HOWEVER WE MUST BE ABLE TO PUT THEM IN THE RIGHT SEQUENCE OR THE STORY THEY TELL DOESN T MAKE SENSE, JUST LIKE A BOOK WITH ITS PAGES OUT OF ORDER

Size: px
Start display at page:

Download "HOWEVER WE MUST BE ABLE TO PUT THEM IN THE RIGHT SEQUENCE OR THE STORY THEY TELL DOESN T MAKE SENSE, JUST LIKE A BOOK WITH ITS PAGES OUT OF ORDER"

Transcription

1 HOWEVER WE MUST BE ABLE TO PUT THEM IN THE RIGHT SEQUENCE OR THE STORY THEY TELL DOESN T MAKE SENSE, JUST LIKE A BOOK WITH ITS PAGES OUT OF ORDER DOESN T MAKE SENSE: ACCURATE DATING METHODS ARE ESSENTIAL TO THIS PROCESS

2 SOME INITIAL DEFINITIONS: FOSSIL: THE REMAINS OF PLANT/ANIMAL SKELETAL STRUCTURE CAN BE AN IMPRESSION OR THE REAL THING

3 IF STRUCTURE EXISTS, IT S MADE OF MINERAL/STONE, NOT BONE!

4 ARTIFACT: OBJECTS OR MATERIALS MADE OR MODIFIED FOR USE BY HOMINIDS

5

6 CONTEXT THE RELATIONSHIP BETWEEN AND AMONG ARTIFACTS AND OTHER MATERIALS THIS CONCEPT IS CRITICAL TO THE EXAMINATION AND UNDERSTANDING OF FOSSILS AND ARTIFACTS W/O CONTEXT, ARCHAEOLOGICAL DISCOVERIES DON T HAVE MUCH MEANING

7 DATING METHODS RELATIVE DATING PROCEDURES: STRATIGRAPHY: THE LAYERING OF DIRT, ROCK FORMATIONS, AND FOSSILS THE LOWER THE DEPTH THE OLDER THE AGE

8

9 TAPHONOMY STUDY OF PROCESSES OF SITE DISTURBANCE AND DESTRUCTION

10 CHEMICAL DATING: MEASURES FLUORINE, URANIUM, & NITROGEN IN TEETH & BONES SAMPLES MUST BE FOUND IN GROUNDWATER AND IN CLOSE PROXIMITY SITES

11 HOW IT OPERATES: AS TIME GOES BY: FLOURIDE AND URANIUM= INCREASES IN SAMPLE NITROGEN= DECREASES URANIUM DOESN T DESTROY SAMPLE,SO PREFERRED METHOD

12 ALL ELEMENTS FOUND IN NATURE

13 PALEOMAGNITISM: INVOLVES PERIODIC PAST REVERSALS OF EARTH S MAGNETIC POLES

14 ROCK FORMATIONS (ESP. LAVA) RETAIN EARTH S MAGNETIC FIELD WHEN LAID DOWN

15 LAVA BONES INDIRECTLY MEASURED BY POLARITY DATES

16 BIOSTRATIGRAPHY LOOKS AT FAUNA/FLORA FOSSILS OF SHORT-LIVED SPECIES IN PARTICULAR REGION

17 TONS OF CHARTS & STUDIES

18 PIGS ESP. HELPFUL IN AFRICA

19 CHRONOMETRIC (ie. ABSOLUTE) DATING METHODS DENDROCHRONOLOGY: LOOKS AT TREE RINGS NEED SENSITIVE TREES OVER COMPLACENT TREES THEY RESPOND TO PRECIPITATION, HEAT, ETC

20

21 BEST WHERE WOOD IS PRESERVED (IE. ARID AMERICAN S.W.) CLIMATE VARIATIONS ARE CRITICAL CAN GO BACK 10,000 YA BUT SHAKY (7500 YA BETTER) BRISTLE CONE PINE IS BEST TREE B/C THERE ARE THE WORLD S OLDEST TREES

22 THE METHUSALA TREE : 4,800 YEARS OLD, CALIFORNIA

23 VARVES: LAKE SEDIMENTS DEPOSITED BY ANNUAL GLACIER MELTS FROM LAST ICE AGE SUMMER CLIMATE VARIATIONS TRACKED GOOD UP TO 20,000 YA (BEST 10,000-15,000); USED IN DATING SITES IN N. AMERICA; N. EUROPE

