Session No Tuesday, 3 November 2015: 8:00 AM- 12:00 PM.
|
|
|
- Gladys Griffin
- 8 years ago
- Views:
Transcription
1 FROM NEOPROTEROZOIC PRE-CURSOR CLAMS TO THE KLAMATHS: DOCUMENTING THE PALEOGEOGRAPHIC EVOLUTION OF THE EASTERN KLAMATH TERRANES, AN EDUCATION OUTREACH MODEL ROBERTI, Gina M.1, ROTH, John2 and LEDFORD, Audrey Jane2, (1)National Park Service, Oregon Caves National Monument, Caves Highway, Cave Junction, OR 97523, (2)National Park Service, Oregon Caves National Monument, Cave Junction, OR 97523, Session No. 184 T76. Geocorps America and Mosaics in Science Programs: Successful Partnerships Promoting Individual Professional Development and Application of Geoscience and Related Fields to Management of America s Public Lands Tuesday, 3 November 2015: 8:00 AM- 12:00 PM.
2 GeoCorps Project Public Education Outreach: Geologic History of the park and surrounding region
3 Field Experience
4 Oregon Caves National Monument receives ~75,000 visitors annually.
5
6 Outreach goal: describe the geologic history in a text accessible to a public audience Why are mountains here? What s with the cave?
7 Current park materials: 250 Ma- present 640 Ma 250 Ma Present day New additions: 640 Ma- 250 Ma Research, Text and Graphics GeoCorps assignment Fall 2014-Spring 2015 Oregon Caves National Monument
8 Where is Oregon Caves located?
9 The Klamaths a microcosm for understanding the geologic history of the entire Western Cordillera.
10 Range in ages of terranes in the Klamaths Ma Ma Ma Ma Ma
11 The Klamaths contain the oldest fossils (to date) of accreted terranes in the Western Cordillera. Ediacaran Fossils of the Antelope Mountain Quartzite. Neoproterozoic (Pre-Cambrian) Cyclomedusoid fossils million years old preserved in sedimentary sandstone of the Yreka terrane in Northern California. collected by John Griffin, Identified as fossils 20 years later; published in scale: 3 inches or less
12 What tools can be used to communicate this complex geologic history? What is a terrane?
13 Problem: the earth looked (and behaved) very differently in the deep past. (It is a dangerous case of unfamiliarity Ron Blakey Colorado Plateau Geosystems Inc.
14 Oregon Caves GeoCorps Project: Creating timeline and text for geologic history pre-250 Ma Combining text with original geologic illustrations, paleogeographic maps and photographs. The supercontinent of Rodinia begins to rift apart as spreading centers rise between continental pieces, pushing them away from each other. The oldest rocks in the Klamath terranes, the Antelope Mountain Quartzite, begins to form from the sandy debris of the nearby continental pieces, which accumulates in the shallow parts of oceans on continental edges. These sedimentary rocks preserve the fossilized impressions of pre-cambrian aged cyclomedusoids. Work at Oregon Caves: Illustrations by Audrey Ledford, text by John Roth, illustration consultation and text by Gina Roberti. 600 Million Years The oldest rock unit in the Klamath terranes, the Antelope Mountain Quartzite, begins to form from the sandy debris eroding from nearby continental pieces between 640 and 575 million years ago (Griffin 2008). This material accumulates on the shallow parts of oceans around continental edges. The Yreka terrane includes a range of shallow to deep marine sandstones and mudstones that accumulated from 600 to 400 million years ago. Cementing sedimentary debris into a sandstone preserved the fossil imprints of the cyclomedusoids, grouped taxonomically with the White Sea Assemblage. Some of these flattish lifeforms may be sponge, jellyfish or left/right symmetrical (like us) ancestors. Some became extinct once bacteria exhaled enough oxygen to seep deep into and keep alive bigger newcomers that replaced some of the older life (MacGabhann et al. Quartz-rich sands and muds washed off from the former pieces of the supercontinent form the oldest rocks in the Klamaths between 640 and 575 million years ago (Griffin 2008). The Antelope Mountain Quartzite is so named because of pressure and heating during burial metamorphose the silica-rich sandstone into quartzite. Fossils were first discovered by John Griffin in the 1970s though not described as Proterozoic fauna and published until 2006.
