2. How do igneous rocks form? 3. How do sedimentary rocks form? 4. How do metamorphic rocks form?
|
|
- Ashlynn Hardy
- 6 years ago
- Views:
Transcription
1 Name: Class: Earth s History Test Review Packet Test: Monday, February 13, 2017 The Rock Cycle 1. Explain why it is called the rock CYCLE. Does it truly have a starting point or end point? 2. How do igneous rocks form? 3. How do sedimentary rocks form? 4. How do metamorphic rocks form? 5. Put the following words into the Venn Diagram below: Pressure, water, heat, cooling, hardening, sediments, magma, lava, erosion, weathering, deposition, Sedimentary Metamorphic Igneous
2 Fossils: 1. Fossils are most common in which type of rock? 2. Summarize how fossils form. 3. What is a paleontologist? 4. Explain why fossils do not form in igneous and metamorphic rock. 5. Examine the diagram below. Did this area used to be underwater or dry land? Explain how you know based on the diagram. Is this area currently underwater or dry land? Explain how you know based on the diagram. 6. Besides in rock, what other four substances can fossils form in?
3 7. True or False: The fossil record contains all found and unfound fossils on Earth? 8. Define body fossil and list examples: 9. Define trace fossil and list examples: 10. Explain WHY a turtle would fossilize better than a caterpillar Relative age of rocks/fossils 1. Define Relative Age. 2. Relative Dating- put letters in order from oldest to youngest and list any geologic events/processes (faulting, folding, tilting, erosion/unconformity) that occur in each diagram. Also, label any igneous intrusions. C C F B A D B E
4 3. Define Uniformitarianism. 4. Define the Law of Superposition. 5. Define the Principle of Original Horizontality. 6. Define the Principle of Cross-Cutting Relationships. 7. Define Unconformity.
5 8. Use the diagram below. Pick THREE 3 letters and explain what they are/what they represent. 9. Use the diagram below. R T N A What does letter N represent? What does letter A represent? What do letters R and T represent? What type of rock are letters G, C, P, and W made of?
6 10. Use the diagram below. Draw (preferably in a different color!) where the unconformity is. 11. Use the diagram below. Draw (preferably in a different color!) where the unconformity is. Absolute age of rocks/fossils (based on radiometric dating) 1. Define Absolute Age. Use the chart below the answer questions 2-9. Method Half-life time Materials Dating Range Carbon/Nitrogen 5,730 years shells, limestone, organic matter ,000 years Potassium/Argon 1.3 billion years biotite, volcanic rock Rubidium/Strontium 47 billion years Micas Uranium-238/Lead billion years Zircon 100, billion years 10 million-4.5 billion + years 10 million-4.5 billion + years Uranium-235/Lead million years Zircon 10 million-4.5 billion + years 2. If scientists find a fossilized elephant bone, what parent isotope should they use to date the fossils?
7 3. What does Rubidium decay into? 4. What is the parent isotope of Nitrogen? 5. If scientists want to date a sample that is estimated to be about 850,000 years old, which parent isotope should they use? 6. If scientists want to date a sample that contains mica, which parent isotope should they use? 7. What is the half-life of Uranium-235? 8. How many years does it take for a 100 g sample of Uranium-238 to decay to 50 g? 9. CHALLENGE QUESTION: If a rock sample started out with 100 g sample of Rubidium, and now contains 25 g of Rubidium, how old is the rock? 10. How is the bracketing method used to determine the absolute age of rocks/fossils? 11. What is a half-life? 12. What are index fossils and how are they used? *The answer key will be posted to Schoology on Friday (February 10 th ) after school if you would like to check your answers!