24 EXAMPLES OF VARVES

25 THERMOLUMINESCENCE: MEASURES LIGHT EMITED FROM SAMPLES PREVIOUSLY HEATED IN PREHISTORIC TIMES EXAMINES RADIOACTIVE PROPERTIES EXCELLENT UP TO ABOUT 10,000 YA (BUT BEEN USED TO 70,000 YA) EX S: CAMPFIRE STONES, BURNT POTSHARDS, FLINT

26

27 ELECTRON SPIN RESONANCE DATING LIKE THERMO, MEASURES TRAPPED ELECTRONS SPINS MATERIAL W/IN MAGNETIC FIELDS AND MEASURES MICROWAVES/RADIATION

28 NO HEAT INVOLVED: GOOD FOR BONE AND SHELL

29 CARBON-14: MEASURES AMOUNT OF RADIOACTIVE CARBON ISOTOPE C- 14 DEAD FAUNA/FLORA DECLINES AT CONSTANT RATE AFTER DEATH GOOD UP TO 40,000-50,000 YA WHICH IS WHEN H. sapiens ENTER EUROPE

30 C-14 PHIALS AND MACHINE

31 SHROUD OF TURIN: C-14 TESTING 1988 U. OF OXFORD, U. OF ARIZONA, SWISS FEDERAL INSTITUTE OF TECHNOLOGY

32 RESULTS: DATED BETWEEN AD (MIDDLE AGES) 3 PEER-REVIEWED ARTICLES DISPUTE RESULTS BASED ON: SITE OF SHROUD SAMPLES POSSIBILITY REPAIRS OR CONTAMINATION AFFECT DATES

33 POTASSIUM-ARGON (K-Ar): INVOLVES STEADY DECAY OF K-40 INTO Ar-39 POT-40 S ½ LIFE IS 1250 MILLION YEARS DECAYS INTO ARGON BLAST SAMPLE W/ NEUTRON BEAM, MEASURE TRAPPED ARGON

34 DATES P-RICH ROCK SURROUNDING FOSSILS, NOT FOSSILS THEMSELVES EXTREMELY VALUABLE IN E. AFRICA MIOCENE (5-22 MILLION YA BUT CAN GO BACK 3+BILLION YA)

35 V. SCIENTIFIC: THOUSANDS OF DOLLARS A SAMPLE, WEEKS FOR RESULTS

36 FISSION TRACKING: COUNTS TRACKS ACROSS SAMPLE BY DISINTEGRATING URANIUM ATOMS (U-238) ACCURATE FROM 20 YEARS TO 5 BILLION YA

37 NEED ELECTRON MICROSCOPE AND COMPUTER TO COUNT TRACKS

38 CROSS-REFERENCING: COMBINING ABOVE METHODS HELPS ELIMINATE ERRORS K-AR DATING W/ FISSION TRACKING IS VERY ACCURATE USUALLY COSTS DETERMINE DATING METHOD

3 Absolute Dating: A Measure of Time

3 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 information

Measuring the Age of things (Astro 202 2/12/08) Nomenclature. Different Elements. Three Types of Nuclear Decay. Carbon 14 Decay.

Measuring the Age of things (Astro 202 2/12/08) Nomenclature. Different Elements. Three Types of Nuclear Decay. Carbon 14 Decay. Measuring the Age of things (Astro 202 2/12/08) Nomenclature + Proton Different Elements Neutron Electron Element: Number of Protons Carbon 12 6 protons 6 neutrons 6 electrons Nitrogen 14 7 protons 7 neutrons

More information

SCIENTIFIC DATING IN ARCHAEOLOGY

SCIENTIFIC DATING IN ARCHAEOLOGY SCIENTIFIC DATING IN ARCHAEOLOGY Tsuneto Nagatomo 1. AGE DETERMINATION IN ARCHAEOLOGY Relative Age: stratigraphy, typology Absolute Chronology: historical data Age Determination by (natural) Scientific

More information

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

Unit 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 information

Determining Absolute Age

Determining 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 information

DATING HOW OLD IS THIS THING?