15 Independent Graphic Design: Gina Roberti
16 To ERR on the side of effective science communication: 1. Engagin g 2. Exciting 3. Relevant
17 START: a complex 4D problem.
18 Simplifying. Overlays.
19 Using analogies.
20 Using jargon as a teaching tool.
21 Simplifying concepts with a combination of visuals and text.
22 With many thanks to the support of John Roth, Audrey Ledford, GeoCorps America, and the staff and resources of Oregon Caves National Monument.
23 FROM NEOPROTEROZOIC PRE-CURSOR CLAMS TO THE KLAMATHS: DOCUMENTING THE PALEOGEOGRAPHIC EVOLUTION OF THE EASTERN KLAMATH TERRANES, AN EDUCATION OUTREACH MODEL Primary Literature: Blakey, Ron Paleogeographic reconstructions. Web source: Blodgett and Stanley "The Terrane Puzzle: New Perspectives on Paleontology and Stratigraphy from the North American Cordillera". GSA Special Paper 442. Canfield, Poulton, Narbonne "Late-Neoproterozoic Deep-Ocean Oxygenation and the Rise of Animal Life". Science. Vol Cocks, Torsvik "The Paleozoic geography of Laurentia and western Laurussia: A stable craton with mobile margins". Earth Science Reviews. Colpron and Nelson, "A Paleozoic Northwest Passage: incursion of Caledonian, Baltican and Siberian terranes into eastern Panthalassa, and the early evolution of the North American Cordillera". GSA Special publications v. 318 p Dickinson "Anatomy and Global Context of the North American Cordillera". Geologic Society of America Memoirs: 204; Griffin ea "Ediacaran cyclomedusoids and the paleogeographic setting of the Neoproterozoic-early Paleozoic Yreka and Trinity terranes, eastern Klamath Mountains" from Geologic Studies of the Klamath Mountains pg. 411.; Griffin ea "Ediacaran Cyclomedusoids" in The Terrane Puzzle. Griffin, John and Nancy Lindsley-Griffin, personal correspondence January Sigloch "Intra-oceanic subduction shaped the assembly of Cordilleran North America." Nature vo April Snoke, Barnes "The Development of tectonic concepts for the Klamath Mountains province, California and Oregon". In Geologic Studies in the Klamath Mountain Province, GSA Special Paper 410. Stewart, John "Reconstructing Rodinia by Fitting Neoproterozoic Continental Margins". USGS Open File report publication, Secondary Sources: Frisch, Meschede, Blakey Plate Tectonics: Continental Drift and Mountain Building. Springer textbook. Miller, Marli B. Roadside Geology of Oregon: Second Edition Mountain Press Publishing Company. Individual citations for photographs and images used in this presentation listed on slides.
ES Chapter 10 Review. Name: Class: Date: Multiple Choice Identify the choice that best completes the statement or answers the question.
Name: Class: Date: ES Chapter 10 Review Multiple Choice Identify the choice that best completes the statement or answers the question. 1. Scientists used the pattern of alternating normal and reversed
TECTONICS ASSESSMENT
Tectonics Assessment / 1 TECTONICS ASSESSMENT 1. Movement along plate boundaries produces A. tides. B. fronts. C. hurricanes. D. earthquakes. 2. Which of the following is TRUE about the movement of continents?
