Progressive waves
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Progressive waves transmit energy as they propagate from one place to another through a medium. They are generated when a vibrating object does work on the particles of a medium, causing them to oscillate and transmit energy from one point to the next. Examples include waves spreading out on the surface of water when a pebble is dropped in, with the disturbance moving outward in all directions at the same rate.
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Waves
Waves are disturbances that transfer energy through a medium. They are caused by vibrations in the medium and can be transverse, longitudinal, or a combination. Key properties of waves include amplitude, wavelength, frequency, and speed. Waves interact with each other and surfaces through reflection, refraction, diffraction, interference, and can form standing waves through the combination of incoming and reflected waves.
Wave motion
Wave motion is the transfer of energy through a medium by vibration or oscillation of its particles. There are two types of waves: transverse waves, where particles vibrate perpendicular to the direction of energy transfer, and longitudinal waves, where particles vibrate parallel to the direction of transfer. Transverse waves occur in solids and liquids while longitudinal waves can occur in all media and involve changes in pressure.
Earthquakes
An earthquake is caused by the release of energy stored in rocks that are sliding past one another deep underground. When the rocks finally slip, they snap back into position, releasing this stored energy in the form of waves that travel outward in all directions through the earth. There are different types of earthquake waves that move the ground in various ways and travel at separate speeds, allowing scientists to determine the distance to the earthquake's origin. Earthquake waves can travel great distances depending on the magnitude of the quake, sometimes going around the entire planet multiple times for very large seismic events.
Learning objective 2
1) When two waves undergo destructive interference, their energy does not disappear but is instead transferred into potential energy in the form of pressure variations.
2) The total energy of two waves is equal to the sum of their individual energies. During destructive interference, the frequency and wavelength change in a way that maintains the total energy.
3) For sound waves, destructive interference results in a cancellation of pressure changes and velocities between the waves, rather than a loss of energy. The energy is contained as potential energy in the altered pressure field.
151207 tajikistan
A 7.2 magnitude earthquake occurred in a sparsely populated area of Tajikistan, approximately 349km east of the capital city of Dushanbe. The earthquake shook buildings in nearby countries but caused no reported injuries or damage. An estimated 5,000 people experienced strong ground shaking during the earthquake. The earthquake occurred as a result of strike-slip faulting within the crust of the Eurasian tectonic plate.
Presentation About Seismic Wave
1. Earthquakes generate seismic waves that travel through the earth's crust and cause the ground to shake when they reach the surface.
2. The characteristics of earthquake ground shaking, such as duration, amplitude, and frequency, are important for how buildings respond.
3. A building's natural frequency determines how much it will vibrate in response to seismic waves - if the ground motion matches this frequency, resonance can amplify shaking and damage.
Krystal+ross
This document provides information about earthquakes including:
1) Earthquakes are caused by a sudden slip on a fault when stress overcomes friction, releasing energy as seismic waves.
2) The magnitude of an earthquake is measured on the Richter scale based on the amplitude of seismic waves.
3) The 2011 Tohoku earthquake in eastern Japan was magnitude 9.0 and caused tsunamis, damage to buildings/infrastructure, economic impacts, and loss of life.
Seismic waves.
This document discusses seismic waves and different types of seismic waves:
- Seismic waves are vibrations that travel through the Earth carrying energy from earthquakes. There are two main types - body waves and surface waves.
- Body waves include P-waves and S-waves. P-waves are fastest and cause a push/pull motion. S-waves are slower and cause side-to-side motion. They travel through the Earth's interior.
- Surface waves include Rayleigh and Love waves. Rayleigh waves cause up/down and side-to-side motions along the surface. Love waves cause only horizontal motions. They are constrained to the Earth's surface.
- Surface waves are responsible
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Waves
Waves are disturbances that transfer energy through a medium. They are caused by vibrations in the medium and can be transverse, longitudinal, or a combination. Key properties of waves include amplitude, wavelength, frequency, and speed. Waves interact with each other and surfaces through reflection, refraction, diffraction, interference, and can form standing waves through the combination of incoming and reflected waves.
