Earth and Life Science Quarter 1 Module 13: Geologic Time Scale, Relative and Absolute Dating

This is the Self-Learning Module (SLM) for Earth and Life Science, Quarter 1, Module 13: Geologic Time Scale: Relative and Absolute Dating. It is a Senior High School module (First Edition, 2021) from DepEd Region IV-A CALABARZON, written for learners studying at home under the Alternative Delivery Mode. It explains how geologists use rocks and fossils to describe Earth’s past. It also shows how the geologic time scale is divided and how relative and absolute dating give evidence of geologic history.

What learners will learn

After going through this module, learners are expected to:

  1. Name the divisions of the geologic time scale.
  2. Characterize each major division and subdivision in the geologic time scale.
  3. Describe how relative and absolute dating provide evidence of geologic history.

The module has one lesson: Lesson 1: Geologic Time Scale: Relative and Absolute Dating. It builds on earlier lessons about stratified rocks and Nicolas Steno’s laws of stratigraphy.

The geologic time scale

The module calls the geologic time scale the “calendar” for events in Earth’s history. It is a standard timeline that describes the age of rocks and fossils and the events that formed them. It covers Earth’s 4.6 billion years. Its time intervals are not like the hours on a clock. They are divided by major events in Earth’s history, such as the mass extinction of many plants and animals.

The time scale has four levels of division, from longest to shortest: eons, eras, periods, and epochs. Eons are the largest division.

Eons and eras

  • Precambrian makes up about 88% of Earth’s history. It is divided into three eons:
    • Hadean (from 4,600 million years ago): the beginning of Earth. Few rocks were deformed and metamorphosed.
    • Archean (from 3,800 million years ago): marine rocks hold fossils of microscopic algae and bacteria, the oldest fossils.
    • Proterozoic (from 2,500 million years ago): the continental crust rifted, and the gaps filled with sedimentary and volcanic rocks. Bacteria and blue-green algae lived in this time.
  • Phanerozoic Eon means “visible life.” It has three eras:
    • Paleozoic Era (542 to 251 million years ago): the beginning of early life. Land plants developed quickly, and the continents came together to form the supercontinent Pangea. Its Devonian Period is known as the age of fishes.
    • Mesozoic Era (251 to 65.5 million years ago): the Age of Dinosaurs. Pangea split into Laurasia and Gondwanaland.
    • Cenozoic Era (65.5 million years ago to the present): the age of recent life, or age of mammals. It has the most complete record of any era because its rocks are easier to reach.

Periods and epochs

The module’s table lists these periods, oldest to youngest:

EraPeriods
PaleozoicCambrian, Ordovician, Silurian, Devonian, Mississippian, Pennsylvanian, Permian
MesozoicTriassic, Jurassic, Cretaceous
CenozoicTertiary (Paleocene to Pliocene epochs), Quaternary (Pleistocene and Holocene epochs)

The module also divides the Cenozoic Era this way:

  • Paleogene Period (Paleocene, Eocene, and Oligocene epochs): Earth’s climate was mostly tropical, and continents drifted apart.
  • Neogene Period (Miocene and Pliocene epochs): early primates appeared.
  • Quaternary Period (Pleistocene and Holocene epochs): the most recent period, also called the Anthropogene. Human civilization arose in the Holocene, the epoch we live in now.

Relative and absolute dating

Scientists first built the time scale by studying rock layers and index fossils. Geologic time is described in two ways:

Relative datingAbsolute dating
Puts rocks and events in order, from oldest to youngestGives numerical ages, in millions of years or another measure
Based on position in the rock layers and on fossilsBased on radioactive dating of suitable rocks
Tells which rock is older or younger, not its exact ageMeasures radioactive elements to date each division

In an undisturbed rock profile, the oldest layers are at the bottom and the youngest are at the top. The time scale is drawn the same way.

The module uses a simple example from daily life. Listing the events of your life in order (“I was born,” then “my sister was born”) is relative dating. Writing the exact date beside each event, such as Jan. 28, 2001, is absolute dating.

