Earth and Life Science Formation of Rock Layers - 2021 PDF

Senior High School Earth and Life Science Quarter 1 – Module 11: Formation of Rock Layers CO_Q1_ ELS SHS Module 11 Earth and Life Science Alternative Delivery Mode Quarter 1 – Module 10: Movements of Plates and Formation of Folds and Faults First Edi...

Senior High School Earth and Life Science Quarter 1 – Module 11: Formation of Rock Layers CO_Q1_ ELS SHS Module 11 Earth and Life Science Alternative Delivery Mode Quarter 1 – Module 10: Movements of Plates and Formation of Folds and Faults First Edition, 2021 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 Secretary: Leonor Magtolis Briones Undersecretary: Diosdado M. San Antonio Development Team of the Module Writer: Chris B. De Jesus Editors: Erwin R. Abrencillo Jocelyn M. Manset Reviewers: Dominic P. Almirez, Franz Kevin Manalo Princess Paolah L. De Guzman, Marissa C. Betchaida, Louie L. Alvarez Gregorio M. De Chavez, Jr., Jocelyn M. Manset, Mario B. Maramot, Elaine T. Balaogan, Job S. Zape Jr., Avelyn A. Cajayon, Victoria M. Magpantay, Fernando M. Villanueva Illustrator: Ednelinda Robles, Cherry Amor Laroza Lovely Joy La Rosa, Charles Erick A. Jusay, Sandro Carlo B. Tablizo Layout Artist: Elizalde L. Piol, Anselma M. Ebero Jocelyn M. Manset Management Team: Wilfredo E. Cabral Job S. Zape Jr. Eugenio S. Adrao Elaine T. Balaogan Merthel M. Evardome Nadine C. Celindro Nicolas M. Burgos Mario B. Maramot Fe M. Ong-ongowan Rosalinda A. Mendoza Printed in the Philippines by ________________________ Department of Education – Region 4A CALABARZON Office Address: Gate 2 Karangalan Village, Brgy. San Isidro, Cainta, Rizal Telefax: 02-8682-5773/8684-4914/8647-7487 E-mail Address: [email protected]  Senior High School Earth and Life Science Quarter 1 – Module 11: Formation of Rock Layers Introductory Message 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 you’re 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.  What I Need to Know The content of this module focuses on the concepts of rock layer formation and its correlation. Every rock layer is, for the most part, one of various parallel rock layers that lies upon another which exhibits specific or similar characteristics. Since the concept about rocks and its types were discussed in the previous lesson, this module serves as a continuation of how rocks produce strata and what they may become once they are separated from its original rock layer. It also involves the possibilities of knowing the relative age of each rock layer due to the presence of fossils it contains. The module is divided into two lessons, namely: Lesson1: Rock Layers Lesson 2: Correlation of Rock Layers After going through this module, you are expected to: 1. describe how layers of stratified rocks are formed. 2. describe the different laws of stratigraphy. 3. determine how geologists correlate rock layers. 4. reflect on human environmental practices that may contribute to the alteration on the Earth surface, particularly the rock layers; and 5. illustrate an outcrop of rock layers applying the law of stratigraphy. 1 CO_Q1_ ELS SHS Module 11  What I Know Before you use this module, take the Pretest below. Directions: Read each item carefully. Choose the letter of the best answer and write the chosen letter on a separate sheet of paper. 1. Which field of science deals with the study of rock layers? A. Geology B. Paleontology C. Petrology D. Stratigraphy 2. Which processes most often cause fossil evidence to be preserved in rock? A. melting and faulting B. weathering and erosion C. folding and metamorphism D. cementation and deposition 3. Which of the following laws of stratigraphy gives emphasis on the assemblage of fossils embedded on rock layers. A. Law of Conformities B. Law of Superposition C. Law of Faunal Succession D. Law of Original horizontality 4. What can be concluded if a dike protrudes through several layers of rock? A. A batholith resides nearby. B. A volcano is within the area. C. It is formed before the rock layer. D. The rock layers are formed before the dike protrudes. 