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An introduction to plate tectonics, explaining the structure of the earth's surface, the concept of tectonic activity, and the different types of plate boundaries. It includes activities, questions, and exercises designed to help students understand the relationship between tectonic plates, earthquake epicenters, and active volcanoes. The document also covers the formation of geological features such as mountain belts, oceanic ridges, and trenches.
Typology: Schemes and Mind Maps
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SCIENCE– Grade 10 Alternative Delivery Mode Quarter 1 – Module 1: Earth and Space Revised Edition, 202 2 Republic Act 8293, section 176 states that: No copyright shall subsist in any work of the Government of the Philippines. However, prior approval of the government agency or office wherein the work is created shall be necessary for exploitation of such work for profit. Such agency or office may, among other things, impose as a condition the payment of royalties. Borrowed materials (i.e., songs, stories, poems, pictures, photos, brand names, trademarks, etc.) included in this module are owned by their respective copyright holders. Every effort has been exerted to locate and seek permission to use these materials from their respective copyright owners. The publisher and authors do not represent nor claim ownership over them. Published by the Department of Education Sec: Sara Z. Duterte-Carpio Printed in the Philippines by ________________________ Department of Education – National Capital Region – SDO VALENZUELA Office Address: Pio Valenzuela St., Marulas, Valenzuela City Telefax: (02) 292 – 3247 E-mail Address: [email protected] Development Team of the Module Writers: Czarina Bea Saberon Jeanne E. Acelo Mylene Rosco Ada D. Laguitan Flerida P. Velez Jovit Angelo L. David Zacarie Jo P. Del Rosario Donna Marie P. Sabalza Marivic S. Ferrer Earlene G. De Vera Eric M. Masela Jonathan A. Aballe Ma. Suzette S. Falcunitin Mark E. Embuido Alma V. Manalo Juanito D. Bartolome Jr Irene C. Cular Edward A. Ramos Jai Rabbai A. Eugenio Agnes B. Panuncialman Florida B. Cabrera Maricar DR. Espiritu Clarissa Igana Mark Kenneth D. Mongaya Marion Edward P. De Guzman Reviewers: Amelita V. Yumang, Ed. D., Juliana T. Alvarez Editors: Zacarie Jo P. Del Rosario, Donna Marie P. Sabalza, Kelvin T. Silvestre Illustrator: Jayson P. Delechos Layout Artist: Zacarie Jo P. Del Rosario, Roselle G. Hutamariz Management Team: MELITON P. ZURBANO, Schools Division Superintendent FILMORE A. CABALLERO, CID Chief JEAN A. TROPEL, Division EPS In-Charge of LRMS MA. LEA Q. PRONDO Education Program Supervisor – Science
This Self-Learning Module (SLM) is prepared so that you, our dear learners, can continue your studies and learn while at home. Activities, questions, directions, exercises, and discussions are carefully stated for you to understand each lesson. Each SLM is composed of different parts. Each part shall guide you step-by- step as you discover and understand the lesson prepared for you. Pre-tests are provided to measure your prior knowledge on lessons in each SLM. This will tell you if you need to proceed on completing this module or if you need to ask your facilitator or your teacher’s assistance for better understanding of the lesson. At the end of each module, you need to answer the post-test to self-check your learning. Answer keys are provided for each activity and test. We trust that you will be honest in using these. In addition to the material in the main text. Notes to the Teacher are also provided to our facilitators and parents for strategies and reminders on how they can best help you on your home-based learning. Please use this module with care. Do not Put Unnecessary marks on any part of this SLM. Use a separate sheet of paper in answering the exercises and tests. And read the instructions carefully before performing each task. If you have any questions in using this SLM or any difficulty in answering the tasks in this module, do not hesitate to consult your teacher or facilitator. Thank you.
According to the plate tectonics model, the entire lithosphere of the Earth is broken into numerous segments called tectonic plates. The plates move very slowly but constantly. Get a hard-boiled egg and strike it with a spoon until the shell is cracked in several places. This is what the lithosphere is like. At the end of this unit, the learners are expected to: ● Describe and relate the distribution of active volcanoes, earthquake epicenters, and major mountain belts to Plate Tectonic Theory (S10ES – Ia-j-36.1). Directions: Encircle the letter of the BEST answer.
Have you ever wondered more about our lithosphere? Have you ever wondered about its characteristics? its interior? Well, the lithosphere is the solid, outer part of the Earth, including the crust and the upper portion of the mantle. This part of the module will focus on the outermost layer which is called the crust. We will find out more about such as our course discussion proceed.