DATING HOW OLD IS THIS THING? DATING HOW OLD IS THIS THING? WHY? u CROSS-CULTURAL COMPARISON v UNDERSTANDING DEVELOPMENT AND CHANGE OF A PARTICULAR GROUP OR CULTURE w UNDERSTANDING SITE FORMATION PROCESSES x UNDERSTANDING REGIONAL

More information

Chimpanzees. Chimpanzees (Pan troglodytes) 11/13/11. Week 12. Chimpanzees Dating things Intro to Human Origins

Chimpanzees. Chimpanzees (Pan troglodytes) 11/13/11. Week 12. Chimpanzees Dating things Intro to Human Origins Week 12 Chimpanzees Dating things Intro to Human Origins Chimpanzees (Pan troglodytes) Chimpanzees Chimpanzees are perhaps the best known of all nonhuman primates. Most of us experience captive or trained

More information

What we will learn about Fossils?

What we will learn about Fossils? The fossil Record What we will learn about Fossils? We will learn how fossils form? What types of fossils exist? How do scientists determine the age of fossils? What do fossils reveal to scientists? What

More information

4/4/17. Dating Methods. Dating in Archaeology. These things date to 2500 B.C. (but there are no completion dates written anywhere on or near them)

4/4/17. Dating Methods. Dating in Archaeology. These things date to 2500 B.C. (but there are no completion dates written anywhere on or near them) Dating in Archaeology These things date to 2500 B.C. (but there are no completion dates written anywhere on or near them) Dating Methods One of the biggest questions in archaeology is WHEN? Successfully

More information

Absolute Ages of Rocks

Absolute Ages of Rocks Benchmarks SC.A..3.5 (pp. 269 273); SC.A.2.3.2 (pp. 269 273); SC.D..3.2 Annually Assessed (pp. 273 276): knows that over the whole Earth, organisms are growing, dying, and decaying ; SC.D..3.3 (pp. 273

More information

Basic background for the geo- and archaeo- magnetist. Time scales Stratigraphy Site types Material types Field methods

Basic background for the geo- and archaeo- magnetist. Time scales Stratigraphy Site types Material types Field methods Basic background for the geo- and archaeo- magnetist Time scales Stratigraphy Site types Material types Field methods Field Observations Geology Archaeology Materials Geology Rocks and minerals Archaeology

More information

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.

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. 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 information

Unit A (225 m.y. old) Unit B (how old is it?) Unit C (275 m.y. old)

Unit A (225 m.y. old) Unit B (how old is it?) Unit C (275 m.y. old) Radiometric Dating Relative dating techniques are based on principles can be used to differentiate the relative age rock units and landforms. Relative dating techniques by themselves cannot be used to

More information

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

Studying 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 information

Absolute Dating Introduction Type of Absolute Dating:

Absolute Dating Introduction  Type of Absolute Dating: Absolute Dating Introduction Prehistory deals with a long span of time. Therefore, one of the most important aims of prehistorian is to establish the chronological sequence of the past events. In the early

More information

Geochronology. study of 'Earth time' Historical Geology. study of the physical and biological evolution of the Earth & its life

Geochronology. study of 'Earth time' Historical Geology. study of the physical and biological evolution of the Earth & its life http://talc.geo.umn.edu/courses/100i/1001kirkby/ss6.html Page I of II 3/17/2006 Geochronology study of 'Earth time' time scale of geologic processes & methods of measuring time Historical Geology study

More information

Chronology Introduction Definition of Chronology Dating Methods for Building Chronology

Chronology Introduction Definition of Chronology Dating Methods for Building Chronology Chronology Introduction The emergence of man through the process of biological and cultural evolution is a story of long span of time. For the archaeologist and the prehistorian who deals with that long

More information

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

CHAPTER 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 information

Chapter Archaeological Dating Methods

Chapter Archaeological Dating Methods Chapter 3 3.1. Archaeological Dating Methods Everything which has come down to us from heathendom is wrapped in a thick fog; it belongs to a space of time we cannot measure. We know that it is older than

More information

Martin David Kamen (August 27, 1913 August 31, 2002) and Sam Ruben (November 5, 1913 September 28, 1943) discovered how to synthesize the isotope

Martin David Kamen (August 27, 1913 August 31, 2002) and Sam Ruben (November 5, 1913 September 28, 1943) discovered how to synthesize the isotope Martin David Kamen (August 27, 1913 August 31, 2002) and Sam Ruben (November 5, 1913 September 28, 1943) discovered how to synthesize the isotope Carbon-14 in February 27, 1940. Ruben was studying the

