cities that depict the compact city model.
- An earthquake is a vibration in the earth's crust caused by the sudden release of stored energy in rocks along fault lines.
- Factors like population density, level of preparedness, distance from the epicenter, time of occurrence, and soil type determine the extent of damage from an earthquake in addition to its magnitude.
- Earthquakes can cause hazards like disruption of services, destruction of property, landslides, destruction of infrastructure, loss of life, fires, and tsunamis.
The document discusses the global distribution of tectonic hazards such as earthquakes, volcanoes, and tsunamis. It explains that most earthquakes occur along well-defined plate boundaries, including subduction zones where one plate slides under another, and collision boundaries. Narrow earthquake belts are associated with constructive margins where new crust is forming and plates are moving apart. Broadly, the document provides an overview of the types and causes of tectonic hazards around the world.
10 Earthquake prone counrtries.Information about Earthquake (2).pdfAyshaPandey
10 EARTHQUAKE PRONE COUNTRIES IN THE WORLD?which country is most prone to earthquake?where do 90% earthquake occur?Earthquake Facts.where do 90% earthquake occur?
1. An earthquake occurs when built-up tension along fault lines in the Earth's crust is suddenly released, causing the ground to shake.
2. The effects of an earthquake depend on several factors, including its magnitude on the Richter scale, distance from the epicenter, and the level of development in the affected area.
3. The 1995 Kobe earthquake in Japan caused over 30,000 injuries, left over 300,000 homeless as buildings collapsed, and led to long-term economic and social impacts as the city was rebuilt.
The document discusses tectonic plate processes and earthquakes. It describes how earthquakes occur at plate boundaries due to stresses from plate movements. Earthquakes at divergent boundaries pose little risk while those at convergent boundaries can be very hazardous, as seen in the 1985 Mexico City earthquake that killed over 10,000 people. The document also discusses earthquake measurement scales, the different types of seismic waves, and secondary hazards like tsunamis, landslides and liquefaction that can amplify earthquake damage.
Study of earthquake hazards or disaster Jahangir Alam
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:
Earthquake: A Tragedy to life and propertyVanshika Singh
An earthquake is the shaking of the Earth's surface caused by a sudden release of energy in the Earth's lithosphere. This social science project discusses earthquakes, including what they are, their causes, effects, and protection against them. Some key points made are that earthquakes result from the movement of tectonic plates and built-up pressure being released. Their effects include ground shaking, ground ruptures, landslides, tsunamis, and fires. Protection involves earthquake-resistant building construction and safety precautions during shaking. Some of the deadliest earthquakes mentioned caused thousands of deaths, such as in Nepal in 2015 and Japan in 2011.
The document discusses earthquakes, including their causes, effects, and notable examples. It explains that earthquakes occur when built-up pressure causes rocks underground to break along faults, releasing energy. Effects can include shaking, tsunamis, landslides, fires, and damage to buildings and infrastructure. The largest recorded earthquakes include the 2004 Sumatra quake and 2005 Kashmir quake. Recent major earthquakes in India are also listed. The ongoing 2015 Nepal earthquake that has caused thousands of deaths is described.
The document discusses different types of natural and man-made disasters. It categorizes natural disasters as meteorological, topographical/geological, and environmental. Man-made disasters are categorized as technological, industrial, and warfare. Specific natural disasters discussed include floods, cyclones, earthquakes, tsunamis, volcanoes, landslides, and more. Man-made disasters include accidents, pollution, industrial accidents, and wars. The document also provides details on the causes and impacts of various disasters like earthquakes, floods, oil spills, and epidemics. Classification schemes for different types of disasters are presented.
Earthquakes occur along plate boundaries and release seismic energy that can cause significant damage. The extent of damage depends on factors like population density, preparedness level, distance from the epicenter, time of occurrence, and soil type. Earthquakes pose several risks such as triggering tsunamis, disrupting services, causing landslides, destroying property and infrastructure, and loss of lives. The distribution of earthquakes corresponds to plate tectonics, with most occurring at convergent boundaries due to high stress levels.
