earth science quarter 2- module 11 stratified rocks, Summaries of Earth Sciences

Download earth science quarter 2- module 11 stratified rocks and more Summaries Earth Sciences in PDF only on Docsity! a DepED DEPARTMENT Wf OF EDUCATION Earth Science for STEM Quarter 2 - Module 11: Relative and Absolute Dating CO_Q2_ESS SHS Module 11 Earth Science for STEM Alternative Delivery Mode Quarter 2 —- Module 11: Relative and Absolute Dating 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 Editors: Illustrator: Development Team of the Module Writer: Jorgie A. Aguado Reviewers: Czarina Portia M. Villalobos, Jessica H. Cabaces, Cyrus T. Festijo Layout Artist: Annaliza Q. Aviles Management Team: Francis Cesar B. Bringas Job S. Zape Jr. Ramonito O. Elumbaring Reicon C. Condes Elaine T. Balaogan Fe M. Ong-ongowan Sacoro R. Comia Fe M. Fallurin Marieta N. Perez Printed in the Philippines by Department of Education — Region IV-A CALABARZON Office Address: Telefax: E-mail Address: Gate 2 Karangalan Village, Barangay San Isidro Cainta, Rizal 1800 02-8682-5773/8684-4914/8647-7487 region4a@deped.gov.ph What I Need to Know This module was designed and written with you in mind. It is here to help you master the nature of Biology. The scope of this module permits it to be used in many different learning situations. The language used recognizes the diverse vocabulary level of students. The lessons are arranged to follow the standard sequence of the course. But the order in which you read them can be changed to correspond with the textbook you are now using. In this lesson, the learner will identify relative and absolute dating. To achieve this learning competency, the learner should explain how relative and absolute dating was used to determine the subdivisions of geologic time. After going through this lesson, you are expected to: 1. Define relative and absolute dating 2. Analyze the different methods (relative and absolute dating) of determining the age of stratified rocks. 3. Portray the subdivisions of geologic time. 1 CO_Q2_ESS SHS Module 11 What I Know Choose the letter of the correct answer and write it in your answer sheet. 1. Which is true about absolute dating? a. breakdown isotopes b. arrange the historical remains in order of their ages c. depends on the traces of radioactive isotopes found in fossils d. all of the above 2. Which absolute dating technique depends on the traces of radioactive isotopes found in fossils? a. Amino acid b. Dendrochronology c, Radiometric d. Thermo luminescence 3. Which geological dating technique is very effective in estimating the age of fossils through comparing it with fossils of known ages? Relative Ages Relative Dating Radiometric Dating Radioactive Isotopes ao Tp 4. Which of the following refers to the breakdown of isotopic energy? Half-life Isotopes Radioactive decay Radioactive metric dating a2oTp 5. Which of the following refers to atoms of the same element that have the same number of protons but different numbers of neutrons? a. Absolute dating b. Isotopes c. Radioactive Decay d. Relative Dating 6. What do you mean by strata? a. Rock ages b. Rock layers c. Rock particles d. Rock sediments 7. Which law of stratigraphy describes that sedimentary rocks are formed particle by particle and bed by bed, and the layers are piled one on top of the other? a. Law of deposition b. Law of superposition c. Law of lateral continuity d. Law of cross-cutting relationships 2 CO_Q2_ESS SHS Module 11 8. What is the science that deals with all the characteristics of layered rocks and how these rocks relate to time? a. Absolute Dating b. Relative dating c. Stratigraphy d. Unconformities 9. Which law of stratigraphy states that any rock, fault or structure that cuts another rock or other structure is younger than the rock or structure it cuts? a. Law of deposition b. Law of superposition c. Law of lateral continuity d. Law of cross-cutting relationships 10.Which is true about sedimentary rocks? a. Formed from particles of older rocks that have been broken apart by water or wind b. May contain remnants from dead animals and plants settled at lake or sea bottom c. With the passage of time and the accumulation of more particles, and often with chemical changes, the sediments at the bottom of the pile become rock. d. all of the above 11.What is the originally deposited horizontal layers that folded or tilted and then eroded? a. Angular unconformity b. Disconformity c. Nonconformity d. Paracomformity 12. Which of the following refers to the layer of sediments which are uplifted without folding but exposed to erosion and weathering? a. Angular unconformity b. Disconformity c. Nonconformity d. Paracomformity 13.Which system is used by scientists to relate stratigraphy and time to any geologic events? a. Time scale b. Period scale c. Half-life Scale d. Geological time