earthquakesandfaults-171023070052 (1).pdf
•
0 likes•90 views
This document provides learning objectives and tasks about faults and earthquakes. It defines a fault as a break in the Earth's crust where movement has occurred. When plates move apart it can cause earthquakes and form faults. Activities are described to help students understand this through building a "faulty" model using cardboard and clay to demonstrate how a fault is formed when plates pull apart, and to identify different types of faults in drawings.
Report
Share
Report
Share
Download to read offline
Recommended
1. Earthquake and Faults
Convection currents in the earth's mantle cause the movement of tectonic plates. Faults form at the boundaries of these plates where the rocks are weak. When stress builds up along fault lines from the movement of plates, it causes the faults to slip suddenly and generate earthquakes. There are three main types of faults - normal, reverse, and strike-slip - which move in different ways due to tensional, compressional, or shear stresses. Active faults have generated earthquakes within the last 10,000 years and may continue to do so, while inactive faults have not produced quakes recently but could still be capable of generating future seismic activity.
Continental Drift Theory
Alfred Wegener first proposed the theory of continental drift in the early 20th century. He noticed that the continents appeared to fit together and were once attached in a supercontinent called Pangaea. Wegener provided evidence from matching coastlines, fossil and rock formations, and paleoclimatic data to support his theory. However, he was unable to explain the mechanism of continental drift. Most geologists at the time rejected his theory due to the lack of a clear explanation for how and why the continents would move. It was not until the 1950s when the theory of plate tectonics was developed that Wegener's concept of continental drift became widely accepted.
Types of plate boundaries
This document discusses different types of plate boundaries: divergent boundaries where plates move apart, convergent boundaries where plates collide, and transform boundaries where plates slide past one another. It focuses on convergent boundaries, describing the processes that occur when an oceanic plate collides with a continental plate or when two oceanic plates collide. These processes include subduction, the formation of volcanoes and mountain ranges, and earthquakes.
Sea floor spreading
Scientists in the 1950s used sonar to map the mid-ocean ridge and discovered it was not flat but contained underwater mountains. This discovery led them to research what the ridge was and how it formed. Evidence from molten rock samples, magnetic stripes in the ocean crust, and the ages of rocks drilled from the ocean floor supported Harry Hess' theory from 1960 of sea-floor spreading, where new crust forms at mid-ocean ridges and spreads outward over time.
1. Distribution of Volcanoes and Earthquakes
The document discusses volcanoes and earthquakes, including where they occur and why. It provides learning objectives about knowing where volcanoes and earthquakes happen and why. It includes maps showing the distribution of volcanoes and earthquakes around the world. The patterns are explained by the locations of tectonic plates and different plate boundary types where movement occurs. Iceland is used as a specific example, noting it is at the Mid-Atlantic Ridge plate boundary, resulting in earthquakes and volcanoes like Eyjafjallajökull.
concave mirror activity sheet
This document outlines an experiment to construct ray diagrams and describe images formed by a concave mirror as the object position is varied. The experiment involves placing an object at different positions (at C, at F, beyond C, between F and C, between F and V, and between F and C) and drawing the corresponding ray diagram to determine the image position, size, orientation, and type (real or virtual). The document then asks the student to analyze how the image changes as the object position varies and to discuss the importance of concave mirrors and examples of devices that use them.
18. magnetic reversal
This document contains a detailed lesson plan for a Grade 10 Science class on magnetic reversals and seafloor spreading. The plan outlines the objectives, topics, materials, procedures, and evaluation for a 60 minute lesson. Students will analyze a magnetic polarity map, calculate seafloor spreading rates, and present their findings. They will learn that magnetic reversals are caused by changes in Earth's core and prove seafloor spreading by magnetic patterns in ocean floor rocks. The lesson aims to help students understand how new seafloor is created at mid-ocean ridges and how this relates to plate tectonics.
LESSON PLAN SHS-COT.docx
The document outlines the objectives, content, learning resources, and procedures for a lesson on Earth's four major subsystems - atmosphere, geosphere, hydrosphere, and biosphere. The teacher will lead the class in an activity where students are divided into groups to watch a video and complete a concept map explaining the interconnection of the four subsystems. The lesson aims to help students identify, differentiate, and appreciate the importance of each subsystem and how they work together to sustain life on Earth.
Recommended
1. Earthquake and Faults
Convection currents in the earth's mantle cause the movement of tectonic plates. Faults form at the boundaries of these plates where the rocks are weak. When stress builds up along fault lines from the movement of plates, it causes the faults to slip suddenly and generate earthquakes. There are three main types of faults - normal, reverse, and strike-slip - which move in different ways due to tensional, compressional, or shear stresses. Active faults have generated earthquakes within the last 10,000 years and may continue to do so, while inactive faults have not produced quakes recently but could still be capable of generating future seismic activity.
Continental Drift Theory
Alfred Wegener first proposed the theory of continental drift in the early 20th century. He noticed that the continents appeared to fit together and were once attached in a supercontinent called Pangaea. Wegener provided evidence from matching coastlines, fossil and rock formations, and paleoclimatic data to support his theory. However, he was unable to explain the mechanism of continental drift. Most geologists at the time rejected his theory due to the lack of a clear explanation for how and why the continents would move. It was not until the 1950s when the theory of plate tectonics was developed that Wegener's concept of continental drift became widely accepted.
Types of plate boundaries
This document discusses different types of plate boundaries: divergent boundaries where plates move apart, convergent boundaries where plates collide, and transform boundaries where plates slide past one another. It focuses on convergent boundaries, describing the processes that occur when an oceanic plate collides with a continental plate or when two oceanic plates collide. These processes include subduction, the formation of volcanoes and mountain ranges, and earthquakes.
Sea floor spreading
Scientists in the 1950s used sonar to map the mid-ocean ridge and discovered it was not flat but contained underwater mountains. This discovery led them to research what the ridge was and how it formed. Evidence from molten rock samples, magnetic stripes in the ocean crust, and the ages of rocks drilled from the ocean floor supported Harry Hess' theory from 1960 of sea-floor spreading, where new crust forms at mid-ocean ridges and spreads outward over time.
1. Distribution of Volcanoes and Earthquakes
The document discusses volcanoes and earthquakes, including where they occur and why. It provides learning objectives about knowing where volcanoes and earthquakes happen and why. It includes maps showing the distribution of volcanoes and earthquakes around the world. The patterns are explained by the locations of tectonic plates and different plate boundary types where movement occurs. Iceland is used as a specific example, noting it is at the Mid-Atlantic Ridge plate boundary, resulting in earthquakes and volcanoes like Eyjafjallajökull.
concave mirror activity sheet
This document outlines an experiment to construct ray diagrams and describe images formed by a concave mirror as the object position is varied. The experiment involves placing an object at different positions (at C, at F, beyond C, between F and C, between F and V, and between F and C) and drawing the corresponding ray diagram to determine the image position, size, orientation, and type (real or virtual). The document then asks the student to analyze how the image changes as the object position varies and to discuss the importance of concave mirrors and examples of devices that use them.