Notes to the Teacher This module is an interactive module that includes the overview, pre assessment, discussion proper, activities and post assessment. In this lesson, it is focused on describing and relating the distribution of active volcanoes, earthquake epicenters, and major mountain belts to Plate Tectonics Theory. Activity: Decode Me Directions: Replace the number with the corresponding letter as indicated in the code to unlock the hidden word. Describe the word. A=1, B=2, C=3, D=4, E=5, F=6, G=7, H=8, I=9, J=10, K=11, L=12, M=13, N=14, O=15, P=16, Q=17, R=18, S=19, T=20, U=21, V=22, W=23, X=24, Y=25, Z=
Earth’s surface is covered by a layer of rock called crust. The crust is part of the top layer of Earth called the lithosphere. Crust is the outermost solid shell which is made of a variety of solid rocks and made up of mostly oxygen, silicon, aluminum, iron, sodium, potassium and magnesium. It has an average density of 2.8 g/cm^3 and its thickness ranges from 5 to 50 km. The crust is thickest in a part where a relatively young mountain is present and thinnest along the ocean floor. According to the plate tectonics model, the entire lithosphere of the Earth is broken into numerous segments called tectonic plates. The plates move very slowly but constantly. CONTINENTAL CRUST VS OCEANIC CRUST You will notice from Figure 1.2. that Earth's crust is divided into two types: the thicker but less dense continental crust and the oceanic crust which is relatively thinner but denser than continental crust. Figure 1.2. Types of crust Tectonic plates can transport both continental crust and oceanic crust, or they may be made of only one kind of crust. Oceanic crust is denser than continental crust. At a subduction zone, the oceanic crust sinks into the mantle beneath lighter continental crust. It’s important to know what type of crust covers a tectonic plate because the type of crust determines what happens at a boundary between plates. Continental Crust
The earth’s interior is divided into three layers namely crust, mantle and core. Each layer is different on thickness, temperature and minerals present. In Figure 1.4, Lithosphere is the upper portion and outer part of the earth that is composed of crust and upper mantle. Beneath the lithosphere is the asthenosphere which is the soft, weak upper portion of the mantle where the lithospheric plates float and move around. The heat in the mantle creates convection current. The movement in the mantle causes the plate to lift, split and move around. This convection causes the lithospheric plates (Fig. 1.3) to break and crack due to slowly moving current underneath the Earth’s surface. SEVEN MAJOR PLATES
Activity 1.1: Continental vs Oceanic Crust Directions : Look at the picture below. Fill in the Venn diagram to compare and contrast continental and oceanic crust.
Activity 1.2 : Identify This Directions: Identify the 7 major lithospheric plates pointed to by the labels A, B, C, D, E, F, and G. Activity 1.3: Seismic Waves Directions: Complete the table. TYPE OF SEISMIC WAVE COMPARISON IN TERMS OF SPEED CAN TRAVEL THROUGH MOVEMENT TYPE STRENGTH IN TERMS OF DESTRUCTION P-wave S-wave Surface waves Answer the following questions:
Why is the lithosphere broken into plates? What do you think is the importance of understanding the mechanism of tectonic plates? Explain.
Directions: Encircle the letter of the BEST answer.
Activity: Decode Me rth the outermost solid layer of the Ea - 1.CRUST the solid, outer part of the Earth co posed of crust and upper - 2.LITHOSPHERE mantle the hot and very dense center of the Earth made up of iron and nickel.- 3.CORE heated core and its thin outer- lies between Earth's dense, super - 4.MANTLE r, the crust laye means relating to the structure of the Earth's surface or crust- 5.TECTONIC Continental vs Oceanic Cr Activity 1.
Identify This Activity 1. A. North American Plate B. Pacific Plate an Plate C. South Americ D. Eurasian Plate E. African Plate Australian Plate- F. Indo G. Antarctic Plate Seismic Waves Activity 1. TYPE OF SEISMIC WAVE COMPARISON IN TERMS OF SPEED CAN TRAVEL THROUGH MOVEMENT TYPE STRENGTH IN TERMS OF DESTRUCTION Fast wave- P Solid, uid, Gas Liq Destructive Parallel Perpendicular Solid Slower wave- S Less Destructive Solid Slowest Surface waves Horizontal/ Vertical Most Destructive (Answers may vary) (Answers may vary)
Complete Me Activity 1.Lithosphere
“Earthquake - Natural Disaster Manangement". 2022. Sites.Google.Com. https://sites.google.com/site/disasterportal/earthquake."Kinds Of Crust - Google Search". 2022. Google.Com. https://www.google.com/search?q=kinds+of+crust&source=lnms&tbm=isch &sa=X&ved=2ahUKEwjL7aXj8aPpAhXUc94KHZVIDQQQ_AUoAXoECA8QAw &biw=931&bih=445#imgrc=9-J485ssWwROOM. "Mt. Everest From Space". 2022. NASA. https://www.nasa.gov/multimedia/imagegallery/image_feature_152.html. "Seismic Waves". 2022. Earth Science
. Pavico, J.M., Ramos, A.C.M., Bayquen, A.V., Silverio, A.A., & Ramos, J.D.A.(2015). Exploring Life Through Science Series The New Grade 10. Phoenix Publishing House, INC. "Plate Tectonics". 2022. Phet. https://phet.colorado.edu/en/simulation/plate- tectonics. Science 10 Learner’s Module Science 10 Teacher’s Guide "The Structure Of The Earth And Plate Tectonics". 2022. Slideshare.Net. https://www.slideshare.net/mobile/stevenheath148/plates- 36189164. "7 Major Tectonic Plates: The World's Largest Plate Tectonics - Earth How".
