Use of Megasequences to Re-Create Pre-Flood Geography
|
|
- Roxanne Quinn
- 5 years ago
- Views:
Transcription
1 Use of Megasequences to Re-Create Pre-Flood Geography Timothy L. Clarey and Davis J. Werner Institute for Creation Research
2 Goals of the Study 1. Examine the Sedimentological Record Megasequence-by-Megasequence Across Three Continents 2. Analysis of the Fossil Record by Megasequence 3. Establish Criteria For Pre-Flood Geography
3 Methods Compiled Stratigraphic Columns-Rockworks Lithologies, 6 megasequences Published Columns, Oil Wells, Outcrops, Seismic and Cross-section Data 710-N. America, 429-Africa, 405-S. America
4 Example Column Michigan Basin
5 Sloss-type Sequences
6
7 Transgressive/Regressive Cycles
8 Sequences Make Good Reflectors Seismic Stratigraphy
9 Correlated the Sequences Globally
10 Results 1. Similarity in Areal Extent of Sauk, Tippecanoe, and Kaskaskia Megasequences
11
12
13
14 Results 2. Similarity in Fossils within the Sauk, Tippecanoe and Kaskaskia Megasequnces
15 The Geologic Column Kask. Tippe. Sauk
16 Sauk Fossils Shallow Marine
17 Tippecanoe Fossils Shallow Marine
18 Kaskaskia Fossils Shallow Marine
19 Results 3. Limited Sediment Volume in Sauk, Tippecanoe and Kaskaskia Megasequences
20 In Cubic Kilometers
21 In Cubic Kilometers
22 In Cubic Kilometers
23 Combined Sauk, Tippecanoe, Kaskaskia Thickness Maps
24 Results 4. Increasing Terrestrial Fossils in the Absaroka, Zuni and Tejas Megasequences
25 Absaroka Megasequence
26 Animal Fossil Occurrences in Paleobiology Database 12 Aquatic Phyla Sauk-Kask. Abs.-Zuni 3 Terrestrial Phyla, Mammals, Reptiles, Insects
27 Plant Occurrences in Paleobiology Database Courtesy of Dr. Nate Jeanson
28 Results 5. Increasing Areal Volume and/or Coverage of Absaroka Megasequence
29 Sauk, Tippecanoe, Kaskaskia Absaroka
30
31 Sauk, Tippecanoe Kaskaskia Absaroka
32
33 Sauk, Tippecanoe Kaskaskia Absaroka
34
35 Creation of a New Ocean Crust
36 Sedimentary Wedge from West Coast Subduction Continental crust
37 Splitting Up of the Continents
38 Shift in Depositional Pattern Reflects Change in Tectonics Sauk-Kaskaskia Thickness Absaroka Thickness
39 Absaroka: 1st Global Appearance of Large Sand Waves
40 1 st Appearance of Extensive Coal Beds
41 Absaroka Fossils Large Land/Marine Reptiles Mix
42 Results 6. Maximum Extent/Volume Globally During Zuni Megasequence
43
44
45 Tejas
46
47
48 Tejas
49 Zuni Fossils Large Land/Marine Reptiles Mix
50 Zuni Absar.
51
52
53 Tejas
54
55 Assumptions 1. Pre-Flood lows would be filled in first Sauk, Tippecanoe, Kaskaskia 2. Higher land would be filled in later Absaroka 3. Flood reached a maximum height at 150 Days Zuni was the maximum extent/volume
56 Identified Three Environments 1. Shallow Seas-S,T,K level 2. Lowlands-Absaroka/Zuni Level 3. Uplands- Shield Areas Tejas level
57 How did Dinosaurs survive the early Flood?
58 How did the Dinosaurs Survive the early Flood?
59
60 How did the Dinosaurs Survive the early Flood? Sauk-Kaskaskia Thickness
61
62
63 Uplands Dinosaur Peninsula
64 Tejas Likely Wiped Off Highest Areas And the Lord said, I will wipe off man whom I have created from the face of the land, from man to animals to creeping things and to birds of the sky; for I am sorry that I have made them. Gen 7:23 (Russ Humphreys).
