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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.
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The document discusses earthquakes and how they occur. It explains that earthquakes are caused by sudden movement along faults in the Earth's crust due to a build up of stress. There are three main types of faults - normal, reverse, and strike-slip - each forming in a different way due to tension or compression in the crust. When friction along a fault is overcome, the fault will slip and move, causing seismic waves that produce shaking during an earthquake. The intensity of shaking and damage decreases further from the earthquake's epicenter.
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1) Students conducted an experiment to determine the relationship between force and acceleration by pulling a cart with varying numbers of rubber bands (1, 2, 3, 4) and measuring the cart's acceleration using a ticker tape timer.
2) Analysis of the ticker tape charts showed that as the number of rubber bands increased, representing greater force, the length of the strips increased, indicating higher average velocity over time intervals.
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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.
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The document discusses earthquakes and how they occur. It explains that earthquakes are caused by sudden movement along faults in the Earth's crust due to a build up of stress. There are three main types of faults - normal, reverse, and strike-slip - each forming in a different way due to tension or compression in the crust. When friction along a fault is overcome, the fault will slip and move, causing seismic waves that produce shaking during an earthquake. The intensity of shaking and damage decreases further from the earthquake's epicenter.
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This teacher's guide provides instruction for a series of lessons on solutions. The lessons are designed to gradually develop students' understanding of key concepts related to solutions through hands-on activities. Students will start by identifying solutions found in their home. Later activities explore the properties of solutions, what makes a solution saturated or unsaturated, and how temperature and solute size affect dissolution rates. The overarching goal is for students to understand common properties of solutions and factors that influence how quickly solids dissolve in water through guided scientific inquiries.
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This document defines typhoons and their development. It explains that typhoons form over warm ocean waters through the process of cyclogenesis, where converging winds and rising humid air lead to the formation of clouds and rotating storm systems. The Philippines is prone to typhoons because it is located in the western Pacific Ocean, an area where typhoons frequently develop and make landfall due to its warm waters and location within the typhoon belt.
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1) Students conducted an experiment to determine the relationship between force and acceleration by pulling a cart with varying numbers of rubber bands (1, 2, 3, 4) and measuring the cart's acceleration using a ticker tape timer.
2) Analysis of the ticker tape charts showed that as the number of rubber bands increased, representing greater force, the length of the strips increased, indicating higher average velocity over time intervals.
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