This document provides information about earthquakes, including what causes them, different types of faults, seismic waves, measuring earthquake intensity, effects of earthquakes, and preparedness and response. It explains that earthquakes are caused by a sudden slip along a fault due to built up stresses in the earth's crust. There are three main types of faults - strike-slip, thrust, and normal - depending on the type of plate motion and rock. When an earthquake occurs, seismic waves are generated including body waves (P and S waves) and surface waves (Love and Rayleigh waves). Earthquake intensity can be measured using the Mercalli scale or Richter magnitude scale. Earthquakes can cause damage through ground shaking, landslides
Causes, Effects and Precautions against Earthquakesaqlain_01
1. Earthquakes are caused by the movement of tectonic plates deep below the Earth's surface. As the plates shift and grind against each other, they release energy in the form of seismic waves.
2. Major earthquakes can cause widespread damage to infrastructure like buildings, bridges and dams, resulting in loss of life and property. They can also trigger secondary hazards such as landslides, tsunamis and fires.
3. Pakistan is prone to earthquakes, with major fault lines running along its western border. Some of the deadliest quakes in the country's history include the 2005 Kashmir earthquake that killed over 80,000 people and the 2013 Balochistan earthquake that killed 825.
Earthquakes occur at tectonic plate boundaries and major fault lines. They can be measured using the Richter Scale, which quantifies the magnitude of tremors on a logarithmic scale. The 1995 Kobe earthquake in Japan caused widespread damage and loss of life due to factors such as its proximity to a densely populated urban area built on reclaimed land. Modern earthquake-resistant building techniques aim to absorb vibrations through methods like base isolation and dampening systems.
An earthquake occurs due to a sudden release of energy in the Earth's crust that creates seismic waves. There are three main types of seismic waves - P waves, S waves, and surface waves. Earthquakes are caused by movements of tectonic plates. The effects of earthquakes include shaking, ground rupture, tsunamis, landslides and damage to infrastructure. Earthquake preparedness and mitigation measures can help reduce risks and impacts, such as retrofitting buildings, developing emergency response plans, and educating the public. Dhaka, Bangladesh is at high risk of earthquakes due to its location in a seismically active zone, with over 13 million people vulnerable to damage and loss of life from a major qu
project on different types of disasters.
Also planning for disasters.
Project for every class.
Pictures from various sources.
best chosen animations.
Have very detailed and explained in formation.
The document discusses earthquakes and related topics in three main sections. Section one describes how earthquakes are caused by movement along tectonic plate boundaries and outlines the different types of seismic waves generated by earthquakes. Section two explains how earthquakes are measured, located and recorded using seismographs. Section three discusses the damage earthquakes can cause to buildings and properties from ground shaking and liquefaction. It also describes tsunamis and provides safety tips for earthquake preparedness.
The document provides information about natural hazards caused by geological processes such as earthquakes, volcanic eruptions, and landslides. It defines these hazards and describes their effects. Maps are shown to illustrate hazard-prone areas for earthquakes, tsunamis, and volcanoes in the Philippines based on historical data. Specific past events that caused damage, like the 2013 Bohol earthquake and 1991 Mount Pinatubo eruption, are discussed. Guidelines are provided on preparing for, responding to, and recovering from geological hazards.
Natural hazards and disaster,types,mitigation and managementkamal brar
This document provides an introduction to natural hazards and discusses several specific types of hazards including earthquakes, tsunamis, and tropical cyclones. It explains that a geohazard involves an earth process interacting with human activity to cause loss of life or property. Understanding the human element is critical because population growth is increasing the number of people living in hazard-prone areas. While the geological processes cannot be stopped, efforts can be made to mitigate hazards through scientific study, education, engineering practices, and emergency management. Specific natural hazards like earthquakes, tsunamis, and tropical cyclones are then examined in more detail including how they form and the damage they can cause.
The document defines an earthquake as the sudden release of energy in the earth's crust that creates seismic waves. It identifies the focus as the point where rupture occurs underground, and the epicenter as the point directly above the focus on the surface. It discusses various earthquake measurement scales and zones of seismic activity. Effects of earthquakes include loss of life and property, infrastructure damage, landslides, fires, floods and tsunamis. Safety tips are provided such as taking shelter under sturdy furniture if indoors and moving away from hazards if outdoors during shaking. The strongest earthquakes on record include one in Chile in 1960 measuring 9.5 magnitude that killed over 8,000 people.
An earthquake is caused by the release of built-up pressure within the Earth's crust along fault lines. The focus is where the pressure is released within the crust, and the epicenter is the point on the surface directly above the focus. Earthquakes are measured on the Richter scale using seismometers, which detect the different types of waves that propagate during an earthquake: P-waves, S-waves, and surface waves. The effects of earthquakes can be primary, occurring directly from ground shaking, or secondary, resulting from primary effects like tsunamis or fires.