18. magnetic reversal
This document contains a detailed lesson plan for a Grade 10 Science class on magnetic reversals and seafloor spreading. The plan outlines the objectives, topics, materials, procedures, and evaluation for a 60 minute lesson. Students will analyze a magnetic polarity map, calculate seafloor spreading rates, and present their findings. They will learn that magnetic reversals are caused by changes in Earth's core and prove seafloor spreading by magnetic patterns in ocean floor rocks. The lesson aims to help students understand how new seafloor is created at mid-ocean ridges and how this relates to plate tectonics.
LESSON PLAN SHS-COT.docx
The document outlines the objectives, content, learning resources, and procedures for a lesson on Earth's four major subsystems - atmosphere, geosphere, hydrosphere, and biosphere. The teacher will lead the class in an activity where students are divided into groups to watch a video and complete a concept map explaining the interconnection of the four subsystems. The lesson aims to help students identify, differentiate, and appreciate the importance of each subsystem and how they work together to sustain life on Earth.
Continental Drift
1) Alfred Wegener proposed the theory of continental drift, which suggested that the continents were once joined together in a supercontinent called Pangaea before drifting apart over millions of years.
2) To support his theory, Wegener presented four pieces of evidence: the matching shapes of continental edges, identical fossil distributions, matching rock formations, and evidence of past climate zones that no longer align with the continents' current locations.
3) Despite this evidence, Wegener's contemporaries rejected his theory because he could not explain the mechanism that caused the continents to move. Acceptance of the theory required understanding how and why continental drift occurred.
Plate Tectonics
The document discusses the theory of plate tectonics, including what plates are made of, how they move at boundaries, and the evidence that supports plate tectonics. The lithosphere comprises the crust and rigid upper mantle, floating on the asthenosphere. Plates move at boundaries in three types - divergent, convergent, and transform - which are associated with volcanoes, earthquakes, and other surface phenomena. Evidence like matching continents, widespread fossil distributions, and matching rock formations support plate tectonics and the past connection of continents.
2.2 active faults & other earthquakes source zones
This document discusses active faults and earthquake source zones in the Philippines. It defines an active fault as one that has moved within the last 10,000 years. The three types of faults are described as normal, thrust/reverse, and strike-slip. Some of the most destructive earthquakes in Philippine history are noted, including the 1990 Luzon earthquake. The Philippine Fault Zone and Valley Fault System are identified as two of the most important active faults. Trenches are also described as earthquake generators where tectonic plates are subducting. The potential impacts of worst case earthquakes on the West Valley Fault and Manila Trench impacting Metro Manila are presented.
Types of Faults
This document provides information about earthquake terminology and fault lines in the Philippines. It defines key terms like epicenter, hypocenter, fault plane, and fault zone. It also lists the major fault lines in the country, including the Marikina Valley Fault, Western Philippine Fault, and Central Philippine Fault. Different types of faults are described based on the displacement of plates and the orientation of the fault, including dip-slip, strike-slip, and oblique-slip faults.
Diastrophism
Diastrophism refers to movements and deformations of the Earth's crust. Forces acting on the crust can cause it to fold, fault, or trench. Folding occurs when crust crumples and bends, faulting when it fractures, and trenching when large rock masses slide against each other. These movements are driven by processes like plate tectonics, where continental plates slowly move and interact at boundaries, which can cause earthquakes and volcanic activity. Evidence like matching fossil and rock formations between separated continents supports the theory of plate tectonics and the past existence of supercontinents like Pangaea.
2. Continental Drift.pptx
Here are the answers to the guide questions:
1. The edges and shapes of the torn pieces helped fit them together perfectly like a jigsaw puzzle.
2. The lines of prints and texts continued seamlessly across the pieces when fitted together correctly, proving they were originally part of the same page.
3. With the pieces fitted together, the newspaper/magazine page is complete and legible again without any gaps or overlaps in the text/images, demonstrating it has been reassembled perfectly.
Seismic waves 6th
Seismic waves are vibrations that travel through the Earth caused by earthquakes. There are three main types of seismic waves: primary (P-) waves, secondary (S-) waves, and surface waves. P-waves are the fastest waves and can travel through solid and liquid materials. S-waves are slower and only travel through solids. Surface waves are the slowest and only travel along the Earth's surface. These seismic waves transmit the energy and effects of earthquakes through the Earth.
Earthquakes
1. The document discusses earthquakes and faults, explaining that the Philippines is prone to earthquakes due to its location along the Ring of Fire.
2. It defines a fault as a break in the earth's crust where significant movement has occurred, and explains how faults produce earthquakes through the buildup and sudden release of energy from inside the earth.
3. The document provides information on earthquake waves, intensity scales, and safety tips for both indoors and outdoors during and after an earthquake.
Seafloor Spreading
Earth and Life Science
Earth Materials and Processes: Deformation of the Crust
The learners shall be able to:
1) explain how the seafloor spreads (S11/12ESId-23);
2) describe the structure and evolution of ocean basins (S11/12ES-Id-24); and
3) explain how the movement of plates leads to the formation of folds and faults (S11/12ES-Id-22).
Specific Learning Outcomes
At the end of the lesson, the learners will be able to:
1. Discuss the history behind the Theory of Continental Drift;
2. Describe the Continental Drift Theory;
3. Enumerate and explain the evidence used to support the idea of drifting continents;
4. Identify major physiographic features of ocean basins
5. Describe the process of seafloor spreading
2. plate boundaries
This lesson plan summarizes a Grade 10 Science lesson on plate tectonics and plate boundaries. The lesson objectives are for students to differentiate the three types of plate boundaries, describe the distribution of volcanoes and earthquakes, determine the scientific basis for dividing plates, and understand the importance of identifying earthquake-prone areas. The lesson contains activities where students analyze maps of earthquakes and volcanoes to identify plate boundaries and classify them as divergent, convergent or transform.
Volcanoes intro
Volcanoes come in different types and erupt in various ways. They form where tectonic plates meet in the Earth's crust. The main types are shield volcanoes which erupt fluid lava flows, composite volcanoes which alternate between explosive eruptions and lava flows, and cinder cone volcanoes which erupt ash and cinders. Volcanoes can be active, dormant, or extinct depending on how recently they have erupted.