Wave motion
Wave motion is the transfer of energy through a medium by vibration or oscillation of its particles. There are two types of waves: transverse waves, where particles vibrate perpendicular to the direction of energy transfer, and longitudinal waves, where particles vibrate parallel to the direction of transfer. Transverse waves occur in solids and liquids while longitudinal waves can occur in all media and involve changes in pressure.
Earthquakes
An earthquake is caused by the release of energy stored in rocks that are sliding past one another deep underground. When the rocks finally slip, they snap back into position, releasing this stored energy in the form of waves that travel outward in all directions through the earth. There are different types of earthquake waves that move the ground in various ways and travel at separate speeds, allowing scientists to determine the distance to the earthquake's origin. Earthquake waves can travel great distances depending on the magnitude of the quake, sometimes going around the entire planet multiple times for very large seismic events.
Learning objective 2
1) When two waves undergo destructive interference, their energy does not disappear but is instead transferred into potential energy in the form of pressure variations.
2) The total energy of two waves is equal to the sum of their individual energies. During destructive interference, the frequency and wavelength change in a way that maintains the total energy.
3) For sound waves, destructive interference results in a cancellation of pressure changes and velocities between the waves, rather than a loss of energy. The energy is contained as potential energy in the altered pressure field.
151207 tajikistan
A 7.2 magnitude earthquake occurred in a sparsely populated area of Tajikistan, approximately 349km east of the capital city of Dushanbe. The earthquake shook buildings in nearby countries but caused no reported injuries or damage. An estimated 5,000 people experienced strong ground shaking during the earthquake. The earthquake occurred as a result of strike-slip faulting within the crust of the Eurasian tectonic plate.
Presentation About Seismic Wave
1. Earthquakes generate seismic waves that travel through the earth's crust and cause the ground to shake when they reach the surface.
2. The characteristics of earthquake ground shaking, such as duration, amplitude, and frequency, are important for how buildings respond.
3. A building's natural frequency determines how much it will vibrate in response to seismic waves - if the ground motion matches this frequency, resonance can amplify shaking and damage.
Krystal+ross
This document provides information about earthquakes including:
1) Earthquakes are caused by a sudden slip on a fault when stress overcomes friction, releasing energy as seismic waves.
2) The magnitude of an earthquake is measured on the Richter scale based on the amplitude of seismic waves.
3) The 2011 Tohoku earthquake in eastern Japan was magnitude 9.0 and caused tsunamis, damage to buildings/infrastructure, economic impacts, and loss of life.
Seismic waves.
This document discusses seismic waves and different types of seismic waves:
- Seismic waves are vibrations that travel through the Earth carrying energy from earthquakes. There are two main types - body waves and surface waves.
- Body waves include P-waves and S-waves. P-waves are fastest and cause a push/pull motion. S-waves are slower and cause side-to-side motion. They travel through the Earth's interior.
- Surface waves include Rayleigh and Love waves. Rayleigh waves cause up/down and side-to-side motions along the surface. Love waves cause only horizontal motions. They are constrained to the Earth's surface.
- Surface waves are responsible
Seismic Waves
Seismic waves are waves that travel through the Earth due to earthquakes or explosions. There are three main types of seismic waves: P waves, which travel fastest; S waves, which travel slower than P waves; and surface waves, which are the slowest and cause the most damage. Seismographs can detect and measure seismic waves, recording the ground shaking on paper to indicate the strength of the waves.
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2. Tide Notes
Tides are long period waves in the oceans caused by the gravitational forces of the Sun and Moon. High tide occurs when the crest of the tidal wave reaches a location, while low tide is when the trough arrives. Flood tides bring water inland from the coasts at high tide, while ebb tides carry water back out to sea at low tide. The Moon has a stronger tidal influence than the Sun due to its closer proximity to Earth. This causes two high tides and two low tides each day as the Earth rotates through the tidal bulges created by the Moon's gravity.
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Gravity is a force that attracts objects toward each other. Isaac Newton mathematically described gravity and its universal effects in 1666. The heavier an object is and the closer it is to another object, the greater the gravitational force. Gravity keeps the atmosphere and objects on Earth's surface and causes orbits and cycles like tides. The moon's gravity pulls on Earth's oceans, creating high tides, but the sun's more distant gravity does not have as strong an effect.