This document discusses key geographical skills including topographical map reading, geographical data techniques, and conducting geographical investigations. It covers topics such as reading grid references, measuring distances on maps, interpreting map symbols and scales, describing landforms and relief, settlement patterns, and using compasses to find bearings. It also discusses creating and interpreting various types of graphs to display geographical data, such as line graphs, bar graphs, pie charts, scatterplots, climographs, and histograms. Finally, it discusses the phases of conducting geographical fieldwork and how to develop hypotheses or guiding questions.
This document discusses various weather elements such as temperature, rainfall, relative humidity, air pressure, and wind. It defines these elements and describes the instruments used to measure them. For temperature, it explains how factors such as latitude, altitude, distance from the sea, and cloud cover can influence temperatures in different locations. It also provides examples to illustrate these effects. For rainfall, it distinguishes between convective and relief rainfall and includes diagrams to explain their formation. The document is intended to build understanding of key weather concepts.
Natural hazards include tectonic hazards like volcanic eruptions and earthquakes, as well as climate-related hazards such as typhoons and floods. The internal structure of Earth includes the crust, mantle, and core. The crust varies in thickness and composition depending on whether it is oceanic crust or continental crust. Oceanic crust is thinner and denser, while continental crust is thicker and less dense. Tectonic plates move due to convection currents in the mantle, with plates separating at mid-ocean ridges and coming together at subduction zones.
The document discusses different types of tourism:
1) Honeypot tourism refers to popular attractions that attract large numbers of tourists, such as the Taj Mahal and Colosseum.
2) MICE tourism focuses on destinations that provide amenities for meetings, incentives, conferences, and exhibitions, like convention centers in Singapore.
3) Medical tourism has risen with destinations offering good medical facilities and procedures, like cosmetic surgery in South Korea.
1. The document outlines the steps of a geographic inquiry (GI) including forming a hypothesis, collecting and analyzing data, and presenting conclusions.
2. It discusses methods for collecting data through surveys, questionnaires, and observation and includes tips for effective survey design and administration.
3. Finally, it addresses evaluating the reliability and limitations of the collected data, identifying trends or anomalies, and assessing whether the hypothesis is supported.
1. The document outlines the steps of conducting a geographic inquiry (GI) including forming a hypothesis, collecting and analyzing data, and presenting a conclusion.
2. It discusses methods for collecting data through surveys, questionnaires, and observation and includes tips for effective survey design and administration.
3. The document also presents different sampling methods and examples of ways to organize and present collected data including tables, flow maps, and desire line maps.
This chapter discusses key geographical skills like map reading, interpreting data representations, and conducting fieldwork investigations. It covers topics such as reading grid references, compass directions, scales, measuring distances, interpreting reliefs and landforms on maps, and analyzing photographs and satellite images. Various types of graphs like line graphs, bar graphs, pie charts, and climographs are introduced to represent geographical data. The three phases of fieldwork - pre-fieldwork, during fieldwork, and post-fieldwork - are also outlined.
Tectonic plates move due to convection currents in the mantle and slab pull forces. There are different types of plate boundaries including divergent where plates move apart, convergent where they move together, and transform where they slide past each other. These boundaries result in different landforms through geological processes. Divergent boundaries form rift valleys and volcanoes, convergent boundaries form fold mountains, volcanoes and trenches, and transform boundaries cause earthquakes. Natural hazards occur near plate boundaries like earthquakes, volcanic eruptions and tsunamis.
This document discusses weather, climate, and climate change. It begins by defining weather and climate, and describes the key elements of weather including temperature, relative humidity, clouds, rainfall, air pressure, and wind. It then explains the major climate types and their locations: equatorial, monsoon, and cool temperate marine west coast climates. The document goes on to discuss evidence that the global climate has changed in recent decades due to both natural and human factors like the greenhouse effect. It may lead to more extreme weather and affect people. Responses to address climate change are also mentioned.
The document discusses various types and concepts related to tourism. It begins by defining tourism and a tourist. It then outlines different types of tourism such as honeypot tourism, MICE tourism, medical tourism, and religious tourism. It also discusses factors that influence the growth of global tourism like increasing disposable income and leisure time as well as investments in destination infrastructure. The document notes some impacts of tourism including positive economic benefits but also potential negative socio-cultural and environmental impacts. It identifies key stakeholders involved in tourism development and discusses the importance of sustainable tourism.