More information

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

Earth 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 information

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

Geologic 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 information

Radiometric Dating and the Age of the Earth

Radiometric Dating and the Age of the Earth Radiometric Dating and the Age of the Earth How to tell time: Relative Time: putting events in time order. Law of Superposition Correlation of rock layers using fossils. There is a wonderful order and

More information

Radioactive Clocks or Radiometric Dating

Radioactive Clocks or Radiometric Dating Radioactive Clocks or Radiometric Dating The time span of relevant events varies from a few centuries to billions of years historians archeologists, anthropologists, geologists, astrophysicists Radioactive

More information

NOTES: The Fossil Record and Geologic Time

NOTES: The Fossil Record and Geologic Time NOTES: The Fossil Record and Geologic Time Vocabulary: Paleontologist Fossil record extinct Relative dating Absolute dating Geologic time scale Objectives: What are fossils? How are they made? How do scientists

More information

DATING METHODS IN PREHISTORY

DATING METHODS IN PREHISTORY DATING METHODS IN PREHISTORY Introduction: Prehistory denotes a period for which we do not have any written records. It deals with a long span of time. Therefore, whenever any kind of prehistoric remain

More information

NOTES 1. Fossils. The BIG Idea Rocks, fossils, and other types of natural evidence tell Earth s story.

NOTES 1. Fossils. The BIG Idea Rocks, fossils, and other types of natural evidence tell Earth s story. Name Period Date UNIT 6 NOTES 1 Fossils Objectives Identify and describe the types of fossils. Define fossils Explain fossil formation Explain how different kinds of fossils show traces of life from Earth

More information

Chapter: Clues to Earth s Past

Chapter: Clues to Earth s Past Table of Contents Chapter: Clues to Earth s Past Section : Section 2: Relative Ages of Rocks Section 3: Absolute Ages of Rocks Traces of the Distant Past Paleontologists, scientists who study fossils,

More information

Geologic 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 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 information

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

TRACE 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 information

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

Lecture 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 information

Clues to Earth s Past. Fossils and Geologic Time

Clues 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 information

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

Objectives. 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 information

Warm ups *Name and briefly describe one of Africa s geographic regions.

Warm ups *Name and briefly describe one of Africa s geographic regions. Warm ups 2.28.2017 *Name and briefly describe one of Africa s geographic regions. Lesson Objective: *describe general time periods that the study of African history can be divided into *describe methods

More information

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

Studying The Past. Why Do We Study Fossils Found in Rocks? I. What is a Fossil? Studying The Past A. Definition: The evidence or remains of once-living plants or animals Why Do We Study Fossils Found in Rocks? QQ#1 what is a fossil? Why are they important? A.

More information

FOSSILS. Book G Chapter 4 Section 1

FOSSILS. 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 information

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

The 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 information

Geologic History. Earth is very, very old

Geologic 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 information

Lecture Title ( Fossils ) & Date. Main Ideas/Lecture Topics/Questions. Big Ideas or Chunking the Lecture

Lecture Title ( Fossils ) & Date. Main Ideas/Lecture Topics/Questions. Big Ideas or Chunking the Lecture Lecture Title ( Fossils ) & Date Main Ideas/Lecture Topics/Questions Big Ideas or Chunking the Lecture Fossil Trilobites Point of View #1 Natural selection provides a scientific explanation for the fossil

More information

Rules to a story!!what?!!when?!!where?!!why?! ANTH 42: Primates in Nature! WHEN: Dating methods! Lecture 2:! Primate evolution!

Rules to a story!!what?!!when?!!where?!!why?! ANTH 42: Primates in Nature! WHEN: Dating methods! Lecture 2:! Primate evolution! ANTH 42: Primates in Nature! Lecture 2:! Primate evolution! http://weber.ucsd.edu/~jmoore/courses/anth42web/! Rules to a story! What?! When?! Where?! Why?! but today, not in that order:! When? Dating methods

More information

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

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

More information

Introduction to Archaeology: Notes 9 Chronology, part 2 Copyright Bruce Owen 2009 Trapped-charge dating methods Several different kinds, one basic

Introduction to Archaeology: Notes 9 Chronology, part 2 Copyright Bruce Owen 2009 Trapped-charge dating methods Several different kinds, one basic Introduction to Archaeology: Notes 9 Chronology, part 2 Copyright Bruce Owen 2009 Trapped-charge dating methods Several different kinds, one basic principle All measure the accumulated damage (displaced

More information

Geohistory Review. Things you need to know:

Geohistory 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 information

Determining Earth's History Rocks and Ice Cores

Determining 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 information

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

6/30/2018. Geologic Time. Earth, Chapter 9 Chapter 9 Geologic Time 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 Geologic Time Earth, Chapter 9 Chapter 9 Geologic Time The Importance of a Time Scale Interpreting Earth s history is an important goal of the science of

More information

1 Looking at Fossils. What are fossils? How are fossils formed? What can fossils tell us about the history of life on earth?

