The topic of plate tectonics is largely based on Alfred Wegner's theory of continental drift, which became accepted with the discovery of seafloor spreading in the Atlantic Ocean, and after fossil, flora, and geological studies in Africa and South America. In this lesson, students will learn about Earth’s structure, differences between various types of tectonic plate boundaries, their outcomes, and their connection to locations of volcanoes and earthquake activity.
This virtual fieldwork experience is written so that students can "go" to a copper mine and examine the geology, biology, etc. The owner of the mine may be contacted to purchase rock samples in order to make it even more interactive.
Plate tectonics is the theory that the Earth's outermost shell is divided into plates that constantly move and interact with one another. At plate boundaries, where the plates meet, seismic activity like earthquakes and volcanic eruptions occur. The three main types of plate boundaries are divergent boundaries, where plates move apart; convergent boundaries, where plates collide; and transform boundaries, where plates slide past one another. Each boundary type results in different geological features and phenomena.
This tacklesabout locating epicenter,3 typesof plate boundaries hotspot.
A ppt presentation for module 1 in 1st quarter in grade 10sciencein the Philippines.
Feel free tomessage mefor any corrections/suggestions forimprovement.
Plate tectonics is the theory that the Earth's outermost shell is divided into plates that constantly move and interact with one another. Earthquakes, volcanoes, and mountain ranges occur primarily at plate boundaries. There are three main types of plate boundaries: divergent boundaries where plates move apart, convergent boundaries where plates move together, and transform boundaries where plates slide past one another. Each boundary type results in different geological effects depending on whether oceanic or continental crust is involved in the plate interaction.
The document discusses plate tectonics and how it shapes Earth. Plate tectonics involves large plates in Earth's lithosphere that slowly move over time. When plates meet, they form boundaries which can result in volcanoes and earthquakes. Convection currents in the mantle drive the plate movements. Plates diverge at mid-ocean ridges, where new crust is formed, and converge in some places, causing volcanoes or mountains to form.
The topic of plate tectonics is largely based on Alfred Wegner's theory of continental drift, which became accepted with the discovery of seafloor spreading in the Atlantic Ocean, and after fossil, flora, and geological studies in Africa and South America. In this lesson, students will learn about Earth’s structure, differences between various types of tectonic plate boundaries, their outcomes, and their connection to locations of volcanoes and earthquake activity.
This virtual fieldwork experience is written so that students can "go" to a copper mine and examine the geology, biology, etc. The owner of the mine may be contacted to purchase rock samples in order to make it even more interactive.
Plate tectonics is the theory that the Earth's outermost shell is divided into plates that constantly move and interact with one another. At plate boundaries, where the plates meet, seismic activity like earthquakes and volcanic eruptions occur. The three main types of plate boundaries are divergent boundaries, where plates move apart; convergent boundaries, where plates collide; and transform boundaries, where plates slide past one another. Each boundary type results in different geological features and phenomena.
This tacklesabout locating epicenter,3 typesof plate boundaries hotspot.
A ppt presentation for module 1 in 1st quarter in grade 10sciencein the Philippines.
Feel free tomessage mefor any corrections/suggestions forimprovement.
Plate tectonics is the theory that the Earth's outermost shell is divided into plates that constantly move and interact with one another. Earthquakes, volcanoes, and mountain ranges occur primarily at plate boundaries. There are three main types of plate boundaries: divergent boundaries where plates move apart, convergent boundaries where plates move together, and transform boundaries where plates slide past one another. Each boundary type results in different geological effects depending on whether oceanic or continental crust is involved in the plate interaction.
The document discusses plate tectonics and how it shapes Earth. Plate tectonics involves large plates in Earth's lithosphere that slowly move over time. When plates meet, they form boundaries which can result in volcanoes and earthquakes. Convection currents in the mantle drive the plate movements. Plates diverge at mid-ocean ridges, where new crust is formed, and converge in some places, causing volcanoes or mountains to form.
A report about earthquakes. Inside this powerpoint are: the meaning of earthquakes, types of plate movement, and how does an earthquake occur. Have Fun!