How to use this module

The module follows the usual SLM parts. Work through them in this order:

  1. What I Know: a 15-item pretest to check what you already know.
  2. What’s In: a review of the laws of stratigraphy, using two rock-layer diagrams.
  3. What’s New: a sequence drill where you list five to seven events in your life on a relative scale and an absolute scale.
  4. What Is It: the lesson on the time scale and on relative and absolute dating.
  5. What’s More: Activity 1.1 (It’s a Date) uses each era’s share of Earth’s history to work out how long it lasted. Activity 1.2 (You Complete It) is a timeline, and Activity 1.3 (Word Pool) asks you to identify terms.
  6. What I Have Learned: concept definition maps for geologic time scale, relative dating, and absolute dating, plus a “Things to Ponder” summary.
  7. What I Can Do: a one-week diary of events you can relate to the geologic time scale.
  8. Assessment, then Additional Activities: a geologic time scale model made from discarded materials, graded on organization, creativity, and content.

For learners: Write your answers on a separate sheet of paper, not on the module. Check your work honestly with the answer key at the end.

For parents: Help your child keep to the order of the parts. Contact the teacher if a task is unclear.

For teachers: The Notes to the Teacher ask you to have learners explain how the stratigraphy laws describe rock layers. Give them enough time to review relative and absolute dating from the previous lesson. Check the answer key before you use it for grading, because some answers do not match the items.

Frequently asked questions

What grade and quarter is this module for?

It is a Senior High School Earth and Life Science module for Quarter 1, Module 13. The module does not name a specific grade.

What is the difference between relative and absolute dating?

Relative dating puts rocks and events in order from oldest to youngest, using rock layer positions and fossils. Absolute dating gives an actual age in millions of years, found by radioactive dating of rocks.

What are the divisions of the geologic time scale?

The module divides it into eons, eras, periods, and epochs. Eons are the largest division, and epochs are the shortest.

Which division covers most of Earth’s history?

The Precambrian covers about 88% of Earth’s history. It includes the Hadean, Archean, and Proterozoic eons.

Does the module have an answer key?

Yes. The last pages have answers for the pretest, the activities, and the assessment. Teachers should check some items before using them for grading.

Full text of the module

The text below is a transcription of the PDF above, as printed.

CO_Q1_ELS SHS Module 13

[logo: Senior High School badge] [logo: DepEd, Department of Education]

Earth and Life Science Quarter 1 – Module 13: Geologic Time Scale: Relative and Absolute Dating

[illustration: students learning at home and outdoors, with a teacher, a globe, and a child working by lamplight]

GOVERNMENT PROPERTY NOT FOR SALE

Earth and Life Science Alternative Delivery Mode Quarter 1 – Module 13: Geologic Time Scale: 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

Printed in the Philippines by ________________________

Development Team of the Module

Writer: Lucila D. Castor

Editors: Melanie I. Samudio, Jocelyn M. Manset

Reviewers: Jason Ricaforte, Angelica Beriña, 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., Jonathan V. Mayo

Illustrator: Ednelinda Robles, 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: Francis Cesar B. Bringas, Job S. Zape, Jr., Ramonito Elumbaring, Reicon C. Condes, Elaine T. Balaogan, Fe M. Ong-ongowan, Merthel M. Evardome, Nadine C. Celindro, Nicolas M. Burgos, Mario B. Maramot, Fe M. Ong-ongowan, Rosalinda A. Mendoza

Department of Education – Region IV-A CALABARZON

Office Address: Gate 2 Karangalan Village, Barangay San Isidro, Cainta, Rizal 1800 Telefax: 02-8682-5773/8684-4914/8647-7487 E-mail Address: region4a@deped.gov.ph

Earth and Life Science Quarter 1 – Module 13: Geologic Time Scale: Relative and Absolute Dating

Senior High School

Earth and Life Science Quarter 1 – Module 13: Geologic Time Scale: Relative and Absolute Dating

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 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.

CO_Q1_ELS SHS Module 13

What I Need to Know

This module covers the scientific principles that the historical geologists used to describe the Earth’s past. This will also serve as a guide to the clues that were left on Earth, the different events, and the time it took these events to happen which are depicted in the geologic time scale.

In this module, you will be able to determine the different divisions that comprise the geologic time scale which uses the two methods of record: the absolute and the relative dating.

The module is composed of the:

  • Lesson 1: Geologic Time Scale: Relative and Absolute Dating

After going through this module, you are expected to:

  1. Name the divisions of the geologic time scale.
  2. Characterize each major and subdivisions in the geologic time scale.
  3. Describe how relative and absolute dating provide evidence of geologic history.