GEL 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
Chapter 8: Plate Tectonics -- Multi-format Test
Name: Class: Date: ID: A Chapter 8: Plate Tectonics -- Multi-format Test Modified True/False Indicate whether the statement is true or false. If false, change the identified word or phrase to make the
Carbonate Rock Formation
Limestone, dolomite (or dolostone), and marble are often collectively referred to as carbonate rocks because the main mineral is calcite. The chemical name of calcite is calcium carbonate. Limestone, dolomite,
History of the Earth/Geologic Time 5E Unit
History of the Earth/Geologic Time 5E Unit Description: Students will create a timeline of Earth history in the classroom and learn about major changes to the Earth and life through time. Standards Targeted:
How Did These Ocean Features and Continental Margins Form?
298 10.14 INVESTIGATION How Did These Ocean Features and Continental Margins Form? The terrain below contains various features on the seafloor, as well as parts of three continents. Some general observations
Alfred Wegener s Theory of Continental Drift Became Modern Plate Tectonics. Wegener in Greenland about 1912. He froze to death there in 1930.
Alfred Wegener s Theory of Continental Drift Became Modern Plate Tectonics Wegener in Greenland about 1912. He froze to death there in 1930. Science is self correcting. The Scientific Method The history
Tectonic plates push together at convergent boundaries.
KEY CONCEPT Plates converge or scrape past each other. BEFORE, you learned Plates move apart at divergent boundaries In the oceans, divergent boundaries mark where the sea floor spreads apart On land,
Rocks and Plate Tectonics
Name: Class: _ Date: _ Rocks and Plate Tectonics Multiple Choice Identify the choice that best completes the statement or answers the question. 1. What is a naturally occurring, solid mass of mineral or
Continents join together and split apart.
KEY CONCEPT Continents change position over time. BEFORE, you learned Earth s main layers are the core, the mantle, and the crust The lithosphere and asthenosphere are the topmost layers of Earth The lithosphere
11A Plate Tectonics. What is plate tectonics? Setting up. Materials
11A Plate Tectonics What is plate tectonics? Earth s crust plus the upper mantle forms the lithosphere. Earth s lithosphere is broken in a number of different pieces. How these pieces move and interact
Chapter 9: Earth s Past
Chapter 9: Earth s Past Vocabulary 1. Geologic column 2. Era 3. Period 4. Epoch 5. Evolution 6. Precambrian time 7. Paleozoic era 8. Shield 9. Stromatolite 10. Invertebrate 11. Trilobite 12. Index fossil
Interactive Plate Tectonics
Interactive Plate Tectonics Directions: Go to the following website and complete the questions below. http://www.learner.org/interactives/dynamicearth/index.html How do scientists learn about the interior
4. Plate Tectonics II (p. 46-67)
4. Plate Tectonics II (p. 46-67) Seafloor Spreading In the early 1960s, samples of basaltic ocean crust were dredged up from various locations across the ocean basins. The samples were then analyzed to
Unit 2 Lesson 4 The Geologic Time Scale. Copyright Houghton Mifflin Harcourt Publishing Company
Once Upon a Time How have geologists described the rate of geologic change? Geology is the scientific study of the origin, history, and structure of Earth and the processes that shape it. Early geologists
GLY2100C Historical Geology Course Information Spring 2015. Dr. Rachel Walters
GLY2100C Historical Geology Course Information Spring 2015 Dr. Rachel Walters Credits: 4 Pre-requisites: Physical Geology GLY2010C, Environmental and Engineering Geology GLY 2030C or instructor permission.
Geologic Time Scale Notes
Name: Date: Period: 1 2 3 4 5 6 7 Notes Essential Question: What is the geologic time scale? Vocabulary: Geology: the scientific study of the origin, history, and structure of Earth and the processes that
Unit 4 Lesson 2 Plate Tectonics. Copyright Houghton Mifflin Harcourt Publishing Company
Puzzling Evidence What evidence suggests that continents move? In the late 1800s, Alfred Wegener proposed his hypothesis of continental drift. According to this hypothesis, the continents once formed a
Name Score /225. (Make sure you identify each key concept by identifying the section [1.1, 1.2, etc.].]