5. What can you infer when a sandstone comes in contact with a granite? A. The granite is older than the sandstone. B. The granite is younger than the sandstone. C. The granite was intruded into the sandstone. D. The granite and the sandstone have the same age. 6. Who proposed the Law of Uniformitarianism? A. Aristotle B. Nicolas Steno C. James Hutton D. James Chadwick 2 CO_Q1_ ELS SHS Module 11 7. Which principle states that the physical, chemical, and biological processes that work today are the same forces that worked in the past? A. Principle of Intrusions B. Principle of Unconformities C. Principle of Uniformitarianism D. Principle of Original Horizontality For item nos.8-10, refer to the diagram of rock strata to answer the questions that follow. 8. What principle of stratigraphy is depicted in the picture? A. Principle of Unconformities B. Principle of Uniformitarianism C. Principle of Original Horizontality D. Principle of Cross-cutting relationship 9. Which layer of rock is the youngest? A. Layer F B. Layer G C. Layer E D. Layer A 10. What is the correct sequence in the relative age of rock from youngest to oldest? A. Layer A, B, C, D, E, F, G B. Layer G, F, E, D, C, B, A C. Layer A, B, G, C, D, E, F D. Layer G, F, E, D, C, B, A 3 CO_Q1_ ELS SHS Module 11 11. Which type of dating method can be used in rock layers applying the Law of Superposition? A. Absolute Dating B. Isotopic Dating C. Radioactive Dating D. Relative Dating 12. According to the Law of Superposition, where are the oldest fossils usually found? A. somewhat near the surface B. at the top of the rock layers C. in the middle of the rock layers D. near the bottom of the rock layers 13. Which principle uses dikes and faults in sequencing events? A. Inclusions B. Faunal succession C. Original Horizontality D. Cross-cutting relationship 14. Which of the following is NOT generally part of angular unconformity? A. Erosion B. Folding C. Marine Regression D. Metamorphism 15. How is the principle of original horizontality described? A. All rocks were originally horizontal. B. Each layer of rock is older than the one above it. C. The original crust of the earth was almost perfectly flat. D. Layers of sediments are deposited in a nearly horizontal orientation. 4 CO_Q1_ ELS SHS Module 11  Lesson 1 Rock Layers Are the current features of the Earth the same as they were 4.6 billion years ago? Well, the answer is no. The Earth had undergone geological alterations and evolutionary processes that changed its features. The exogenic and endogenic processes that happened on the surface and within the inner portion of the Earth may contribute to these alterations that occurred. The rocks are being studied by geologists because they contain clues of what the Earth had been in the past. In this module, the formation of rock strata will be determined including the order of rock layers, the manner on how rock layers are formed or deformed due to physical factors and the age of rocks using the relative and absolute dating method. What’s In Before proceeding to the content of this module, let us first have a review on the learnings that you gained in our previous lesson related to rocks and rock cycle. Try to complete the rock cycle using the terms and the processes given. Write the term/s in the box/circles and processes/events in between the arrows to show the connections in the rock cycle. 5 CO_Q1_ ELS SHS Module 11  Notes to the Teacher The learners shall be given time to complete the rock cycle. This serves as the springboard for the lesson in rock layers. In the review, they may use the choices twice, thrice, and more according to the concept behind the rock cycle. The teacher may call a learner to discuss his/her output. What’s New If you will be given a cake for your birthday, how many layers do you wish to have? How many flavors do you want? What will be the order of flavor in each layer? If you apply pressure on cakes, it will be deformed, flattened, or twisted. Just like the layers in the cake, rocks can also form layers due to sediments deposited on rocks or some forces that act on it which causes its deformation. These are forces that may bring alteration to rock layers or the change in its formation in the Earth’s surface. 