Plate Tectonics Photographic Evidence - QiHua
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ihsl1) There are several types of plate boundaries including convergent boundaries where plates collide and form mountains, divergent boundaries where plates separate and form rift valleys, and transform boundaries where plates slide past each other causing earthquakes. 2) Earthquakes occur when rocks underground suddenly break along a fault line. Major earthquakes can cause extensive damage to infrastructure and loss of life. They also sometimes trigger tsunamis. 3) Tsunamis are large sea waves caused by earthquakes or other seismic events under the sea. The 2011 tsunami in Japan was triggered by a powerful earthquake and resulted in over 3,000 deaths as well as nuclear radiation leaks.
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Earthquakes powerpoint
The document discusses earthquakes, including their causes, measurement, effects, and preparedness. Earthquakes occur due to the sudden release of built-up stress along fault lines in the earth's crust, causing seismic waves. Their magnitude is measured using scales like the Richter scale or moment magnitude scale. Earthquakes can damage infrastructure and the environment through ground shaking and secondary events like tsunamis or landslides. While earthquakes cannot be prevented, preparation through emergency planning and building design can reduce risks.
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An earthquake is caused by the sudden release of built-up energy along fault lines in the earth's crust. Most earthquakes occur along plate boundaries and fault lines, especially around the Pacific Ring of Fire. Earthquakes can cause tremendous damage through ground shaking and secondary effects like tsunamis. Recent major quakes in Nepal and Japan killed over 9,000 and led to widespread destruction. While earthquakes can't be prevented, communities can take steps to minimize damage by strengthening buildings and infrastructure and preparing emergency plans.
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The document provides information about earthquakes, including what they are, the types of seismic waves produced, causes, effects, classification, and mitigation measures. It also discusses earthquakes in Northeast India and provides a case study on the 2015 Nepal earthquake. Key points include: Earthquakes are caused by the sudden release of energy along fault lines in the earth's crust. They produce different seismic waves and can have devastating primary effects like land subsidence as well as secondary effects like damage to infrastructure. The Nepal earthquake measured 7.8 magnitude, killed over 8,000 people, and caused billions in damages.
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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.
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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.
Earthquake powerpoint
An earthquake occurs when two blocks of the earth's crust slip past one another, causing the ground to shake. Most earthquakes happen along the edges of tectonic plates that slowly move and bump against each other deep underground. Earthquakes can cause massive damage and loss of life, such as the 1556 Shaanxi earthquake in China that killed over 800,000 people. Modern solutions aim to better predict, withstand, and prepare for earthquakes to minimize harm.
Earthquake Hazards
I do not have enough context to answer those specific questions. The document provided discusses different types of earthquake hazards and their effects, but does not mention fault types in the Philippines or bringing cookies to class.
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Earthquakes powerpoint
The document discusses earthquakes, including their causes, measurement, effects, and preparedness. Earthquakes occur due to the sudden release of built-up stress along fault lines in the earth's crust, causing seismic waves. Their magnitude is measured using scales like the Richter scale or moment magnitude scale. Earthquakes can damage infrastructure and the environment through ground shaking and secondary events like tsunamis or landslides. While earthquakes cannot be prevented, preparation through emergency planning and building design can reduce risks.
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An earthquake is caused by the sudden release of built-up energy along fault lines in the earth's crust. Most earthquakes occur along plate boundaries and fault lines, especially around the Pacific Ring of Fire. Earthquakes can cause tremendous damage through ground shaking and secondary effects like tsunamis. Recent major quakes in Nepal and Japan killed over 9,000 and led to widespread destruction. While earthquakes can't be prevented, communities can take steps to minimize damage by strengthening buildings and infrastructure and preparing emergency plans.
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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.
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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.
Earthquake powerpoint
An earthquake occurs when two blocks of the earth's crust slip past one another, causing the ground to shake. Most earthquakes happen along the edges of tectonic plates that slowly move and bump against each other deep underground. Earthquakes can cause massive damage and loss of life, such as the 1556 Shaanxi earthquake in China that killed over 800,000 people. Modern solutions aim to better predict, withstand, and prepare for earthquakes to minimize harm.
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I do not have enough context to answer those specific questions. The document provided discusses different types of earthquake hazards and their effects, but does not mention fault types in the Philippines or bringing cookies to class.