![Name Score /225. (Make sure you identify each key concept by identifying the section [1.1, 1.2, etc.].]](/thumbs/40/21046969.jpg "Name Score /225. (Make sure you identify each key concept by identifying the section [1.1, 1.2, etc.].]")
Name Score /225 Changing Earth Chapter 1 Worksheet Before reading Chapter 1 (pages 9 37). On a separate sheet of paper, make two columns. Title the first column Before I Read. Title the second column After
The Dynamic Crust 2) EVIDENCE FOR CRUSTAL MOVEMENT
The Dynamic Crust 1) Virtually everything you need to know about the interior of the earth can be found on page 10 of your reference tables. Take the time to become familiar with page 10 and everything
6.E.2.2 Plate Tectonics, Earthquakes and Volcanoes
Name: Date: 1. The road shown below was suddenly broken by a natural event. 3. The convergence of two continental plates would produce Which natural event most likely caused the crack in the road? island
www.amnh.org Continental Drift is the movement of the Earth s continents in relation to one another.
A Plate Tectonic Puzzle Introduction The Earth s crust is not a solid shell. It is made up of thick, interconnecting pieces called tectonic plates that fit together like a puzzle. They move atop the underlying
Geologic History Review
1. The climate that existed in an area during the early Paleozoic Era can best be determined by studying (1) the present climate of the area (2) recorded climate data of the area since 1700 (3) present
SECOND GRADE PLATE TECTONICS 1 WEEK LESSON PLANS AND ACTIVITIES
SECOND GRADE PLATE TECTONICS 1 WEEK LESSON PLANS AND ACTIVITIES PLATE TECTONIC CYCLE OVERVIEW OF SECOND GRADE VOLCANOES WEEK 1. PRE: Investigating the parts of a volcano. LAB: Comparing the parts of a
Plate Tectonics Web-Quest
Plate Tectonics Web-Quest Part I: Earth s Structure. Use the following link to find these answers: http://www.learner.org/interactives/dynamicearth/structure.html 1. Label the layers of Earth in the diagram
Evolution (18%) 11 Items Sample Test Prep Questions
Evolution (18%) 11 Items Sample Test Prep Questions Grade 7 (Evolution) 3.a Students know both genetic variation and environmental factors are causes of evolution and diversity of organisms. (pg. 109 Science
Teaching the Dynamic Earth Plate Tectonics Interactive Master sheets
Teaching the Dynamic Earth Plate Tectonics Interactive Master sheets Contents Page Master Sheets for continental jigsaws Gondwanaland continents (blank outlines)...2 Four continents, showing gaps and overlap
Unit 5: Formation of the Earth
Unit 5: Formation of the Earth Objectives: E5.3B - Explain the process of radioactive decay and explain how radioactive elements are used to date the rocks that contain them. E5.3C - Relate major events
Georgia Performance Standards Framework for Science Grade 6. Unit Organizer: Geology: Inside the Earth (Approximate Time: 7 Weeks)
The following instructional plan is part of a GaDOE collection of Unit Frameworks, Performance Tasks, examples of Student Work, and Teacher Commentary. Many more GaDOE approved instructional plans are
Name Class Date WHAT I KNOW. about how organisms have changed. grown in complexity over time.
History of Life Evolution Q: How do fossils help biologists understand the history of life on Earth? 19.1 How do scientists use fossils to study Earth s history? WHAT I KNOW SAMPLE ANSWER: Fossils give
Continental Drift, Sea Floor Spreading and Plate Tectonics
Page 1 of 13 EENS 1110 Tulane University Physical Geology Prof. Stephen A. Nelson Continental Drift, Sea Floor Spreading and Plate Tectonics This page last updated on 26-Aug-2015 Plate Tectonics is a theory
Plate Tectonics: Big Ideas. Plate Tectonics. Plate Tectonics. The unifying concept of the Earth sciences.