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This document discusses different types of waves including mechanical/elastic waves, electromagnetic waves, transverse waves, and longitudinal waves. Mechanical waves require a medium and include sound and water waves, while electromagnetic waves can propagate through a vacuum such as radio waves. Transverse waves involve particles vibrating perpendicular to the propagation direction, while longitudinal waves involve particles vibrating parallel. Other topics covered include wavelength, amplitude, frequency, wave velocity, interference, stationary waves, beats, and simple harmonic motion.
Seismic waves
Seismic waves are energy propagated through the earth by earthquakes or artificial sources. There are two types of body waves (P and S waves) that travel through the earth and surface waves (Rayleigh and Love waves) that travel along the earth's surface. Seismic wave velocities depend on the elastic properties and density of the earth materials and are used to determine subsurface layering and structures. Analysis of travel times and slopes of seismic wave arrivals on record sections allows calculation of subsurface velocities and reflection/refraction of waves at interfaces between subsurface layers.
Seismic Waves
The document discusses different types of seismic waves that are produced during earthquakes. There are three main types of seismic waves: P-waves (primary waves), S-waves (secondary waves), and L-waves (surface waves). P-waves are the first to arrive after an earthquake as they travel fastest, pushing and pulling the ground. S-waves arrive next and cause side-to-side shaking. L-waves cause up and down motion and travel along the surface, causing the most damage. Seismographs are used to detect and measure the different seismic waves from an earthquake.
Seismic Waves
The document discusses different types of seismic waves that are produced during earthquakes. There are three main types of seismic waves: P-waves (primary waves), S-waves (secondary waves), and L-waves (surface waves). P-waves are the first to arrive after an earthquake as they travel fastest, pushing and pulling the ground. S-waves arrive next and cause side-to-side motions. L-waves cause up and down motions and travel along the surface, causing the most damage. The waves radiate out from the hypocenter, where the earthquake initiated underground.
Seismic waves
Deep underground, rocks are under constant pressure until the strain becomes too great and the rocks suddenly break, releasing seismic waves. These waves travel outward from the hypocenter in three types - P waves which push and pull, S waves which move sides to side, and L waves which cause surfaces to bob up and down. When recorded by a seismograph, the first indication of an earthquake is typically the P waves, followed by larger S waves, with surface L waves arriving last.
Earthquakes Notes
This document defines key terms related to earthquakes and seismic waves. It explains that earthquakes are caused by a sudden release of energy along fault lines in the earth. The focus is the location within the earth where the earthquake starts, while the epicenter is the point on the surface directly above the focus. There are three main types of seismic waves: P-waves which move in the direction of travel, S-waves which move sideways, and surface waves which cause the most damage. The timing and speed of P and S waves detected by seismic stations can be used to locate the epicenter of an earthquake.
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Waves transfer energy through matter or space without transferring matter. There are two main types of waves: mechanical waves, which require matter to transfer energy, and electromagnetic waves, which do not require matter. Mechanical waves can be transverse, where the matter moves perpendicular to the direction of energy transfer, or compressional, where the matter moves parallel to the direction of energy transfer. Sound waves are an example of compressional mechanical waves that transfer energy through the compression and rarefaction of matter like air molecules.
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Seismic waves
Seismic waves are energy transferred within the Earth's interior from one area to another. There are two main types of seismic waves: body waves, which can travel through the Earth's interior, and surface waves, which travel along the Earth's surface. Body waves include P-waves and S-waves, where P-waves are compressional and the fastest, and S-waves are slower shear waves. Surface waves include L-waves and Rayleigh waves, where L-waves move horizontally and Rayleigh waves move both vertically and horizontally in a rolling motion.
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This document provides an overview of key concepts related to waves and oscillation. It defines equilibrium as a physical state where opposing forces are balanced. Simple harmonic motion is described as periodic motion about a point of equilibrium. Oscillation is defined as a repetitive variation between two or more different states about equilibrium. Examples of oscillators and simple harmonic oscillators are given. The document then discusses three types of waves - mechanical, electromagnetic, and matter waves - and defines transverse and longitudinal waves. Key concepts such as force, friction, inertia, elasticity, amplitude, frequency, displacement, and compression are also defined.