The document discusses the strengths and limitations of locals and tourists in protecting tourist areas. For locals, community-based tourism provides jobs and business opportunities, as seen in a village in Java. However, locals may lack skilled labor to manage tourism's impacts. For tourists, their spending supports conservation, but they can damage areas through littering and vandalism. Overall, locals play a largely effective role, but would benefit from training to improve conservation skills.
This document provides an overview of topics covered in an elective geography exam, including:
1. Forming and testing hypotheses about tourism relationships.
2. Designing surveys, identifying limitations, and making improvements to data collection methods.
3. Representing and analyzing data using graphs, charts, and maps to identify trends in tourism numbers and flows over different time periods and locations.
The document discusses the risks and benefits of living near volcanic areas. It describes some key risks such as destruction from volcanic materials, landslides, pollution and effects on weather. It also outlines some benefits including fertile volcanic soil which supports agriculture, building materials and precious minerals, tourism attractions, and geothermal energy. While there are benefits, the document argues that there are more risks compared to benefits of living in volcanic areas, given the threats posed by potential eruptions. Proper management is needed to mitigate the risks and leverage the resources volcanoes provide.
The document discusses a REC that was cancelled on March 10th and rescheduled for either March 18th or 19th from 10am to 12pm at Xinnovate on the topic of convergent plate boundaries. It provides examples of transform plate boundaries like the San Andreas Fault in California and North Anatolian Fault in Turkey, describing how an earthquake in 1906 along the San Andreas Fault caused several hundred kilometers of the North American Plate to shift up to 7 meters in under a minute due to stresses building up and releasing where the Pacific and North American Plates slide past each other.
The document discusses transform plate boundaries and provides examples of the San Andreas Fault in the United States and the North Anatolian Fault in Turkey. It notes that at transform boundaries, plates slide past each other building stress until an earthquake occurs. It then provides details about a 1906 earthquake in California on the San Andreas Fault that caused hundreds of kilometers of movement between tectonic plates in under a minute. The document asks how future plate movement might affect two nearby cities.
Convergent plate boundaries occur where tectonic plates move towards one another. There are three main types:
1) Oceanic-oceanic, where two oceanic plates collide and one subducts under the other, forming ocean trenches.
2) Oceanic-continental, where an oceanic plate subducts under a continental plate, pushing up mountains.
3) Continental-continental, where collision resists subduction and the plates break and fold, forming mountains.
- The document discusses plate tectonics topics including oceanic-oceanic divergence and continental-continental divergence.
- Oceanic-oceanic divergence involves two oceanic plates moving apart, causing magma to rise and form new sea floor through sea-floor spreading, creating a mid-ocean ridge.
- Continental-continental divergence can form rift valleys as the land between diverging continental plates sinks, such as the East African Rift Valley, and may eventually lead to the formation of new oceans.
1) Oceanic plates diverge from each other at mid-ocean ridges. Magma rises from the mantle to fill the gap between separating plates, cooling to form new ocean crust. The youngest ocean crust is closest to the ridge.
2) Continental plates can diverge, resulting in rift valleys like East Africa's Great Rift Valley. The stretched crust fractures and the land between sinks, forming a low-lying valley. Continental divergence can also form seas like the Red Sea.
3) Faulting occurs as the crust fractures along tensional forces during plate divergence. Rift valleys form along fault lines, and block mountains are uplifted crustal blocks surrounded by sinking land.
Mental Health and well-being Presentation. Exploring innovative approaches and strategies for enhancing mental well-being. Discover cutting-edge research, effective strategies, and practical methods for fostering mental well-being.
CHAPTER 1 SEMESTER V COMMUNICATION TECHNIQUES FOR CHILDREN.pdfSachin Sharma
Here are some key objectives of communication with children:
Build Trust and Security:
Establish a safe and supportive environment where children feel comfortable expressing themselves.
Encourage Expression:
Enable children to articulate their thoughts, feelings, and experiences.
Promote Emotional Understanding:
Help children identify and understand their own emotions and the emotions of others.
Enhance Listening Skills:
Develop children’s ability to listen attentively and respond appropriately.
Foster Positive Relationships:
Strengthen the bond between children and caregivers, peers, and other adults.