8 VOCAB Sedimentary rock Metamorphic rock Igneous rock Magma vs. Lava Uniformitarianism Fossil Paleontologist Trace Fossil Body Fossil Ice core Tree ring Relative Age Relative Dating Law of Superposition Unconformity Principle of Original Horizontality Principle of Crossing Cutting Relationships Tilting Erosion Faulting Folding Absolute Age Absolute Dating Radioactive Decay Half-life Radiometric-dating Index Fossil
Chapter 09 Geologic Time
Physical Geology 1330 116-S&R 1 Chapter 09 Geologic Time Lectures 12 & 13 Dr. Mike Murphy mmurphy@mail.uh.edu 333-S&R-1 www.uh.edu/~mamurph2/homepage.html Two Ways to Date Geologic Events 1. Relative Dating
More informationGeologic History Unit Notes. Relative age - general age statement like older, younger more recent
Geologic History Unit Notes Relative age - general age statement like older, younger more recent Absolute age - specific age like 4,600 million years old Fundamental Principles of Relative Dating 1. Uniformitarianism
More informationTOPIC 1: RELATIVE DATING ESSENTIAL QUESTION: HOW DO WE DETERMINE A ROCK S AGE BY THE SURROUNDING ROCKS?
TOPIC 1: RELATIVE DATING ESSENTIAL QUESTION: HOW DO WE DETERMINE A ROCK S AGE BY THE SURROUNDING ROCKS? TOPIC 1: RELATIVE DATING UNIFORMITARIANISM: THE IDEA THAT THE SAME FORCES HAVE BEEN AND CONTINUE
More informationGEOLOGIC EVENTS SEDIMENTARY ROCKS FAULTING FOLDING TILTING
RELATIVE TIME (DATING) ABSOLUTE TIME (DATING) GEOLOGIC TIME List the order in which events occurred, without regard to the amount of time separating them. Refers to the age of a rock in relation to other
More informationThe Geology of Pacific Northwest Rocks & Minerals Activity 1: Geologic Time
Name: Age: I. Introduction There are two types of geologic time, relative and absolute. In the case of relative time geologic events are arranged in their order of occurrence. No attempt is made to determine
More informationDirected Reading page
Skills Worksheet Directed Reading page 185-190 Section: Determining Relative Age 1. How old is Earth estimated to be? 2. Who originated the idea that Earth is billions of years old? 3. On what did the
More informationCHAPTER 8 DETERMINING EARTH S AGE RELATIVE AND ABSOLUTE ROCK AGES. Loulousis
CHAPTER 8 DETERMINING EARTH S AGE RELATIVE AND ABSOLUTE ROCK AGES Loulousis Bellringer What are 5 visual clues that help you determine if someone is older or younger than you? Color of hair Wrinkles in
More informationPLEASE DO NOT WRITE ON THIS QUIZ! Relative Dating and Stratigraphic Principles Quiz
PLEASE DO NOT WRITE ON THIS QUIZ! Relative Dating and Stratigraphic Principles Quiz TEST NO A Multiple Choice Identify the letter of the choice that best completes the statement or answers the question.
More informationFOSSILS. Book G Chapter 4 Section 1
FOSSILS Book G Chapter 4 Section 1 OVERVIEW Explain what fossils are and how most fossils form. Describe what fossils tell about how organisms have changed over time. Identify and describe different types
More informationNotepack 18 AiM: How can we tell the age of rock layers? Do now: Which Jenga piece was placed first to build this tower? Support your answer with
Notepack 18 AiM: How can we tell the age of rock layers? Do now: Which Jenga piece was placed first to build this tower? Support your answer with complete sentences. How old is the Earth? The Earth is
More information3 Absolute Dating: A Measure of Time
CHAPTER 3 3 Absolute Dating: A Measure of Time SECTION The Rock and Fossil Record BEFORE YOU READ After you read this section, you should be able to answer these questions: How can geologists learn the
More informationClues to Earth s Past
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.
More informationb. atomic mass H What is the density of an object with a volume of 15cm 3 and a mass of 45g?
Name Period Date Earth Science Midterm Review 2015-2016 Quarter 1 Review Assign #1 Basic Chemistry An atom is a basic chemical building block of matter. An atom consists of protons, neutrons, and electrons.