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Seismic Waves
Seismic waves are waves of energy caused by the sudden breaking of rock within the Earth or explosions. There are two main types of seismic waves: body waves and surface waves. Body waves include P waves and S waves, which travel through the Earth's interior. Surface waves such as Love waves and Rayleigh waves travel along the Earth's surface and cause the most shaking during an earthquake. Seismic waves are recorded by seismographs and can provide information about the Earth's interior structure.
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2. Tide Notes
Tides are long period waves in the oceans caused by the gravitational forces of the Sun and Moon. High tide occurs when the crest of the tidal wave reaches a location, while low tide is when the trough arrives. Flood tides bring water inland from the coasts at high tide, while ebb tides carry water back out to sea at low tide. The Moon has a stronger tidal influence than the Sun due to its closer proximity to Earth. This causes two high tides and two low tides each day as the Earth rotates through the tidal bulges created by the Moon's gravity.
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An earthquake is caused by the sudden movement of parts of the Earth's crust and results in shaking and trembling of the ground. There are over one million earthquakes each year, with around twenty having the potential to cause severe damage. Earthquakes are caused by faults in the Earth's crust, such as the San Andreas Fault in California where the land west of the fault moves north and the land east moves south. Underwater earthquakes can generate destructive tsunamis. The focus is the depth below the surface where the earthquake occurs, and the epicenter is directly above on the surface. Seismographs detect seismic waves that travel out from the epicenter, including fast P waves and slower S waves.
Gravity
Gravity is a force that attracts objects toward each other. Isaac Newton mathematically described gravity and its universal effects in 1666. The heavier an object is and the closer it is to another object, the greater the gravitational force. Gravity keeps the atmosphere and objects on Earth's surface and causes orbits and cycles like tides. The moon's gravity pulls on Earth's oceans, creating high tides, but the sun's more distant gravity does not have as strong an effect.
Wave motion and its applications
This document discusses different types of waves including mechanical/elastic waves, electromagnetic waves, transverse waves, and longitudinal waves. Mechanical waves require a medium and include sound and water waves, while electromagnetic waves can propagate through a vacuum such as radio waves. Transverse waves involve particles vibrating perpendicular to the propagation direction, while longitudinal waves involve particles vibrating parallel. Other topics covered include wavelength, amplitude, frequency, wave velocity, interference, stationary waves, beats, and simple harmonic motion.
Seismic waves
Seismic waves are energy propagated through the earth by earthquakes or artificial sources. There are two types of body waves (P and S waves) that travel through the earth and surface waves (Rayleigh and Love waves) that travel along the earth's surface. Seismic wave velocities depend on the elastic properties and density of the earth materials and are used to determine subsurface layering and structures. Analysis of travel times and slopes of seismic wave arrivals on record sections allows calculation of subsurface velocities and reflection/refraction of waves at interfaces between subsurface layers.
Seismic Waves
The document discusses different types of seismic waves that are produced during earthquakes. There are three main types of seismic waves: P-waves (primary waves), S-waves (secondary waves), and L-waves (surface waves). P-waves are the first to arrive after an earthquake as they travel fastest, pushing and pulling the ground. S-waves arrive next and cause side-to-side shaking. L-waves cause up and down motion and travel along the surface, causing the most damage. Seismographs are used to detect and measure the different seismic waves from an earthquake.
Seismic Waves
The document discusses different types of seismic waves that are produced during earthquakes. There are three main types of seismic waves: P-waves (primary waves), S-waves (secondary waves), and L-waves (surface waves). P-waves are the first to arrive after an earthquake as they travel fastest, pushing and pulling the ground. S-waves arrive next and cause side-to-side motions. L-waves cause up and down motions and travel along the surface, causing the most damage. The waves radiate out from the hypocenter, where the earthquake initiated underground.
Seismic waves
Deep underground, rocks are under constant pressure until the strain becomes too great and the rocks suddenly break, releasing seismic waves. These waves travel outward from the hypocenter in three types - P waves which push and pull, S waves which move sides to side, and L waves which cause surfaces to bob up and down. When recorded by a seismograph, the first indication of an earthquake is typically the P waves, followed by larger S waves, with surface L waves arriving last.