Support Learning and Development:
Aid cognitive and language development through engaging and meaningful conversations.
Teach Social Skills:
Encourage polite, respectful, and empathetic interactions with others.
Resolve Conflicts:
Provide tools and guidance for children to handle disagreements constructively.
Encourage Independence:
Support children in making decisions and solving problems on their own.
Provide Reassurance and Comfort:
Offer comfort and understanding during times of distress or uncertainty.
Reinforce Positive Behavior:
Acknowledge and encourage positive actions and behaviors.
Guide and Educate:
Offer clear instructions and explanations to help children understand expectations and learn new concepts.
By focusing on these objectives, communication with children can be both effective and nurturing, supporting their overall growth and well-being.
As Mumbai's premier kidney transplant and donation center, L H Hiranandani Hospital Powai is not just a medical facility; it's a beacon of hope where cutting-edge science meets compassionate care, transforming lives and redefining the standards of kidney health in India.
The Importance of Black Women Understanding the Chemicals in Their Personal C...bkling
Certain chemicals, such as phthalates and parabens, can disrupt the body's hormones and have significant effects on health. According to data, hormone-related health issues such as uterine fibroids, infertility, early puberty and more aggressive forms of breast and endometrial cancers disproportionately affect Black women. Our guest speaker, Jasmine A. McDonald, PhD, an Assistant Professor in the Department of Epidemiology at Columbia University in New York City, discusses the scientific reasons why Black women should pay attention to specific chemicals in their personal care products, like hair care, and ways to minimize their exposure.
This particular slides consist of- what is hypotension,what are it's causes and it's effect on body, risk factors, symptoms,complications, diagnosis and role of physiotherapy in it.
This slide is very helpful for physiotherapy students and also for other medical and healthcare students.
Here is the summary of hypotension:
Hypotension, or low blood pressure, is when the pressure of blood circulating in the body is lower than normal or expected. It's only a problem if it negatively impacts the body and causes symptoms. Normal blood pressure is usually between 90/60 mmHg and 120/80 mmHg, but pressures below 90/60 are generally considered hypotensive.
Sectional dentures for microstomia patients.pptxSatvikaPrasad
Microstomia, characterized by an abnormally small oral aperture, presents significant challenges in prosthodontic treatment, including limited access for examination, difficulties in impression making, and challenges with prosthesis insertion and removal. To manage these issues, customized impression techniques using sectional trays and elastomeric materials are employed. Prostheses may be designed in segments or with flexible materials to facilitate handling. Minimally invasive procedures and the use of digital technologies can enhance patient comfort. Education and training for patients on prosthesis care and maintenance are crucial for compliance. Regular follow-up and a multidisciplinary approach, involving collaboration with other specialists, ensure comprehensive care and improved quality of life for microstomia patients.
Joker Wigs has been a one-stop-shop for hair products for over 26 years. We provide high-quality hair wigs, hair extensions, hair toppers, hair patch, and more for both men and women.
TEST BANK FOR Health Assessment in Nursing 7th Edition by Weber Chapters 1 - ...rightmanforbloodline
TEST BANK FOR Health Assessment in Nursing 7th Edition by Weber Chapters 1 - 34.
TEST BANK FOR Health Assessment in Nursing 7th Edition by Weber Chapters 1 - 34.
TEST BANK FOR Health Assessment in Nursing 7th Edition by Weber Chapters 1 - 34.
Hypertension and it's role of physiotherapy in it.Vishal kr Thakur
This particular slides consist of- what is hypertension,what are it's causes and it's effect on body, risk factors, symptoms,complications, diagnosis and role of physiotherapy in it.
This slide is very helpful for physiotherapy students and also for other medical and healthcare students.
Here is summary of hypertension -
Hypertension, also known as high blood pressure, is a serious medical condition that occurs when blood pressure in the body's arteries is consistently too high. Blood pressure is the force of blood pushing against the walls of blood vessels as the heart pumps it. Hypertension can increase the risk of heart disease, brain disease, kidney disease, and premature death.
3. Hazards associated with living in earthquakes zones
- Disruption of services
- Destruction of properties
- Landslides
- Destruction of infrastructure
- Threat of tsunamis
- Loss of lives
- Fires
SPLIT LIKE FLOWER
Earthquakes
4. Disruption of services
• An earthquake can
disrupt services such
as the supply of
electricity, gas and
water.