65
66 Tejas
67 Tejas Fossils Large Land Mammals/ Marine Mix
68 Conclusions 1. Results Based on observable data 2. Pre-Flood world segregated by topography 3. Propose Ecological Zonation-Megasequence Model 4. Defined by the extent of Megasequences
69
70
71
USE OF SEDIMENTARY MEGASEQUENCES TO RE-CREATE PRE-FLOOD GEOGRAPHY
Clarey, T.L., and D.J. Werner. 2018. Use of sedimentary megasequences to re-create pre-flood geography. In Proceedings of the Eighth International Conference on Creationism, ed. J.H. Whitmore, pp. 351
More informationGLOBAL STRATIGRAPHY AND THE FOSSIL RECORD VALIDATE A FLOOD ORIGIN FOR THE GEOLOGIC COLUMN
Clarey, T.L., and D.J. Werner. 2018. Global stratigraphy and the fossil record validate a Flood origin for the geologic column. In Proceedings of the Eighth International Conference on Creationism, ed.
More informationPLATE TECTONICS. SECTION 17.1 Drifting Continents
Date Period Name PLATE TECTONICS SECTION.1 Drifting Continents In your textbook, read about continental drift. Circle the letter of the choice that best completes each statement. 1. Early mapmakers thought
More informationGeosphere Final Exam Study Guide
Geosphere Final Exam Study Guide Chapter 1 Intro to Earth Systems 1. Name and describe Earth s 4 major spheres Geosphere-- nonliving, mostly solid rock divided into crust, mantle, and core Atmosphere a
More informationGEL 113 Historical Geology
GEL 113 Historical Geology COURSE DESCRIPTION: Prerequisites: GEL 111 Corequisites: None This course covers the geological history of the earth and its life forms. Emphasis is placed on the study of rock
More informationLecture Outlines PowerPoint. Chapter 12 Earth Science 11e Tarbuck/Lutgens
Lecture Outlines PowerPoint Chapter 12 Earth Science 11e Tarbuck/Lutgens 2006 Pearson Prentice Hall This work is protected by United States copyright laws and is provided solely for the use of instructors
More informationMesozoic Earth History
Mesozoic Earth History The Mesozoic Era 251-66 MYA Breakup of Pangea Changes in air and oceanic currents Evolution of new terrestrial and marine life Opening of the Atlantic Ocean Basin Rocky Mountains
More informationPLATE TECTONICS THEORY
PLATE TECTONICS THEORY Continental drift Sea floor spreading CONTINENTAL DRIFT CONTINENTAL DRIFT 1. The fitness of continents and Continental Reconstruction Earth ~200 million years ago 1.1 Geometrical
More informationDepositional Environments. Depositional Environments
Depositional Environments Geographic area in which sediment is deposited Characterized by a combination of geological process & environmental conditions Depositional Environments Geological processes:
More informationQuestion #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 informationLecture 24: Paleozoic 1:
UNIVERSITY OF SOUTH ALABAMA GY 112: Earth History Lecture 24: Paleozoic 1: Laurentia Instructor: Dr. Douglas W. Haywick Last Time (before the exam) The Cambrian Explosion A) Why a Cambrian explosion B)
More informationSediment and Sedimentary rock
Sediment and Sedimentary rock Sediment: An accumulation of loose mineral grains, such as boulders, pebbles, sand, silt or mud, which are not cemented together. Mechanical and chemical weathering produces
More information* If occurs, fossils that formed in shallow water may be found in water. Subsidence mean the crust is.
Name Notes: Topic 5B Topic 5B: The Dynamic Crust A. What evidence exists that proves the Earth s Crust is and has moved? Earth Science 1. Tilted, folded or faulted strata Strata is a term that refers to.
More informationThe shape and geology of the continents suggests that they were once joined together.
Drifting Continents Section 17.1 Drifting Continents The shape and geology of the continents suggests that they were once joined together. Review Vocabulary hypothesis: testable explanation of a situation
More informationDO NOT WRITE ON THIS EXAM ONLY WRITE ON THE ANSWER SHEET!