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The document discusses several natural disasters including tsunamis, volcanoes, hurricanes, droughts, and earthquakes. It provides definitions and descriptions of each phenomenon. Tsunamis are large waves caused by undersea earthquakes or landslides that can reach heights of 30 meters. Volcanoes form when molten rock rises from below the surface due to tectonic plate movement, and can cause additional disasters when erupting. Hurricanes are large storms formed over warm ocean waters that rotate anti-clockwise and contain strong winds. Drought occurs when a long period passes without rain, preventing crop growth. Earthquakes are sudden releases of stress in the Earth's crust that cause shaking.
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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
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Causes, Effects and Precautions against Earthquake
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.
Earthquake and its impact
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.
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The document discusses earthquakes and tsunamis. It defines an earthquake as the shaking of the Earth caused by the sudden breaking and shifting of tectonic plates. Earthquakes occur when these plates in the Earth's surface break and shift, releasing energy through shockwaves. Undersea earthquakes can cause tsunamis by disturbing the ocean's surface. The document provides safety tips, advising people to take shelter under sturdy furniture during an earthquake and evacuate buildings afterwards. It also mentions the San Andreas Fault as an example of a slip fault where the rocks have moved horizontally, creating earthquakes.
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The document discusses earthquakes and tsunamis, their causes and effects. Earthquakes are caused by shifting tectonic plates and can damage structures, cause landslides and flash floods. Tsunamis are large sea waves typically caused by underwater earthquakes that can damage property, cause flooding and loss of life. The document recommends remedies like responsible planning, seismic retrofitting and high seawalls to minimize damage from these disasters.
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Earthquakes are caused by slow movements within the Earth as it continues to cool. Some human activities like constructing dams, extracting groundwater, fracking, and building skyscrapers can also induce earthquakes by adding stress that destabilizes existing faults. Earthquakes have both primary effects of immediate damage through collapsing buildings, and secondary effects like tsunamis, landslides, fires, disease outbreaks, and soil liquefaction that prolong suffering after the initial quake.
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- 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.
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1) The document discusses different types of plate boundaries including convergent boundaries which form mountains, divergent boundaries which form rift valleys, transform boundaries where plates slide past each other, and subduction zones where one plate moves under another.
2) It provides examples of specific geological features formed by these boundaries such as the Himalayan Mountains from the Indian and Eurasian plate collision, and mid-ocean ridges formed at divergent boundaries.
3) The document also discusses various natural hazards associated with plate tectonics including earthquakes, tsunamis, volcanic eruptions, and discusses the devastating 2011 Tohoku earthquake and tsunami that struck Japan.
Untitled presentation
The document discusses the four main types of plate boundaries:
1) Convergent boundaries, where plates collide, can form mountains, trenches, or volcanic islands depending if the plates are continental or oceanic. Examples given are the Himalayas and Mauna Loa volcano in Hawaii.
2) Transform boundaries, where plates slide past each other, can cause earthquakes like the 1906 San Andreas quake or tsunamis like the 2011 Japan event.
3) Divergent boundaries, where plates move apart, form rift valleys like in East Africa or mid-ocean ridges like the Juan de Fuca Ridge.
4) Examples of each boundary type are analyzed in more detail, explaining how the
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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.
Earthquake and its impact
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.
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- Ground Rapture
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Earthquakes can cause significant damage to human structures and trigger tsunamis. Structures are designed to withstand seismic activity but the level of damage depends on the duration and intensity of shaking. The 2011 Tōhoku earthquake in Japan, measured at a magnitude 8.9, caused widespread damage including moving the city of Sendai over 8 feet and generating a tsunami over 4 kilometers high along the coast. Broken power lines and gas mains are also common due to collapsed buildings and pose fire and air quality hazards.
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The document provides information about earthquakes, earthquake hazards, and tips for before, during, and after an earthquake. It defines an earthquake and describes fault lines, hypocenters, and epicenters. It discusses intensity and magnitude scales and identifies three earthquake source zones in the region. Hazards like ground shaking, surface rupturing, liquefaction, tsunamis, and landslides are explained. Maps show ground shaking, liquefaction and tsunami hazards. Alert levels and recommendations during a tsunami are outlined. The document provides tips for preparing for, responding to, and recovering from an earthquake. Contact information for emergency services is also included.