More information9. RELATIVE AND RADIOMETRIC AGES
LAST NAME (IN CAPS): FIRST NAME: Instructions: 9. RELATIVE AND RADIOMETRIC AGES Your work will be graded on the basis of its accuracy, completion, clarity, neatness, legibility, and correct spelling of
More informationName Class Date. 1. In your own words, write a definition for each of the following terms: superposition, geologic column, and geologic time scale.
Skills Worksheet Chapter Review USING KEY TERMS 1. In your own words, write a definition for each of the following terms: superposition, geologic column, and geologic time scale. For each pair of terms,
More informationTRACE FOSSIL FOSSIL ICE CORE RELATIVE DATING SUPERPOSITION ABSOLUTE DATING GEOLOGIC COLUMN UNIFORMITARIANISM HALF-LIFE RADIOACTIVE DECAY
THIS IS NOT THE SAME TEST. YOU MUST ANSWER ALL QUESTIONS. NAME: Bubble the circle below U3L1 Write the letter next to the vocab term VOCAB MATCH 1 A. O B. O C. O D. O 1 2 A. O B. O C. O D. O 2 3 A. O B.
More informationEarth s Changing Surface Chapter 4
Name Hour Due Date Earth s Changing Surface Chapter (You do not need your book) Page 1 Fossils Summary Page 2 Traces of Tracks Page 3 Finding the Relative Age of Rocks Summary. Page - Finding the Relative
More informationUnit 6: Interpreting Earth s History
Unit 6: Interpreting Earth s History How do we know that the Earth has changed over time? Regent s Earth Science Name: Topics Relative Dating Uniformitarianism Superposition Original Horizontality Igneous
More information8. GEOLOGIC TIME LAST NAME (ALL IN CAPS): FIRST NAME: Instructions
LAST NAME (ALL IN CAPS): FIRST NAME: Instructions 8. GEOLOGIC TIME Refer to Exercise 6 in your Lab Manual on pages 151-168 to answer the questions in this work sheet. Your work will be graded on the basis
More informationNotepack 19. AIM: How can we tell the age of rocks? Do Now: Regents Question: Put the layers of rock in order from oldest to youngest.
Notepack 19 AIM: How can we tell the age of rocks? Do Now: Regents Question: Put the layers of rock in order from oldest to youngest. Geological Time Geological Time refers to time as it relates to the
More informationLaw of Superposition Law of Superposition
History of Earth Relative Dating In the same way that a history book shows an order of events, layers of rock (called strata) show the sequence of events that took place in the past. Using a few basic
More information9. DATING OF ROCKS, FOSSILS, AND GEOLOGIC EVENTS
LAST NAME (IN CAPS): FIRST NAME: Instructions: 9. DATING OF ROCKS, FOSSILS, AND GEOLOGIC EVENTS Refer to Laboratory 8 in your Lab Manual on pages 207-226 to answer the questions in this work sheet. Your
More informationBefore the 1700 s, scientists thought that the Earth was only 6,000 years old. This mindset was based on biblical references.
Before the 1700 s, scientists thought that the Earth was only 6,000 years old. This mindset was based on biblical references. However, as scientists began to better understand the processes that shape
More informationENVI.2030L Geologic Time
Name ENVI.2030L Geologic Time I. Introduction There are two types of geologic time, relative and absolute. In the case of relative time geologic events are arranged in their order of occurrence. No attempt
More informationEarth Science 11: Geologic Time Unit
Earth Science 11: Geologic Time Unit Text: Chapters 8 Lab: Exercise 6 Name Earth Science 11: Geologic Time Page 1 Geology 12: Geologic Time 8.1: The Geologic Time Scale Today, we know that Earth is approximately
More informationRelative Dating. How do we determine a rocks age by the surrounding rocks?