Plate Tectonics: Big Ideas Our understanding of Earth is continuously refined. Earth s systems are dynamic; they continually react to changing influences from geological, hydrological, physical, chemical,
Hot Spots & Plate Tectonics
Hot Spots & Plate Tectonics Activity I: Hawaiian Islands Procedures: Use the map and the following information to determine the rate of motion of the Pacific Plate over the Hawaiian hot spot. The volcano
Geologic Time Scale Newcomer Academy Visualization Three
Geologic Time Newcomer Academy Visualization Three Chapter Subtopic/Media Key Points of Discussion Notes/Vocabulary Introduction Title NA NA Various Pictures of Geologic Time It s About Time Personal Timeline
Plate Tectonics. Plate Tectonics The unifying concept of the Earth sciences. Continental Drift
Plate Tectonics The unifying concept of the Earth sciences. The outer portion of the Earth is made up of about 20 distinct plates (~ 100 km thick), which move relative to each other This motion is what
Plate Tectonics Short Study Guide
Name: Class: Date: Plate Tectonics Short Study Guide Multiple Choice Identify the letter of the choice that best completes the statement or answers the question. 1. The existence of coal beds in Antarctica
Chapter 2. Plate Tectonics. Plate Tectonics: Learning Goals
Plate Tectonics Chapter 2 Interactions at depend on the direction of relative plate motion and the type of crust. Which kind of plate boundary is associated with Earthquake activity? A. Divergent Boundary
Ride the Rock Cycle. Suggested Goals: Students will gain an understanding of how a rock can move through the different stages of the rock cycle.
Illinois State Museum Geology Online http://geologyonline.museum.state.il.us Ride the Rock Cycle Grade Level: 5 6 Purpose: To teach students that the rock cycle, like the water cycle, has various stages
Tectonic plates have different boundaries.
KEY CONCEPT Plates move apart. BEFORE, you learned The continents join and break apart The sea floor provides evidence that tectonic plates move The theory of plate tectonics helps explain how the plates
Plate Tectonics Practice Questions and Answers Revised August 2007
Plate Tectonics Practice Questions and Answers Revised August 2007 1. Please fill in the missing labels. 2. Please fill in the missing labels. 3. How many large plates form the outer shell of the earth?
FROM SEDIMENT INTO SEDIMENTARY ROCK. Objectives. Sediments and Sedimentation
FROM SEDIMENT INTO SEDIMENTARY ROCK Objectives Identify three types of sediments. Explain where and how chemical and biogenic sediments form. Explain three processes that lead to the lithification of sediments.
Earth Science Module 21. Plate Tectonics: The Earth in Motion. Plate Tectonics Module Study Notes and Outline. Creationist Model
Earth Science Module 21 Plate Tectonics: The Earth in Motion Plate Tectonics Module Study Notes and Outline Creationist Model I. Scientists shift their paradigm A. When the data supporting plate tectonics
Lesson Plan Title. Toilet Paper Tape Measure of Geologic Time
Lesson Plan Title Toilet Paper Tape Measure of Geologic Time Name (last, first): Serratos, Danielle J. Scientific Theme(s): Life Science *Changes in Life Forms over Time Earth Science *Forces that Shape
Step 2: Learn where the nearest divergent boundaries are located.
What happens when plates diverge? Plates spread apart, or diverge, from each other at divergent boundaries. At these boundaries new ocean crust is added to the Earth s surface and ocean basins are created.
All sediments have a source or provenance, a place or number of places of origin where they were produced.