1 Looking at Fossils. What are fossils? How are fossils formed? What can fossils tell us about the history of life on earth? CHAPTER 9 SECTION The History of Life on Earth 1 Looking at Fossils California Science Standards 7.3.c, 7.4.c, 7.4.e BEFORE YOU READ After you read this section, you should be able to answer these questions:

More information

NAME GEOL.2150 FORENSIC GEOLOGY CARBON-14 DATING

NAME GEOL.2150 FORENSIC GEOLOGY CARBON-14 DATING NAME GEOL.2150 FORENSIC GEOLOGY CARBON-14 DATING I. Introduction One of the tools available to scientists who study ancient history (natural and human) is carbon-14 dating (also known as carbon dating

More information

HISTORICAL GEOLOGY. Relative & Absolute age, fossils and geologic time

HISTORICAL GEOLOGY. Relative & Absolute age, fossils and geologic time HISTORICAL GEOLOGY Relative & Absolute age, fossils and geologic time Historical Geology A. Measuring Time 1. Relative Time (Relative Age) Measurement of time using comparison. No numbers used; uses words

More information

Question #1: What are some ways that you think the climate may have changed in the area where you live over the past million years?

Question #1: What are some ways that you think the climate may have changed in the area where you live over the past million years? Reading 5.2 Environmental Change Think about the area where you live. You may see changes in the landscape in that area over a year. Some of those changes are weather related. Others are due to how the

More information

Humanity on the Record

Humanity on the Record Humanity on the Record Humanity on the Record In the summer of 2012, paleontologists working on a fossil excavation in Kenya announced that the human race, as we know it, was never alone. Scientists unveiled

More information

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

Name Class Date. What are fossils? How are fossils formed? What can fossils tell us about the history of life on earth? CHAPTER 5 2 Looking at Fossils SECTION The Fossil Record BEFORE YOU READ After you read this section, you should be able to answer these questions: What are fossils? How are fossils formed? What can fossils

More information

How Old is the Solar System?

How Old is the Solar System? How Old is the Solar System? Earth s crust is constantly changing due to volcanoes, erosion, and plate tectonics. So Earth rocks do not preserve a record of the early days of the Solar System. Instead,

More information

Fossils. Ch. 29 and 30 Overview

Fossils. 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 information

TOPIC 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 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 information

geologic age of Earth - about 4.6 billion years

geologic 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 information

Chapter 2 Notes Methods of Studying the Human Past pp

Chapter 2 Notes Methods of Studying the Human Past pp Chapter 2 Notes Methods of Studying the Human Past pp. 31-51 Objectives: What are archaeological sites and fossil localities and how are they found? How are sites and localities investigated? How are archaeological

More information

1. What is the definition of uniformitarianism? 2. What is the definition of organic? 4. What is the definition of inorganic?

1. What is the definition of uniformitarianism? 2. What is the definition of organic? 4. What is the definition of inorganic? Earth Science Unit 3- History of the Earth Knowledge Packet Learning Target 3B: Have you ever thought about the history of the Earth? No, well you should have because it s pretty cool. Things like mountain

More information

Lesson Checkpoint: Name one animal that you know is extinct.

Lesson Checkpoint: Name one animal that you know is extinct. FOSSILS AND EXTINCT ANIMALS Extinct Animals Many animals have become extinct over millions of years. Extinct means that no longer living on Earth. When a species is extinct, it means there aren t any animals

More information

GEOLOGIC EVENTS SEDIMENTARY ROCKS FAULTING FOLDING TILTING

GEOLOGIC 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 information

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

Geologic 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 information

Guided Notes Geologic History

Guided 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 information

6. Relative and Absolute Dating

6. 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 information

Chapter 4. Archaeological. Dating Methods

Chapter 4. Archaeological. Dating Methods Chapter 4. Archaeological 4.1. Dentrochronology and other tools 4.2. Dating with radioactive clocks 4.3. Mapping change and development 4.4. Migration and colonization 4.5. Accelerator mass spectrometry