Continental drift is the hypothesis that the Earth's continents have moved over geologic time relative to each other. Plate tectonics studies the movement of continents on tectonic plates. There are three main types of tectonic plate boundaries: subduction zones where plates converge, divergent margins where plates spread apart, and transform margins where plates slide past each other. Seafloor spreading occurs at divergent boundaries as heat from the Earth's mantle causes the seafloor crust to crack and new crust is formed, pushing the plates apart over millions of years. The 2004 Sumatra-Andaman earthquake, measured at over 9.0 on the Richter scale, was caused by movement along the Sumatra fault line and
Earth is the third planet from the sun, formed 4.54 billion years ago. It rotates on its axis 366.26 times per year while orbiting the sun, creating seasons and years. The moon stabilizes Earth's axis and causes ocean tides. Earth's surface is divided into tectonic plates that migrate over millions of years. 71% is water and 29% is land with rivers and lakes. The interior remains active with a molten core generating a magnetic field and mantle driving plate tectonics. Earth system science considers interactions between the atmosphere, hydrosphere, cryosphere, geosphere, biosphere, and magnetosphere and human impacts on these. Climate change and the carbon cycle are central to
The document discusses plate tectonics and how it shapes the Earth's surface. It explains that plate tectonics involves several large plates and smaller plates that make up the Earth's outer shell. These plates are constantly and very slowly moving in relation to each other, either pulling apart, crashing together, or sliding past one another. The movement of these plates through processes like rifting, earthquakes, and volcanic activity is what creates and alters the Earth's landforms and features over long periods of time.
Geology is the scientific study of the all constituents of planets, their internal and external forms and processes. More precisely, it is the study of nature, structure and history of the planet. Earth is the home to all life, well known to the humankind. Geology, itself, is a major part of The Earth and atmospheric sciences, which were born as twins . The subject of geology encompasses all aspects including the composition, structure, physical properties, and history of a planets'( like Earth's) inter-related components and the processes that are shaping the features on the surface. Geologists are the scientists who study the origin, occurrence, distribution and utilities of all materials(metallic, non-metallic, inorganic, etc), minerals, rocks, sediments, soils, water, oil and all other inorganic natural resources. It is a very vast subject covering a wide spectrum of scientific principles and holding hundred and fifty plus scientific branches. This report enumerates and highlights most of them, in a nutshell, for all those who intends to know for planning their career path.
Plate tectonics is a scientific theory that describes the large-scale motions of tectonic plates on Earth's surface. The lithosphere is broken into these plates which move at rates of up to 100 mm per year. Where the plates meet, their relative motion determines the type of boundary which can result in earthquakes, volcanoes, or mountain building. The theory proposes that Earth's eight major plates and several minor plates fit together like puzzle pieces and their movements over millions of years have resulted in changing ocean and continent configurations.
Describing earthquakes more in detail about what, how, why, when and from whom are these caused, affected and what makes it so important to study this in current spatial and geographical scenario taking in mind the historical events.
unraveling the secrets of plate tectonics.pptxShubash Sah
Plate tectonics is the scientific theory that explains the movement and interaction of Earth's lithospheric plates, which are large slabs of the planet's crust and upper mantle. This theory has revolutionized our understanding of geological processes, including the formation of mountains, earthquakes, and volcanic activity. Here's an overview of the key aspects and developments in the field of plate tectonics:
Historical Background
Continental Drift Theory:
Proposed by Alfred Wegener in 1912, the idea suggested that continents were once connected in a supercontinent called Pangaea and have since drifted apart.
Wegener's theory was based on the fit of the continents, fossil correlations, and geological similarities across continents.
Development of Plate Tectonics:
In the mid-20th century, technological advances such as seafloor mapping and the study of magnetic anomalies led to the formulation of the plate tectonics theory.
The discovery of mid-ocean ridges and the symmetrical patterns of magnetic stripes on the ocean floor provided evidence for seafloor spreading.
Structure and Movement of Plates
Lithospheric Plates:
Earth's lithosphere is divided into several major and minor plates, including the Pacific, North American, Eurasian, and African plates.
These plates float on the semi-fluid asthenosphere beneath them.
Plate Boundaries:
Divergent Boundaries: Plates move apart, forming new crust, as seen at mid-ocean ridges.
Convergent Boundaries: Plates collide, leading to subduction (one plate sinking beneath another) or mountain building.
Transform Boundaries: Plates slide past each other, causing earthquakes.
Mechanisms of Plate Movement
Mantle Convection:
Heat from Earth's interior causes the mantle to convect, driving the movement of plates.
Hot material rises at mid-ocean ridges, cools, and then sinks at subduction zones.
Ridge Push and Slab Pull:
Ridge Push: Elevated mid-ocean ridges push plates away due to gravity.
Slab Pull: The weight of a subducting plate pulls the rest of the plate along.
Geological Implications
Mountain Building:
At convergent boundaries, the collision of continental plates can create mountain ranges, such as the Himalayas.
Oceanic-continental convergence leads to volcanic mountain ranges.
Earthquakes and Volcanoes:
Most earthquakes occur along plate boundaries due to the release of stress accumulated from plate movements.
Volcanic activity is prominent at divergent and convergent boundaries and hotspots.
Ocean Basin Formation:
Divergent boundaries lead to the creation of new oceanic crust, expanding ocean basins over time.