CO_Q1_ELS SHS Module 13

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. This division comprises a time span of 88% in the geologic time scale, where rocks containing the earliest evidence of complex forms of life were discovered. Which division is being described by these statements?
    A. Cenozoic Era
    B. Mesozoic Era
    C. Paleozoic Era
    D. Precambrian


  2. As climate change sea levels rose worldwide and seas expanded across the center of North America. Some of the discovered fossils include dinosaur bones, teeth, and diverse plant fossils. Which division is being referred to in the given statement?
    A. Cenozoic
    B. Mesozoic
    C. Paleozoic
    D. Precambrian


  3. If you will study the relative age of a rock layer, which indicator below is the more appropriate to use?
    A. The thickness of the layer
    B. The chemical makeup of the layer
    C. The distance of the layer extends over the Earth
    D. The position of the layer compared to other layers


  4. Where are the oldest rocks found in an undisturbed rock profile?
    A. at the bottom
    B. in the middle
    C. on the top
    D. anywhere


  5. Radiometric dating is used to estimate how geologic rocks are formed and infer the ages of fossils contained within those rocks. In which of the given rocks is Radiometric dating least useful?
    A. basaltic
    B. granitic
    C. metamorphic
    D. sedimentary


CO_Q1_ELS SHS Module 13

  1. When naming the subdivisions of the Earth’s geology in a specific order, which method must be considered?
    A. Absolute dating
    B. Isotopic dating
    C. Radiometric dating
    D. Relative dating


  2. Which division in the geologic time shows evidence of molten rocks in the Earth’s surface due to its high temperature?
    A. Mesozoic Era
    B. Miocene Epoch
    C. Precambrian
    D. Tertiary Period


  3. The geologic time scale is a system of chronological dating that relates geological strata to time. In which portion of the Earth’s history is embraced by the geologic time scale?
    A. Evolution of life
    B. Formation of Earth
    C. Formation of universe
    D. Formation of the solar system


  4. How are the geologic eras largely determined?
    A. Average global temperature
    B. Distribution of rock sequences
    C. Earth’s orbital position
    D. Shifts in the fossil record


  5. In what geological periods did trilobites and other early arthropods appear?
    A. Cambrian
    B. Devonian
    C. Eocene
    D. Permian


  6. The Holocene epoch is Earth at present. It is during this period when the recorded history of man existed. In which geologic era does the Holocene epoch include?
    A. Cenozoic
    B. Mesozoic
    C. Paleozoic
    D. None of the above


CO_Q1_ELS SHS Module 13

  1. The earliest fossils that appeared during this time were large colonies of bacteria. If you were to trace when these bacteria evolved in the geologic time scale, what Eon will it be?
    A. Archaean Eon
    B. Hadean Eon
    C. Phanerozoic Eon
    D. Proterozoic Eon


  2. Which of the given statements does NOT represent the geologic time scale?
    A. The geologic history of the universe.
    B. The fossil record of flora and fauna.
    C. The age of the Earth and its inhabitants.
    D. Evolution of life dating back 4.6 billion years ago.


  3. What probability will take place when organisms have not adapted to their environment due to new diseases, new predators, and climate change?
    A. They will become extinct.
    B. Their bodies will be fossilized.
    C. Their bodies will be petrified.
    D. They will be buried as sedimentary materials.


  4. What causes the extinction of dinosaurs?
    A. Climate and geological changes that interrupted their food supply.
    B. An event impact of an asteroid or a comet may have caused the extinction.
    C. Small mammals ate dinosaur’s eggs thereby reducing their populations.
    D. Dinosaurs were cold-blooded animals which obtained body heat from the Sun-they would not have been able to survive in cooler climates.


Lesson 1 Geologic Time Scale

Deposition of sediments contribute to reshaping the surface of the Earth. Deposits are laid down by different environmental factors such as volcanic eruption, erosion, weathering debris of rocks (clay and silts), and even all its fossil content and historical information.

Earth history including its rock strata, the rock study, and discovery, as well as the fossils, are engraved in one of the most important materials known as geologic records. The geologic time scale is the “calendar” for events in Earth’s history.

The importance of the geologic time scale is, it serves as a standard timeline used to describe the age of rocks, fossils, and the events that formed them. It is a device which is of great help to the science of geology, and it is owed to the explorations and studies recorded by geologists.