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Earthquakes occur along fault lines as a result of tectonic plate movement and built up stress being released. They can cause significant damage depending on their magnitude, proximity to populated areas, and local soil and construction practices. Major earthquake zones exist along plate boundaries where tectonic plates converge, diverge, or move past each other. The largest, most destructive quakes occur in subduction zones. To minimize earthquake risk, communities can educate citizens, construct earthquake-resistant buildings, and implement emergency planning and insurance.
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This document provides information about earthquakes, including their causes, effects, historical examples, and safety procedures. It discusses how earthquakes are the result of the sudden release of energy in the Earth's crust. Key points covered include how earthquakes are measured, where they occur depending on tectonic plate movement, the damage they can cause to infrastructure from ground shifting and liquefaction, and what to do during and after an earthquake strikes to remain safe.
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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.
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Various Hazards that May happen in the event of Earthquake
Reference:
https://www.gns.cri.nz/Home/Learning/Science-Topics/Earthquakes/Earthquake-Hazards
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The document discusses earthquakes and tsunamis, their causes and effects. Earthquakes are caused by shifting tectonic plates and can damage structures, cause landslides and flash floods. Tsunamis are large sea waves typically caused by underwater earthquakes that can damage property, cause flooding and loss of life. The document recommends remedies like responsible planning, seismic retrofitting and high seawalls to minimize damage from these disasters.
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- Earthquakes can cause hazards like disruption of services, destruction of property, landslides, destruction of infrastructure, loss of life, fires, and tsunamis.
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Geo @HU Notes.pptx
Geohazards are natural hazards caused by geological processes within the Earth, such as volcanoes, earthquakes, floods, tsunamis, and cyclones, which can cause damage and loss of life. Earthquakes occur along faults in the Earth's crust due to the sudden release of accumulated strain, generating seismic waves that can damage infrastructure and trigger other hazards like tsunamis and landslides. Volcanic eruptions result from the buildup of pressure from magma and gases below the Earth's surface, which are released through explosions or lava flows that can endanger nearby populations and environments.
The most dangerous country
This document compares the natural disaster risks of earthquakes and volcanoes in Indonesia and Japan. It discusses how tectonic plates cause earthquakes and volcanoes, and provides charts showing the history of volcanic eruptions and major earthquakes in each country. Based on more frequent, larger earthquakes and proximity to the ocean, the document concludes that Japan is a more dangerous place to live than Indonesia due to natural disasters.
Submarine earthquake
Submarine earthquakes occur underwater at the bottom of bodies of water and are caused by the movement of tectonic plates under the sea floor. When pressure builds up at plate boundaries due to friction, it is suddenly released, causing the earthquake. This can generate destructive tsunamis that travel across the ocean and heavily damage coastal areas. Understanding plate tectonics helps explain why different types of plate boundaries like convergent or transform faults result in submarine quakes. Historic examples include the 1960 Chile earthquake, the largest ever at magnitude 9.5.
Quakes by Matthew Falzon, 3.05
Earthquakes are caused by the sudden movement of tectonic plates. Over time, strain builds up along plate boundaries until the accumulated energy is released, causing the plates to shift in an earthquake. While earthquakes can cause damage near fault lines, most of the energy released travels as seismic waves. In ancient times, earthquakes were attributed to gods like Neptune, who was thought to control both the sea and earth tremors. Underwater earthquakes, or seaquakes, can generate destructive tsunamis by displacing large volumes of water. Tsunamis are a series of enormous waves that travel very quickly but are relatively small in the open ocean.
Tsunami
Tsunami is a Japanese word Tsu means ‘harbour’ and nami means ‘wave’.
They are called tidal waves but they have actually nothing to do with the tides. However their appearance from shore is similar to rapidly rising or falling tides.
Tsunami is a series of wave created when water is moved very quickly.
Tsunami is gravity wave system, triggered by vertical disturbances in ocean. They are long waves sometime with hundreds of miles b/w their crests, just like the concentric waves generated by an object dropped into a pool.
First tsunami was recorded in 1480 B.C. in eastern Mediterranean, when the Minoan civilization was wiped out.
A large tsunami accompanied by the earthquake of Lisbon in 1755.
The Kutch earthquake of June 16, 1819 generated strong tsunami which submerged the coastal areas and damage to ships and country made boats of fishermen.
North and South American records have dated such
events back to 1788 for Alaska and 1562 for Chile. Records of Hawaiian tsunami go back to 1821.