scale 14.Which of the following is commonly used to date rocks? a, Carbon-14 b. Potassium-Argon c. Rubidium d. Uranium 15.Which of the following is a layer that indicates a period of uplift and erosion? Angular unconformity Disconformity Nonconformity Paracomformity a0 Tp 3 CO_Q2_ESS SHS Module 11 What is It Based on the previous activity, how are relative and absolute dating used to determine the subdivisions of geologic time? What is relative and absolute dating? Figure 2. Subdivision of Geologic time Relative dating — subdivisions of the Earth's geology in a specific order based upon relative age relationships most commonly in vertical/stratigraphic position. These subdivisions are given names, most of which can be recognized globally, usually on the basis of fossils. Volcanic ash (50 million years old) Paleocene sand Basalt dike (80 million years old) , a7 4 ee MUI S Ee bt fo fd a Say Oh PI 7 feed LID LL IE se LLL? EP te pie 5 millio fo PA? 7 we 4 4 “/ +) Granité (12 Ce os , Figure 3. Subdivision of Geologic time CO_Q2_ESS SHS Module 11 Absolute dating — numerical ages in "millions of years" or some other measurement. These are most obtained via radiometric dating methods performed on appropriate rock types. It is important to realize that with new information about subdivision or correlation of relative time, or new measurements of absolute time, the dates applied to the time scale can and do change. In addition, like any good scientific measurement, every dated boundary has an uncertainty associated with it, expressed as "+- X millions of years". These cannot be included in the diagram for practical reasons but can be found in Harland et al. (1990), along with a detailed description of the history of earlier-proposed time scales and the terminology, methodology and data involved in constructing this geological time scale. Let us now differentiate relative and absolute dating. Relative Vs. Absolute Dating: The Ultimate Face-off Relative Dating Absolute Dating »It determines if an object/event is younger or older than another object/event from history. » Relative dating is qualitative. » It determines the age of a rock/object using radiometric techniques. » Absolute dating is quantitative. » This technique helps determine the » This technique helps determine the relative age ofthe remains. » It is less specific than absolute dating. » Relative dating is comparatively less exact age of the remains. » It is more specific than relative dating. » Absolute dating is expensive and time- consuming. expensive and time-efficient. » It works best for sedimentary having layered arrangement of sediments. > Itworks best for metamorphic rocks. igneous and rocks The following are the major methods of relative dating. Stratigraphy: The oldest dating method which studies the successive placement of layers. It is based on the concept that the lowest layer is the oldest and the topmost layer is the youngest. Biostratigraphy: An extended version of stratigraphy where the faunal deposits are used to establish dating. Faunal deposits include remains and fossils of dead animals. Cross dating: This method compares the age of remains or fossils found in a layer with the ones found in other layers. The comparison helps establish the relative age of these remains. Fluorine dating: Bones from fossils absorb fluorine from the groundwater. The amount of fluorine absorbed indicates how long the fossil has been buried in the sediments. 7 CO_Q2_ESS SHS Module 11 The following are the major methods of absolute dating. Radiometric dating: This technique solely depends on the traces of radioactive isotopes found in fossils. The rate of decay of these elements helps determine their age, and in turn the age of the rocks. Amino acid dating: Physical structure of living beings depends on the protein content in their bodies. The changes in this content help determine the relative age of these fossils. Dendrochronology: Each tree has growth rings in its trunk. This technique dates the time or period during which these rings were formed. Thermoluminescence: It determines the period during which certain object was last subjected to heat. It is based on the concept that heated objects absorb light and emit electrons. The emissions are measured to compute the age. The Law of Superposition states that younger strata lie on top of older strata. The Principle of Cross-Cutting Relationships states that intrusions and faults that cut across rock are necessarily younger than that rock. Inclusions, or foreign bodies, found inside the rock are necessarily older than that rock. What’s More Activity 1: Differentiation Using a Venn diagram A Venn diagram tells both dating methods as two individual sets. The area of intersection of both sets tells the purpose common to both. Although absolute dating methods determine the