Sedimentary Rocks, Processes, and Environments Sediments are loose grains and chemical residues of earth materials, which include things such as rock fragments, mineral grains, part of plants or animals,
The Fossil Record and Geologic Time Scale
Two Conceptions of Earth History: Catastrophism Assumption: Great Effects Require Great Causes Earth History Dominated by Violent Events Uniformitarianism Assumption: We Can Use Cause And Effect to Determine
California Standards Grades 9 12 Boardworks 2009 Science Contents Standards Mapping
California Standards Grades 912 Boardworks 2009 Science Contents Standards Mapping Earth Sciences Earth s Place in the Universe 1. Astronomy and planetary exploration reveal the solar system s structure,
Plate tectonics states that the Earth's crust and upper mantle are broken into sections, called plates.
Notes on Plate Tectonics Plate tectonics states that the Earth's crust and upper mantle are broken into sections, called plates. These plates move around the mantle. Plates are composed of the crust and
FOURTH GRADE PLATE TECTONICS 1 WEEK LESSON PLANS AND ACTIVITIES
FOURTH GRADE PLATE TECTONICS 1 WEEK LESSON PLANS AND ACTIVITIES PLATE TECTONIC CYCLE OVERVIEW OF FOURTH GRADE VOLCANOES WEEK 1. PRE: Comparing different structures of volcanoes. LAB: Modeling three types
Fourth Grade Geology: The Earth and Its Changes Assessment
Fourth Grade Geology: The Earth and Its Changes Assessment 1a. What is the center layer of the Earth called? a. crust b. core c. mantle d. middle 1b. Label each layer of the Earth. 1c. What are the Earth
Continental Drift. Alfred Wegener (1880-1930) Proposed that all of the continents were once part of a large supercontinent - Pangaea Based on:
Plate Tectonics and Continental Drift Continental Drift Alfred Wegener (1880-1930) Proposed that all of the continents were once part of a large supercontinent - Pangaea Based on: Similarities in shorelines
Plate Tectonics Lab Assignment
Plate Tectonics Lab Assignment After reading the introduction to the Plate Tectonics exercises in the lab manual, complete the questions on a hard copy of this Lab Assignment. When finished, transfer your
Name: Period: # Plate Tectonics. Journey to the center of the Earth
Plate Tectonics Journey to the center of the Earth Use pages 124 129 to answer the following questions. Exploring Inside Earth (p. 125-126) 1. What are the two main types of evidence that Geologist use
OCEANOGRAPHY Vol.II Morphology of Ocean Floor and Plate Tectonics - Chengsung Wang MORPHOLOGY OF OCEAN FLOOR AND PLATE TECTONICS
MORPHOLOGY OF OCEAN FLOOR AND PLATE TECTONICS Chengsung Wang National Taiwan Ocean University, Keelung 202, Taiwan, China Keywords: Morphology of sea floor, continental margins, mid-ocean ridges, deep-sea
Introductory Geosciences I: Historical Geology GEOL 1122, Sec. 01, Spring 2009 M, W 12:30 1:45 Calloway 205 Instructor E mail Office Office hours
Introductory Geosciences I: Historical Geology GEOL 1122, Sec. 01, Spring 2009 M, W 12:30 1:45 Calloway 205 Instructor: Dr. Phil Novack Gottshall E mail: pnovackg@westga.edu Office: Calloway G1 Office
Geological Timeline Challenge
Geological Timeline Challenge Suggested Grade Levels: 8-12 Description: Students will create a timeline of Earth history in the classroom and learn about major changes to the Earth and life through time.
Foundations of Earth Science (Lutgens and Tarbuck, 5 th edition, 2008)
EAS 100 Study Guide to Textbook Foundations of Earth Science (Lutgens and Tarbuck, 5 th edition, 2008) STUDY GUIDE 1/08 The textbook for EAS 100, Foundations of Earth Science, by Lutgens and Tarbuck is
The Geology of the Marginal Way, Ogunquit, Maine
Geologic Site of the Month February, 2002 The Geology of the Marginal Way, Ogunquit, Maine 43 14 23.88 N, 70 35 18.36 W Text by Arthur M. Hussey II, Bowdoin College and Robert G. Marvinney,, Department
Earthquakes and Plate Boundaries Deborah Jordan and Samuel Spiegel
Earthquakes and Plate Boundaries Deborah Jordan and Samuel Spiegel Jordan, Deborah and Spiegel, Samuel: Learning Research Development Center, University of Pittsburgh. Earthquakes and Plate Boundaries.