Relative Dating How do we determine a rocks age by the surrounding rocks? 1 Geologic History 2 Relative Dating Uniformitarianism - the idea that forces working on our planet today worked on our planet
More informationDetermining geological ages
Determining geological ages Relative ages placing rocks and geologic events in their proper sequence, oldest to youngest. Absolute dates define the actual numerical age of a particular geologic event.
More informationGeologic Time. Decoding the Age of our Planet & North Carolina
Geologic Time Decoding the Age of our Planet & North Carolina The Geologic Time Scale Objectives Describe the geologic time scale. Distinguish among the following geologic time scale divisions: eon, era,
More informationII. Knowing and Understanding the Six Principles of Stratigraphy:
Student Name(s): Physical Geology 101 Laboratory Relative Dating of Rocks Using Stratigraphic Principles Grade: I. Introduction & Purpose: The purpose of this lab is to learn and apply the concepts of
More informationBefore the 1700 s, scientists thought that the Earth was only 6,000 years old. This mindset was based on biblical references.
Before the 1700 s, scientists thought that the Earth was only 6,000 years old. This mindset was based on biblical references. However, as scientists began to better understand the processes that shape
More informationGeohistory Review. Things you need to know:
Geohistory Review Things you need to know: a) The earth and the solar system are 4.5 billion years old (4.5 X 10 9 ) b) Law of original horizontality: Sedimentary rock layers are always deposited as horizontal
More informationGeology Test Review Answers
Name: Geology Test Review Answers Core: Fill in the blanks: 1. Sediments get compacted and cemented into sedimentary rock. 2. Igneous rocks can be intrusive or extrusive from a volcano. 3. Adding heat
More informationEarth s History. The principle of states that geologic processes that happened in the past can be explained by current geologic processes.
Earth s History Date: Been There, Done That What is the principle of uniformitarianism? The principle of states that geologic processes that happened in the past can be explained by current geologic processes.
More informationA Trip Through Geologic Time
Date Class _ A Trip Through Geologic Time Chapter Test A Multiple Choice Write the letter of the correct answer on the line at the left. 1. Late in the Paleozoic Era, the supercontinent Pangaea formed.
More informationLecture 10 Constructing the geological timescale
Lecture 10 Constructing the geological timescale Geologic Time Discovering the magnitude of the Earth s past was a momentous development in the history of humanity This discovery forever altered our perception
More informationStudying The Past. II. Why Do We Study Fossils Found in Rocks?
Studying The Past I. What is a Fossil? A. Definition: The evidence or remains of once-living plants or animals II. Why Do We Study Fossils Found in Rocks? A. To provide evidence of the past existence of
More informationGeologic Time Test Study Guide
Geologic Time Test Study Guide Chapter 12 Section 1 The Earth s Story and Those Who First Listened 1. What is the difference between uniformitarianism and catastrophism? Uniformitarianism: the same geologic
More informationDirected Reading. Section: Determining Relative Age. conclusions? UNIFORMITARIANISM. geology? of Earth? Skills Worksheet
Skills Worksheet Directed Reading Section: Determining Relative Age 1. How old is Earth estimated to be? 2. Who originated the idea that Earth is billions of years old? 3. On what did the 18th-century
More informationEarth Science - Lab #11 Geologic Time
Earth Science - Lab #11 Geologic Time Page # Below are standard geologic symbols for the 3 main categories of rocks. Although these symbols are not universal, they are generally accepted by most geologists
More informationDetermining Earth's History Rocks and Ice Cores
Earths History Reu2.notebook November 14, 2013 Determining Earth's History Rocks and Ice Cores One goal of geology is to develop a timeline of Earth's past, including both geological and biological events.