Recent Advances and Research
GPS and Satellite Technology:
Modern GPS technology allows precise measurement of plate movements, enhancing our understanding of tectonic processes.
Seismic Tomography:
This technique provides images of the Earth's interior, revealing details about mantle convection and plate interactions.
Computer Modeling:
Advanced simulations help scientists predict plate
Geomorphology is the study of landforms and the processes that shape the Earth's surface. Some key concepts in geomorphology include:
- The present is key to understanding the past, as the same surface processes have operated over geologic time.
- Geological structure influences landform evolution and is reflected in landforms.
- Geomorphic processes each develop characteristic landforms.
- Landforms evolve in an orderly sequence as erosional processes act over time.
- Geomorphic systems dominate large areas and landscapes can be summarized in physiographic maps.
The document discusses plate tectonics and earthquakes. It describes how the Earth's crust is broken into tectonic plates that move slowly over time, interacting at their boundaries in ways that cause earthquakes and volcanic activity. During an earthquake, seismic waves travel outward from the epicenter, including P waves, S waves, and surface waves. Seismographs are used to detect and measure these waves to determine the location and magnitude of earthquakes.
This document discusses the theory of continental drift and plate tectonics. It explains that continental drift is the movement of continents across Earth's surface over geologic time. The theory was first proposed in the early 20th century by Alfred Wegener and helped explain the formation of supercontinents like Pangaea and the matching of continental margins. It also introduced the concept of plates and how their movement causes geologic phenomena like earthquakes and volcanoes.
Page 313 13.1 InTroduCTIonIt was the deadliest day in .docxgerardkortney
Page | 313
13.1 InTroduCTIon
It was the deadliest day in the
history of Mt. Everest. On April
25, 2015, a 7.8 magnitude earth-
quake hit Nepal. This triggered
an avalanche that killed 19 climb-
ers on Mt. Everest. In Nepal, over
8,800 people died, and many more
were injured and made homeless.
Hundreds of aftershocks (smaller
earthquakes that follow a larger
earthquake) have occurred since
(Figure 13.1).
Earthquakes are not new to this
region. A similar death toll was ex-
perienced in a 1934 earthquake, and
many other smaller earthquakes
have occurred within historical
times. An 1833 quake of similar
magnitude resulted in less than 500
deaths, though this was most likely due to two very large foreshocks (smaller earth-
quakes that precede the main earthquake) that sent most residents out of doors in
alarm, which was safer for them. Worldwide, there have been much deadlier and
stronger earthquakes just in this century (Haiti, 2010 – 316,000 dead; Sumatra,
2004 – 227,000 dead, both with deaths related to ground shaking and the other
hazards that were created by the earthquake). Earthquakes give geologists valuable
information about the Earth, both the interior, as we learned about in the Earth’s In-
terior chapter, and about conditions at the Earth’s surface (most earthquakes occur
at plate boundaries, as we learned in the Plate Tectonics chapter, Figure 4.8).
figure 13.1 | A map of the main earthquake to hit Nepal
on April 25, 2015, along with a major aftershock on May 12,
and numerous (>100) other aftershocks (in red – note the
magnitude scale in the upper right).
Author: USGS
Source: USGS
License: Public Domain
13 earthquakesRanda Harris
Page | 314
Introductory GeoloGy earthquakes
13.1.1 learning outcomes
After completing this chapter, you should be able to:
• Compare and contrast the different types of seismic waves
• Understand the different scales used to measure earthquakes, and
apply them to the amount of devastation
• Understand how different geologic materials behave during an
earthquake, and the resulting impact on structures
• Explain how an earthquake epicenter is located
• Explore the relationship between the fracking industry and seismicity
13.1.2 Key Terms
13.2 The ePICenTer, foCus, and waves
An earthquake is a like a telegram from the Earth. It sends a message about the
conditions beneath the Earth’s surface. The shaking or trembling experienced
during an earthquake is the result of a rapid
release of energy within the Earth, usually
as a result of movement along geologic
faults. Think back to the strike-slip fault
from the Crustal Deformation chapter.
Rocks on either side of the fault are sliding
past each other. As they move in opposite
directions, the rocks become deformed, as
they will bend slightly and build up pres-
sure. Eventually they will reach a breaking
point. Once the strength of the rock has
been exceeded, the rocks will snap back to
their normal shape, rel.
1. Earthquakes occur along faults in the Earth's crust due to the buildup and sudden release of strain energy from tectonic plate movement.
2. Seismic waves generated by earthquakes travel through the Earth and are used to determine the internal structure, including distinct layers of the crust, mantle, and core.
3. The core is determined to be liquid based on seismic evidence showing the disappearance of different wave types in certain regions.