Folds and faults ppt
The document provides information about folds and faults. It defines folds as bent or curved rock layers, and describes common fold types like anticlines and synclines. It also defines various fault types including normal faults, thrust faults, strike-slip faults, and oblique faults. Specific structures are described like the San Andreas Fault, which is a major strike-slip fault in California. Dip, strike, heave and throw are also defined in relation to describing the orientation and movement of geological structures.
FINDING THE EPICENTER ACTIVITY SHEET
This document provides instructions for locating the epicenter of an earthquake using triangulation from seismic station data. The procedure involves using the time difference between P and S wave arrivals at three stations to calculate the distance from each station to the epicenter. Circles are drawn on a map using these distances to find the point where all three intersect, which identifies the epicenter. Determining the epicenter is important for understanding the earthquake's location and effects.
Earthquakes and faults
An earthquake is caused by the sudden release of stored energy in the Earth's crust that creates seismic waves. Faults in the Earth's surface develop from movement or displacement of rock and are zones of weakness where earthquakes can occur. There are three main types of faults - strike-slip, normal, and reverse - which are defined by the movement of the rock on either side. Seismographs use a pendulum that remains fixed while the ground moves beneath it to record the intensity and duration of seismic waves, including primary P waves, secondary S waves, and surface L waves, generated by earthquakes.
Earthquakes and faults (Grade 8 Lesson)
This document describes a learning competency on faults. It defines a fault as a break in the Earth's crust where movement has occurred. When plates move apart, it can result in earthquakes and faults. The objectives are to define fault, describe the consequences of diverging plates, and draw a fault. Activities include defining key terms, watching a video, and doing a hands-on modeling activity to simulate how a fault forms when plates pull apart.
seafloor spreading theory LP
This science lesson plan aims to teach 10th grade students about seafloor spreading through various classroom activities. Students will learn how seafloor spreading happens, how drill samples provided evidence of spreading, and the lines of evidence that support plate tectonics theory. The lesson involves engaging students with an animation and video on seafloor spreading, think-pair-share discussions, and an activity using a seafloor spreading model. Formative assessments include student diagrams illustrating seafloor spreading and additional activities on magnetic reversals are suggested for application and remediation.
Lesson in science mitosis
This lesson plan teaches 8th grade students about the cell cycle and mitosis. It has three main parts: concepts, objectives, and lesson proper. The concepts explain the stages of the cell cycle (interphase, mitosis, cytokinesis) and phases of mitosis. The objectives are for students to analyze the cell cycle stages, identify mitosis phases, and understand the importance of mitosis. The lesson proper uses an engaging activity and diagrams to explain the cell cycle and mitosis phases through exploration, explanation, and evaluation. The goal is for students to understand how cells reproduce through mitosis and its importance.
CONTINENTAL DRIFT THEORY EVIDENCES ppt
The document discusses evidence that supports the continental drift theory proposed by Alfred Wegener. It describes an activity where students reconstruct the supercontinent Pangaea by fitting together continent landmass cutouts. The activity aims to showcase two key evidence: 1) the apparent fit of continents and 2) fossil correlations found across different continents. It also discusses two additional evidence put forth by Wegener: 3) past climate data like glacial striations found in present-day equatorial regions, and 4) correlations between mountain ranges and rock formations between separated continents.
Folds
The document defines and provides examples of different types of geological folds including anticlines, synclines, monoclines, recumbent folds, overturned folds, plunging folds, ptygmatic folds, chevron folds, and drag folds. Examples show the folded rock strata, describing the plate tectonics settings and rock types involved. Different terminology is introduced for upwardly arched anticlines versus downwardly arched synclines and other specialized fold patterns.
Continental Drift theory evidences LP
This semi-detailed science lesson plan aims to teach 10th grade students about the Continental Drift Theory. The lesson involves students recreating the supercontinent Pangaea by arranging cut-out continents. Students will then discuss the positions of the continents in Pangaea and two pieces of evidence that supported Alfred Wegener's Continental Drift Theory: the apparent fit of continents and fossil correlation between continents. To check understanding, students will predict where the Philippines may be located in the future and discuss if the two presented evidence were enough to convince people in Wegener's time of continental drift.
science 8 powerpoint presentation for earthquake and faults
This document provides learning objectives and tasks about faults. It defines a fault as a break in the Earth's crust where movement has occurred. When plates move apart, it can cause earthquakes and form faults. Learners will view a video about earthquakes, do an activity using modeling clay and cardboard to simulate a fault, then draw and label their observation. They will be assessed on their understanding of faults and asked to create models showing the differences between normal and reverse faults.
Earthquakes final
The document discusses dynamics of the Earth's crust and evidence of its motion over time. It provides examples of marine fossils found in high elevations as evidence of crustal uplift. Sedimentary layers deposited horizontally also indicate regions were once under water. Earthquakes provide direct evidence of crustal movement through effects like fault lines and changes in land elevation recorded after quakes.
More Related Content
What's hot
Continental Drift
1) Alfred Wegener proposed the theory of continental drift, which suggested that the continents were once joined together in a supercontinent called Pangaea before drifting apart over millions of years.
2) To support his theory, Wegener presented four pieces of evidence: the matching shapes of continental edges, identical fossil distributions, matching rock formations, and evidence of past climate zones that no longer align with the continents' current locations.
3) Despite this evidence, Wegener's contemporaries rejected his theory because he could not explain the mechanism that caused the continents to move. Acceptance of the theory required understanding how and why continental drift occurred.
Plate Tectonics
The document discusses the theory of plate tectonics, including what plates are made of, how they move at boundaries, and the evidence that supports plate tectonics. The lithosphere comprises the crust and rigid upper mantle, floating on the asthenosphere. Plates move at boundaries in three types - divergent, convergent, and transform - which are associated with volcanoes, earthquakes, and other surface phenomena. Evidence like matching continents, widespread fossil distributions, and matching rock formations support plate tectonics and the past connection of continents.
2.2 active faults & other earthquakes source zones
This document discusses active faults and earthquake source zones in the Philippines. It defines an active fault as one that has moved within the last 10,000 years. The three types of faults are described as normal, thrust/reverse, and strike-slip. Some of the most destructive earthquakes in Philippine history are noted, including the 1990 Luzon earthquake. The Philippine Fault Zone and Valley Fault System are identified as two of the most important active faults. Trenches are also described as earthquake generators where tectonic plates are subducting. The potential impacts of worst case earthquakes on the West Valley Fault and Manila Trench impacting Metro Manila are presented.
Types of Faults
This document provides information about earthquake terminology and fault lines in the Philippines. It defines key terms like epicenter, hypocenter, fault plane, and fault zone. It also lists the major fault lines in the country, including the Marikina Valley Fault, Western Philippine Fault, and Central Philippine Fault. Different types of faults are described based on the displacement of plates and the orientation of the fault, including dip-slip, strike-slip, and oblique-slip faults.