Knowing about how life began in the past, the events, and principles behind the Earth’s history enables us to conform with the alterations or consequences that we might encounter or experience in the near future. As a part of the new generation, we should be appreciative and accept that all things that are present in our time were the outcomes of the Earth’s history.

What’s In

In the previous lessons, you had learned that stratified rocks are products of sedimentary processes which include weathering and erosion of pre-existing rocks. Wherein, these sediments will be transported by the agent of erosion such as water, wind, or ice, and deposited in seas and acted upon by the process of compaction and lithification. As time goes by, these sedimentary rocks will form layers or stratification representing periods of deposition of sediments. Based on this, there are several laws that govern stratigraphy as proposed by Nicolas Steno.

Nicolas Steno’s Law of Stratigraphy opens our eyes to the world of rock layers and its formation. It also shows how endogenic and exogenic geological processes cause alteration in rocks that lead to the formation and deformation of rock layers.

Let us find out if you can still recall how these laws are depicted in the rock strata. Identify the law of stratigraphy the following diagrams represent.

[illustration: block diagram of rock strata with layers A to F, a Younger arrow at the top and an Older arrow at the bottom] A

[illustration: block diagram of rock strata with Layer A to Layer F and a vertical dike cutting through the layers] B

Guide questions:

  1. What laws of stratigraphy does the picture in letter A tell us?_____________
  2. In picture B, new rocks were introduced. What law is best explained in this kind of rock stratum? _____________________________
  3. How old is the rock that was intruded in stratum B? ____________________
  4. What geologic processes existed in stratum B which causes its deformation? _____________________________
  5. If you want to determine the age of the rocks in the rock layer, what method are you going to use? _____________________________

Notes to the Teacher

Let the learners describe how the laws explain the formation of rock strata. Give the learners enough time to review what they had learned in the previous lesson regarding relative and absolute dating.

What’s New

Sequence Drill

In a sequential manner, make five to seven relative events that happened in your life. For example, the day you were born, the day your brother or sister was born, or your first date with your boyfriend or girlfriend. Write your answer in the table below.

[transcriber’s note: the title “Time Scale” spans all four columns of the table below]

Relative ScaleAbsolute Scale
I was bornI was bornExample (Jan.28,2001)

The way the relative events are arranged in your data is similar to how the geologists studied the Earth’s history: its geological time scale of Earth’s age and how it is determined.

What Is It

Since the beginning, geologists have been studying the Earth to unwrap the secrets of the past. They have been analyzing rock samples gathered from different continents in the world including its layers and its correlation with the fossils. This helps in relating the sequence of events in the Earth’s history which is clearly presented in the geologic time scale.

The geologic time scale is divided into a series of time intervals which are equal in length. These time intervals are different from that of a clock. They are divided according to the significant events in the history of Earth such as the mass extinction of a large population of fauna and flora.

Table 2. Geologic Time Scale

EonsEraPeriodEpochAge (Mya)
PhanerozoicCenozoicQuaternaryHolocene0.01
Pleistocene1.8
TertiaryPliocene5.3
Miocene23.0
Oligocene33.9
Eocene55.8
Paleocene65.5
MesozoicCretaceous145
Jurassic200
Triassic251
PaleozoicPermian299
Pennsylvanian318
Mississippian359
Devonian416
Silurian444
Ordovician488
Cambrian542

[transcriber’s note: table continued from the previous page]

EonsEraPeriodEpochAge (Mya)
PrecambrianProterozoicbacteria and blue green algae2500
Archeanoldest fossil3800
HadeanBeginning of earth4600

The table represents the divisions of the geologic time in Earth’s history that are separated into eons, periods, and epochs. The Earth’s age which is 4.6 billion years, was separated into different spans of time to handily indicate the events.

DIVISION IN THE GEOLOGIC TIME SCALE

[chart: flowchart; DIVISION IN THE GEOLOGIC TIME SCALE]