6 CO_Q1_ ELS SHS Module 11  What is It The idea behind the concept that the Earth is billions of years old originated in the work of James Hutton. Hutton concluded that there are forces that change the landscape of the Earth in the past. This conclusion is based on his observation in the geological processes that were taking place in his farm. His Principle of Uniformitarianism states that the current geologic processes, such as volcanism, erosion, and weathering, are the same processes that were at work in the past. This idea was refined by other geologists that although the process of the past and the present are the same, the rates of this process may vary over time. The Earth’s history was studied using the different records of past events preserved in rocks. The layers of rocks are like the pages in our history books. How are rock layers formed? Stratified rocks, also known as derivatives rock, may be fragmental or crystalline. These rocks are products of sedimentary processes. These are made of visible layers of sediments. The formation of rock layers depends on its stratigraphy and stratification. Stratigraphy Stratification It is also known as bedding, which It is the branch of geology that is the layering that happens in deals with the description, sedimentary and igneous rocks correlation, and interpretation of stratified sediments and stratified formed at the surface of the Earth rocks on and within the Earth. that comes from lava flows or other It is the study of the rock volcanic activity. layers(strata). It is expressed by rock layers Likewise, it will give you clues to (units) of a general tabular or the location of ancient seas, lenticular form that differ in rock mountains, plateaus and plains. type. As early as the mid 1600s, Danish scientist Nicholas Steno studied the relative position of sedimentary rocks. Sedimentary rocks are formed particle by particle, bed by bed, and the layers are piled one on top of the other. These rock layers are also called strata. 7 CO_Q1_ ELS SHS Module 11 Stratigraphic Laws Stratigraphic laws are basic principles that all geologists use in decoding or deciphering the spatial and temporal relationships of rock layers. These include the following: Original Horizontality, Lateral Continuity, Superposition, Cross Cutting, Law of Inclusions and the Law of Faunal Succession. Law of Superposition Law of Inclusions The largest and heaviest rock A rock mass that contains layer that settled first at the pieces of rocks called bottom is the oldest rock layer. inclusions are younger than The lightest and smallest that the other rock masses. settled last is the youngest rock layer. LAWS OF STRATIGRAPHY Law of Cross Cutting Law of Original Horizontality Relationship sediments are deposited in a fault or dike- a slab rock flat layers, if the rock cuts through another rock maintains in horizontal when magma intrudes to the layers, it means it is not yet rock, that fault or magma is disturbed and still has its younger than the rock original horizontality Law of Unconformities Law of Faunal Succession rock layers that are formed without interruptions are first recognized by William conformable. Smith Describes a layer of rock that different strata contain have been deformed or eroded assemblage of fossils by which before another layer is rocks may be identified and deposited, resulting in rock layer correlated over long distances mismatching 8 CO_Q1_ ELS SHS Module 11  Figure 1. The Steno’s Law of Stratigraphy The Law of Stratigraphy shown -in Figure 1 indicates deposition, reshaping and deformations of the rock layers due to geological processes. Three Types of Unconformities: Disconformity Angular unconformity It originates from horizontally It originates from horizontal parallel strata of sedimentary sedimentary rock layers that is rock that are deposited on tilted lifted and the top layers eroded. and eroded layers. New sediments are deposited It produced an angular when they are submerged discordance with underlying beneath a freshwater or horizontal layers. saltwater. Non -conformity It originates between sedimentary rocks, metamorphic or igneous rock when sedimentary rock lies above and was deposited on the pre-existing and eroded metamorphic or igneous rock. 9 CO_Q1_ ELS SHS Module 11  What’s More Activity 1.1 - Who’s Older, Who’s Younger? The rock layers below labelled A to F undergo a sedimentary process that results in changes in rock form. Use the diagram of a rock layer below to complete and answer the questions. Guide Questions: 1. In what layer was the first rock formed? ________ 2. What letter is the second layer of the rock? ________ 3. What happens in the rock represented by letter D? (cutting, or insertion) _______ 4. What three layered letters is cut by letter