• The earthquake in
Kobe, Japan, in 1995
disrupted electricity,
gas and water
supplies to about a
million of Kobe city’s
1.4 million residents.
Hazards associated with
earthquakes
5. Fire
• Earthquakes may
rupture gas pipes
and this can
provide fuel to
start fires.
• For example, the
earthquake in
Kobe, Japan, in
1995 caused
extensive fires.
Hazards associated
with earthquakes
Children stand near houses in Padang, Indonesia
that caught fire after the earthquake
6. Landslides
• Landslides are
rapid
downslope
movements of
soil, rock and
vegetation.
• Mudflows may
also occur when
there is heavy
rainfall.
Hazards associated with earthquakes
Damage Caused by Offshore Earthquake Near
World's Largest Nuclear Power Plant in Japan
in 2008
7. Destruction of
properties
• Earthquakes can
cause
destruction to
many homes.
• People may be
without homes
after the
disaster.
Hazards associated with earthquakes
(Kobe, Japan earthquake)
8. Hazards associated with earthquakes
Destruction of
infrastructure
Earthquakes may
cause cracks to form
in infrastructure such
as roads and
bridges.
Transportation can
be disrupted as it is
unsafe to use the
damaged roads.
9. Loss of lives
• Earthquakes and
their associated
hazards often
threaten the lives
of those living in
earthquake
zones.
Hazards associated with earthquakes
A person approaches a body lying in the
rubble along Delmas road, the day after an
earthquake struck Port-au-Prince, Haiti.
A 7.0-magnitude earthquake, the largest
ever recorded in the area, rocked Haiti on
Jan 2010.
10. Case study: Earthquake in Tōhoku, Japan
What are the effects of the earthquake on people and
the environment?
• Occurred in 2011
• Generated large tsunami
• Destroyed the Fukushima
nuclear power plant
11. Case study: Earthquake in Tōhoku, Japan
How have people responded to the earthquake ?
• Sent out 100,000 members
of the Self-Defence Forces
• Set up rescue centres
• The bank of Japan pumped
US$183 billion into the
economy.
• Trained personnel dealt
with post anxiety and
depression.
12.
13. • Extent of earthquakes
- The Richter Scale is used to measure the magnitude
of an earthquake
16. • Apart from its magnitude, the extent of
damage caused by an earthquake may
vary based on other factors:
- Population density
- time of occurrence
- level of preparedness
- distance from the epicentre
- type of soil
Earthquakes
17. Definition More severe Less severe
Population
density
Number of people
living in the area
Dense population
eg city
Less dense
population eg
countryside
Level of
preparedness
Evacuation plans,
trained rescue workers
Not prepared Prepared eg
Emergency Drills
Distance from
epicentre
Point on the earth's
surface vertically above
the focus of an EQ
Nearer the
epicentre eg
Christchurch, NZ
2011
Further away from
epicentre
Time of
occurrence
Time of occurrence Day hours Night hours
(sleeping, more
deaths)
Types of soil Liquefaction: ground
becomes unstable and
soil flows like liquid
Loose and
unconsolidated
sediments
Stable and
consolidated soil
18. P67
• Seismic wave
• Distance to the surface
• Built up area
• Time it occurred
• Magnitude of earthquake
19. • In 2011, Christchurch is within the first seismic wave which is
very near to the epicenter of the earthquake, while in 2010,
Christchurch is at the third seismic wave.
• In 2011, the earthquake occurred very near to the surface at a
focal depth of 5km so the impact is greater.
• Christchurch is a densely built up area with many buildings and
the infrastructure is not built to withstand the stronger vibration
felt in 2011.
• In 2011, earthquake occurred at 12.51pm where many people
are still in offices working when buildings collapsed, while in
2010 at 4.35am, when most people are not in high-rise offices.
• Magnitude : 2011 – 6.3 , 2010 – 7.1 (Both are strong magnitude
earthquakes)
P67
20. P68
“The extent of damages caused by an earthquake is solely
determined by an area’s proximity to the epicentre.”
How true is this statement? Give reasons and relevant
examples in your answer
Answer in PEE format
1.Magnitude of Earthquake
2.Population density
3.Level of preparedness
4.Distance from epicentre
5.Time of occurrence
6.Type of soil
21. Magnitude of the Earthquake
P : The strength of an earthquake, based on the energy released from
the focus.