DO NOT WRITE ON THIS EXAM ONLY WRITE ON THE ANSWER SHEET! Multiple Choice Questions (30 points) for each question, please choose the best answer and circle your answer on the answer sheet (do not write
More informationCopyright 2016 Edmentum - All rights reserved.
Copyright 2016 Edmentum - All rights reserved. SI: Quiz 13 Question #1 The Earth's crust is made up of plates that can move. Which of the following topographic features could be directly formed by the
More informationSpring th Grade
Spring 2015 8 th Grade The geologic time scale is a record of the major events and diversity of life forms present in Earth s history. The geologic time scale began when Earth was formed and goes on until
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 informationMOR SEAWAY TEACHERS. A CHANGING LANDSCAPE Activity Overview BIG IDEA
MOR SEAWAY 03 Activity Overview BIG IDEA The Earth and its landscapes change over time. Scientists use the fossil record to understand the Earth s environments and climates millions of years ago. OBJECTIVE
More informationCh 17 Plate Tectonics Big Idea: Most geologic activity occurs at the boundaries between plates.
Ch 17 Plate Tectonics Big Idea: Most geologic activity occurs at the boundaries between plates. 17.1 Drifting Continents 17.2 Seafloor Spreading 17.3 Plate Boundaries 17.4 Causes of Plate Motions Learning
More informationTerrain Units PALEOGEOGRAPHY: LANDFORM CREATION. Present Geology of NYS. Detailed Geologic Map of NYS
NYS TOPOGRAPHY Why so? PALEOGEOGRAPHY: LANDFORM CREATION Prof. Anthony Grande AFG 014 Present Geology of NYS Detailed Geologic Map of NYS Generalized Geology Detailed Geology Hot links to the fold out
More informationPlate Tectonics Practice Test
Plate Tectonics Practice Test 1. What is the main idea Alfred Wegner proposed in the Theory of Continental Drift that he published in 1915? a. The continents float on a liquid layer that allows them to
More informationA) B) C) D) 4. Which diagram below best represents the pattern of magnetic orientation in the seafloor on the west (left) side of the ocean ridge?
1. Crustal formation, which may cause the widening of an ocean, is most likely occurring at the boundary between the A) African Plate and the Eurasian Plate B) Pacific Plate and the Philippine Plate C)
More informationWarm Up Name the 5 different types of fossils
Warm Up Name the 5 different types of fossils Timeline that organizes the events in Earths history. Earth is about 4.7 billion years old. More complex organism such as land plants and fish evolved only
More information1. I can describe evidence for continental drift theory (e.g., fossil evidence, mountain belts, paleoglaciation)
Science 10 Review Earth Science Vocabulary asthenosphere continental drift theory converging plates diverging plates earthquakes epicentre fault hot spot inner core lithosphere mantle mantle convection
More informationLab 7: Sedimentary Structures
Name: Lab 7: Sedimentary Structures Sedimentary rocks account for a negligibly small fraction of Earth s mass, yet they are commonly encountered because the processes that form them are ubiquitous in the
More information5 Time Marches On. TAKE A LOOK 1. Identify What kinds of organisms formed the fossils in the picture?
CHAPTER 6 5 Time Marches On SECTION The Rock and Fossil Record BEFORE YOU READ After you read this section, you should be able to answer these questions: How do geologists measure time? How has life changed
More informationEARTH SURFACE PROCESSES AND SEDIMENTATION!
Sed and Strat EARTH SURFACE PROCESSES AND SEDIMENTATION! 2/27 Lecture 7- Exposure: Weathering and the Sediment Factory 3/04 Lecture 8 - Rivers and Landscapes 3/06 Lecture 9 - Waves (not Tides) 3/11 Lecture
More informationThe Mesozoic. Wednesday, November 30, 11
The Mesozoic Periods of the Mesozoic Triassic- First period of the Mesozoic era Jurassic Cretaceous- Last period of the Mesozoic era Breakup of Pangaea Stage one (Triassic) Rifting and volcanism, normal
More informationGeography 3202 Unit 4 S.C.O. 4.3 & 4.5. Primary Resource Activities Offshore Oil And Gas
Geography 3202 Unit 4 S.C.O. 4.3 & 4.5 Primary Resource Activities Offshore Oil And Gas Factors Affecting The Decision To Recover Offshore Oil And Gas (4.3.1) Physical Factors 1. Ocean Related Factors
More information3. [ES 3] 1. [ST8.2] Some processes that shape Earth s surface are slow. Other processes are rapid. Which statement describes a rapid change?