Diastrophism
Diastrophism refers to movements and deformations of the Earth's crust. Forces acting on the crust can cause it to fold, fault, or trench. Folding occurs when crust crumples and bends, faulting when it fractures, and trenching when large rock masses slide against each other. These movements are driven by processes like plate tectonics, where continental plates slowly move and interact at boundaries, which can cause earthquakes and volcanic activity. Evidence like matching fossil and rock formations between separated continents supports the theory of plate tectonics and the past existence of supercontinents like Pangaea.
2. Continental Drift.pptx
Here are the answers to the guide questions:
1. The edges and shapes of the torn pieces helped fit them together perfectly like a jigsaw puzzle.
2. The lines of prints and texts continued seamlessly across the pieces when fitted together correctly, proving they were originally part of the same page.
3. With the pieces fitted together, the newspaper/magazine page is complete and legible again without any gaps or overlaps in the text/images, demonstrating it has been reassembled perfectly.
Seismic waves 6th
Seismic waves are vibrations that travel through the Earth caused by earthquakes. There are three main types of seismic waves: primary (P-) waves, secondary (S-) waves, and surface waves. P-waves are the fastest waves and can travel through solid and liquid materials. S-waves are slower and only travel through solids. Surface waves are the slowest and only travel along the Earth's surface. These seismic waves transmit the energy and effects of earthquakes through the Earth.
Earthquakes
1. The document discusses earthquakes and faults, explaining that the Philippines is prone to earthquakes due to its location along the Ring of Fire.
2. It defines a fault as a break in the earth's crust where significant movement has occurred, and explains how faults produce earthquakes through the buildup and sudden release of energy from inside the earth.
3. The document provides information on earthquake waves, intensity scales, and safety tips for both indoors and outdoors during and after an earthquake.
Seafloor Spreading
Earth and Life Science
Earth Materials and Processes: Deformation of the Crust
The learners shall be able to:
1) explain how the seafloor spreads (S11/12ESId-23);
2) describe the structure and evolution of ocean basins (S11/12ES-Id-24); and
3) explain how the movement of plates leads to the formation of folds and faults (S11/12ES-Id-22).
Specific Learning Outcomes
At the end of the lesson, the learners will be able to:
1. Discuss the history behind the Theory of Continental Drift;
2. Describe the Continental Drift Theory;
3. Enumerate and explain the evidence used to support the idea of drifting continents;
4. Identify major physiographic features of ocean basins
5. Describe the process of seafloor spreading
2. plate boundaries
This lesson plan summarizes a Grade 10 Science lesson on plate tectonics and plate boundaries. The lesson objectives are for students to differentiate the three types of plate boundaries, describe the distribution of volcanoes and earthquakes, determine the scientific basis for dividing plates, and understand the importance of identifying earthquake-prone areas. The lesson contains activities where students analyze maps of earthquakes and volcanoes to identify plate boundaries and classify them as divergent, convergent or transform.
Volcanoes intro
Volcanoes come in different types and erupt in various ways. They form where tectonic plates meet in the Earth's crust. The main types are shield volcanoes which erupt fluid lava flows, composite volcanoes which alternate between explosive eruptions and lava flows, and cinder cone volcanoes which erupt ash and cinders. Volcanoes can be active, dormant, or extinct depending on how recently they have erupted.
Folds and faults ppt
The document provides information about folds and faults. It defines folds as bent or curved rock layers, and describes common fold types like anticlines and synclines. It also defines various fault types including normal faults, thrust faults, strike-slip faults, and oblique faults. Specific structures are described like the San Andreas Fault, which is a major strike-slip fault in California. Dip, strike, heave and throw are also defined in relation to describing the orientation and movement of geological structures.
FINDING THE EPICENTER ACTIVITY SHEET
This document provides instructions for locating the epicenter of an earthquake using triangulation from seismic station data. The procedure involves using the time difference between P and S wave arrivals at three stations to calculate the distance from each station to the epicenter. Circles are drawn on a map using these distances to find the point where all three intersect, which identifies the epicenter. Determining the epicenter is important for understanding the earthquake's location and effects.
Earthquakes and faults
An earthquake is caused by the sudden release of stored energy in the Earth's crust that creates seismic waves. Faults in the Earth's surface develop from movement or displacement of rock and are zones of weakness where earthquakes can occur. There are three main types of faults - strike-slip, normal, and reverse - which are defined by the movement of the rock on either side. Seismographs use a pendulum that remains fixed while the ground moves beneath it to record the intensity and duration of seismic waves, including primary P waves, secondary S waves, and surface L waves, generated by earthquakes.
Earthquakes and faults (Grade 8 Lesson)
This document describes a learning competency on faults. It defines a fault as a break in the Earth's crust where movement has occurred. When plates move apart, it can result in earthquakes and faults. The objectives are to define fault, describe the consequences of diverging plates, and draw a fault. Activities include defining key terms, watching a video, and doing a hands-on modeling activity to simulate how a fault forms when plates pull apart.
seafloor spreading theory LP
This science lesson plan aims to teach 10th grade students about seafloor spreading through various classroom activities. Students will learn how seafloor spreading happens, how drill samples provided evidence of spreading, and the lines of evidence that support plate tectonics theory. The lesson involves engaging students with an animation and video on seafloor spreading, think-pair-share discussions, and an activity using a seafloor spreading model. Formative assessments include student diagrams illustrating seafloor spreading and additional activities on magnetic reversals are suggested for application and remediation.
Lesson in science mitosis
This lesson plan teaches 8th grade students about the cell cycle and mitosis. It has three main parts: concepts, objectives, and lesson proper. The concepts explain the stages of the cell cycle (interphase, mitosis, cytokinesis) and phases of mitosis. The objectives are for students to analyze the cell cycle stages, identify mitosis phases, and understand the importance of mitosis. The lesson proper uses an engaging activity and diagrams to explain the cell cycle and mitosis phases through exploration, explanation, and evaluation. The goal is for students to understand how cells reproduce through mitosis and its importance.
CONTINENTAL DRIFT THEORY EVIDENCES ppt
The document discusses evidence that supports the continental drift theory proposed by Alfred Wegener. It describes an activity where students reconstruct the supercontinent Pangaea by fitting together continent landmass cutouts. The activity aims to showcase two key evidence: 1) the apparent fit of continents and 2) fossil correlations found across different continents. It also discusses two additional evidence put forth by Wegener: 3) past climate data like glacial striations found in present-day equatorial regions, and 4) correlations between mountain ranges and rock formations between separated continents.