D? ________ 5. What takes place in letter F? (fault, folds) ________ 6. What environmental factors occur in letter E? (weathering and erosion, volcanic eruption) ________ 7. Which rock layer is the oldest? ________ 8. Which rock layer is the youngest? ________ 9. Which layer describes the law of horizontal continuity? ________ 10. Which layer shows an angular conformity? ________ 10 CO_Q1_ ELS SHS Module 11 Activity 1.2 Word Pool Read the words in the box and the statements below. Fill the blanks with the words/phrases that best complete the sentences. cross-cutting sedimentary erosion stratification extrusive superposition fault unconformity intrusion younger 1. The process in which sedimentary rocks are arranged in layers is called _________________. 2. The law of _________________ relationship happens when a layer of rocks torn apart and igneous rock fill in the spaces. 3. On the Earth’s surface, weathering and _________________ make rock fragments. 4. The law of _________________ states that sedimentary rocks are layered from the oldest to the youngest and oldest rocks are found at the bottom. 5. A/an _________________ is a break in the rocks that make up the Earth’s crust, along which rocks on either side have moved past each other. 6. A/an _________________ rock is formed when a magma never makes it to the surface. 7. In the law of _________________ rock was uplifted, eroded from the surrounding rock, and will be replaced by sediments. 8. A/an _________________ rock is formed by the accumulation, deposition, and cementation of organic particles or minerals. 9. When lava solidifies upon reaching the surface, it usually forms a/an _________________ rock in rock layers. 10. Rock that forms intrusions on other rocks is _________________ than the other rock layer. 11 CO_Q1_ ELS SHS Module 11 Activity 1.3 Match it! Match the descriptions in Column A with the terms in Column B. Choose the letter of the correct answer. COLUMN A COLUMN B 1. Unconformities are sedimentary rock layers that are tilted to form a A. Superposition wave or angle in rock layers. 2. Rock layers contain embedded fossils by which rock may be B. Angular conformity identified. 3. Magma intrudes to the rocks; this C. Cross cutting relationship magma is younger than the rock. 4. Exist between sedimentary and metamorphic rocks when sedimentary rocks lie above and were deposited in the pre-existing D. Faunal Succession and eroded rocks. 5. Largest and heaviest rock layer that settled first at the bottom is the oldest rock layer: E. Non conformity Activity 1.4 Brain Pop Study the rock strata on the right and try to answer the questions in the left. 1. What geologic process takes place in cracks or breaks in the rock? 2. If an igneous rock is introduced in the breaks, what law of stratigraphy best explains this occurrence? 3. How will you characterize the dikes in the cracks, is it older or younger than layer F? 4. What law best describes the position of rock layers in layer A to F 5. Which is younger, layer F or the intrusions in the rock? 12 CO_Q1_ ELS SHS Module 11  Lesson Correlation of Rock Layers 2 Have you experienced playing or fitting cut out patterns or puzzles? One of the pieces of evidence used by geologists in tracing the history of the Earth was with the identifications and the correlations of rock layers. Rock layers were subjected to alteration due to different geologic processes that act or apply on it. Such forces could result in tilting, uplifting, compression, and subductions of rock layers. These rock layers have the tendency to be separated from each other. One way of how these rock layers are identified is with the utilization of correlation. Why do geologists need to correlate rock layers? The history of earth is preserved in its rock layers. Unfortunately, no single location on earth has a continuous set of layers due to erosion or ceased deposition. Instead, geologists study rock sequences at many places around the world, measure the depth of the layers, record what kind of rock is in each layer, and see if there are any fossils present. Geologists represent the layers of rock by drawing a picture of the sequence – this is called a stratigraphic column. Geologists need to correlate rocks from one place to another to get a more complete record of Earth’s history over time. They try to determine the relative age of widely separated strata or rock layers. They used correlation, trying to fit together sedimentary strata in different places, just like a cut-out puzzle. What’s In In the previous lesson, you had learned that rock layers may undergo different formations due to several geologic processes taking place in each rock layer. These concepts of stratigraphy are all stated in the Steno’s Law of Stratigraphy. 