This document provides an introduction to the field of geoscience/geology. It discusses key topics like the formation of rocks through igneous, sedimentary, and metamorphic processes. It also covers plate tectonics theory and how the motion of tectonic plates generates earthquakes. The objectives of the course are to understand rock and mineral formation, Earth's structure and composition, sea floor spreading via plate tectonics, landforms, and natural hazards like earthquakes.
The earth is more than 4.5 billion years old! During this unimaginable expanse of time, our planet has undergone drastic changes. For the earliest part of earth’s history, the planet was a molten inferno. As the planet slowly cooled, rocks and minerals began to form, and continents and ocean basins took shape. Earth’s continents today look nothing like they did hundreds of millions of years ago. In fact, the continents move around through a process called plate tectonics.
The Theory of Plat Tectonics is relatively modern and is very different from historic thought, which included ideas ranging from shrinking earth to continents moving across the ocean floor. Fossil evidence paired with lithographic correlation helped solidify the concept of plate tectonics to the theory we know today.
Earth Science is a major Subject of life. Earth Science encompasses hundreds of branches. Geology is the scientific study of the all constituents of planets, their internal and external forms and processes. More precisely, it is the study of nature, structure and history of the planet. Earth is the home to all life, well known to the humankind. Geology, itself, is a major part of The Earth and atmospheric sciences, which were born as twins . The subject of geology encompasses all aspects including the composition, structure, physical properties, and history of a planets'( like Earth's) inter-related components and the processes that are shaping the features on the surface.
Contents:
>Introduction to Earthquake.
>Causes of Earthquake.
>How the Ground shakes?
>Effects of Earthquake on Structures.
>Examples.
>Relationship & world wide distribution of earthquake and volcanoes.
>Earthquake and Bangladesh.
The document discusses the theory of plate tectonics, which proposes that Earth's outer shell is broken into plates that move over time. As the plates move, they will converge and collide, causing volcanic activity and mountain building, or pull apart, creating ocean floors and divergent boundaries. The types of landforms that form depend on whether the colliding plates are oceanic or continental. Plate tectonics explains how forces inside Earth shape its surface features and drive continental drift over hundreds of millions of years.
Venus and Earth have remarkably diferent
surface conditions, yet the lithospheric
thickness and heat fow on Venus may be
Earth-like. This fnding supports a tectonic
regime with limited surface mobility and
dominated by intrusive magmatism.
This document discusses several topics related to earthquakes and earthquake engineering:
- Earthquakes are caused by the sudden movement of tectonic plates along fault lines in the earth's crust.
- The interior structure of the earth is layered, with a solid crust, highly viscous mantle, liquid outer core, and solid inner core.
- Earthquake ground motions can be amplified by local surface geology and sediment thickness, influencing seismic damage. Proper understanding of ground conditions is important for hazard assessment and mitigation.
The document discusses several prominent composers from the Romantic period, including Niccolò Paganini, who became a famous violin virtuoso and inspired other composers. Franz Liszt was known as one of the most virtuosic pianists of the era, performing widely in Vienna and Paris. Hector Berlioz composed the Symphonie Fantastique, showcasing his innovative use of tone color and orchestration.
This document discusses properties of gases and how mass, volume, temperature, and pressure are related for gases. It provides information on gas laws including Boyle's law, Charles' law, Gay-Lussac's law, combined gas law, Avogadro's principle, ideal gas law, Dalton's law, and Graham's law. Equations for each gas law are given and example problems are worked through applying the various gas laws.
A report about earthquakes. Inside this powerpoint are: the meaning of earthquakes, types of plate movement, and how does an earthquake occur. Have Fun!
Continental drift is the hypothesis that the Earth's continents have moved over geologic time relative to each other. Plate tectonics studies the movement of continents on tectonic plates. There are three main types of tectonic plate boundaries: subduction zones where plates converge, divergent margins where plates spread apart, and transform margins where plates slide past each other. Seafloor spreading occurs at divergent boundaries as heat from the Earth's mantle causes the seafloor crust to crack and new crust is formed, pushing the plates apart over millions of years. The 2004 Sumatra-Andaman earthquake, measured at over 9.0 on the Richter scale, was caused by movement along the Sumatra fault line and
Earth is the third planet from the sun, formed 4.54 billion years ago. It rotates on its axis 366.26 times per year while orbiting the sun, creating seasons and years. The moon stabilizes Earth's axis and causes ocean tides. Earth's surface is divided into tectonic plates that migrate over millions of years. 71% is water and 29% is land with rivers and lakes. The interior remains active with a molten core generating a magnetic field and mantle driving plate tectonics. Earth system science considers interactions between the atmosphere, hydrosphere, cryosphere, geosphere, biosphere, and magnetosphere and human impacts on these. Climate change and the carbon cycle are central to
The document discusses plate tectonics and how it shapes the Earth's surface. It explains that plate tectonics involves several large plates and smaller plates that make up the Earth's outer shell. These plates are constantly and very slowly moving in relation to each other, either pulling apart, crashing together, or sliding past one another. The movement of these plates through processes like rifting, earthquakes, and volcanic activity is what creates and alters the Earth's landforms and features over long periods of time.