Geol 101: Physical Geology PAST EXAM QUESTIONS LECTURE 4: PLATE TECTONICS II
Geol 101: Physical Geology PAST EXAM QUESTIONS LECTURE 4: PLATE TECTONICS II 4. Which of the following statements about paleomagnetism at spreading ridges is FALSE? A. there is a clear pattern of paleomagnetic
Geologic Time. Relative Dating. Principle of Original Horizontality. Relative Time. Absolute Time. Geologic Column
Geologic Time Relative Time 5 Principles of Relative Dating Absolute Time Radiometric Dating Geologic Column Relative Dating principle of horizontality principle of superposition principle of cross-cutting
Regents Questions: Plate Tectonics
Earth Science Regents Questions: Plate Tectonics Name: Date: Period: August 2013 Due Date: 17 Compared to the oceanic crust, the continental crust is (1) less dense and more basaltic (3) more dense and
Plate Tectonics Lab. Continental Drift. The Birth of Plate Tectonics
Plate Tectonics Lab Continental Drift Take a look at a globe sometime and observe the remarkable fit between South America and Africa. Could they have, in fact, been connected? During the 19th and early
Engaging Students Through Interactive Activities In General Education Classes
Engaging Students Through Interactive Activities In General Education Classes On the Cutting Edge: Early Career Geoscience Faculty Workshop 14-18 June 2009 Presented by Randy Richardson Department of Geosciences,
Transform Boundaries
Lecture 7 Plates and Mantle Plumes Transform Boundaries Transform boundaries occur where one segment of rigid lithosphere slides horizontally past another in response to stresses in the lithosphere. The
II. Earth Science (Geology) Section (9/18/2013)
EAPS 100 Planet Earth Lecture Topics Brief Outlines II. Earth Science (Geology) Section (9/18/2013) 1. Interior of the Earth Learning objectives: Understand the structure of the Earth s interior crust,
SIXTH GRADE PLATE TECTONICS 1 WEEK LESSON PLANS AND ACTIVITIES
SIXTH GRADE PLATE TECTONICS 1 WEEK LESSON PLANS AND ACTIVITIES PLATE TECTONIC CYCLE OVERVIEW OF SIXTH GRADE VOLCANOES WEEK 1. PRE: Comparing the structure of different types of volcanoes. LAB: Plotting
MINES AND ENERGY MINISTRY OF COLOMBIA. Geological Survey of Colombia National Mineral Agency of Colombia
MINES AND ENERGY MINISTRY OF COLOMBIA Geological Survey of Colombia National Mineral Agency of Colombia STRATEGIC MINING AREAS AN OPPORTUNITY TO INVEST IN COLOMBIA Toronto, March 2013 AGENDA 1. GEOLOGICAL
A Collection of Curricula for the STARLAB Plate Tectonics Cylinder
A Collection of Curricula for the STARLAB Plate Tectonics Cylinder Including: The Changing Earth by Gerald L. Mallon, Ed.D. v. 616-2008 by Science First /STARLAB, 86475 Gene Lasserre Blvd., Yulee, FL.