13 CO_Q1_ ELS SHS Module 11 Let us find out if you can still remember how this law can characterize each rock layer pictured below. Identify the pictures which are best explained by the Laws of Stratigraphy in the box below. Choose the letter of the correct answer. A. Original Horizontality D. Superposition B. Cross Cutting Relationship E. Unconformity C. Lateral Continuity What’s New How do geologists correlate rock layers? The process of showing that rocks or geologic events occurring at different locations are of the same age is called correlation. Geologists have developed a system for correlating rocks by looking for similarities in composition and rock layer sequences at different locations. The geological technique of correlation provides information that has taken place in Earth’s history at various times that occurred. There are different methods in correlating rock layers, these include: 1. Rock types and its characteristics ⮚ color, texture, hardness, composition, or its mineral content ⮚ the harder and more densely packed the particles are, the older the rock and the deeper the layer it came from. 14 CO_Q1_ ELS SHS Module 11  2. Index fossil ⮚ also known as guide fossils or indicator fossils, are fossils used to define and identify geologic periods (or faunal stages) 3. Bedrock ⮚ a deposit of solid rock that is typically buried beneath soil and other broken or unconsolidated material (regolith). ⮚ made up of igneous, sedimentary, or metamorphic rock, and it often serves as the parent material for regolith and soil. How to match correlate rock layers? Matching of rock layers may be determined by merely looking at its features. Look at the three columns of rock layers below. Let us determine how they are correlated. Figure 2. Stratigraphic Column in Different Location These three columns represent rock layers from three separate locations or outcrops. Some columns may be missing layers due to erosion. No single column represents a complete record. Your job is to line them up, so a complete record of the region can be seen. Find one or more layers present in all columns that can be matched like a puzzle. 15 CO_Q1_ ELS SHS Module 11  Figure 3. Stratigraphic Column Matching up of Rock Layers Figure 4. Strategic Column Fitting of the Rock Layers After matching correlated rock layers, we can determine the relative age of each layer according to the law of superposition. Limestone in location A is the oldest and limestone in location C is the youngest rock layer. While those rock layers having the same composition, textures, and fossil content were considered as rock layers with the same age. In matching up rock layers, superposition and crosscutting are helpful. When rocks are touching one another, the lateral continuity rock layers aid to match up with the layers that are nearby. Geologists then match, or correlate, the different shorter sequences to create a geological column that spans further back into earth’s past. Correlations involve matching a particular rock unit in one exposure with its counterpart at a different locality. By correlating various rock vulnerabilities separated by great distances, geologic maps can be constructed, and the original geographical extent of the rocks can be estimated. 16 CO_Q1_ ELS SHS Module 11 Types of Correlation A) Physical Correlation is accomplished by using several criteria such as color, texture, and types of minerals contained within a stratum which make it possible for geologists to classify a stratum specifically. B) Fossil Correlation is a principle that geologists use to determine the age of rock. It uses fossils with unique characteristics, such as geologically short lifespan and easily identifiable features, and uses this information to estimate the age of a rock layer in other areas that contain the same type of fossil or group of fossils. There are fossils which are used to date the layers of rock that they are found in. Fossils that can be used in this way are called index fossils, and rock layers with the same index fossils in them can be correlated. Criteria to be considered in identifying index fossils include: 1. The fossilized organism must be easily recognizable, and it must be easy to identify because of its uniqueness. 