Geology is the scientific study of the all constituents of planets, their internal and external forms and processes. More precisely, it is the study of nature, structure and history of the planet. Earth is the home to all life, well known to the humankind. Geology, itself, is a major part of The Earth and atmospheric sciences, which were born as twins . The subject of geology encompasses all aspects including the composition, structure, physical properties, and history of a planets'( like Earth's) inter-related components and the processes that are shaping the features on the surface. Geologists are the scientists who study the origin, occurrence, distribution and utilities of all materials(metallic, non-metallic, inorganic, etc), minerals, rocks, sediments, soils, water, oil and all other inorganic natural resources. It is a very vast subject covering a wide spectrum of scientific principles and holding hundred and fifty plus scientific branches. This report enumerates and highlights most of them, in a nutshell, for all those who intends to know for planning their career path.
Plate tectonics is a scientific theory that describes the large-scale motions of tectonic plates on Earth's surface. The lithosphere is broken into these plates which move at rates of up to 100 mm per year. Where the plates meet, their relative motion determines the type of boundary which can result in earthquakes, volcanoes, or mountain building. The theory proposes that Earth's eight major plates and several minor plates fit together like puzzle pieces and their movements over millions of years have resulted in changing ocean and continent configurations.
Describing earthquakes more in detail about what, how, why, when and from whom are these caused, affected and what makes it so important to study this in current spatial and geographical scenario taking in mind the historical events.
unraveling the secrets of plate tectonics.pptxShubash Sah
Plate tectonics is the scientific theory that explains the movement and interaction of Earth's lithospheric plates, which are large slabs of the planet's crust and upper mantle. This theory has revolutionized our understanding of geological processes, including the formation of mountains, earthquakes, and volcanic activity. Here's an overview of the key aspects and developments in the field of plate tectonics:
Historical Background
Continental Drift Theory:
Proposed by Alfred Wegener in 1912, the idea suggested that continents were once connected in a supercontinent called Pangaea and have since drifted apart.
Wegener's theory was based on the fit of the continents, fossil correlations, and geological similarities across continents.
Development of Plate Tectonics:
In the mid-20th century, technological advances such as seafloor mapping and the study of magnetic anomalies led to the formulation of the plate tectonics theory.
The discovery of mid-ocean ridges and the symmetrical patterns of magnetic stripes on the ocean floor provided evidence for seafloor spreading.
Structure and Movement of Plates
Lithospheric Plates:
Earth's lithosphere is divided into several major and minor plates, including the Pacific, North American, Eurasian, and African plates.
These plates float on the semi-fluid asthenosphere beneath them.
Plate Boundaries:
Divergent Boundaries: Plates move apart, forming new crust, as seen at mid-ocean ridges.
Convergent Boundaries: Plates collide, leading to subduction (one plate sinking beneath another) or mountain building.
Transform Boundaries: Plates slide past each other, causing earthquakes.
Mechanisms of Plate Movement
Mantle Convection:
Heat from Earth's interior causes the mantle to convect, driving the movement of plates.
Hot material rises at mid-ocean ridges, cools, and then sinks at subduction zones.
Ridge Push and Slab Pull:
Ridge Push: Elevated mid-ocean ridges push plates away due to gravity.
Slab Pull: The weight of a subducting plate pulls the rest of the plate along.
Geological Implications
Mountain Building:
At convergent boundaries, the collision of continental plates can create mountain ranges, such as the Himalayas.
Oceanic-continental convergence leads to volcanic mountain ranges.
Earthquakes and Volcanoes:
Most earthquakes occur along plate boundaries due to the release of stress accumulated from plate movements.
Volcanic activity is prominent at divergent and convergent boundaries and hotspots.
Ocean Basin Formation:
Divergent boundaries lead to the creation of new oceanic crust, expanding ocean basins over time.
Recent Advances and Research
GPS and Satellite Technology:
Modern GPS technology allows precise measurement of plate movements, enhancing our understanding of tectonic processes.
Seismic Tomography:
This technique provides images of the Earth's interior, revealing details about mantle convection and plate interactions.
Computer Modeling:
Advanced simulations help scientists predict plate
Geomorphology is the study of landforms and the processes that shape the Earth's surface. Some key concepts in geomorphology include:
- The present is key to understanding the past, as the same surface processes have operated over geologic time.