More informationUnit 2 Lesson 3 Absolute Dating. Copyright Houghton Mifflin Harcourt Publishing Company
It s About Time! How can the absolute age of rock be determined? Determining the actual age of an event or object in years is called absolute dating. Scientists often use radioactive isotopes to find the
More informationStation Look at the fossil labeled # 16. Identify each of the following: a. Kingdom b. Phylum c. Class d. Genus
Station 1 1. Look at the fossil labeled # 16. Identify each of the following: a. Kingdom b. Phylum c. Class d. Genus 2. Look at the fossil labeled #7. Identify each of the following: a. Kingdom b. Phylum
More informationLecture Outline Friday Feb. 21 Wednesday Feb. 28, 2018
Lecture Outline Friday Feb. 21 Wednesday Feb. 28, 2018 Questions? Key Points for today What are the 5 relative age dating principles and how do you apply the principles to determine a geologic history
More information3. Bedrock from which entire geologic time period is missing between rock units 5 and 6? The fault most likely occurred after
Homework # 4 Relative Dating Name: Section: Date: 1. The cross section below represents a portion of Earth s crust. Letters through D are locations within the rock units. 5. The sequence of rock types
More information6. Relative and Absolute Dating
6. Relative and Absolute Dating Adapted by Sean W. Lacey & Joyce M. McBeth (2018) University of Saskatchewan from Deline B, Harris R, & Tefend K. (2015) "Laboratory Manual for Introductory Geology". First
More informationClues to Earth s Past. Fossils and Geologic Time
Clues to Earth s Past Fossils and Geologic Time Fossils A. Paleontologists study fossils and reconstruct the appearance of animals. Fossils B. Fossils remains, imprints, or traces of prehistoric organisms
More informationgeologic age of Earth - about 4.6 billion years
Geologic Time Geologic Time geologic age of Earth - about 4.6 billion years Geologic Time very difficult to appreciate from our human perspective necessary to understand history of Earth two basic ways
More informationA Trip Through Geologic Time
A Trip Through Geologic Time A Trip Through Geologic Time Review In: Have the same animals that live today always been on Earth? Illustrate and JUSTIFY. When finished with this In Question, show Ms. Johnson
More informationObjectives. Vocabulary. Describe the geologic time scale. Distinguish among the following geologic time scale divisions: eon, era, period, and epoch.
The Geologic Time Scale Objectives Describe the geologic time scale. Distinguish among the following geologic time scale divisions: eon, era, period, and epoch. Vocabulary geologic time scale eon era period
More informationDirected Reading A. Section: Relative Dating: Which Came First?
Skills Worksheet Directed Reading A Section: Relative Dating: Which Came First? Write the letter of the correct answer in the space provided. 1. Determining the age of objects or events in relation to
More informationChapter 17. Geologic Time: Concepts and Principles
Chapter 17 Geologic Time: Concepts and Principles Introduction The Grand Canyon - Major John Wesley Powell, in 1869, led a group of explorers down the Colorado River. Powell was impressed with the geology
More informationYour quiz will have some multiple-choice questions, matching, fill-in-the-blank questions, and short answer. To review, study DQs, notes from class,
Review for Strata & Fossil Quiz Name: Quiz Date: Your quiz will have some multiple-choice questions, matching, fill-in-the-blank questions, and short answer. To review, study DQs, notes from class, labs,
More informationState the principle of uniformitarianism. Explain how the law of superposition can be used to determine the relative age of rocks.
Objectives State the principle of uniformitarianism. Explain how the law of superposition can be used to determine the relative age of rocks. Compare three types of unconformities. Apply the law of crosscutting
More informationStudying The Past. II. Why Do We Study Fossils Found in Rocks?