More information

Before 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. 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 information

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

Principle 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 information

Our Origins Discovering Physical Anthropology

Our Origins Discovering Physical Anthropology W. W. Norton & Company Our Origins Discovering Physical Anthropology Second Edition by Clark Spencer Larsen Chapter 8 Clark Spencer Larsen Our Origins DISCOVERING PHYSICAL ANTHROPOLOGY C. Milner-Rose Chapter

More information

Evolutionary Evidence of Evolution

Evolutionary Evidence of Evolution Evolutionary Evidence of Evolution Evolution - the process in which relative changes in the genetic makeup (characteristics) of a species occurs over time Sometimes changes in populations are environmental

More information

Chapter 17. Geologic Time: Concepts and Principles

Chapter 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 information

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

Integrated 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 information

Chapter 3 Time and Geology

Chapter 3 Time and Geology Chapter 3 Time and Geology Methods of Dating Rocks 1. Relative dating - Using fundamental principles of geology (Steno's Laws, Fossil Succession, etc.) to determine the relative ages of rocks (which rocks

More information

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

Strata Sample. 1. Make a drawing of the strata sample (beaker) in your fold. Be sure to add color :) strata: layer of sedimentary rock/soil Strata Sample 1. Make a drawing of the strata sample (beaker) in your fold. Be sure to add color :) 2. Identify which layer is the OLDEST and which layer is the YOUNGEST

More information

Geologic Time. Trilobites

Geologic Time. Trilobites Trilobites Geologic Time A major difference between geologists and most other scientists is their concept of time. A "long" time may not be important unless it is greater than 1 million years 1 Two Ways

More information

Geologic Time: Concepts and Principles

Geologic 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 information

FOSSILS Uncovering Clues to the Earth s Past

FOSSILS Uncovering Clues to the Earth s Past FOSSILS Uncovering Clues to the Earth s Past Fossils form when water replaces the cells of dead animals or plants with minerals. These minerals then petrify into rock to form the fossils we see in museums.

More information

Lesson Learning Goal

Lesson 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 information

Hard Parts of Organisms: Bones Shells Hard Parts of Insects Woody Material (trunks) Fossils provide evidence of how life has changed over time.

Hard Parts of Organisms: Bones Shells Hard Parts of Insects Woody Material (trunks) Fossils provide evidence of how life has changed over time. PLEASE, PICK UP OUTLINE FROM THE FRONT TABLE! *recommend adding the extra stuff to the notes Fossus - means to dig up Fossils are preserved remains or traces of living things. Most fossils form when living

More information

An 80 milligram sample of a radioactive isotope decays to 5 milligrams in 32 days. What is the half-life of this element?

An 80 milligram sample of a radioactive isotope decays to 5 milligrams in 32 days. What is the half-life of this element? An 80 milligram sample of a radioactive isotope decays to 5 milligrams in 32 days. What is the half-life of this element? A. 8 days B. 2 days C. 6 days D. 4 days An original sample of a radioisotope had

More information

Chapter 14: The Changing Climate

Chapter 14: The Changing Climate Chapter 14: The Changing Climate Detecting Climate Change Natural Causes of Climate Change Anthropogenic Causes of Climate Change Possible Consequences of Global Warming Climate Change? -Paleo studies

More information

Deep time records showcase: Earth Systems

Deep time records showcase: Earth Systems What is Deep Time? Most geoscientists view Deep Time as pertaining to the pre- Quaternary (>10ka [10 4 ]) Last 10ka witnessed a short duration under anomalous conditions of an Icehouse climate state Earth

More information

A n t h r o p o l o g y

A n t h r o p o l o g y A n t h r o p o l o g y Appreciating Human Diversity Fifteenth Edition Conrad Phillip Kottak University of Michigan McGraw-Hill 2013 McGraw-Hill Companies. All Rights Reserved. C H A P T E R DOING ARCHAEOLOGY

More information

Welcome to General Geology!!