- Geological structure influences landform evolution and is reflected in landforms.
- Geomorphic processes each develop characteristic landforms.
- Landforms evolve in an orderly sequence as erosional processes act over time.
- Geomorphic systems dominate large areas and landscapes can be summarized in physiographic maps.
The document discusses plate tectonics and earthquakes. It describes how the Earth's crust is broken into tectonic plates that move slowly over time, interacting at their boundaries in ways that cause earthquakes and volcanic activity. During an earthquake, seismic waves travel outward from the epicenter, including P waves, S waves, and surface waves. Seismographs are used to detect and measure these waves to determine the location and magnitude of earthquakes.
This document discusses the theory of continental drift and plate tectonics. It explains that continental drift is the movement of continents across Earth's surface over geologic time. The theory was first proposed in the early 20th century by Alfred Wegener and helped explain the formation of supercontinents like Pangaea and the matching of continental margins. It also introduced the concept of plates and how their movement causes geologic phenomena like earthquakes and volcanoes.
Page 313 13.1 InTroduCTIonIt was the deadliest day in .docxgerardkortney
Page | 313
13.1 InTroduCTIon
It was the deadliest day in the
history of Mt. Everest. On April
25, 2015, a 7.8 magnitude earth-
quake hit Nepal. This triggered
an avalanche that killed 19 climb-
ers on Mt. Everest. In Nepal, over
8,800 people died, and many more
were injured and made homeless.
Hundreds of aftershocks (smaller
earthquakes that follow a larger
earthquake) have occurred since
(Figure 13.1).
Earthquakes are not new to this
region. A similar death toll was ex-
perienced in a 1934 earthquake, and
many other smaller earthquakes
have occurred within historical
times. An 1833 quake of similar
magnitude resulted in less than 500
deaths, though this was most likely due to two very large foreshocks (smaller earth-
quakes that precede the main earthquake) that sent most residents out of doors in
alarm, which was safer for them. Worldwide, there have been much deadlier and
stronger earthquakes just in this century (Haiti, 2010 – 316,000 dead; Sumatra,
2004 – 227,000 dead, both with deaths related to ground shaking and the other
hazards that were created by the earthquake). Earthquakes give geologists valuable
information about the Earth, both the interior, as we learned about in the Earth’s In-
terior chapter, and about conditions at the Earth’s surface (most earthquakes occur
at plate boundaries, as we learned in the Plate Tectonics chapter, Figure 4.8).
figure 13.1 | A map of the main earthquake to hit Nepal
on April 25, 2015, along with a major aftershock on May 12,
and numerous (>100) other aftershocks (in red – note the
magnitude scale in the upper right).
Author: USGS
Source: USGS
License: Public Domain
13 earthquakesRanda Harris
Page | 314
Introductory GeoloGy earthquakes
13.1.1 learning outcomes
After completing this chapter, you should be able to:
• Compare and contrast the different types of seismic waves
• Understand the different scales used to measure earthquakes, and
apply them to the amount of devastation
• Understand how different geologic materials behave during an
earthquake, and the resulting impact on structures
• Explain how an earthquake epicenter is located
• Explore the relationship between the fracking industry and seismicity
13.1.2 Key Terms
13.2 The ePICenTer, foCus, and waves
An earthquake is a like a telegram from the Earth. It sends a message about the
conditions beneath the Earth’s surface. The shaking or trembling experienced
during an earthquake is the result of a rapid
release of energy within the Earth, usually
as a result of movement along geologic
faults. Think back to the strike-slip fault
from the Crustal Deformation chapter.
Rocks on either side of the fault are sliding
past each other. As they move in opposite
directions, the rocks become deformed, as
they will bend slightly and build up pres-
sure. Eventually they will reach a breaking
point. Once the strength of the rock has
been exceeded, the rocks will snap back to
their normal shape, rel.
1. Earthquakes occur along faults in the Earth's crust due to the buildup and sudden release of strain energy from tectonic plate movement.
2. Seismic waves generated by earthquakes travel through the Earth and are used to determine the internal structure, including distinct layers of the crust, mantle, and core.
3. The core is determined to be liquid based on seismic evidence showing the disappearance of different wave types in certain regions.
This document provides an introduction to the field of geoscience/geology. It discusses key topics like the formation of rocks through igneous, sedimentary, and metamorphic processes. It also covers plate tectonics theory and how the motion of tectonic plates generates earthquakes. The objectives of the course are to understand rock and mineral formation, Earth's structure and composition, sea floor spreading via plate tectonics, landforms, and natural hazards like earthquakes.