Science 8 SCIENCE QUARTERLY ASSESSMENT 2 3. [ES 3] S 1. [ST8.2] Some processes that shape Earth s surface are slow. Other processes are rapid. Which statement describes a rapid change? A. Glaciers melt
More informationMCAS QUESTIONS: THE EARTH S INTERIOR, CONTINENTAL DRIFT, PLATE TECTONICS
NAME: PER: MCAS QUESTIONS: THE EARTH S INTERIOR, CONTINENTAL DRIFT, PLATE TECTONICS 1. Which of the following statements best explains why the lower mantle of Earth is much more rigid and dense than the
More informationEvidence for Continental Drift and The Theory of Plate Tectonics
Evidence for Continental Drift and The Theory of Plate Tectonics Did you know that the coal that is mined in Pennsylvania was actually formed from tropical plant life near the Equator? How did it travel
More informationTheory of Continental Drift
Plate Tectonics Theory of Continental Drift Alfred Wegener suggested that continents had once been part of a supercontinent named Pangaea, that later broke up. The pieces moved apart over millions of years
More informationB.C. s Offshore Oil and Gas: a Guide to the Geology and Resources.
B.C. s Offshore Oil and Gas: a Guide to the Geology and Resources. Introduction Beneath the offshore regions of British Columbia are four moderately large, geologically young sedimentary basins (Figure
More informationCreation vs. Evolution
Creation vs. Evolution The Biblical Creation Model 1. Special Creation of all things by God in six solar days. 2. The Curse on all things because of sin. All things are dying. 3. The global Flood of Noah
More informationUnit 10 Lesson 2 What Was Ancient Earth Like? Copyright Houghton Mifflin Harcourt Publishing Company
How Rocks and Fossils Tell a Story Sedimentary rock forms in layers. Many sedimentary rocks contain fossils. The oldest rock layers are at the bottom, and the youngest rock layers are at the top. The relative
More informationWhat is the Earth s time scale?
Earth History What is the Earth s time scale? The Geological time scale is a record of the life forms and geological events in Earth s history. Scientists developed the time scale by fossils world wide.
More informationControls on clastic systems in the Angoche basin, Mozambique: tectonics, contourites and petroleum systems
P2-2-13 Controls on clastic systems in the Angoche basin, Mozambique: tectonics, contourites and petroleum systems Eva Hollebeek, Olivia Osicki, Duplo Kornpihl Schlumberger, London, UK Introduction Offshore
More informationOil & Gas. From exploration to distribution. Week 1 V05 Origin of hydrocarbon resources part 1. Jean-Pierre Deflandre
Oil & Gas From exploration to distribution Week 1 V05 Origin of hydrocarbon resources part 1 Jean-Pierre Deflandre W1V5 Origin of hydrocarbon resources1 p. 1 Introduction to hydrocarbon resources You will
More informationSEDIMENTARY BASINS Red Sea Coast of Egypt. by Prof. Dr. Abbas Mansour
SEDIMENTARY BASINS Red Sea Coast of Egypt by Prof. Dr. Abbas Mansour Sedimentary basins Sedimentary basins are, in a very broad sense, all those areas in which sediments can accumulate to considerable
More informationUnit 5 Possible Test Questions Mesozoic and Cenozoic Eras HISTORICAL GEOLOGY
Revised 8/16 Unit 5 Possible Test Questions Mesozoic and Cenozoic Eras HISTORICAL GEOLOGY Mesozoic Era Eons, Eras and Periods 1. List the Mesozoic periods in order (oldest to youngest). End of the Paleozoic
More informationGrand Unifying Theory of everything... for the Geosciences, at least!