  • EONS: are the longest portions in the geologic time.
    • Precambrian: It accounts for 88% Earth’s history. It is subdivided into three eons: Hadean, Archean and Proterozoic.
      • Hadean Eon: Few rocks were deformed and metamorphosed.
      • Archaean Eon: Marine rocks contain fossil remains of microscopic algae and bacteria.
      • Proterozoic Eon: rifting of the continental crust; subsequent filling with sedimentary and volcanic rocks.
    • Phanerozoic Eon: It means visible life. It is subdivided into eras: Paleozoic, Mesozoic and Cenozoic.
      • Paleozoic Era: It is the beginning of early life. All of the continents had come together to form the supercontinent called Pangea. It is characterized by rapid development of terrestrial plants. Devonian period is known as the age of fishes.
      • Mesozoic Era: It is also known as the Age of Dinosaurs. Pangea rifted into Laurasia and Gondwanaland.
      • Cenozoic Era: It is also known as the age of recent life or age of mammals. It has the most complete record of any era because the rocks are more accessible.
DIVISION OF THE CENOZOIC ERA

[chart: flowchart; DIVISION OF THE CENOZOIC ERA]

  • Cenozoic Era: There are three periods in this era: Quaternary, Paleogene, and Neogene.
    • Paleogene Period: Most Earth’s climate was tropical. Continents drifted apart creating vast stretches of oceans. It consists of the Paleocene, Eocene, and Oligocene Epoch.
    • Neogene Period: It gives rise to early primates. It consists of Miocene and Pliocene Epochs.
    • Quaternary Period: It is the most recent period. It is also termed Anthropogene period. It is divided into two epochs: Pleistocene and Holocene. Holocene – when human civilization arose.
Relative and Absolute Dating

Scientists first developed the geologic time scale by studying rock layers and index fossils. The information gathered by the scientists placed the Earth rock strata in order by relative age. Geologic time is often discussed in two forms: relative time and absolute time.

Relative time is a subdivision of the Earth’s geology in a specific order based upon the relative age relationships (commonly, vertical, or stratigraphic position). Relative time can be established usually based on fossils. On the other hand, absolute time refers to the numerical ages in millions of years or some other measurement. These are obtained by radioactive dating methods performed on appropriate rocks.

Relative time can be referred to as the physical aspects found in rocks while absolute time refers to the measurements taken upon those to determine the actual time it expired. The time scale is depicted in its traditional form with the oldest at the bottom and the youngest at the top.

What’s More
Activity 1.1 it’s a Date
  1. Fill in the data table to show the number of millions of years each era lasted based on relative and absolute dating. Choose your answer from the given choices below.


    a. 4.048 mya c. 299 mya e. 4,600mya
    b. 69 mya d. 184mya


The Divisions of Geologic TimePercentMillions of years
The Age of the Earth100%
A. Cenozoic Era1.5%
B. Mesozoic Era4%
C. Paleozoic Era6.5%
D. Precambrian Time88%

Guide Questions:

  1. Based on the data table, which is the oldest era? _________________
  2. How old is the shortest era? _______________
  3. How old is the Cenozoic Era? _______________
  4. What dating method is applied in the activity? Why? _______________
  5. Where can we apply the relative dating method? _______________
Activity 1.2 You Complete it

Complete the timeline of the geologic time scale starting from the oldest to recent time. Indicate each division and year. Use the data table in Activity 1.1 as reference.

[chart: timeline; numbered boxes 1 to 5 in the upper row, each with a downward arrow to boxes 6 to 10 in the lower row]

Activity 1.3 Word Pool

Identify the term being described by the given statement. Select your answer from the word pool below.

Geologic record · Eons · Dinosaurs Relative dating · Cenozoic · Sedimentary Absolute dating · Holocene · Devonian Archaean · Paleozoic

_____________1. It is where all traces of history of earth is recorded in rocks that make up the crust.

_____________2. It is a way on how the age of rocks and fossils can be determined by its numeric value.

_____________3. It is the largest division in the geologic time scale.

_____________4. It refers to the rocks that are deposited and used in dating methods.

_____________5. It is used to determine the geological events in rock strata.

_____________6. It refers to prominent reptiles that evolved during the Mesozoic Era.

_____________7. The fitting of supercontinent Pangea happened in this era.

_____________8. The present human evolved during this age.

_____________9. It refers to the age of the fish.

_____________10. Ancient bacteria and blue green algae existed during this age.

1 2 3 4 5 6 7 8 9 10

What I Have Learned

Activity 1.4 Vocabulary Building

Make a concept definition map for each of the vocabulary terms listed below. Write the term in the central box. Fill in the other boxes by answering the questions. The first term is done for you.

A. Fossil

[chart: concept definition map; A. Fossil]

What information does it give?

What are some of its characteristics?

  • Give clues about Earth’s past
  • FOSSIL
  • Usually found in sedimentary rock
  • Shows only hard parts of plant or animal
  • Shows changes in life and the environment

B. Geologic Time Scale C. Relative Dating D. Absolute Dating

Things to Ponder
  • Geologic time scale is a timeline that illustrates Earth’s past.
  • Geologic time scale describes the order of duration of major events on Earth for the last 4.6 billion years.
  • Geologic time scale was developed after the scientist observed changes in the fossils and rocks going from oldest to youngest sedimentary rocks.
  • Geologic time scale was divided into four divisions which include the Eons, Era, Period, and Epoch.
  • Eons is the largest division in the geologic time scale.
  • Relative dating or age is the order of the rocks from oldest to youngest.
  • Relative dating does not determine the exact age of rock or fossils but does learn which one is older or younger than the other.
  • Relative age of rocks based on the order gives its physical division in the geologic time scale.
  • Absolute dating or age measures the number of radioactive elements in rocks to give the ages to each division of time in the geologic time scale.
  • Absolute time refers to the numerical ages in millions of years or some other measurement.

What I Can Do

Make a diary noting the important events that happened in your life for the day which you can associate with the geologic time scale.

DATEDAYS OF THE WEEKEVENT/ACTIVITY
Monday
Tuesday
Wednesday
Thursday
Friday
Saturday
Sunday

Assessment

Directions: Read each statement and choose the letter of the correct answer. Shade the circle that corresponds to the correct answer.

  1. What information does the geologic time record provide?
  • A. The rate of fossil formation.
  • B. The thickness of sedimentary rock layers.
  • C. The time since the evolution of dinosaurs.
  • D. The life forms and geologic events in Earth’s history.
  1. How do geologists separate time into period?
  • A. By the time the fossil is discovered.
  • B. By looking at the relative time of a fossil.
  • C. By special events that have happened in that period.
  • D. By counting the years that a fossil has been preserved.
  1. What do you call the method of placing geologic events in sequential order as determined by their position in the rock record?
  • A. Absolute dating
  • B. Correlation
  • C. Relative dating
  • D. Uniformitarianism
  1. What is the relevance of absolute time?
  • A. It is useful if fossils are present.It gives a specific date in an object.
  • B. It gives a non-specific date in an object.
  • C. It only gives the sequence in which events have taken place.
  1. Which of the following is the primal in absolute dating method?
  • A. Cross-cutting relationships
  • B. Educated estimates
  • C. Fossils
  • D. Radioactive decay
  1. If geological time will be recognized, which method is primarily used?
  • A. Calculation of alpha decay of isotopes.
  • B. Calculation of beta decay of isotopes.
  • C. Correlation of rock types across vast.
  • D. Distances correlation of magnetic signatures in rocks.
  1. Which of the following era is sometimes called “the age of fish” or “ancient life”?
  • A. Cenozoic
  • B. Mesozoic
  • C. Paleozoic
  • D. Precambrian
  1. What will be the sequence of division in the geologic time scale, if the order of position is from shortest to longest?
  • A. era, period, epoch
  • B. epoch, period, era
  • C. period, epoch, era
  • D. epoch, era, period
  1. Scientists use a criterion to decide where to place the boundaries between the major divisions of the geologic time scale. They consider major changes. Where can these major changes be found?
  • A. written in the fossil record
  • B. occurring in the solar system
  • C. in structure of the Earth’s layer
  • D. in the arrangement of the continent
  1. In which division in the geologic time scale did the continents come together to form the supercontinent called Pangaea?
  • A. Paleozoic Era
  • B. Cenozoic Era
  • C. Triassic Period
  • D. Jurassic Period
  1. How do eras differ from periods?
  • A. They have a longer span of time.
  • B. They have subdivided into epochs.
  • C. They have longer durations than eons
  • D. They have boundaries marked by mass extinctions.
  1. Which epoch in the geologic time scale designates human lives in a very short period of time?
  • A. Eocene
  • B. Holocene
  • C. Pliocene
  • D. Pleistocene
  1. Why are fossils recorded in the geologic time scale said to be incomplete?
  • A. Most organisms never became fossils.
  • B. The absence of tools to be used for tracing.
  • C. The remains of past organisms decayed faster.
  • D. All of the above
  1. How will you describe the arrangement of the rock in the geologic time scale?
  • A. They arranged an absolute dating.
  • B. They are based on its composition.
  • C. They are based on relative dating.
  • D. They are arranged in decades and centuries.
  1. What makes fossils essential to scientists and the history of the Earth?
  • A. It predicts what organisms will become extinct.
  • B. It analyzes the composition of sedimentary rock
  • C. It describes the history of past life and environment.
  • D. It presents the temperature of the oceans in different depths.

Additional Activities

Create your own representation of a geologic time scale on rocks indicating the relative and absolute dating. Use discarded material in your output.

The rubrics below will serve as a basis for grading your output.

Criteria/Points4321
OrganizationProducts appears finished and organized appropriatelyProducts is exactly finished /organized appropriatelyProducts is minimizing arts and it is not organized appropriatelyProducts is not organized
CreativityInforming, engaging, and visually stimulating Use of color, visuals, interest, motivation, and time are clearly reflected. Discarded materials used are keenly observedUse pictures and colors are engaging but not stimulating. Some are interesting, motivated and time span are clearly reflected Use limited discarded materials in the outputWith little use of colors. Not stimulating. Too little interest and motivation. Time is not clearly reflected.Did not use color. Not stimulating or motivating with little interest. Time span and effort is not reflected
ContentThe content provides detailed information regarding the geologic time scale and the organisms that live in the past are well presented.The content provides a few information regarding the geologic time scale and the organisms were also few.Limited information regarding the geologic time scale as well as the organismsThe information regarding the geologic time scale does not contain appropriate details, the organisms was not included

Answer Key

[transcriber’s note: this page is printed upside down; the text below is transcribed in upright reading order]

Pretest

1.C 2.B 3.D 4.A 5.A 6.A 7.C 8.B 9.D 10.D 11.A 12.B 13.A 14.A 15.D

What’s More: Activity 1.1 Its a Date

1.E 2.A 3.B 4.D 5. C

Answer: 1.D 2.A 3.B 4.Absolute dating 5.Precambrian is the oldest era because it is located at the bottom.

What’s More: Activity 2

Precambrian Paleozoic Mesozoic Cenozoic Recent time 4.048mya 299mya 184mya 69mya 4600mya

What’s More: Activity 1.4

1.Geologic Time Scale

  • timeline that illustrates – Earth’s past
  • Characteristics
  • divided into – eons,era,period,epoch
  • uses the relative and – absolute dating
  • Relate dating
  • gives relative age of rocks – Characterisctics;
  • Uses the position of rocks
  • follows the law of – stratigraphy
  • Absolute Dating
  • gives the numeric age of – rocks
What’s More: Activity 1.3
  1. Geologic records
  2. Absolute dating
  3. Eons
  4. Sedimentary
  5. Relative dating
    Dinosaurs
    Paleozoic
    Holocene
    Devonian
    Archaean
Assessment
  1. D
  2. B
  3. C
  4. B
  5. B
  6. C
  7. C
  8. B
  9. A
  10. A
  11. B
  12. B
  13. D
  14. C
  15. C

References

All About Creation. “Relative Dating.” Accessed February 24,2019. https://www.allaboutcreation.org/relative-dating-faq.html

“Centricity.” Accessed February 24,2019. https://www.lcps.org/cms/lib4/VA01000195/centricity

Earth Science Week. “Geological Timescale.” Accessed February 24,2019. https: www.earthsciweek.org/content/geo;ogial-time-scale

Kean. Accessed February 25,2019. http://www.kean.edu/csmart/observing/lecture/homework

“Layers of Rock.” Accessed February 24,2019,https://halletcove.weebly.com/layers-of-rock.html

“Observing Lectures,” Accessed February 25,2019. https://www.kean.edu/~csmart/Observing/Lectures/ Homework08s.doc

Oxford University Press.”The Past in Perspective.” Accessed February 25, 2019. http://global.oup.com/us/companion.websites/9780195391350/student/c hapt2/Quiz/

ProProfsQuizzes.”A Trivia Quiz on Geological Dating.” Accessed February 25, 2019. www.proprofs.com/quiz-school/story.php?title=geological-dating

Quizziz. “Relative and Absolute Dating.” Accessed February 25,2019. https://quizizz.com/admin/quiz/570bb06788512b8d10163a2e

“Relative Vs. Absolute Dating,” accessed February 24,2019, https://science.truck.com/relative-vs-absolute-dating

For inquiries or feedback, please write or call:

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