The earth is more than 4.5 billion years old! During this unimaginable expanse of time, our planet has undergone drastic changes. For the earliest part of earth’s history, the planet was a molten inferno. As the planet slowly cooled, rocks and minerals began to form, and continents and ocean basins took shape. Earth’s continents today look nothing like they did hundreds of millions of years ago. In fact, the continents move around through a process called plate tectonics.
The Theory of Plat Tectonics is relatively modern and is very different from historic thought, which included ideas ranging from shrinking earth to continents moving across the ocean floor. Fossil evidence paired with lithographic correlation helped solidify the concept of plate tectonics to the theory we know today.
Earth Science is a major Subject of life. Earth Science encompasses hundreds of branches. Geology is the scientific study of the all constituents of planets, their internal and external forms and processes. More precisely, it is the study of nature, structure and history of the planet. Earth is the home to all life, well known to the humankind. Geology, itself, is a major part of The Earth and atmospheric sciences, which were born as twins . The subject of geology encompasses all aspects including the composition, structure, physical properties, and history of a planets'( like Earth's) inter-related components and the processes that are shaping the features on the surface.
Contents:
>Introduction to Earthquake.
>Causes of Earthquake.
>How the Ground shakes?
>Effects of Earthquake on Structures.
>Examples.
>Relationship & world wide distribution of earthquake and volcanoes.
>Earthquake and Bangladesh.
The document discusses the theory of plate tectonics, which proposes that Earth's outer shell is broken into plates that move over time. As the plates move, they will converge and collide, causing volcanic activity and mountain building, or pull apart, creating ocean floors and divergent boundaries. The types of landforms that form depend on whether the colliding plates are oceanic or continental. Plate tectonics explains how forces inside Earth shape its surface features and drive continental drift over hundreds of millions of years.
Venus and Earth have remarkably diferent
surface conditions, yet the lithospheric
thickness and heat fow on Venus may be
Earth-like. This fnding supports a tectonic
regime with limited surface mobility and
dominated by intrusive magmatism.
This document discusses several topics related to earthquakes and earthquake engineering:
- Earthquakes are caused by the sudden movement of tectonic plates along fault lines in the earth's crust.
- The interior structure of the earth is layered, with a solid crust, highly viscous mantle, liquid outer core, and solid inner core.
- Earthquake ground motions can be amplified by local surface geology and sediment thickness, influencing seismic damage. Proper understanding of ground conditions is important for hazard assessment and mitigation.
The document discusses several prominent composers from the Romantic period, including Niccolò Paganini, who became a famous violin virtuoso and inspired other composers. Franz Liszt was known as one of the most virtuosic pianists of the era, performing widely in Vienna and Paris. Hector Berlioz composed the Symphonie Fantastique, showcasing his innovative use of tone color and orchestration.
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centuries, evolving its structure over time and space. In the present era, these changes have
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Remote Sensing and Geographic Information Systems
9
Changes in vegetation cover refer to variations in the distribution, composition, and overall
structure of plant communities across different temporal and spatial scales. These changes can
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it describes the bony anatomy including the femoral head , acetabulum, labrum . also discusses the capsule , ligaments . muscle that act on the hip joint and the range of motion are outlined. factors affecting hip joint stability and weight transmission through the joint are summarized.
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Walmart Business+ and Spark Good for Nonprofits.pdfTechSoup
"Learn about all the ways Walmart supports nonprofit organizations.
You will hear from Liz Willett, the Head of Nonprofits, and hear about what Walmart is doing to help nonprofits, including Walmart Business and Spark Good. Walmart Business+ is a new offer for nonprofits that offers discounts and also streamlines nonprofits order and expense tracking, saving time and money.
The webinar may also give some examples on how nonprofits can best leverage Walmart Business+.
The event will cover the following::
Walmart Business + (https://business.walmart.com/plus) is a new shopping experience for nonprofits, schools, and local business customers that connects an exclusive online shopping experience to stores. Benefits include free delivery and shipping, a 'Spend Analytics” feature, special discounts, deals and tax-exempt shopping.
Special TechSoup offer for a free 180 days membership, and up to $150 in discounts on eligible orders.
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Answers about how you can do more with Walmart!"
1. Plate movement, a fundamental geologic process,
occurs due to the continuous motion of Earth's
lithospheric plates, which float on the semi-fluid
asthenosphere beneath them. This movement is the
driving force behind the ever-changing face of our
planet, responsible for the creation and evolution of
continents, the formation of mountain ranges, and
the occurrence of seismic activity along plate
boundaries. Whether plates collide, pull apart, or
slide past each other, their interactions shape
Earth's surface, influencing geological features,
climate patterns, and even the distribution of life on
our dynamic planet.