Plate Tectonics: Grand Unifying Theory of everything... for the Geosciences, at least! The Earth s lithosphere, composed of Oceanic and continental crust, is broken up into pieces that move and interact
More informationThe Nature of Sedimentary Rocks
The Nature of Sedimentary Rocks Sedimentary rocks are composed of: Fragments of other rocks Chemical precipitates Organic matter or biochemically produced materials The Nature of Sedimentary Rocks Sedimentary
More informationHistory of Plate Tectonics
History of Plate Tectonics Continental Drift The hypothesis of how the continents were all once together and then split apart and drifted to their current location. classroomatsea.net Early Thoughts Elie
More informationIntroduction To Plate Tectonics Evolution. (Continents, Ocean Basins, Mountains and Continental Margins)
Introduction To Plate Tectonics Evolution (Continents, Ocean Basins, Mountains and Continental Margins) Geo 386 (Arabian Shield Course) Dr. Bassam A. A. Abuamarah Mohanna G E O 3 8 6 A R A B I A N G E
More informationBefore Plate Tectonics: Theory of Continental Drift
Before Plate Tectonics: Theory of Continental Drift Predecessor to modern plate tectonics Shape and fit of the continents was the initial evidence Snider-Pelligrini (1858) Taylor (1908) Wegner (1915) Fig.
More informationDirected Reading. Section: Precambrian Time and the Paleozoic Era EVOLUTION. beginning of life is called. to. PRECAMBRIAN TIME.
Skills Worksheet Directed Reading Section: Precambrian Time and the Paleozoic Era 1. Where is the geologic history of Earth recorded? 2. What kind of information can scientists get from the types of rock
More informationUNIT 3 GEOLOGY VOCABULARY FLASHCARDS THESE KEY VOCABULARY WORDS AND PHRASES APPEAR ON THE UNIT 3 CBA
UNIT 3 GEOLOGY VOCABULARY FLASHCARDS THESE KEY VOCABULARY WORDS AND PHRASES APPEAR ON THE UNIT 3 CBA A map that shows Earth s Topographic Map surface topography, which is Earth s shape and features Contour
More informationGRADE 7 SCIENCE UNIT 4: THE EARTH S CRUST. 11/12 Earth s Crust is constantly changing Weathering and Erosion
GRADE 7 SCIENCE UNIT 4: THE EARTH S CRUST 11/12 Earth s Crust is constantly changing Weathering and Erosion Earth s Structure - Layers of the Earth Draw a labeled Diagram Layers of the Earth Rap s https://www.youtube.com/watch?v=q9j1xgaxyzy
More informationFossils provide evidence of the change in organisms over time.
Section 1: Fossils provide evidence of the change in organisms over time. K What I Know W What I Want to Find Out L What I Learned Essential Questions What are the similarities and differences between
More informationLaboratory 7 Geologic Time
(Name) Laboratory 7 Geologic Time We will be exploring ideas behind the development of the geological column. The geological column is a general term that is used to describe the template behind which
More informationSediment and sedimentary rocks Sediment
Sediment and sedimentary rocks Sediment From sediments to sedimentary rocks (transportation, deposition, preservation and lithification) Types of sedimentary rocks (clastic, chemical and organic) Sedimentary
More informationWhat Happened to the Dinosaurs?
A great extinction event occurred 65 million years ago, and creatures like these disappeared. What Happened to the Dinosaurs? Great Extinction Event @ 65 MA Walt Disney s view. On land, the big dinosaurs
More informationwater erosion lithosphere Describe the process of erosion and deposition. chemical weathering Dissolving limestone is an example of.