Welcome to General Geology!! Welcome to General Geology!! Professor Weeden: lori_weeden@uml.edu x3344 Olney 402B Class webpage: http://faculty.uml.edu/lweeden/gengeo.htm Text: Murck, BW & Skinner, BJ (2012) Visualizing Geology 3 rd

More information

Phys 214. Planets and Life

Phys 214. Planets and Life Phys 214. Planets and Life Dr. Cristina Buzea Department of Physics Room 259 E-mail: cristi@physics.queensu.ca (Please use PHYS214 in e-mail subject) Lecture 10. Geology and life. Part 1 (Page 99-123)

More information

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

Name 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 information

Timing of Geologic Events. Geologic Time Terms. Laws / Principles of Stratigraphy

Timing of Geologic Events. Geologic Time Terms. Laws / Principles of Stratigraphy Geologic Time Terms Hadean Archean Proterozoic Phanerozoic Paleozoic Mesozoic Cenozoic(Tertiary) Cambrian Unconformity Angular unconformity Half-life Alpha particle Beta particle Gamma ray Neutron UT How

More information

There are actually 5 processes

There are actually 5 processes There are actually 5 processes )WEATHERING hen rocks are roken down nto sediment y Physical and hemical orces 2) ERODE - when sediment is CARRIED to a new location 3) DEPOSIT - when sediment is DROPPED

More information

Chapter 3 Time and Geology

Chapter 3 Time and Geology Chapter 3 Time and Geology Finding the age of rocks: Relative versus Actual Dating The science that deals with determining the ages of rocks is called geochronology. Methods of Dating Rocks 1. Relative

More information

Unit 2 Lesson 1 Geologic Change over Time. Copyright Houghton Mifflin Harcourt Publishing Company

Unit 2 Lesson 1 Geologic Change over Time. Copyright Houghton Mifflin Harcourt Publishing Company Been There, Done That What is the principle of uniformitarianism? The principle of uniformitarianism states that geologic processes that happened in the past can be explained by current geologic processes.

More information

The Earth. February 26, 2013

The Earth. February 26, 2013 The Earth February 26, 2013 The Planets 2 How long ago did the solar system form? Definition: Cosmic Rays High-energy particles that constantly bombard objects in space Mostly they are hydrogen nuclei

More information

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

11/5/2015. Creating a Time Scale - Relative Dating Principles. Creating a Time Scale - Relative Dating Principles. The Geologic Time Scale GEOL 110: PHYSICAL GEOLOGY Why is the Geologic Time Scale important? Rocks record geologic and evolutionary changes throughout Earth s history Without a time perspective, events have little meaning Chapter

More information

Before 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. 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 information

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

Studying 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 information

Homework. Directed Reading Chapter 5 Section 1 #1-17

Homework. Directed Reading Chapter 5 Section 1 #1-17 Homework Directed Reading Chapter 5 Section 1 #1-17 Create a Species Project Learning Targets I can explain how comparing organisms can provide evidence that they have common ancestors. What is the evidence

More information

Fossils. Presented by Kesler Science

Fossils. Presented by Kesler Science Presented by Kesler Science Essential Questions: 1. What are fossils? 2. What are some different types of fossilization? 3. What is the difference between relative and absolute age? 4. What does the fossil

More information

Name Test Date Hour. forms that lived only during certain periods. abundant and widespread geographically. changes to the surface of Earth.

Name Test Date Hour. forms that lived only during certain periods. abundant and widespread geographically. changes to the surface of Earth. Name Test Date Hour Earth Processes#3 - Notebook Earth s History LEARNING TARGETS I can explain the lack of evidence about the Precambrian Time. I can describe possible causes for the mass extinction in

More information

Stratigraphy and Geologic Time. How old are the rocks?

Stratigraphy and Geologic Time. How old are the rocks? Stratigraphy and Geologic Time How old are the rocks? 1 Questions What is the difference between Absolute and Relative dating? How old is the Earth? How can we use fossils to date rocks? How are the absolute

More information

Determining geological ages

Determining 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 information

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

8. 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 information

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

2. Can you name earth s three eras and explain why they are divided that way? Unit: 3 Earth s History LT 3.1 Earth s History: I can map out a basic history of the earth, including key events. 1. Can you place the key events of earth s history in order? #1 Yes I can: 2. Can you name

More information

Name: Period: Half-life and Radiometric Dating

Name: Period: Half-life and Radiometric Dating Name: Period: Half-life and Radiometric Dating Purpose: The purpose of this lab is to understand half-life and how it is used in determining the age of materials. Students will also understand the limitations

More information

Clues to Earth s Past

Clues to Earth s Past chapter 3 3 Clues to Earth s Past section 3 Absolute Ages of Rocks What You ll Learn how absolute age differs from relative age how the half-lives of isotopes are used to tell a rock s age Before You Read

More information