6. A-26, B-25, C-24, D-23, E-22, F-21, G-20, H-19,
I-18,J-17,K-16,L-15,M-14,N-13,O-12,P-11,Q-
10,R-9,S-8,T-7,U-6,V-5,W-4,X-3,Y-2,Z-1
23+9+18+5+18+13+20 and
9+22+8+18+8+7+18+13+20
DRIVING and RESISTING FORCE
7. DRIVING FORCES
-either push tectonic plates toward
each other or pull them apart while
resisting force act against the
driving force
RESISTING FORCE- acts against
the driving force
8. The main driving force behind plate movement is MANTLE
CONVECTION
9. In Physics Convection is a HEAT
TRANSFER..
an energy transfer
from an area of
higher energy to
one of lower
energy.
10. Heat from the
Earth's interior
rises toward the
mantle, increasing
its kinetic energy
and causing it to
expand and spread
out the plate.
11. Kinetic is a type of energy which
means energy in motion, and the other
type is potential which means energy
at rest
12. The upward force of mantle
convection causes the
newly created crust to push
the adjacent plates away
In English when we say
adjacent, it means being in
close proximity.
In Geometry-angles having
a common side and a
common vertex.
22. In 2 minutes construct one or two
sentences in any sheet of paper about
why do we need to study plate
movement? After two minutes I will
be choosing lucky two learners to
share their insight or thoughts.
23. It helps us understand the
dynamic nature of our
planet and the processes
that have formed and
continue to modify its
features.
24. By studying plate movement, scientists
can identify areas where tectonic plates
interact and are more likely to generate
seismic activity. This information is vital
for earthquake prediction and mitigation
efforts, which can save lives and reduce
property damage.
27. Many valuable natural resources,
such as minerals, oil, and
natural gas, are found in regions
associated with plate boundaries
and their movements. Studying
plate tectonics helps locate and
access these resources.
28. Many valuable natural resources,
such as minerals, oil, and
natural gas, are found in regions
associated with plate boundaries
and their movements. Studying
plate tectonics helps locate and
access these resources.
29. 1. Subduction zones generate a gravitational
force known as “_______pull," which contributes
significantly to the movement of tectonic plates.
2. At mid-ocean ridges, the upward force of mantle
convection causes the phenomenon known as
"_______ push.”
3. Mantle convection is primarily driven by heat from
the Earth's interior, causing material in the semi-
fluid _______ to rise and create convection currents.
30. 4. The heat-driven rising and sinking of material
in the asthenosphere create convection currents
that set the lithospheric plates in _______.
5. Ridge push is the force that pushes plates away
from mid-ocean ridges as newly formed oceanic crust
exerts an upward _______.
Editor's Notes
This time let us have a collaborative activity
Let us reveal the word behind the series of numbers.
Direction: I will be giving you series of Mathematics equation;(Collaborative Work)
1. Both of you should work in solving the assigned expression or equation.
2. Decode your answer to reveal the word by replacing the numbers by the letter corresponding to your answer.
HANDA NA BA?all right lets do it!
Let us reveal the word behind the series of numbers.
Direction: I will be giving you series of Mathematics equation;(Collaborative Work)
1. Both of you should work in solving the assigned expression or equation.
2. Decode your answer to reveal the word by replacing the numbers by the letter corresponding to your answer.
HANDA NA BA?all right lets do it!Here are the letters and their corresponding numbers..Now I will be distributing you the sheet of paper where the problems written,alright start you only have 1 minute to solve it.
Now, let us find out the connection of the word in todays’ lesson.
What do you think is the reason why there are presence of break or cracks in the surface?
What is plate movement?
Very good! How huge crustal plates could possibly move are influenced by two types of forces. What do you think are those forces? (give the learners a clue based from activity under explore) 23+9+18+5+18+13+20 and 9+22+8+18+8+7+18+13+20
What is driving forces? resisting force?
In heat transfer how is the movement of energy?
Based from the illustration, how will you describe Mantle convection?
Show to the class below illustration,
how will you describe Ridge push?
What pushes the plate down the ridge?
Are you guys familiar with gravity?
Show to the class below illustration,
how will you describe Ridge push?
Another reason of plate movement (show the class)
Based from the illustration, how is slab pull?
How is slab suction? collide- to strike one another w/forceful impact, come into violent contact, crash
For resisting forces, what do we call the force that opposes motion?FRICTION
Under this we have the SLAB RESISTANCE, how is slab resistance?( show the class illustration.)
Another force that resists the movement of lithospheric plate is the DRAG force.
From the illustration DRAG FORCE resists or opposes the movement of the plates
Here are some of the reason why we need to study plate movement.
Here are some of the reason why we need to study plate movement.
This activity, you may work during your ICL session .