Folds
The document defines and provides examples of different types of geological folds including anticlines, synclines, monoclines, recumbent folds, overturned folds, plunging folds, ptygmatic folds, chevron folds, and drag folds. Examples show the folded rock strata, describing the plate tectonics settings and rock types involved. Different terminology is introduced for upwardly arched anticlines versus downwardly arched synclines and other specialized fold patterns.
Continental Drift theory evidences LP
This semi-detailed science lesson plan aims to teach 10th grade students about the Continental Drift Theory. The lesson involves students recreating the supercontinent Pangaea by arranging cut-out continents. Students will then discuss the positions of the continents in Pangaea and two pieces of evidence that supported Alfred Wegener's Continental Drift Theory: the apparent fit of continents and fossil correlation between continents. To check understanding, students will predict where the Philippines may be located in the future and discuss if the two presented evidence were enough to convince people in Wegener's time of continental drift.
What's hot (20)
2.2 active faults & other earthquakes source zones
2.2 active faults & other earthquakes source zones
Similar to earthquakesandfaults-171023070052 (1).pdf
science 8 powerpoint presentation for earthquake and faults
This document provides learning objectives and tasks about faults. It defines a fault as a break in the Earth's crust where movement has occurred. When plates move apart, it can cause earthquakes and form faults. Learners will view a video about earthquakes, do an activity using modeling clay and cardboard to simulate a fault, then draw and label their observation. They will be assessed on their understanding of faults and asked to create models showing the differences between normal and reverse faults.
Earthquakes final
The document discusses dynamics of the Earth's crust and evidence of its motion over time. It provides examples of marine fossils found in high elevations as evidence of crustal uplift. Sedimentary layers deposited horizontally also indicate regions were once under water. Earthquakes provide direct evidence of crustal movement through effects like fault lines and changes in land elevation recorded after quakes.
Earthquakes & Faults
The document defines earthquakes as the sudden, violent shifting of massive plates underneath Earth's surface that causes wave energy to transmit through bedrock. It identifies the key parts of an earthquake as the focus, epicenter, fault, and fault line. It explains that active faults have recent movement recorded, while inactive faults have no recent or expected future movement. The document also describes the three main types of faults: normal faults where the hanging wall moves down, reverse faults where it moves up, and strike-slip faults where blocks slide past each other horizontally.
FAULTS and ITS TYPES - ENHANCED SCIENCE GRADE 7 (4TH QUARTER)
This document discusses earthquakes and fault types. It begins with a word scramble activity related to plate tectonics concepts. It then defines key earthquake terms like epicenter and hypocenter. The document outlines the three main types of faults: normal, reverse/thrust, and strike slip. Normal faults occur at divergent boundaries, reverse/thrust at convergent boundaries, and strike slip at transform boundaries. Examples of each are given. The final sections discuss the causes of faults and provide an activity to demonstrate how earthquakes start at the focus below the epicenter along a fault plane.
Faults and Earthquakes Grade 8 Science.pptx
The document provides instructions for an experiment to simulate how faults form and cause earthquakes. Students will spread sand on a table between two pieces of cardboard to represent tectonic plates. They will make parallel lines in the sand and pull the cardboard apart to demonstrate how the lines shift and a crack forms, representing a fault. Guide questions ask students to identify what parts of the experiment represent different Earth features and processes, and to define what a fault is. The objectives are to explain how fault movement causes earthquakes and increase awareness of disaster preparedness.
Plate Boundaries ( Plates Slow Dance)
This document contains materials for teaching students about plate tectonics, including three activities and assessments. It includes diagrams of the three types of plate boundaries: divergent boundaries where plates move apart, convergent boundaries where plates move together, and transform boundaries where plates slide past each other. Convergent boundaries are further divided into ocean-ocean, ocean-continental, and continental-continental. The materials provide questions to test students' understanding of which boundaries produce earthquakes and volcanoes, where new ocean crust is created, and other concepts related to plate tectonics.
Lesson 1- Earthquakes and Fault.pptx
Lesson 1 describes earthquakes and faults. It defines key terms like fault, focus, and epicenter. Faults occur along breaks in the earth's crust where significant movement has taken place. There are two main types of faults: dip-slip faults which involve vertical movement, and strike-slip faults which involve horizontal movement. The focus is where an earthquake originates within the fault plane, while the epicenter is the point directly above on the surface. The lesson provides safety tips for before, during, and after an earthquake occurs.
Q2 Week 1 Types of Faults and Stresses.pptx
I apologize, I do not have enough context to determine what specific agency the question is referring to. Could you please rephrase the question or provide more details?
10 1425 web_lec_11_gravitation
The document discusses key concepts of gravitation and Newton's law of universal gravitation. It explains that gravitational force follows an inverse square law with distance and is proportional to the masses of both objects. It describes how Cavendish used experiments to determine the gravitational constant G and calculate the mass of the Earth. Kepler's laws of planetary motion are also summarized.
10 1425 web_lec_11_gravitation
The document discusses key concepts of gravitation and Newton's law of universal gravitation. It explains that gravitational force follows an inverse square law with distance and is proportional to the masses of both objects. It describes how Cavendish used experiments to determine the gravitational constant G and calculate the mass of the Earth. Kepler's laws of planetary motion are also summarized.
Earth-and-Life-Science-Q1-Week-5.pdf
The document discusses how the movement of tectonic plates leads to the formation of folds and faults in the Earth's crust. It explains that compressional, tensional, and shear stresses from plate movements cause rocks to deform through either fracturing or bending. Fractures result in faults or joints, while bending forms folds such as anticlines, synclines, and monoclines. The movement of plates at convergent, divergent, and transform boundaries influences the type of stress and folding or fracturing that occurs. Folds and faults are important in forming new land masses.
4/16
The document discusses convection in the mantle and how it relates to plate tectonics. It explains that convection currents, along with ridge push and slab pull, are responsible for the movement of tectonic plates. Ridge push occurs as new ocean crust is formed at mid-ocean ridges, lifting and pushing the plates apart. Slab pull results from the subduction of ocean plates at trenches, where cooling slabs pull the plates into the mantle.
quarter 1 module 1 week 2.pptx
This document contains notes from a lesson on plate tectonics that describes the distribution of volcanoes, earthquakes, and mountain ranges. It discusses key concepts like the theory of plate tectonics, convection currents in the mantle, and how earthquakes, volcanoes, and mountains are often located along plate boundaries. Maps and figures show the distribution of earthquake epicenters, volcanoes, and plates. Questions guide students to understand the relationships between these geographic features and plate tectonics theory.