2. Fossils must be geographically widespread or found over large areas so that it can be used to match rock layers separated by huge distances. 3. Fossils must have lived for only a short time, so that it appears in only the horizontal layer of sedimentary rocks. 17 CO_Q1_ ELS SHS Module 11  What’s More Activity 1.5 Mind Tickle A. Look at the columns of rock layers. Analyze each figure and answer the questions that follow. Analysis: 1. Arrange the rock layer from oldest to youngest. Use the number in the designated rock layers. Youngest _____ _____ _____ _____ _____ _____ _____ Oldest _____ 2. Is the intrusion of igneous rock younger or older? _________ 3. What rock layer is common in each rock column? _________ 4. What environmental condition takes place in rock layer no.3? (Fault, erosion) 5. In what earth’s feature is the rock layer in outcrop C probably located? (Volcano, sea) 6. Which outcrop/s show examples of unconformity? ___________ 7. What type of igneous rock maybe deposited in outcrop C? (Batholith, granite) 8. Which layer is considered as the beds? ___________ 9. Which outcrop/location shows subsidence? _______ 10. What geologic process happens in outcrop B? (Folding, fault) 18 CO_Q1_ ELS SHS Module 11 B. Building Vocabulary Words Arrange the scrambled letters of the term/s being described by the given statement. TERMS DESCRIPTIONS It is the action of the process of forcing the body of 1. I N T U I S O I R N igneous rock between sedimentary rocks. 2. D X N E I S S O F L I - It is used to define and identify geologic periods. -The action of surface processes that removes soil, 3. N E O R I S N O rock, or dissolved material from one location to another. It is made up of sedimentary and igneous rock that 4. K R O C Y S R L E A was formed at the Earth’s surface. The process of showing that rocks or geologic events 5. N O R L T O I E C R A occurring at different locations are of the same age. What I Have Learned Activity 1.6 Sum It Up! Read the statement in each item and choose the correct answer in the parenthesis. Identify the law or principle of stratigraphy being described by the given statement. 1. A piece of granite contained within a sandstone would be (older, younger than the sandstone. This is an example of the principle of ______________________________________. 2. A fault cutting through a series of layers of rocks is (older, younger) than the rock layers. This is an example of the principle of ______________________________________. 3. In a series of layers, the youngest layer is on the (bottom, middle, top) of the sequence. This is an example of the principle of ______________________________________. 4. Sedimentary rocks that are folded must be (older, younger) than the forces which deformed them. This is an example of the principle of ______________________________________. 5. In undisturbed layers of rocks, sediments that form sedimentary rock are deposited in horizontal layers that are (younger, older) This is an example of the principle of ______________________________________. 19 CO_Q1_ ELS SHS Module 11 Things to Ponder ⮚ Most sedimentary rocks are laid down in flat, horizontal layers. ⮚ Stratigraphy is the science that deals with characteristics of layered rocks and how these rocks are used to trace the history of the Earth. ⮚ Stratification is the layering that happens in sedimentary and igneous rocks which formed at the surface of the Earth that comes from lava flows or other volcanic activity. ⮚ Rock layers are called strata. ⮚ Law of cross-cutting relationships happens when a fault or dike or magma that intrudes into the rock, is younger than the rock. ⮚ Law of inclusions is when the rock mass with inclusion is younger. ⮚ Law of original horizontality is a flat rock that maintains its horizontal layer without being distracted for a long period of time. ⮚ Law of superposition states that older rock layer is found at the bottom while younger rock layer is found at the top. ⮚ Law of faunal succession states that different rock layers contain particular fossils by which the rocks may be identified and correlated. ⮚ Law of unconformity implies a substantial gap or break in rock layer sequence due to uplift and erosion. ⮚ Index fossil are fossils used to define and identify geologic periods. 