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DESCRIBING AND RELATING THE DISTRIBUTION OF ACTIVE VOLCANOES, EARTHQUAKE EPICENTERS, AND LET US STUDY MAJOR MOUNTAIN BELTS TO PLATE TECTONIC THEORY An earthquake is a vibration of the Earth produced by the rapic release of energy most often because of the slippage along a fault in the Earth's crust. This energy radiates in all directions from the focus in the form of waves called seismic waves, which are recorded in seismographs The two main types of seismic waves are body waves and surface waves. LET US KNOW Earthquakes occur when elastic energy is accumulated slowly within the Earth's crust as a result of plate motions and then released suddenly at fractures in the crust called faults. The released energy travels in the form of waves called seismic waves. It is the released energy that puts human beings and human structures in danger. Therefore, it is critical to understand where this energy is released and in what form. Love wave This worksheet contains activities that will describe different types of seismic waves based on where and how the waves move. It will help you understand how these waves provide us with information about the relationship between seismic zones and plate tectonics. Make sure to follow the directions stated in each part of the activity and answer all questions the best that you can. Rayleigh wave Figure 1. Sut Waves LET US REVIEW Surface waves can only travel through the surface of the Earth. They arrive after the main P and S waves and are confined to the outer layers o the Earth. There are two types of surface waves: the Love waves and the Rayleigh waves. Love wave is named after A.E.H. Love, a British mathematician who worked out the mathematical model for this kind o Direction: Write "Ocean" if the phrase describes oceanic crust and "Continent" if it describes continental crust. wave in 1911. It is faster than Rayleigh wave and it moves the ground in a side-to-side horizontal motion, like that of a snake's causing the ground to twist. This is why Love waves cause the most damage to structures during an earthquake. The other kind of surface wave is the Rayleigh wave. It was named after John William Strutt, Lord Rayleigh, who mathematically predicted the existence of this kind of wave in 1885. A Rayleigh wave rolls along the 1. Less dense but thicker 2. Thinner but denser 3. Composed mainly of granite 4. Composed mainly of basalt and gabbro 5. Mainly formed at constructive margins

DESCRIBING AND RELATING THE DISTRIBUTION OF ACTIVE VOLCANOES, EARTHQUAKE EPICENTERS, AND LET US STUDY MAJOR MOUNTAIN BELTS TO PLATE TECTONIC THEORY An earthquake is a vibration of the Earth produced by the rapic release of energy most often because of the slippage along a fault in the Earth's crust. This energy radiates in all directions from the focus in the form of waves called seismic waves, which are recorded in seismographs The two main types of seismic waves are body waves and surface waves. LET US KNOW Earthquakes occur when elastic energy is accumulated slowly within the Earth's crust as a result of plate motions and then released suddenly at fractures in the crust called faults. The released energy travels in the form of waves called seismic waves. It is the released energy that puts human beings and human structures in danger. Therefore, it is critical to understand where this energy is released and in what form. Love wave This worksheet contains activities that will describe different types of seismic waves based on where and how the waves move. It will help you understand how these waves provide us with information about the relationship between seismic zones and plate tectonics. Make sure to follow the directions stated in each part of the activity and answer all questions the best that you can. Rayleigh wave Figure 1. Sut Waves LET US REVIEW Surface waves can only travel through the surface of the Earth. They arrive after the main P and S waves and are confined to the outer layers o the Earth. There are two types of surface waves: the Love waves and the Rayleigh waves. Love wave is named after A.E.H. Love, a British mathematician who worked out the mathematical model for this kind o Direction: Write "Ocean" if the phrase describes oceanic crust and "Continent" if it describes continental crust. wave in 1911. It is faster than Rayleigh wave and it moves the ground in a side-to-side horizontal motion, like that of a snake's causing the ground to twist. This is why Love waves cause the most damage to structures during an earthquake. The other kind of surface wave is the Rayleigh wave. It was named after John William Strutt, Lord Rayleigh, who mathematically predicted the existence of this kind of wave in 1885. A Rayleigh wave rolls along the 1. Less dense but thicker 2. Thinner but denser 3. Composed mainly of granite 4. Composed mainly of basalt and gabbro 5. Mainly formed at constructive margins

Applications and Investigations in Earth Science (9th Edition)
Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
Section: Chapter Questions