Lithosphere 2: Tectonics
This document discusses plate tectonics and the movement of tectonic plates. It provides evidence that supports plate tectonics including: the fit of continental landmasses, matching rock and fossil distributions, and magnetic reversals recorded in ocean crust. It describes the three main plate boundaries and associated landforms: divergent boundaries form mid-ocean ridges and rift valleys, convergent boundaries result in subduction zones and volcanic mountain ranges, and transform boundaries create strike-slip faults. Earthquakes and tsunamis are hazardous events caused by the movement and interactions of tectonic plates. Volcanoes form at plate boundaries and hotspots as magma rises up due to pressure in the crust and mantle.
Ch19 building the earths surface
This document discusses various geological processes that shape Earth's surface over long periods of time. It describes how stress and strain lead to folding and faulting in the crust. It also explains how volcanic activity, earthquakes, and plate tectonics result in mountain building and other surface features. Key points include how the principle of uniformity helps us understand slow, gradual changes versus sudden catastrophic events, and how different rock types respond to stress depending on temperature, pressure, and time.
SCIENCE-FOURTH-QUARTER-Day 1-Day 5- .doc
This document outlines a science lesson plan for 6th grade students on earthquakes and volcanic eruptions. The lesson will take place over 1 week and cover topics like the layers of the earth, crustal plates and their movement, and the differences between earthquake intensity and magnitude. Students will participate in hands-on activities using materials like clay and puzzles to illustrate concepts. They will also view presentations and take a summative test to evaluate their learning. The goal is for students to understand how earthquakes and eruptions impact the earth's surface.
EARTHQUAKE AND FAULTS.pptx
The document outlines a lesson plan on earthquakes and faults. It includes two hands-on activities to teach students about faults and how they generate earthquakes. The first activity involves using sheets of paper to simulate the movement of faults and formation of cracks. The second activity uses an elastic band and boxes to demonstrate the concept of stress buildup and sudden release of energy during an earthquake. The lesson concludes with an assessment of student understanding and a roleplaying activity to discuss safety precautions near fault lines.
Earthquakes final
The document discusses dynamics of the Earth including evidence of crustal motions such as uplift and erosion that create mountains and sedimentary layers. It explains how marine fossils found in high elevations provide evidence of crustal movement over time. Earthquakes are described as being caused by the movement of tectonic plates and release of stress that builds in rocks, sending seismic waves that can be used to locate an earthquake's epicenter. The layers of the Earth are also outlined, with the crust varying in thickness and composition in different regions.
Plate boundaries stresses faults ppt
This document discusses plate tectonics and the three types of plate boundaries: divergent boundaries, convergent boundaries, and transform boundaries. It describes how each boundary type results in different stresses on rocks and the formation of different geological features. Divergent boundaries result in tension stresses that cause normal faults and the formation of rift valleys or sea floor spreading. Convergent boundaries result in compression stresses that cause reverse faults and the uplifting of folded mountains or subduction zones and volcanoes. Transform boundaries result in shearing stresses that cause strike-slip faults like the San Andreas Fault in California.
Eathquake-and-faults.pptx
1. The document discusses electrical wiring and circuits. It defines key concepts like current, parallel circuits, circuit breakers, and grounding/earthing.
2. It also discusses earthquakes and faults. It explains that an earthquake is caused by sudden shifting of underground rock masses. Different types of stresses like tension, compression, and shearing can cause faults.
3. Common types of faults include normal dip-slip faults, reverse dip-slip faults, and strike-slip faults which have left or right lateral movement. Earthquakes commonly occur in places like Japan, Indonesia, and the Philippines due to their location within the Pacific Ring of Fire.
Similar to earthquakesandfaults-171023070052 (1).pdf (20)
science 8 powerpoint presentation for earthquake and faults
science 8 powerpoint presentation for earthquake and faults
FAULTS and ITS TYPES - ENHANCED SCIENCE GRADE 7 (4TH QUARTER)
FAULTS and ITS TYPES - ENHANCED SCIENCE GRADE 7 (4TH QUARTER)
More from Ivy Lynne Esguerra
PARENTS-ORIENTATION STA PEREGRINA HIGH SCHOOL.pptx
Teacher Sarah welcomes students to the new school year and provides an orientation covering the agenda. The orientation outlines the subjects to be covered, the class schedule divided into hourly periods from Monday to Friday, the grading system with percentages for written works, performance tasks, and quarterly exams. Classroom rules are also established regarding being prompt, honest, prepared, participative, respectful, and responsible. Finally, the teacher's contact details are shared for any student needs.
Module 5 Sounds Science 8 Lesson Quarter 1
The speed of sound depends on the properties of the medium it travels through. Pitch is the frequency of a sound as perceived by human ears. When singing in a bathroom, echoes occur because the hard surfaces cause multiple reflections of sound. Pictures show that during the day, sound waves are refracted upwards and may not reach the observer, while at night they are refracted downwards and can reach the observer. Given a 4-second delay between lightning and thunder, the storm is 1376 meters away assuming the speed of sound is 344 m/s. If seen from 600 meters away, the time delay to hear a bat hitting a ball would be 1.74 seconds.
PlantKingdom.ppt
Plants are classified as multicellular eukaryotes that photosynthesize for food. They evolved from green algae and are divided into nonvascular and vascular groups. Vascular plants are further divided into gymnosperms like pine trees and angiosperms like roses. Angiosperms are divided into monocots and dicots. Flowers contain male pollen-producing parts and female ovule-producing parts to sexually reproduce through mutualistic relationships with pollinators.
week 3 health Part 1.pptx
This document discusses sexuality and gender identity. It defines intersex as people born with reproductive or sexual anatomy that does not fit typical definitions of male or female. Sometimes surgeries are performed on intersex babies to make their bodies conform to binary gender norms. It also discusses the components of sexuality, including sexual orientation defined as attraction to others, gender identity as one's personal sense of gender, and gender expression as how one outwardly expresses their gender identity through appearance and behavior.
week 1 arts.pptx
This document summarizes traditional fabrics, arts, and crafts from several Southeast Asian countries. It discusses the silk production processes in Thailand and Vietnam and weaving techniques like ikat and uneven twill used in Cambodia. Batik fabric designs involving wax-resist dyeing techniques are described for Indonesia, Malaysia, and Singapore. Traditional crafts discussed include Thai sky lanterns, Lao and Cambodian paper and basket making, Vietnamese silk painting, Indonesian wayang kulit shadow puppets, and Malaysian kites. Head coverings like the songkok cap of Brunei are also summarized. The document concludes by briefly mentioning stone carving art in Cambodia, Thailand, Laos, Vietnam, Malaysia, and
Speed of Sound presentation.ppt
This document describes an experiment to investigate how the speed of sound varies with temperature in air. The experiment involves using a speaker and microphone to measure the time delay of a sound wave traveling through air at different temperatures, controlled by cooling with liquid nitrogen and heating with lamps. The results are analyzed and found to closely match the theoretical prediction from statistical mechanics that the speed of sound increases with temperature according to the given equation. Sources of experimental error are also discussed.