At one time, there was one large island off the coast of Mississippi and now it is two separate islands. What caused the island to be split into two? water erosion The crust and the top part of the upper
More informationPlate Tectonics Tutoiral. Questions. Teacher: Mrs. Zimmerman. Plate Tectonics and Mountains Practice Test
Teacher: Mrs. Zimmerman Print Close Plate Tectonics and Mountains Practice Test Plate Tectonics Tutoiral URL: http://www.hartrao.ac.za/geodesy/tectonics.html Questions 1. Fossils of organisms that lived
More informationTopic 5: The Dynamic Crust (workbook p ) Evidence that Earth s crust has shifted and changed in both the past and the present is shown by:
Topic 5: The Dynamic Crust (workbook p. 65-85) Evidence that Earth s crust has shifted and changed in both the past and the present is shown by: --sedimentary horizontal rock layers (strata) are found
More information2 Earth s Changing Continents
CHAPTER 9 SECTION The History of Life on Earth 2 Earth s Changing Continents California Science Standards 7.4.a, 7.4.e, 7.4.f BEFORE YOU READ After you read this section, you should be able to answer these
More informationGEOLOGICAL AGE OF ROCKS. Absolute geological age
GEOLOGICAL AGE OF ROCKS Absolute geological age The pioneer of nuclear physics discovered at the turn of centuries that atoms of certain elements, the radioactive ones, spontaneously disintegrate to form
More informationPHYSICAL GEOLOGY AND THE ENVIRONMENT (2 ND CANADIAN EDITION)
Chapter 2: Plate Tectonics Chapter Summary: Plate tectonics is a theory that suggests Earth's surface is divided into several large plates that change position and size. Intense geologic activity occurs
More informationSection 1: How Did Life Begin? Chapter 19: History of Life on Earth. Section 2: The Age of Earth
Chapter 19: History of Life on Earth Section 1: How Did Life Begin? I. The Basic Chemicals of Life A. 1920s B. Earth s early oceans contained large amounts of organic molecules C. Molecules formed spontaneously
More informationGLY Coastal Geomorphology Notes
GLY 4734 - Coastal Geomorphology Notes Dr. Peter N. Adams Spring 2011 2 Coastal Classification In this lecture, we discuss some successful classification schemes of the coastal landscape, and pay particular
More informationFOSSILS 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 informationName Class Date. In the space provided, write the letter of the definition that best matches the term or phrase.
Skills Worksheet Directed Reading Section: The Changing Continents 1. What is the result of slow movements of tectonic plates? RESHAPING EARTH S CRUST In the space provided, write the letter of the definition
More informationEarth History Teacher Rubrics and Directions
Earth History Teacher Rubrics and Directions 1.a. Using the tools provided, observe the three rock samples, A, B, and C. One is sandstone, one is shale, and one is limestone. Make a chart to record your
More informationplate tectonics review #2
plate tectonics review #2 Score: 1. Solid due to high pressure mantle inner core outer core crust 2. why is oceanic crust younger than continental crust subduction reduction mountain building plasticity
More informationPlate tectonics model for the continental collisions during Late Paleozoic
Alleghanian orogeny During Late Paleozoic, northwestern Africa collided with southeastern North America, causing the Alleghanian orogeny, and building the Appalachian mountains. The orogeny began during
More informationMajor geological events fit into a timeline, beginning with the formation of the Earth
Chapter 4 Major geological events fit into a timeline, beginning with the formation of the Earth 4.1 The origin and development of life William Smith was a canal engineer who supervised the excavation
More information2. NAME OF INQUIRY: Geologic Framework of Missoula s Ecoregions
1. CONTRIBUTOR S NAME: Johnny MacLean 2. NAME OF INQUIRY: Geologic Framework of Missoula s Ecoregions 3. GOALS AND OBJECTIVES: a. Inquiry Questions: How does Missoula Valley s geologic history relate to
More informationPhanerozoic (last 0.54 by) Tectonics Climate Life
Phanerozoic (last 0.54 by) Tectonics Climate Life Tools for Locating Past Continent Positions Fossils depending on climate Alignment of geological features Geometrical fit of continental margins Similarity
More informationLECTURE #25: Mega Disasters - Mass Extinctions, Meteorite Impacts...