In Grade 9, you have learned why areas along the Pacific are prone to earthquakes and volcanic eruptions. This is because the region comprises the so- called Ring of Fire. This module describes how plate dynamics leads to the formation and distribution of the world's active volcanoes, earthquake epicenters, and mountain ranges. At the end of this unit, the learners are expected to: ● Describe and relate the distribution of active volcanoes, earthquake epicenters, and major mountain belts to Plate Tectonic Theory (S10ES – Ia-j-36.1). Directions: Encircle the letter of the BEST answer. 1.Where do earthquakes usually happen? A. Oceans C. Mid continents B. Continents D. Edge of the Continental and Oceanic plate 2.Which region is the least prone to earthquakes? A. Southeast Asia B. Uppermost part of Europe C. Western portion of North America D. Western portion of South America
Notes to the Teacher This module is an interactive module that includes the overview, pre assessment, discussion proper, activities and post assessment. In this lesson, it is focused on describing and relating the distribution of active volcanoes, earthquake epicenters, and major mountain belts to Plate Tectonic Theory.
Are you familiar with the triangulation method as a way of determining an earthquake epicenter? Are you already aware of the different location of the world's active volcanoes, earthquake epicenters, and mountain ranges? How will you be describing the distribution of active volcanoes; earthquake epicenters and mountain ranges? Is there any relation among plate tectonics, earthquake epicenters and active volcanoes? We will find the answers to all of that as our course discussion occurs. Activity: Plate Tectonics Directions: Fill in the K-W-H-L Chart below to assess your prior knowledge and understanding of the topic regarding plate dynamics which leads to the formation and distribution of the world's active volcanoes, earthquake epicenters, and mountain ranges.
What do I know? What do I want to find out? How can I found out what I learn? What did I learn?
In your Grade 8 Science, you were taught that earthquakes originate from the Focus. Seismologists need to record the location of Focus in the world map but it’s deep within the Earth’s surface. They instead use the Epicenter to mark the focus’ location on the Earth’s crust because it’s located on the Earth’s surface just above the Focus. Seismologists can determine the epicenter of an earthquake by using the Triangulation Method. As earthquakes occur, seismic waves are released and received by seismic stations. These seismic stations will provide how far it is from the epicenter. Triangulation Method provides the location of an earthquake epicenter by using three seismic recording stations. P waves and S waves interval in time arrival is used to calculate the distance of recording station from the epicenter. The plates are moving and interact along their edges. When this happens, important geological processes take place, such as the formation of mountain belts, earthquakes, and volcanoes which also serve as the basis in dividing the Earth’s lithosphere into plates. The world’s earthquake epicenters are not randomly distributed over the Earth’s surface. They tend to be concentrated in narrow zones. Some are located near the edges of the continents; some are in mid continents while others are in the oceans. Earthquake epicenters and volcanoes are both situated at the same locations. Locating the epicenter of an earthquake is very important to determine which fault lines are active. In that way, people will be aware of the places prone to earthquakes, thus, be able to take safety precautionary measures. Activity 2.1: Earthquake’s Epicenter Directions: Locate the epicenter of an earthquake using triangulation method.
Q2. What difficulty will you encounter if you only have data from two recording stations?
Activity 2.2: Mapping Earthquake Epicenters and Active Volcanoes Directions: Plot the active volcanoes, earthquake epicenters, and major mountain belts. MATERIALS - World map with longitude and latitude - Two markers (blue and red)
Activity 2.3 : Describe Me! Where Am I? Directions : Describe the distribution of active volcanoes, earthquake epicenters, and major mountain belts. Study the picture showing the distribution of active volcanoes and earthquake epicenter around the world and answer the following questions. Figure 2.3. Global distribution of active volcanoes and earthquake epicenter Figure 2.4. Map of world mountain ranges, volcanoes and earthquake Guide Questions:
Figure 2.5. Tectonic Plates Guide Questions:
Answer the following questions: