Clues to Earth s Past

Similar documents
Clues to Earth s Past. Fossils and Geologic Time

Geologic Time. Earth s History

Objectives. Vocabulary. Describe the geologic time scale. Distinguish among the following geologic time scale divisions: eon, era, period, and epoch.

Geologic Time Test Study Guide

CHAPTER 8 DETERMINING EARTH S AGE RELATIVE AND ABSOLUTE ROCK AGES. Loulousis

FOSSILS. Book G Chapter 4 Section 1

Prentice Hall EARTH SCIENCE

Studying The Past. II. Why Do We Study Fossils Found in Rocks?

A Trip Through Geologic Time

Earth Science 11: Geologic Time Unit

Name Date EARTH S HISTORY VOCABULARY

Geologic History Unit Notes. Relative age - general age statement like older, younger more recent

Objectives: Define Relative Age, Absolute Age

Geologic History. Earth is very, very old

Studying The Past. II. Why Do We Study Fossils Found in Rocks?

Geologic Time. Decoding the Age of our Planet & North Carolina

3 Absolute Dating: A Measure of Time

2. How do igneous rocks form? 3. How do sedimentary rocks form? 4. How do metamorphic rocks form?

11/5/2015. Creating a Time Scale - Relative Dating Principles. Creating a Time Scale - Relative Dating Principles. The Geologic Time Scale

Geologic Time Essentials of Geology, 11th edition, Chapter 18 Geologic Time: summary in haiku form Key Concepts Determining geological ages

The Geology of Pacific Northwest Rocks & Minerals Activity 1: Geologic Time

Hot Sync. Materials Needed Today

6/30/2018. Geologic Time. Earth, Chapter 9 Chapter 9 Geologic Time

Studying The Past. Why Do We Study Fossils Found in Rocks?

TRACE FOSSIL FOSSIL ICE CORE RELATIVE DATING SUPERPOSITION ABSOLUTE DATING GEOLOGIC COLUMN UNIFORMITARIANISM HALF-LIFE RADIOACTIVE DECAY

Earth s Changing Surface Chapter 4

What we will learn about Fossils?

Lecture 10 Constructing the geological timescale

Topic 7: Historical Geology

Geology Test Review Answers

9. RELATIVE AND RADIOMETRIC AGES

Fossils. Presented by Kesler Science

GEOLOGIC EVENTS SEDIMENTARY ROCKS FAULTING FOLDING TILTING

A Trip Through Geologic Time

Vocabulary and Section Summary B

8. GEOLOGIC TIME LAST NAME (ALL IN CAPS): FIRST NAME: Instructions

Station Look at the fossil labeled # 16. Identify each of the following: a. Kingdom b. Phylum c. Class d. Genus

Chapter: Clues to Earth s Past

9. DATING OF ROCKS, FOSSILS, AND GEOLOGIC EVENTS

Name Class Date. 1. In your own words, write a definition for each of the following terms: superposition, geologic column, and geologic time scale.

Lesson Learning Goal

Directed Reading. Section: Determining Relative Age. conclusions? UNIFORMITARIANISM. geology? of Earth? Skills Worksheet

Geologic Time. Kentucky Geological Survey Modified McCann

Geologic Time. What is Age? Absolute Age The number of years since the rock formed. (150 million years old, 10 thousand years old.

Answers to Section G: Time and the Fossil Record (Relative Dating)

2. Can you name earth s three eras and explain why they are divided that way?

Directed Reading A. Section: Relative Dating: Which Came First?

Your quiz will have some multiple-choice questions, matching, fill-in-the-blank questions, and short answer. To review, study DQs, notes from class,

GEOLOGICAL TIME / DATING TECHNIQUES

GEOLOGICAL TIME / DATING TECHNIQUES

ENVI.2030L Geologic Time

PLEASE DO NOT WRITE ON THIS QUIZ! Relative Dating and Stratigraphic Principles Quiz

Earth s History. The principle of states that geologic processes that happened in the past can be explained by current geologic processes.

STUDY GUIDE CHAPTERS 12 & 13 GEOLOGIC TIME CHAPTER 12 SECTION 12.1

Unit 2 Lesson 3 Absolute Dating. Copyright Houghton Mifflin Harcourt Publishing Company

Determining geological ages

b. atomic mass H What is the density of an object with a volume of 15cm 3 and a mass of 45g?

Unconformities, Geologic Time Scale, and Uniformitarianism. Ms. P Science 2016

geologic age of Earth - about 4.6 billion years

Geologic Time: Hutton s Outcrop at Siccar Point

Age of Earth/Geologic Time. Vocabulary

Chapter 09 Geologic Time

Rock cycle diagram. Principle of Original Horizontality. Sediment is deposited horizontally

Before the 1700 s, scientists thought that the Earth was only 6,000 years old. This mindset was based on biblical references.

Principle of Uniformitarianism: Laws of nature don t change with time

Clues to Earth s Past

State the principle of uniformitarianism. Explain how the law of superposition can be used to determine the relative age of rocks.

After You Read. Mini Glossary. 130 Rocks and Minerals

Integrated Science. Geologic Time Notes. Section 1: Geologic Time

Geologic Time: Concepts and Principles

Why is quartz one of the most weathering-resistant minerals?

Fossils: evidence of past life

Lecture Outline Friday Feb. 21 Wednesday Feb. 28, 2018

Before the 1700 s, scientists thought that the Earth was only 6,000 years old. This mindset was based on biblical references.

Absolute Ages of Rocks

Chapter 17. Geologic Time: Concepts and Principles

Fossils and EH LT 1 and 2

Relative Dating. The Rock Cycle. Key Concept Scientists can interpret the sequence of events in Earth s history by studying rock layers.

II. Knowing and Understanding the Six Principles of Stratigraphy:

Fossils, Geologic Time, Absolute & Relative Dating, and Natural Resources. Chapters 5 & 6

Fossils. Name Date Class. A Trip Through Geologic Time Section Summary

6. Relative and Absolute Dating

Relative aging, fossils, natural disasters

Remains or traces of prehistoric life

Today: 1) Quiz- Vocabulary Chapter 8 2) Lecture on Telling Time Geologically

Unit 6: Interpreting Earth s History

November 1, Aims: Agenda. SWABT explain the absolute age of rocks using radiometric dating.

LECTURE 2: Taphonomy and Time

Strata Sample. 1. Make a drawing of the strata sample (beaker) in your fold. Be sure to add color :)

test date Name date Review: Geologic Time & Geologic Procesess-: You will record 1-38 answers on the scan sheet! These are worth 1.

Geologic Time Grand Canyon National Park

Page 1. Name:

Today you will be able to: Utilize the SEVEN rules of rock age identification to describe the geologic age of this rock sequence!

GEOL 104 Dinosaurs: A Natural History Geology Assignment. DUE: Mon. Sept. 19

Name Class Date. What are fossils? How are fossils formed? What can fossils tell us about the history of life on earth?

Welcome to General Geology!!

Name Geo 4 Practice Match the principle on the left (column A) with the definition (or part of the definition) on the right (column B).

Rock cycle diagram. Relative dating. Placing rocks and events in proper sequence of formation Deciphering Earth s history from clues in the rocks

Do Now HW due Friday 9/30

HISTORICAL NOTES. Catastrophism. James Usher, mid-1600s, concluded Earth was only a few thousand years old

Transcription:

Chapter Review Clues to Earth s Past Part A. Vocabulary Review Directions: Use the clues below to complete the crossword puzzle. 1 2 3 4 5 6 7 8 9 Across 2. Element found in tissues of most organisms 4. Method using properties of atoms in rocks and other objects to determine their ages 5. Principle stating that Earth s processes occurring today are similar to those that occurred in the past 6. Time it takes for half of the atoms in a radioactive element to decay 10 7. Kind of decay that results in the formation of a different element 9. Method of dating rocks when the amounts of parent and daughter materials are measured 10. Remains, imprints, or traces of once-living organisms Down 1. Gaps found in rock records 3. Actual organism or parts of organism protected from decay 8. Cavity left in rock by a decayed organism Clues to Earth s Past 37