E: The higher the magnitude of an earthquake, the higher the
possibility of infrastructure collapsing, as they are unable to
withstand the force exerted by the earthquake, the greater the
extent of damages. This may result in the death of more people who
are buried under the debris, and the country’s economy will be
crippled as resources will be diverted to rebuild the country while
investors lose confidence in the country.
Eg : The Great Kobe Earthquake in 1995 (7.2 on Richter Scale; lasted
20 secs, 5000 people died, 300000 people became homeless. The
Great East Japan Earthquake in 2011 (8.9 on Richter Scale; 16000
deaths; tsunami with wave height up to 10m)
22. Population density
Point: The higher the population density of an earthquake-prone area,
the higher the chances of people getting killed or injured.
Elaboration: When people are living in close proximity, the destruction
of an infrastructure in an area will have an impact on a larger number
of people. A stampede may also occur when so many people are trying
to escape from an earthquake-prone area at the same time. All these
may lead to a greater extent of damages as lives are loss when high-
rise buildings topple over. Hence, a magnitude 9.0 earthquake will
only cause extensive damages if the area is densely populated.
Example
•Earthquake in Anchorage, Alaska in 1964
•Magnitude 9.2 on the Richter Scale
•Only 115 people died as the area had a small and sparse population
23. Level of preparedness
P : Refers to how well the people know what to do in the event of an
earthquake, such as having evacuation plans and trained rescue
workers.
E: This will reduce the number of casualties that may arise from a
stampede, and will also ensure that those who are injured receive
timely medical assistance. Hence, a magnitude 9.0 earthquake may not
cause extensive damages if the people know what to do and are able
to evacuate safely before getting injured.
Example: In Japan, students are taught how to react when the
earthquake warning signal goes off. They are to crouch under the
nearest table, so as to prevent falling objects from injuring them
24. Distance from epicentre
P : Generally, the nearer to the epicentre, the stronger the
shockwaves receive
E: The energy of the earthquake is absorbed and weakened as it
radiates outwards from the epicentre to the surrounding land. Hence,
a magnitude 9.0 earthquake may not cause extensive damages if the
area involved is located far away from the epicentre.
Eg: During the 2011 Christchurch earthquake in New Zealand, the
epicentre was in a town a few km away from the city centre. Thus, the
city centre suffered more damages than areas further away from the
city.
25. Time of occurrence
P: The time of the day during which the earthquake occurs determines
where people are and what they are doing, which will affect their
chances of survival.
E: If the earthquake occurs when most people are sleeping, there is a
higher chance that these people will be trapped in their houses and
more deaths may occur. Hence, a magnitude 9.0 earthquake may not
cause extensive damages if the earthquake occurs during the day and
people are more aware and thus have sufficient time to escape.
Eg: More than 2400 people died when an earthquake occurred a couple
of hours after midnight in the Sun Moon Lake Region in Taiwan in 1999.
26. Type of soil
P : Where sediments are loose and unconsolidated, the seismic waves
are amplified. Structures built on saturated and unconsolidated
sediments can be affected by liquefaction, where the ground becomes
unstable and the saturated soil flows like a liquid
E: When sediments are loose and unconsolidated or saturated, the
effects of the earthquake are amplified, which could lead to the
collapse of infrastructure. Hence, a magnitude 9.0 earthquake may not
cause extensive damages if the type of soil found in that area is well-
consolidated and more resistant to the movements of the ground.
Eg: In the 2011 Christchurch earthquake in New Zealand, many houses
and buildings had to be abandoned because of liquefaction after the
earthquake.
27. Conclusion
The extent of damages experienced by an area
is not just dependent on the magnitude of the
earthquake, but also other factors as mentioned
above.
These factors are interlinked and will determine
how badly affected an area is.
However, men can reduce the extent of
damages experienced by adopting the various
adaptation measures like earthquake resistant
buildings or installing earthquake monitoring
and warning systems.
28.
29. In December 2004, The Tsunami swamps Phuket's Chedi resort (AFP/Joanne Davis)
Tsunami
30. Threat of tsunamis
• Tsunami refers to an usually large sea wave.
• Tsunamis may be formed by:
- The movement of the sea floor during a large earthquake
at subduction zones;
- An underwater volcanic eruption;
- An underwater landslide; and
- A landslide above sea level which causes materials to
plunge into the water.