GEOL 0820 Ramsey Natural Disasters Spring, 2018 LECTURE #25: Mega Disasters - Mass Extinctions, Meteorite Impacts... Date: 19 April 2018 I. Time & Life on Earth geologic time scale o divided into named
More informationQuestions and Topics
Plate Tectonics and Continental Drift Questions and Topics 1. What are the theories of Plate Tectonics and Continental Drift? 2. What is the evidence that Continents move? 3. What are the forces that
More informationdiscussion of North America s physical features, including its landforms and bodies of
Chapter 7 Natural Environments of North America Chapter 7 focuses on the natural environments of North America. The chapter opens with a discussion of North America s physical features, including its landforms
More informationcore mantle crust the center of the Earth the middle layer of the Earth made up of molten (melted) rock
core the center of the Earth mantle the middle layer of the Earth made up of molten (melted) rock crust the surface layer of the Earth that includes the continents and oceans 1 continental drift the theory
More informationCrustal Activity. Plate Tectonics - Plates - Lithosphere - Asthenosphere - Earth s surface consists of a major plates and some minor ones
Name: Date: Period: Tectonics The Physical Setting: Earth Science CLASS NOTES Tectonics - s - Lithosphere - Asthenosphere - Earth s surface consists of a major plates and some minor ones The plates are
More informationModule 9: Earth's History Topic 3 Content: A Tour of Geologic Time Notes
The geologic time scale holds secrets to the life that has existed on Earth since the beginning of time. It is time for you to take a journey through the history of Earth. 1 Click on each of the segments
More informationEarth History. What is the Earth s time scale? Geological time Scale. Pre-Cambrian. FOUR Eras
The Earth is 4.6 billion years old! Earth History Mrs. Burkey ESS Cy Creek HS 17-18 If the Earth formed at midnight 6:00 am First life appears 10:00 pm First animals/plants on land 11:59 pm First humans
More informationMAR110 Lecture #5 Plate Tectonics-Earthquakes
1 MAR110 Lecture #5 Plate Tectonics-Earthquakes Figure 5.0 Plate Formation & Subduction Destruction The formation of the ocean crust from magma that is upwelled into a pair of spreading centers. Pairs
More informationHow the Earth was formed
How the Earth was formed Short Answer: (2 points a piece) 1) Who was the man that stated the Earth was 6000 yrs old? 2) Hutton determined that this age was incorrect, what lead him to a much later date?
More informationBI 101: Marine Biology
WELCOME BI 101: Marine Biology Contact Info 1. Full Name 2. Student I.D. Number 3. Major 4. Email address 5. Preferred phone contact 6. Have you taken any other BI 101 courses at LBCC? 7. Why did you decide
More informationMarine Science and Oceanography
Marine Science and Oceanography Marine geology- study of the ocean floor Physical oceanography- study of waves, currents, and tides Marine biology study of nature and distribution of marine organisms Chemical
More informationHOW GEOGRAPHY AND GEOLOGY AFFECT BIOLOGICAL DIVERSITY
HOW GEOGRAPHY AND GEOLOGY AFFECT BIOLOGICAL DIVERSITY Factors Affecting Extinction Rates Natural Factors Climate change Cataclysmic event (volcano, earthquake) Human Activities Habitat Loss/Fragmentation
More information3. The diagram below shows how scientists think some of Earth's continents were joined together in the geologic past.
1. The map below shows the present-day locations of South America and Africa. Remains of Mesosaurus, an extinct freshwater reptile, have been found in similarly aged bedrock formed from lake sediments
More informationDo Now: Vocabulary: Objectives. Vocabulary: 1/5/2016. Wegener? (Can they move?) the idea that continents have moved over time?
Do Now: 1. Who was Alfred Wegener? 2. What was Pangaea? 3. Are continents fixed? (Can they move?) 4. What evidence supports the idea that continents have moved over time? Objectives What evidence suggests
More informationBIOGEOCHEMICAL CYCLES
BIOGEOCHEMICAL CYCLES BASICS Biogeochemical Cycle: The complete path a chemical takes through the four major components, or reservoirs, of Earth s system (atmosphere, lithosphere, hydrosphere and biosphere)
More informationClues to the Past. Grades 6-8 Educational Program Guide
Clues to the Past Grades 6-8 Educational Program Guide OAS Science Practices: 1, 2, 3, 4, 6, 7, 8 Program Overview The Clues to the Past program will introduce students to several 300 million years old
More information1. The timeline below represents time on Earth from the beginning of the Paleozoic Era Ato the present B.