More from Ivy Lynne Esguerra (6)
PARENTS-ORIENTATION STA PEREGRINA HIGH SCHOOL.pptx
PARENTS-ORIENTATION STA PEREGRINA HIGH SCHOOL.pptx
Recently uploaded
Pengantar Penggunaan Flutter - Dart programming language1.pptx
Pengantar Penggunaan Flutter - Dart programming language1.pptx
Digital Artifact 1 - 10VCD Environments Unit
Digital Artifact 1 - 10VCD Environments Unit - NGV Pavilion Concept Design
How to Manage Your Lost Opportunities in Odoo 17 CRM
Odoo 17 CRM allows us to track why we lose sales opportunities with "Lost Reasons." This helps analyze our sales process and identify areas for improvement. Here's how to configure lost reasons in Odoo 17 CRM
Azure Interview Questions and Answers PDF By ScholarHat
Azure Interview Questions and Answers PDF By ScholarHat
What is Digital Literacy? A guest blog from Andy McLaughlin, University of Ab...
What is Digital Literacy? A guest blog from Andy McLaughlin, University of Aberdeen
Natural birth techniques - Mrs.Akanksha Trivedi Rama University
Natural birth techniques - Mrs.Akanksha Trivedi Rama UniversityAkanksha trivedi rama nursing college kanpur.
Natural birth techniques are various type such as/ water birth , alexender method, hypnosis, bradley method, lamaze method etcclinical examination of hip joint (1).pdf
described clinical examination all orthopeadic conditions .
LAND USE LAND COVER AND NDVI OF MIRZAPUR DISTRICT, UP
This Dissertation explores the particular circumstances of Mirzapur, a region located in the
core of India. Mirzapur, with its varied terrains and abundant biodiversity, offers an optimal
environment for investigating the changes in vegetation cover dynamics. Our study utilizes
advanced technologies such as GIS (Geographic Information Systems) and Remote sensing to
analyze the transformations that have taken place over the course of a decade.
The complex relationship between human activities and the environment has been the focus
of extensive research and worry. As the global community grapples with swift urbanization,
population expansion, and economic progress, the effects on natural ecosystems are becoming
more evident. A crucial element of this impact is the alteration of vegetation cover, which plays a
significant role in maintaining the ecological equilibrium of our planet.Land serves as the foundation for all human activities and provides the necessary materials for
these activities. As the most crucial natural resource, its utilization by humans results in different
'Land uses,' which are determined by both human activities and the physical characteristics of the
land.
The utilization of land is impacted by human needs and environmental factors. In countries
like India, rapid population growth and the emphasis on extensive resource exploitation can lead
to significant land degradation, adversely affecting the region's land cover.
Therefore, human intervention has significantly influenced land use patterns over many
centuries, evolving its structure over time and space. In the present era, these changes have
accelerated due to factors such as agriculture and urbanization. Information regarding land use and
cover is essential for various planning and management tasks related to the Earth's surface,
providing crucial environmental data for scientific, resource management, policy purposes, and
diverse human activities.
Accurate understanding of land use and cover is imperative for the development planning
of any area. Consequently, a wide range of professionals, including earth system scientists, land
and water managers, and urban planners, are interested in obtaining data on land use and cover
changes, conversion trends, and other related patterns. The spatial dimensions of land use and
cover support policymakers and scientists in making well-informed decisions, as alterations in
these patterns indicate shifts in economic and social conditions. Monitoring such changes with the
help of Advanced technologies like Remote Sensing and Geographic Information Systems is
crucial for coordinated efforts across different administrative levels. Advanced technologies like
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
occur natural.
ISO/IEC 27001, ISO/IEC 42001, and GDPR: Best Practices for Implementation and...
Denis is a dynamic and results-driven Chief Information Officer (CIO) with a distinguished career spanning information systems analysis and technical project management. With a proven track record of spearheading the design and delivery of cutting-edge Information Management solutions, he has consistently elevated business operations, streamlined reporting functions, and maximized process efficiency.
Certified as an ISO/IEC 27001: Information Security Management Systems (ISMS) Lead Implementer, Data Protection Officer, and Cyber Risks Analyst, Denis brings a heightened focus on data security, privacy, and cyber resilience to every endeavor.
His expertise extends across a diverse spectrum of reporting, database, and web development applications, underpinned by an exceptional grasp of data storage and virtualization technologies. His proficiency in application testing, database administration, and data cleansing ensures seamless execution of complex projects.
What sets Denis apart is his comprehensive understanding of Business and Systems Analysis technologies, honed through involvement in all phases of the Software Development Lifecycle (SDLC). From meticulous requirements gathering to precise analysis, innovative design, rigorous development, thorough testing, and successful implementation, he has consistently delivered exceptional results.
Throughout his career, he has taken on multifaceted roles, from leading technical project management teams to owning solutions that drive operational excellence. His conscientious and proactive approach is unwavering, whether he is working independently or collaboratively within a team. His ability to connect with colleagues on a personal level underscores his commitment to fostering a harmonious and productive workplace environment.
Date: May 29, 2024
Tags: Information Security, ISO/IEC 27001, ISO/IEC 42001, Artificial Intelligence, GDPR
-------------------------------------------------------------------------------
Find out more about ISO training and certification services
Training: ISO/IEC 27001 Information Security Management System - EN | PECB
ISO/IEC 42001 Artificial Intelligence Management System - EN | PECB
General Data Protection Regulation (GDPR) - Training Courses - EN | PECB
Webinars: https://pecb.com/webinars
Article: https://pecb.com/article
-------------------------------------------------------------------------------
For more information about PECB:
Website: https://pecb.com/
LinkedIn: https://www.linkedin.com/company/pecb/
Facebook: https://www.facebook.com/PECBInternational/
Slideshare: http://www.slideshare.net/PECBCERTIFICATION
How to Setup Warehouse & Location in Odoo 17 Inventory
In this slide, we'll explore how to set up warehouses and locations in Odoo 17 Inventory. This will help us manage our stock effectively, track inventory levels, and streamline warehouse operations.
Your Skill Boost Masterclass: Strategies for Effective Upskilling
Your Skill Boost Masterclass: Strategies for Effective UpskillingExcellence Foundation for South Sudan
Strategies for Effective Upskilling is a presentation by Chinwendu Peace in a Your Skill Boost Masterclass organisation by the Excellence Foundation for South Sudan on 08th and 09th June 2024 from 1 PM to 3 PM on each day.Hindi varnamala | hindi alphabet PPT.pdf
हिंदी वर्णमाला पीपीटी, hindi alphabet PPT presentation, hindi varnamala PPT, Hindi Varnamala pdf, हिंदी स्वर, हिंदी व्यंजन, sikhiye hindi varnmala, dr. mulla adam ali, hindi language and literature, hindi alphabet with drawing, hindi alphabet pdf, hindi varnamala for childrens, hindi language, hindi varnamala practice for kids, https://www.drmullaadamali.com
ANATOMY AND BIOMECHANICS OF HIP JOINT.pdf
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.