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This document defines key terms related to earthquakes and seismic waves. It explains that earthquakes are caused by a sudden release of energy along fault lines in the earth. The focus is the location within the earth where the earthquake starts, while the epicenter is the point on the surface directly above the focus. There are three main types of seismic waves: P-waves which move in the direction of travel, S-waves which move sideways, and surface waves which cause the most damage. The timing and speed of P and S waves detected by seismic stations can be used to locate the epicenter of an earthquake.
Speeding Up
Speed is the rate of movement over a distance and can be measured using devices like a speedometer, speed trap gun, stopwatch, and light gates. Velocity includes both speed and direction of movement. Acceleration is the rate of change of velocity over time. Friction opposes the motion of objects in contact and can be reduced by lubricants or increased by pressing surfaces together more firmly. Forces like air resistance, water resistance, gravity, and balanced/unbalanced forces all affect an object's speed.
Waves!
Waves transfer energy through matter or space without transferring matter. There are two main types of waves: mechanical waves, which require matter to transfer energy, and electromagnetic waves, which do not require matter. Mechanical waves can be transverse, where the matter moves perpendicular to the direction of energy transfer, or compressional, where the matter moves parallel to the direction of energy transfer. Sound waves are an example of compressional mechanical waves that transfer energy through the compression and rarefaction of matter like air molecules.
Wave Actions
The document discusses different types of wave interactions including absorption, reflection, diffraction, refraction, and scattering. It provides examples of each type of interaction such as sound waves being absorbed by a pillow or light waves being reflected, refracted, and scattered in the atmosphere which causes the sky to appear blue and sunsets to have vibrant colors.
Earthquake
Earthquakes occur along fault lines in the earth's crust and cause shaking or sudden shocks of the earth's surface. They can be measured on the Richter scale, with those below 4.0 typically causing no damage and those over 5.0 capable of causing damage. Earthquake waves called seismic waves travel outward from the epicenter in three main types - P waves that travel fastest, S waves that are slower, and surface L waves that are slowest but can cause the most damage.
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Seismic waves are energy transferred within the Earth's interior from one area to another. There are two main types of seismic waves: body waves, which can travel through the Earth's interior, and surface waves, which travel along the Earth's surface. Body waves include P-waves and S-waves, where P-waves are compressional and the fastest, and S-waves are slower shear waves. Surface waves include L-waves and Rayleigh waves, where L-waves move horizontally and Rayleigh waves move both vertically and horizontally in a rolling motion.
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This document discusses the different types of crustal plate boundaries - convergent, divergent, and transform - and provides examples of each. Convergent boundaries involve plates moving toward each other and can be continental-continental, oceanic-continental, or oceanic-oceanic, resulting in mountains, trenches and volcanoes, or tsunamis respectively. Transform boundaries involve plates sliding past each other, causing earthquakes. Divergent boundaries involve plates moving away from each other at mid-ocean ridges or continental rift valleys.
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This document provides an overview of key concepts related to waves and oscillation. It defines equilibrium as a physical state where opposing forces are balanced. Simple harmonic motion is described as periodic motion about a point of equilibrium. Oscillation is defined as a repetitive variation between two or more different states about equilibrium. Examples of oscillators and simple harmonic oscillators are given. The document then discusses three types of waves - mechanical, electromagnetic, and matter waves - and defines transverse and longitudinal waves. Key concepts such as force, friction, inertia, elasticity, amplitude, frequency, displacement, and compression are also defined.
What is seismology and what are seismic waves
Seismology is the study of earthquakes and seismic waves that move through the earth. There are two main types of seismic waves - body waves and surface waves. Body waves can travel through the earth's interior layers, while surface waves move along the surface. The two main types of body waves are P waves and S waves. P waves are compressional waves that move through solid rock and fluids, while S waves move rock particles side to side and only travel through solid rock. The two main types of surface waves are Love waves and Rayleigh waves. Love waves move the ground side to side, while Rayleigh waves roll along the surface and move the ground up and down and side to side.
Seismic Waves
Seismic waves are waves of energy caused by the sudden breaking of rock within the Earth or explosions. There are two main types of seismic waves: body waves and surface waves. Body waves include P waves and S waves, which travel through the Earth's interior. Surface waves such as Love waves and Rayleigh waves travel along the Earth's surface and cause the most shaking during an earthquake. Seismic waves are recorded by seismographs and can provide information about the Earth's interior structure.
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