Studying The Past I. What is a Fossil? A. Definition: The evidence or remains of once-living plants or animals II. Why Do We Study Fossils Found in Rocks? A. To provide evidence of the past existence of
More informationRelative Dating Exercises
Laboratory 1 Relative Dating Exercises Pamela J. W. Gore Department of Geology, Georgia Perimeter College Clarkston, GA 30021 Copyright 1998-2005 Pamela J. W. Gore Examine the geologic cross sections which
More informationUNCONFORMITY. Commonly four types of unconformities are distinguished by geologists: a) Disconformity (Parallel Unconformity)
UNCONFORMITY Unconformities are gaps in the geologic record that may indicate episodes of crustal deformation, erosion, and sea level variations. They are a feature of stratified rocks, and are therefore
More informationObjectives: Define Relative Age, Absolute Age
S6E5. Students will investigate the scientific view of how the earth s surface is formed. c. Classify rocks by their process of formation. g. Describe how fossils show evidence of the changing surface
More informationDetermining Absolute Age
CHAPTER 8 SECTION 2 The Rock Record Determining Absolute Age KEY IDEAS As you read this section, keep these questions in mind: Why can t scientists use rates of erosion and deposition as the only ways
More informationGeologic Time. What is Age? Absolute Age The number of years since the rock formed. (150 million years old, 10 thousand years old.
Geologic Time There are 2 kinds: What is Age? Absolute Age The number of years since the rock formed. (150 million years old, 10 thousand years old.) Relative Age The age compared to the ages of other
More informationGuided Notes Geologic History
Guided Notes Geologic History Relative Age Sequence of Events Correlation Techniques Volcanic Ash Markers Index Fossils Geologic Time Scale Evolution Radioactive Dating 9) How has Earth changed over time?
More informationHISTORICAL NOTES. Catastrophism. James Usher, mid-1600s, concluded Earth was only a few thousand years old
1 GEOLOGIC TIME HISTORICAL NOTES Catastrophism James Usher, mid-1600s, concluded Earth was only a few thousand years old Uniformitarianism Charles Lyell published Principles of Geology 1830. 3 HOW DO WE
More informationRock cycle diagram. Principle of Original Horizontality. Sediment is deposited horizontally
Geologic Time Rock cycle diagram Leaves of History Chapter 21 Lateral Continuity Principle of Original Horizontality Sediment is deposited horizontally Principle of Superposition Oldest rock A Younger
More informationPrentice Hall EARTH SCIENCE
Prentice Hall EARTH SCIENCE Tarbuck Lutgens Chapter 12 Geologic Time 12.1 Discovering Earth s History Rocks Record Earth History Rocks record geological events and changing life forms of the past. We have
More informationUnit V: Earth s History
Rock Outcrop on Rte. 12 Depauville Unit V: Earth s History Review Book pp.97-112. Original photo taken by Mr. O on 8/11/10. Objective #1 Describe processes that formed the atmosphere and oceans of early
More informationPage 1. Name:
Name: Questions 1 through 3 refer to the following: The diagrams below represent two rock outcrops found several miles apart in New York State. Individual rock layers are lettered, and fossils and rock
More informationGeologic Time. Earth s History
Geologic Time Chapter 12 Earth s History Earth s history is recorded in rocks Rocks record geological events and changing life forms of the past. We have learned that Earth is much older than anyone had
More informationGEOLOGIC TIME AND GEOLOGIC MAPS
NAME GEOLOGIC TIME AND GEOLOGIC MAPS I. Introduction There are two types of geologic time, relative and absolute. In the case of relative time geologic events are arranged in their order of occurrence.