Hazards associated with earthquakes
31. • In 2004, a 9.2 magnitude triggered a tsunami with
waves spreading throughout the Indian Ocean.
Aceh before and after the tsunami hit the area
Hazards associated with earthquakes
33. • The tsunami is formed by the movement of the sea floor during a
large earthquake at the ________ zone. [1]
• The offshore earthquake forces out a ____________. [1]
• On reaching shallower water, greater friction slows the waves
and forces the waves to increase in __________. [1]
• At the point of impact on the coast, the tsunami waves could
reach heights of 15m. [1]
P64
34. • The tsunami is formed by the movement of the sea floor during a
large earthquake at the subduction zone. [1]
• The offshore earthquake forces out a mass of sea water. [1]
• On reaching shallower water, greater friction slows the waves
and forces the waves to increase in height. [1]
• At the point of impact on the coast, the tsunami waves could
reach heights of 15m. [1]
P64
35. Singapore is protected to a significant degree
[1]
by the southern end of Malaysia Peninsula [1]
and the island of Sumatra to the west [1].
The energy of waves travelling southwards
would have been absorbed by the coastlines of
those land masses. [1]
P64
Explain why the impact of the tsunami on Singapore was
minimal.
[4]
36. The spread of the tsunami waves caused by the tsunami
Hazards associated with earthquakes
37. P=Point Tsunamis can have an impact on the lives of the people.
D=Describe Tsunamis are unusually large waves caused by underwater earthquakes.
E=Explain Tsunamis can travel long distances and caused great destruction to coastal areas when they
sweep inland. At the point of contact on the coast, the tsunami waves could be travelling at
50km/h and may reach heights of around 15metres.
E=Example In 2004, a 9.2 magnitude earthquake occurred in the Indian Ocean and caused a tsunami with
waves that spread throughout the Indian Ocean. The most damage was experienced in the low-
lying coastal areas of western Sumatra, Indonesia.
There was loss of lives and destruction of properties along this stretch of the coast.
P=Point Earthquakes can have an impact on the lives of the people. Earthquakes can cause fire.
D=Describe Earthquakes may rupture gas pipes and the gas can provide fuel to start fires. Earthquakes may
expose electrical cables which may ignite flammable items like gas and oil.
E=Explain Once these items are ignited, fires can spread quickly to a large area, increasing the number of
deaths and injured.
E=Example For example, the 1995 earthquake in Kobe, Japan. The earthquake caused extensive fires that went
on for 2 days. Firemen were unable to control the fires as the ruptured water pipes meant that
there was no water supply to put out the fire.
Complete Worksheet
‘The impact of a tsunami on people’s lives can be more devastating than that of an
earthquake.’ How far do you agree with this statement? Give reasons for your answer.
[6]
Impact of a tsunami on people’s lives (1 example)
Impact of an earthquake on people’s lives (1 example)
Editor's Notes
Suggested activity:
Ask students to describe the location of the earth’s major earthquakes.
Along plate boundaries.
How does earthquakes lead to landslides ?
Suggested activity:
Allow students to visit the website: http://abcnews.go.com/Archives/video/jan-17-1995-earthquake-japan-9421417.
Ask them about the effects of the earthquake they observe from the video.
Fires, collapsed buildings and infrastructure, floods, lives lost, people made homeless, people trapped under rubble
Suggested activity
Show students satellite images of the impact of the Tōhoku earthquake and tsunami from the website: http://earthobservatory.nasa.gov/Features/Gallery/tsunami.php
Suggested activity:
Ask students to explain why the earthquake that took place in Haiti (magnitude 7.0) caused more damage and higher number of deaths than the earthquake that took place in Tohoku, Japan (magnitude 9.0).
The earthquake in Haiti could have taken place in areas that are densely populated as compared to Tohoku.
The people in Tohoku, Japan could be more prepared to deal with earthquakes than the people in Haiti.
The structures of the buildings in Japan are more earthquake-resistant.
Qns 1 - Using what you have learnt about plate boundaries, identify the type of plate boundary
caused the tsunami. (Express/Normal) -transform boundary, divergent boundary
2. From the series of photos above, describe different stages of tsunami in your own words.
-calm conditions on the sea surfaces.
-heightened level of seawater
-seawall approaching the shore, flooding the structures and buildings
-seawater level remained high and did not subside.
-
2. Suggest why the tsunami was able to reach inland. (Express)