20 CO_Q1_ ELS SHS Module 11  What I Can Do From the lists of human activities and practices, tell how these practices may trigger the alterations of rock layers. Human Activities/Practices How it will affect the rock layers? 1. Mining 2. Quarrying 3. Kaingin system of farming 4. Converting elevated areas into subdivisions and roads 5. Forest denudation Analysis: 1. Which in the list of human practices can be considered as detrimental to human and other living things? 2. What will be the impact of this human practices in geological processes such as weathering and erosion? 3. How will you address the result of these practices and its magnitude to the government since your generation are considered as the hope of the motherland? 21 CO_Q1_ ELS SHS Module 11  Assessment Directions: Read each statement and choose the letter of the correct answer. 1. What is the relative position of the oldest rock layer as stated in the principle of Superposition? A. at top B. at the bottom C. at the middle D. at random location 2. Which process is involved when sedimentary rocks are arranged in layer? A. Deposition B. Foliation C. Sedimentation D. Stratification 3. Which term in the list is associated with rock layers? A. Defoliation B. Extrusion C. Intrusion D. Strata 4. What type of rock/s usually undergo cross- cutting on rock layers? A. Igneous Rock B. Metamorphic Rock C. Sedimentary Rock D. Stratified Rock 5. Why is there a need for correlation of rock layers? A. It gives the relative age of the rocks. B. Fossils embedded in the rock layers serve as a proof of their correlation. C. It provides information that the rock layers are connected to each other long ago. D. All of the above 6. Which principles states that geological processes operating at the present time are same processes that have operated in the past? A. Cross-cutting relationship B. Original horizontality C. Uniformitarianism D. Inclusion 22 CO_Q1_ ELS SHS Module 11 7. Which of the following shows a method of correlation? A. similarity of rock types B. presence of index fossil C. sequence of mineral content on rock D. all of the above 8. If an igneous rock A crosscuts sedimentary rock B, what will be the relative age/position of igneous rock A? A. Igneous rock A will be on top of rock B. B. Igneous rock A is older than sedimentary rock B. C. Igneous rock A is younger than sedimentary rock B. D. Igneous rock A is at the same age with sedimentary rock B. 9. Which of the following is NOT a type of unconformity? A. Angular B. Disconformity C. Nonconformity D. Uniformity 10. When sedimentary rocks deposited in flat layers are left undisturbed it follows the statement in which of the given principles? A. Cross-cutting Relationship B. Fauna Succession C. Original Horizontality D. Superposition 11. What can be inferred if you find an outcrop of mud cracks in gray shale? It can be inferred that the area was once ________. A. a beach B. a desert C. a tidal flat D. deep under the ocean 12. Which of the following occurrences alters a rock layer quickly? A. earthquakes B. rain C. rivers D. snow 13. What makes index fossils useful in identifying the relative age of rocks? A. They are short-lived. B. They are radioactive. C. They are old enough to be analyzed. D. They are present in both young and older rocks. 23 CO_Q1_ ELS SHS Module 11 14. Which type of conformities state that sedimentary rocks, when tilted or folded, are overlain by more flat- lying layer of rock? A. Angular Conformity B. Disconformity C. Nonconformity D. Inclusion 15. What will be the position of the youngest beds in undisturbed sedimentary deposits? A. They stay at the bottom. B. They are found on the top rock layer. C. Youngest beds are separated from sedimentary deposits. D. Neither b nor c 24 CO_Q1_ ELS SHS Module 11  Additional Activities Illustrate an outcrop of a rock layer applying the principle or the laws of stratigraphy similar to your previous activity. Use the legend of what will be present in these particular layers in the outcrop. The guide of what you’re going to put in your outcrop are found in the table below. Indicate them in your outcrop or block diagram. Be creative in presenting your output. Place