More informationGEOLOGIC TIME. Smith and Pun, Chapter 7 DETERMINING THE ORDER OF EVENTS
GEOLOGIC TIME Smith and Pun, Chapter 7 DETERMINING THE ORDER OF EVENTS Examination of ancient rocks reveals the history of our planet. Sedimentary and volcanic rocks record processes that occur on the
More informationPrinciple of Uniformitarianism: Laws of nature don t change with time
G e o l o g i c T i m e Principle of Uniformitarianism: Laws of nature don t change with time Radical idea proposed by Hutton in 1780 s Proposed that past events could be explained by modern processes
More informationHow old is Earth? Bishop of Ireland James Ussher
Geologic Time How old is Earth? Bishop of Ireland James Ussher Not so long ago, the Bible was regarded as the ultimate source of truth. Through the 18th and 19th centuries it was believed that the world
More informationGeologic History. Earth is very, very old
Geologic History Earth is very, very old Earth s History The history of Earth and the ages of rocks can be investigated and understood by studying rocks and fossils. Evidence of ancient, often extinct
More informationAnswers to Section G: Time and the Fossil Record (Relative Dating)
Answers to Section G: Time and the Fossil Record (Relative Dating) Use the following sketch of a geological cross section to answer questions 1 to 3. 1. The most important principle used to determine the
More informationExploring Geology Chapter 9 Geologic Time
Exploring Geology Chapter 9 Geologic Time Copyright The McGraw-Hill Companies, Inc. Permission required for reproduction or display. Chapter 9: Geologic Time Stratigraphic Principles Relative Age Dating
More informationFossils. Ch. 29 and 30 Overview
Ch. 29 and 30 Overview What you need to know: Chapter 29: Fossils, Relative Time, Absolute Time Chapter 30: Geologic Time Fossils Study of fossils called paleontology Original remains rare usually dead
More informationGeologic Time: Concepts and Principles
Geologic Time: Concepts and Principles Introduction - An appreciation for the immensity of geologic time is essential for understanding the history of our planet - Geologists use two references for time
More informationFossils: evidence of past life
Fossils: evidence of past life Remains or traces of prehistoric life Petrified Cavities and pores are filled with precipitated mineral matter Petrified Formed by replacement Cell material is removed and
More informationLearning Target: I can create a foldable about the geologic principles that are used to relatively date rock sequences.
Geologic Principles Learning Target: I can create a foldable about the geologic principles that are used to relatively date rock sequences. 1 Geologic Principles Foldable You will need 3 pieces of paper
More informationRelative Geologic Time Scale. Geologic Time Scale
Dating the Earth The Map That Changed the World The Map That Changed the World William Smith, 1815 Geologic map of England, Wales, part of Scotland Relative Geologic Time Scale The relative geologic time
More information2/5/17. #7 Geologic Time #7 Geologic Time
#7 #7 = all of time since Earth formed (4.6 billion years ago, b.y.a.). Geologists study rocks, fossils, geologic structures (faults, folds) to characterize Earth's history. Natural disasters involve present-day.
More informationGeologic Time Essentials of Geology, 11th edition, Chapter 18 Geologic Time: summary in haiku form Key Concepts Determining geological ages
1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 Geologic Time Essentials of Geology, 11 th edition, Chapter 18 Geologic Time: summary in haiku form Superposition and horizontality tell stories in rocks. Key
More informationEARTH S HISTORY. Geological Evolution
EARTH S HISTORY Geological Evolution EVIDENCE FOR EARTH S AGE ROCK LAYERS FOSSILS UNIFORMITARIANISM RELATIVE VS. EXACT DATING ROCK LAYERS Many thousands of sedimentary rock layers Takes thousands to millions
More informationGEOLOGICAL TIME / DATING TECHNIQUES
DATE DUE: INSTRUCTOR: TERRY J. BOROUGHS Geology 305 NAME: SECTION: GEOLOGICAL TIME / DATING TECHNIQUES Instructions: Read each question carefully before selecting the BEST answer. Provide specific and
More informationAge of Earth/Geologic Time. Vocabulary
Age of Earth/Geologic Time Vocabulary Big Ideas Geologic Time Earth Structures Identify current methods for measuring the age of Earth and its parts, including the law of superposition and radioactive
More informationGEOLOGICAL TIME / DATING TECHNIQUES
DATE DUE: INSTRUCTOR: TERRY J. BOROUGHS Geology 305 NAME: SECTION: GEOLOGICAL TIME / DATING TECHNIQUES Instructions: Read each question carefully before selecting the BEST answer. Provide specific and
More informationGeologic Time. How old is Earth?
Geologic Time How old is Earth? Not so long ago, the Bible was regarded as the ultimate source of truth. Bishop of Ireland James Ussher Through the 18th and 19th centuries it was believed that the world
More informationRelative Dating. The Rock Cycle. Key Concept Scientists can interpret the sequence of events in Earth s history by studying rock layers.