accurate age compared to the relative methods, both are good in their own ways. Look at the diagram to understand their common purpose. When you observe the intersection in this diagram comparing these two dating techniques, we can conclude that they both have two things in common: a. give an idea of the sequence in which events have occurred and b. tell the age of fossils or rocks. Complete the Venn diagram using the words inside the box. Write the letter of your correct answer on your answer sheet. A. age B. qualitative C. quantitative D. remains E. radiometric F. stratigraphic 8 CO_Q2_ESS SHS Module 11 4. Youngest Oldest 5. Youngest Oldest Figure 8. Subdivision of Geologic time (Layers of rock) Outline the sequence of events in the cross sections below by numbering each rock unit or event in the order in which it occurred or was deposited. A D 6. Youngest Oldest Figure 9. SUbdivision of Geologic time (Layers of rock) UW CO_Q2_ESS SHS Module 11 Refer to the cross-section on the left. For each of the following pairs of rock layers, identify the relative dating law that would be used to determine which bed was older and which was younger. Write the letter of the older bed and through the two combined letters state if it is superposition or cross-cutting. Figure 10. Subdivision of Geologic time (Layers of rock) 1) A&B 3) C&D 2)D&E 4) J&K Youngest Figure 11. Subdivision of Geologic time (Layers of rock) Oldest Refer to the cross-section above. For each of the following pairs of rock layers identify the relative dating law that you used to determine which bed was older and which was younger. Write the letter of the younger bed and through the two combined letters state if it is superposition or cross-cutting. 9.1) M&A 9,2) J&N 9.3) H&C 9.4) D&M 12 CO_Q2_ESS SHS Module 11 © ‘@@) f Activity 1: Guide Questions 1G What I Can Do Answer the following in a complete statement. Write your answer on your answer sheet 1. What are the four methods of relative dating? 2. Give the four methods of absolute dating. 3. This type of dating determines the exact age of the remains and is more expensive. 4. The technique used in dating sedimentary rocks and is qualitative in nature. 5. Why are layers of rocks related to one another? Activity 2: Geologic Time Scale Time span of Earth’s past is so great that geologists use the geologic time scale to show Earth’s history. The geologic time scale is a record of the geologic events and the evolution of life forms. 1. On a separate sheet of paper, draw and complete a Brace Map showing the Geologic Time Scale Eras and Periods as shown on the Geologic Time Scale Reference Chart below. (Sample brace map) Events Years single-celled organisms 3,500 million years ago Trilobites 500 million years ago Early land plants 430 million years ago Reptiles 280 my.a. Fish 395 my.a. Whales 20 m.y.a. Dinosaurs 225-65 m.y.a. Mammals 65 my.a. Humans 2.5 m.y.a. Birds 120 m.y.a. Pangaea starts to separate 225 m.y.a. 13 CO_Q2_ESS SHS Module 11 8. Fossils are the preserved remains or traces of plants and animals that have lived on Earth throughout Earth’s history. How does the fossil record of animals compare to animals that exist today? a. Animals in the fossil record are the same as animals that exist today. b. Animals in the fossil record are ancestors of animals that exist today. c, Animals in the fossil record have no similarities to animals that exist today. d. Animals in the fossil record are more complex than animals that exist today. 9. A geologist is studying three layers of sedimentary rock in an area. The layers have not shifted from their original positions. The geologist records the relative ages of the rocks. The bottom layer is listed as the oldest. The top layer is listed as the youngest. What did the geologist use to determine the relative ages of the rocks? mineral content radioactive decay the law of superposition . the principle of unconformity 10. What is a geologic column? a. a rock structure that is shaped like a column b. a body of rock that cuts through sedimentary rock layers c. a group of rock layers that are taken out of the ground to study d. a group of rock layers that are placed in order of their relative ages Ro op 16 CO_Q2_ESS SHS Module 11 "| Additional Activities Reflection Complete the paragraph below. Write your answer on a separate sheet of paper. T’ve learned that absolute dating, also called that arranges the historical remains in order of their ages. Whereas relative dating arranges them in the of their formation. Most absolute dates for are obtained with radiometric methods. 17 CO_Q2_ESS SHS Module 11 - Answer Key aa's av'b av'e aa‘ aa't & Sanov ~Onadto a 6 = gids wer aaaaaad aaneyuenb aaneyenb orgder3nens omomorper sureuror ose T Sunoy ew SEU mouyy J Sy ysysss momommmogissaaa qa0acmaMo Brito eworda ey }ueurs: 18 CO_Q2_ESS SHS Module 11