Name Roy G Biv 1. The timeline below represents time on Earth from the beginning of the Paleozoic Era Ato the present B. Which numbered position best represents the time when humans first appeared in the
More information24. Ocean Basins p
24. Ocean Basins p. 350-372 Background The majority of the planet is covered by ocean- about %. So the majority of the Earth s crust is. This crust is hidden from view beneath the water so it is not as
More information6. What is the absolute location (latitude and longitude) and relative location of your home town or the town in which you attend school?
Social Studies 10 Chapter 1 Worksheet Directions: Be sure to complete reading the chapter before you attempt these questions. Be aware that the Chapter Test will cover everything you read in the chapter,
More informationEssential Question: How are the geological features that exist on land similar to the geological features on the ocean floor?
Essential Question: How are the geological features that exist on land similar to the geological features on the ocean floor? Geography of the Oceans The world ocean can be divided into four main ocean
More informationLearning Goal: Students will review their understanding of earth s history Success Criteria: Students will solve a variety of problems Agenda: 1.
Learning Goal: Students will review their understanding of earth s history Success Criteria: Students will solve a variety of problems Agenda: 1. Review 2. Earth history review Why are ancient volcanic
More informationCONTENT. A. Changes in the Crust Facts Changes Construction and Destruction. B. Continental Drift What is it? Evidence
Name Earth Science Date Period TOPIC THE DYNAMIC EARTH CONTENT A. Changes in the Crust Facts Changes Construction and Destruction B. Continental Drift What is it? Evidence C. Theory of Plate Tectonics
More informationTopic 12: Dynamic Earth Pracatice
Name: Topic 12: Dynamic Earth Pracatice 1. Earth s outer core is best inferred to be A) liquid, with an average density of approximately 4 g/cm 3 B) liquid, with an average density of approximately 11
More informationSection 7. Reading the Geologic History of Your Community. What Do You See? Think About It. Investigate. Learning Outcomes
Chapter 3 Minerals, Rocks, and Structures Section 7 Reading the Geologic History of Your Community What Do You See? Learning Outcomes In this section, you will Goals Text Learning Outcomes In this section,
More informationGeologic Time. What have scientists learned about Earth s past by studying rocks and fossils?
Name Geologic Time What have scientists learned about Earth s past by studying rocks and fossils? Before You Read Before you read the chapter, think about what you know about geologic time Record your
More informationGeology 101. Reading Guide for Plate Tectonics
Geology 101 Chapter 1: Plate Tectonics (p. 21) Reading Guide for Plate Tectonics Name You should have read this section during the first week of the quarter. You should re-read this section and review
More informationToday we will discuss places mobility Natural disasters lead to California s beauty Aesthenosphere
Agenda 2. Geologic History Today we will discuss What Physical Geography is Brief geologic history of California Geography 106 California Geography M. Pesses Antelope Valley College Physical Geographers
More informationPaleogeography, Part 2: Epeiric Seas
Paleogeography, Part 2: Epeiric Seas Epeiric seas are extensive bodies of marine water overlying continental crust rather than oceanic. Because continental crust stands higher in the asthenosphere than
More informationChapter Nineteen: Changing Earth
Chapter Nineteen: Changing Earth 19.1 Inside Earth 19.2 Plate Tectonics 19.3 Plate Boundaries 19.4 Metamorphic Rocks 19.2 Learning Goals Discuss hypotheses which ultimately led to plate tectonics theory.
More informationThe 1700/01/26 Cascadia subduction zone Earthquake and Tsunami
Jason R. Patton GEO 142 1/13/15 Abstract: Cascadia subduction zone earthquakes (CSZ) can generate strong ground shaking and deadly tsunamis. Geologists used sediment cores and stream bank exposures to
More information