2 What You Will Learn The rock cycle includes the formation and recycling of rock. Relative dating establishes the order in which rocks formed or events took place. The principle of superposition states
More informationVocabulary and Section Summary B
The Study of Earth s History After you finish reading the section, try this puzzle! Use the clues given to fill in the blanks below. Then, copy the numbered letters into the corresponding boxes below to
More informationB) color B) Sediment must be compacted and cemented before it can change to sedimentary rock. D) igneous, metamorphic, and sedimentary rocks
1. Which characteristic of nonsedimentary rocks would provide the least evidence about the environment in which the rocks were formed? A) structure B) color C) crystal size D) mineral composition 2. Which
More informationScience 20. Unit C: The Changing Earth. Assignment Booklet C1
Science 20 Unit C: The Changing Earth Assignment Booklet C FOR TEACHER S USE ONLY Summary Teacher s Comments Chapter Assignment Total Possible Marks 60 Your Mark Science 20 Unit C: The Changing Earth Assignment
More informationRemains or traces of prehistoric life
Fossils: evidence of past life Remains or traces of prehistoric life Petrified Cavities and pores are filled with precipitated p mineral matter Petrified Formed by replacement Cell material is removed
More informationLesson Learning Goal
Rock Dating Lesson Learning Goal 4/12 n I can identify current methods for measuring the age of Earth and its parts, including the law of superposition and radioactive dating. Think About It... How old
More informationUnconformities, Geologic Time Scale, and Uniformitarianism. Ms. P Science 2016
Unconformities, Geologic Time Scale, and Uniformitarianism Ms. P Science 2016 Do Now due tomorrow! 1. Compare and contrast relative dating to absolute dating. 2. The Law of Superposition states that younger
More informationStratigraphy. Stratigraphy deals with the study of any layered (stratified) rock, but primarily with sedimentary rocks and their
Stratigraphy Stratigraphy deals with the study of any layered (stratified) rock, but primarily with sedimentary rocks and their composition origin age relationships geographic extent Stratified Sedimentary
More information5. Compare the density of the oceanic crust to continental crust. 6. What kind of plate boundary is this? convergent
The youngest rock is in the middle (at ridge) and it gets older on either side as you move away in a symmetrical pattern. 1. How does the age of the seafloor compare on either side of the ridge? A = youngest
More informationGeologic Time: Hutton s Outcrop at Siccar Point. How do we determine age (relative & absolute) What is the age of the earth? How do we know?
Geologic Time: How do we determine age (relative & absolute) What is the age of the earth? How do we know? What is the age of the Earth? A. 4.44 million years B. 1 million years C. 4.55 billion years D.
More informationDating the age of the Earth
Dating the age of the Earth What is the age of the Earth? A. 4.44 million years B. 1 million years C. 4.55 billion years D. 10000 years Discuss this with your neighbor: How do we know the age of the Earth?
More informationIntegrated Science. Geologic Time Notes. Section 1: Geologic Time
Integrated Science Geologic Time Notes Section 1: Geologic Time To help in the analysis of Earth s rocks, geologists have divided the history of Earth into time units based upon the fossils contained in
More informationClues to Earth s Past
chapter 13 3 Clues to Earth s Past section 2 Relative Ages of Rocks Before You Read Think of two friends. You want to know who is older. What information do you need to figure out who s older? What You
More informationTopic 7: Historical Geology
Topic 7: Historical Geology (ES. 8 b, 9 a-e, 10 a-d, 12 a, b, e) ES.8 The student will investigate and understand geologic processes including plate tectonics. Key concepts include: b) processes (faulting,
More informationRock Cycle and Rock Types Homework
Rock Cycle and Rock Types Homework Completion Complete each statement. 1. A(n) is a solid mass of mineral or mineral-like matter that occurs naturally. 2. Rocks are generally classified as igneous,, or
More information