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DESCRIBING AND RELATING THE DISTRIBUTION OF ACTIVE VOLCANOES, EARTHQUAKE EPICENTERS, AND LET US STUDY MAJOR MOUNTAIN BELTS TO PLATE TECTONIC THEORY An earthquake is a vibration of the Earth produced by the rapid release of energy most often because of the slippage along a fault in the Earth's crust. This energy radiates in all directions from the focus in the form of waves called seismic waves, which are recorded in seismographs. The two main types of seismic waves are body waves and surface waves. LET US KNOW Earthquakes occur when elastic energy is accumulated slowly within the Earth's crust as a result of plate motions and then released suddenly at fractures in the crust called faults. The released energy travels in the form of waves called seismic waves. It is the released energy that puts human beings and human structures in danger. Therefore, it is Love wave critical to understand where this energy is released and in what form. This worksheet contains activities that will describe different types wave drecien of seismic waves based on where and how the waves move. It will help you understand how these waves provide us with information about the relationship between seismic zones and plate tectonics. Make sure to follow the directions stated in each part of the activity and answer al1 questions the best that you can. Rayleigh wave Figure 1. Surface Waves LET US REVIEW Surface waves can only travel through the surface of the Earth. They arrive after the main P and S waves and are confined to the outer layers of the Earth. There are two types of surface waves: the Love waves and the Rayleigh waves. Love wave is named after A.E.H. Love, a British Direction: Write "Ocean" if the phrase describes oceanic crust and "Continent" if it describes continental crust. mathematician who worked out the mathematical model for this kind of wave in 1911. It is faster than Rayleigh wave and it moves the ground in a side-to-side horizontal motion, like that of a snake's causing the ground to twist. This is why Love waves cause the most damage to structures during an earthquake. 1. Less dense but thicker 2. Thinner but denser 3. Composed mainly of granite 4. Composed mainly of basalt and gabbro 5. Mainly formed at constructive margins The other kind of surface wave is the Rayleigh wave. It was named after John William Strutt, Lord Rayleigh, who mathematically predicted the existence of this kind of wave in 1885. A Rayleigh wave rolls along the 11 12
Transcribed Image Text:DESCRIBING AND RELATING THE DISTRIBUTION OF ACTIVE VOLCANOES, EARTHQUAKE EPICENTERS, AND LET US STUDY MAJOR MOUNTAIN BELTS TO PLATE TECTONIC THEORY An earthquake is a vibration of the Earth produced by the rapid release of energy most often because of the slippage along a fault in the Earth's crust. This energy radiates in all directions from the focus in the form of waves called seismic waves, which are recorded in seismographs. The two main types of seismic waves are body waves and surface waves. LET US KNOW Earthquakes occur when elastic energy is accumulated slowly within the Earth's crust as a result of plate motions and then released suddenly at fractures in the crust called faults. The released energy travels in the form of waves called seismic waves. It is the released energy that puts human beings and human structures in danger. Therefore, it is Love wave critical to understand where this energy is released and in what form. This worksheet contains activities that will describe different types wave drecien of seismic waves based on where and how the waves move. It will help you understand how these waves provide us with information about the relationship between seismic zones and plate tectonics. Make sure to follow the directions stated in each part of the activity and answer al1 questions the best that you can. Rayleigh wave Figure 1. Surface Waves LET US REVIEW Surface waves can only travel through the surface of the Earth. They arrive after the main P and S waves and are confined to the outer layers of the Earth. There are two types of surface waves: the Love waves and the Rayleigh waves. Love wave is named after A.E.H. Love, a British Direction: Write "Ocean" if the phrase describes oceanic crust and "Continent" if it describes continental crust. mathematician who worked out the mathematical model for this kind of wave in 1911. It is faster than Rayleigh wave and it moves the ground in a side-to-side horizontal motion, like that of a snake's causing the ground to twist. This is why Love waves cause the most damage to structures during an earthquake. 1. Less dense but thicker 2. Thinner but denser 3. Composed mainly of granite 4. Composed mainly of basalt and gabbro 5. Mainly formed at constructive margins The other kind of surface wave is the Rayleigh wave. It was named after John William Strutt, Lord Rayleigh, who mathematically predicted the existence of this kind of wave in 1885. A Rayleigh wave rolls along the 11 12
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