your illustration in the box. Label Description This was the last layer to be formed before the rocks Lost before tilt tilted. Oldest rock The rock layer is below all the others. Youngest rock This is the younger rock above all the others. Second oldest rock The rock layer is just above the oldest. It is the thinnest rock layer found between the fifth Thinnest rock and the third rock layer This layer forms on top of earlier rocks after it was Above the erosion tilted and eroded away. 25 CO_Q1_ ELS SHS Module 11  Module 11 CO_Q1_ ELS SHS 26 ACTIVITY 1.5 B ACTIVITY 1.2 LESSON I: Rock Layer Stratification What I Know Intrusion Cross-cutting Relationship 1. D Index fossil Erosion 2. D Erosion Superposition 3. C Rock layers Fault 4. A Correlation Intrusion 5. A Unconformity 6. C What I’ve Learned Sedimentary 7. C Unconformity, younger Extrusive 8. D Cross cutting, younger 9. B Younger Superposition, top 10. B ACTIVITY 1.3 Angular conformity 11. D B Original horizontality, younger 12. D D 13. D C 14. D Assessment E 15. D B A D Activity 1.4 C ROCK LAYER 1 Fault C What’s in Cross cutting D Magma Younger C Solidification Superposition D Igneous Rock Intrusion is younger D Weathering and Erosion LESSON 2: CORRELATION D Sediments C What’s In Deposition and burial D D Weathering and erosion A A Sedimentary rock D E Weathering and erosion C C Metamorphism 15. B B tamorphic Rocks ACTIVITY 1.5 A 12.Heat and pressure Youngest - 6 13.Melting 4 14.Weathering and erosion 1 What's More 7.9 ACTIVITY 1.1 2 B 10 A 3 Cutting 5 C,A,B Oldest 8 Fault Younger Erosion 3.Layer 7 A 4.Erosion E 5.Volcano C 6.Location C & D 10. B 7.Batholith 8.Layer 8 9.Location A or Outcrop A 10.Folding Answer Key Rubrics for the Additional Activities Criteria 4 3 2 1 Organization Exceeds all of As specified in One or more of Several the the directions/ the needed necessary requirements instructions, elements as component outlined in the include all of mentioned in s are guidelines and the essential the missing instructions. elements. directions/instr from the uctions are not outcrop present. Creativity Exceptionally Thoughtfully A few unique Shows little intelligent and and distinctively touches creativity, one-of-a-kind delivered; at improve the originality in times smart in project and and/or demonstrating demonstrating demonstrate a effort in profound comprehension grasp of the understand comprehensio of the topic material. ing the n material Content Demonstrates Demonstrates Demonstrates a Does not a comprehension fairly limited demonstrat comprehensive of the lesson's comprehension e knowledge of main concepts of the lesson. comprehen the work's sion of the topics lesson Misses plot points and has several misinterpre tations 27 CO_Q1_ ELS SHS Module 11 References BOOK Olivar II, Tolentino, Jose et al. 2016. Earth Science. Phoenix Publishing House ELECTRONIC RESOURCES Astro, accessed February 18,2019, http://astro.hopkinsschools.org/course_documents Global, accessed May 20,2020, https://global.oup/us/companion.websites Introduction to Stratigraphy, accessed February 19,2019, http://grandcanyonnaturalhistory.com/pages_nature/geology/intro-to- strata.html Natural Trust for Historic Preservation, accessed February 19, 2019, https://savingplaces.org/place/grand-canyon#XGyrBh7mgSw.html Nature, accessed February 19,2019, https://www.nps.gov.nature Quora, accessed February 19,2019, http://ww.quora.com Relative Rock Layers, Science Learning Hub, accessed May 31, 2020, https://www.sciencelearn.org.nz/labelling_interactives/4-relative-rock-layers Rocks and Layers, USGS, accessed February 18,2019, http://pubs.usgs.gov/gip/fossils/rocks-layers.html Sedimentary Rock, accessed February 19,2019, https://en.m.encyclopedia.org.wiki>sedimentary/rock Stratification, Encyclopedia Britannica, accessed February 19,2019, http://www.britannica.com/science/stratification-geology Stratum, Wikipedia, accessed February 18,2019, https://en.m.wikipedia.org/wiki/stratum Stratified Rocks, accessed May 20,2020, https://mindat.org/glossar/stratified_rocks 28 CO_Q1_ ELS SHS Module 11 For inquiries or feedback, please write or call: Department of Education - Bureau of Learning Resources (DepEd-BLR) Ground Floor, Bonifacio Bldg., DepEd Complex Meralco Avenue, Pasig City, Philippines 1600 Telefax: (632) 8634-1072; 8634-1054; 8631-4985 Email Address: [email protected] * [email protected]