Tsunami hits the Mona Passage off Puerto Rico in 1918, grand banks of Canada in 1929.
Earthquake , Tsunami and Subduction zone
Earthquakes are caused by the sudden release of energy along fault lines in the earth's crust. The effects of earthquakes vary based on their magnitude and can include widespread destruction and loss of life. Seismic waves, including compressional P-waves and shear S-waves, travel outward from the hypocenter or focus of the earthquake. The location of the epicenter at the earth's surface directly above the focus can be determined using seismic data from multiple monitoring stations. Earthquakes are measured on scales such as the Richter scale and Modified Mercalli intensity scale.
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Photographic evidence Joanne
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Convection currents
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Photographic evidence - Plate Tectonics
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Plate Tectonics Photographic Evidence - QiHua
- 1. Convergent boundary When two plates come together that is convergent boundary.
- 2. Himalaya Mountains When two plates beneath the earth’s surface collided, the edges of one or both are pushed upwards that creates a mountain. It formed in continental crust.
- 3. Divergent Boundary - when two tectonic plates separate. Rift valley Mid-Ocean Ridge
- 4. Great Rift Valleys Formed by the continental plates breaking apart that creates rift valleys.
- 5. Mid Atlantic Ridges When two plates separate by plate tectonic. it’s oceanic spreading water. The effect is formed by lava erupted from the mid-ocean ridges that the volcano can attached to it form the ridges.
- 6. Transform Boundary- slide past to each other. Earthquake Tsunami
- 7. Earthquake It formed by when the rock underground suddenly breaks along a fault. It is at a transform boundary in Japan in 2012. The effect of the earthquake are many people died, damage the houses and buildings and so on. It is so terrible.
- 8. Tsunami The tsunami formed by earthquakes must occur underneath or near the ocean, be large and create movements in the sea floor. The effect of the tsunami are wash away property, destroy the live, make people scared that have nightmares.
- 9. Subduction Zone– two plates come up together and one of them moves on top of the other. Volcanic Arc Trench
- 10. Volcanic Arc Volcanic Arc is the Line of the volcano. It will create the volcano. The effect of this is the volcanic eruptions.
- 11. Fault Zone-A fault line is a break in the surface of the Earth where one side of the break is pushed up against the other. Fault lines are caused by Earthquakes. It has three types of the faults. They are reverse fault (one side moves down) normal fault(one side moves up)strikeslip fault(slide past to each other.) 12/17/13
- 12. Banning strand of the San Andreas fault zone, Riverside County, California—III It caused by the reverse fault. The effect of this is it will be created the terrible earthquakes. 12/17/13
- 13. Hot spot-part of the mantle and always stay in the same locations. Hot spots are places within the mantle where rocks melt to general magma.And the it will have the heat to push the magma up that create 12/17/13 the hot spot volcano.
- 14. Ring of Fire-is no longer active of the volcano. The Ring of Fire is a ring of volcanoes around the Pacific Ocean that result from subduction of oceanic plates beneath lighter continental plates.And it always happen in Japan.In addition,if it erupts,it will cause 12/17/13 the volcanic eruptions under the ocean.
- 15. Earthquake in Japan It happened at 13:46 on March 11, 2011.It was in Miyagi Prefecture in northeastern Japan region. It was really terrible and the magnitude is 9.0 earthquake. It had big consequences. For example the earthquake has caused 14,063 people were killed,13,691 were missing. Moreover, it had 9.0 earthquake caused a tsunami about 10 meters high, and caused nuclear power plant explosion. It was the highest in the world in the history of the observed magnitude earthquake. On the other hand, it damages many buildings and effect the economic conditions. That was made Japan had a big accident for this that make people feel scared. 12/17/13
- 16. The effect of the earthquake in Japan 12/17/13
- 17. Tsunami in Japan In this case it shows the tsunami caused by the earthquake. This earthquake, not only hit the Japanese homeland, hit the Japanese economy, but also on the Japanese caused the tsunami. Tsunami disaster has caused 3373 deaths and 15,000 people missing. The big effect of this is Nuclear and nuclear radiation leak. There caused the people might got the diseases from the radiation explosion. It is really harmful, it is not just for Japan, it should harm all over the world. 12/17/13
- 18. The effect the tsunami in Japan 12/17/13