Chapter Review (continued) Part B. Concept Review Directions: Complete the chart to describe different types of fossils. Type of fossil Description 1. Permineralized remains 2. Carbonaceous film 3. Mold 4. Cast 5. Trace fossils 6. Index fossils Directions: Answer the questions on the lines provided. 7. Explain what the concept of uniformitarianism means. 8. How do geologists use fossils to determine rock ages? What are these fossils called? 9. Explain how a dead organism may become a fossil. 38 Clues to Earth s Past

Chapter Test Clues to Earth s Past I. Testing Concepts Directions: Match the terms in Column I with their descriptions in Column II. Write the letter of the correct descriptions in the blank at the left. Column I Column II 1. cast 2. carbonaceous film a. produced when sediments fill in a cavity made when an object decayed b. cavity in rock made when an organism decayed 3. index fossils 4. fossil 5. half-life c. principle that Earth s processes occurring today are similar to those that occurred in the past d. process that uses the properties of atoms in rocks and other objects to determine their ages 6. principle of superposition 7. absolute dating 8. mold 9. radioactive decay 10. relative dating 11. unconformities 12. radiometric dating 13. uniformitarianism 14. permineralized remains e. states that in a sequence of undisturbed rocks, the oldest rocks are on the bottom and the rocks become progressively younger toward the top f. gaps in rock records made when agents of erosion remove existing rock layers g. method by which a geologist can calculate the absolute age of the rock by knowing the half-life of an isotope h. time it takes for half of an isotope s atoms to decay i. fossil of thin layer of carbon atoms and molecules j. formed when original materials in skeletal remains are replaced by minerals k. method by which order of events or age of rocks is determined by examining the position of rocks in a layer l. remains, imprints, or traces of once-living organisms m. process that occurs when the number of protons in an atom is changed and a new element is formed n. fossils of species that existed for short periods and were widespread Clues to Earth s Past 39

Chapter Test (continued) Directions: Determine whether each of the following statements is true or false. Write true or false in the blank. Rewrite each false statement to make it true. 15. A fossil may tell a geologist when, where, and how an organism lived. 16. A permineralized bone is composed of calcium. 17. The soft parts of organisms are most likely to become fossils. 18. Preserved animal tracks are trace fossils. 19. Only a radioactive isotope will have a half-life. 20. Any fossil can be dated by the amount of carbon-14 it contains. II. Understanding Concepts Skill: Concept Mapping Directions: Complete the concept map below by writing the conditions for fossil formation and the types of fossils in the circles. carbonaceous fossils 3. Quick burial provide the conditions to create fossils that can be 1. 2. original remains mold 5. 4. 40 Clues to Earth s Past

Chapter Test (continued) 6. What is the difference between relative and absolute dating? Skill: Interpreting Data Directions: Study the figure of the rock record. Then answer the questions on the lines provided. Limestone Sandstone Shale Igneous intrusion Fault F 7. List events A F in the order they occurred, beginning with the oldest event. A B C D E 8. When did the fault occur? Skill: Using Tables 9. Complete the table below to show the amounts of parent and daughter materials left of a radioactive element after three half-lives if the original parent had a mass of 80 g. III. 1 2 3 Number of half-lives Applying Concepts Parent material Writing Skills Directions: Answer the following questions using complete sentences. Daughter product 1. If horizontal layers of sedimentary rock have a vertical fault running through them, how might a geologist use relative dating to determine when the fault occurred? Clues to Earth s Past 41

Chapter Test (continued) 2. Explain how a trace fossil can provide information on how an organism lived. 3. Explain what is meant by correlating rock layers. 4. Do all rocks contain fossils? Describe the conditions necessary for fossils to form. 5. Explain what the term half-life means and how knowing the half-life of an isotope can help a geologist establish the age of a rock or fossil. 42 Clues to Earth s Past