The simplified electron and muon model, Oscillating Spacetime: The Foundation...
Discover the Simplified Electron and Muon Model: A New Wave-Based Approach to Understanding Particles delves into a groundbreaking theory that presents electrons and muons as rotating soliton waves within oscillating spacetime. Geared towards students, researchers, and science buffs, this book breaks down complex ideas into simple explanations. It covers topics such as electron waves, temporal dynamics, and the implications of this model on particle physics. With clear illustrations and easy-to-follow explanations, readers will gain a new outlook on the universe's fundamental nature.
বাংলাদেশ অর্থনৈতিক সমীক্ষা (Economic Review) ২০২৪ UJS App.pdf
বাংলাদেশের অর্থনৈতিক সমীক্ষা ২০২৪ [Bangladesh Economic Review 2024 Bangla.pdf] কম্পিউটার , ট্যাব ও স্মার্ট ফোন ভার্সন সহ সম্পূর্ণ বাংলা ই-বুক বা pdf বই " সুচিপত্র ...বুকমার্ক মেনু 🔖 ও হাইপার লিংক মেনু 📝👆 যুক্ত ..
আমাদের সবার জন্য খুব খুব গুরুত্বপূর্ণ একটি বই ..বিসিএস, ব্যাংক, ইউনিভার্সিটি ভর্তি ও যে কোন প্রতিযোগিতা মূলক পরীক্ষার জন্য এর খুব ইম্পরট্যান্ট একটি বিষয় ...তাছাড়া বাংলাদেশের সাম্প্রতিক যে কোন ডাটা বা তথ্য এই বইতে পাবেন ...
তাই একজন নাগরিক হিসাবে এই তথ্য গুলো আপনার জানা প্রয়োজন ...।
বিসিএস ও ব্যাংক এর লিখিত পরীক্ষা ...+এছাড়া মাধ্যমিক ও উচ্চমাধ্যমিকের স্টুডেন্টদের জন্য অনেক কাজে আসবে ...
Advanced Java[Extra Concepts, Not Difficult].docx
This is part 2 of my Java Learning Journey. This contains Hashing, ArrayList, LinkedList, Date and Time Classes, Calendar Class and more.
Recently uploaded (20)
Pengantar Penggunaan Flutter - Dart programming language1.pptx
Pengantar Penggunaan Flutter - Dart programming language1.pptx
How to Manage Your Lost Opportunities in Odoo 17 CRM
How to Manage Your Lost Opportunities in Odoo 17 CRM
Azure Interview Questions and Answers PDF By ScholarHat
Azure Interview Questions and Answers PDF By ScholarHat
What is Digital Literacy? A guest blog from Andy McLaughlin, University of Ab...
What is Digital Literacy? A guest blog from Andy McLaughlin, University of Ab...
Natural birth techniques - Mrs.Akanksha Trivedi Rama University
Natural birth techniques - Mrs.Akanksha Trivedi Rama University
LAND USE LAND COVER AND NDVI OF MIRZAPUR DISTRICT, UP
LAND USE LAND COVER AND NDVI OF MIRZAPUR DISTRICT, UP
ISO/IEC 27001, ISO/IEC 42001, and GDPR: Best Practices for Implementation and...
ISO/IEC 27001, ISO/IEC 42001, and GDPR: Best Practices for Implementation and...
How to Setup Warehouse & Location in Odoo 17 Inventory
How to Setup Warehouse & Location in Odoo 17 Inventory
Your Skill Boost Masterclass: Strategies for Effective Upskilling
Your Skill Boost Masterclass: Strategies for Effective Upskilling
The simplified electron and muon model, Oscillating Spacetime: The Foundation...
The simplified electron and muon model, Oscillating Spacetime: The Foundation...
বাংলাদেশ অর্থনৈতিক সমীক্ষা (Economic Review) ২০২৪ UJS App.pdf
বাংলাদেশ অর্থনৈতিক সমীক্ষা (Economic Review) ২০২৪ UJS App.pdf
earthquakesandfaults-171023070052 (1).pdf
- 3. Learning Competency: • Describe what a fault is.
- 4. OBJECTIVES: a. define fault; b.determine the consequences of plates that are moving apart; and c. draw the appearance of a fault.
- 6. Unlocking of terms: • Fault – is a break in the Earth’s crust, and along the break which movement has occurred. • Earthquake – vibration of Earth due to rapid release of energy • Plate – rigid section of the lithosphere that moves as a unit • Epicenter – the point on the earth's surface vertically above the focus of an earthquake. • Magnitude – a number that shows the power of an earthquake
- 7. A. Review:
- 10. B. Motivation:
- 11. Directions: • Identify the 4 given pictures that depict one situation. • Guess what the pictures say all about. • Jumbled letters are provided.
- 12. GAME?
- 13. E A R T H E F A T H L R E F A T H L R
- 14. E A R T H Q U A K E K E E F A T H Q L RU A K E E F A T H Q L RU A
- 15. U L T A F L E U F A T R L E U F A T R
- 16. SHORT FILM SHOWING (Earthquake related video) C. Learning Procedure: ACTIVITY 1:
- 17. ACTIVITY 2: IT IS OUR FAULT: THE FAULT-Y SET UP
- 18. Procedure: • Arrange the two sheets of cardboard, edge to edge. It could be horizontally or vertically arranged.
- 19. • Flattened the modeling clay and place it at the center of the two cardboards. Clay should be along the boundary.
- 20. • Slowly pull the two cardboards away from each other. Observe what happens to the clay.
- 21. •Draw your observation based on the result of your fault-y set up in ¼ cartolina and post your work on the board.
- 22. Draw your observatio n FLOW OF PROCEDURE
- 23. Look at the picture!
- 24. FAULT - a break in the Earth’s crust, and along the break, significant movement has taken place. When plates are moving away from each other, it results to: *Earthquake *Fault
- 26. • ASSESSMENT: ½ CW. ______ 1. It is a break in the crust to which significant movement has occurred. ______ 2. When two plates are moving away from each other, the consequences are: _____ and ____. • For 3 points: Draw the appearance of a fault. Fault Fault Earthquake Earthquake Fault Fault
- 27. ASSIGNMENT: • What is the difference between a normal fault and reverse fault? To find out, create a 2D model of a normal fault and of a reverse fault.