Students explore the mechanism behind plate motion as they investigate convection currents. KEY CONCEPTS AND PROCESS SKILLS
Convection Currents 40- to 1 50-minute session ACTIVITY OVERVIEW 46 L A B O R AT O R Y Students explore the mechanism behind plate motion as they investigate convection currents. KEY CONCEPTS AND PROCESS
Global Geoparks in Norway
Global Geoparks in Norway Global Geoparks are listed in order of acceptance into the Global Geoparks Network Gea Norvegica. 2 Magma.. 4 Disclaimer The Secretariat of UNESCO does not represent or endorse
Chapter Overview. Bathymetry. Measuring Bathymetry. Echo Sounding Record. Measuring Bathymetry. CHAPTER 3 Marine Provinces
Chapter Overview CHAPTER 3 Marine Provinces The study of bathymetry charts ocean depths and ocean floor topography. Echo sounding and satellites are efficient bathymetric tools. Most ocean floor features
Plate Tectonics Chapter 2
Plate Tectonics Chapter 2 Does not include complete lecture notes. Continental drift: An idea before its time Alfred Wegener First proposed his continental drift hypothesis in 1915 Published The Origin
GEOL 104 Dinosaurs: A Natural History Geology Assignment. DUE: Mon. Sept. 18
GEOL 104 Dinosaurs: A Natural History Geology Assignment DUE: Mon. Sept. 18 Part I: Environments of Deposition Geologists can use various clues in sedimentary rocks to interpret their environment of deposition:
Chesapeake Bay Governor School for Marine and Environmental Science
Choose the best answer and write on the answer sheet provided. 1. Which of the following is LEAST likely to be an effect of global warming? (a) Loss of fertile delta regions for agriculture (b) Change
1. Foliation or schistose textures are easily seen in rocks consisting of. 2. Which of these tectonic settings will be hottest at 20km depth?
2nd Midterm Questions Metamorphic Rocks 1. Foliation or schistose textures are easily seen in rocks consisting of. a. framework silicates (quartz, feldspar) b. platy minerals (micas) c. chain-silicates
WEATHERING, EROSION, AND DEPOSITION PRACTICE TEST. Which graph best shows the relative stream velocities across the stream from A to B?
NAME DATE WEATHERING, EROSION, AND DEPOSITION PRACTICE TEST 1. The diagram below shows a meandering stream. Measurements of stream velocity were taken along straight line AB. Which graph best shows the
Rocks & Minerals. 10. Which rock type is most likely to be monomineralic? 1) rock salt 3) basalt 2) rhyolite 4) conglomerate
1. Of the Earth's more than 2,000 identified minerals, only a small number are commonly found in rocks. This fact indicates that most 1) minerals weather before they can be identified 2) minerals have
Foundations of Earth Science (Lutgens and Tarbuck, 6 th edition, 2011)
EAS 100 Study Guide to Textbook Foundations of Earth Science (Lutgens and Tarbuck, 6 th edition, 2011) STUDY GUIDE 8/2010 The textbook for EAS 100, Foundations of Earth Science, by Lutgens and Tarbuck
The Ice Age By: Sue Peterson
www.k5learning.com Objective sight words (pulses, intermittent, isotopes, chronicle, methane, tectonic plates, volcanism, configurations, land-locked, erratic); concepts (geological evidence and specific
Sedimentary Rocks Practice Questions and Answers Revised September 2007
Sedimentary Rocks Practice Questions and Answers Revised September 2007 1. Clastic sedimentary rocks are composed of and derived from pre-existing material. 2. What is physical weathering? 3. What is chemical
FIRST GRADE PLATE TECTONICS 1 WEEK LESSON PLANS AND ACTIVITIES
FIRST GRADE PLATE TECTONICS 1 WEEK LESSON PLANS AND ACTIVITIES PLATE TECTONIC CYCLE OVERVIEW OF FIRST GRADE VOLCANOES WEEK 1. PRE: Learning the shapes of volcanoes. LAB: Experimenting with "lava." POST:
principles of stratigraphy: deposition, succession, continuity and correlation
Relative Age Dating Comparative Records of Time Nature of the rock record principles of stratigraphy: deposition, succession, continuity and correlation Stratigraphic tools biological succession of life:
Exploring Our World with GIS Lesson Plans Engage
Exploring Our World with GIS Lesson Plans Engage Title: Exploring Our Nation 20 minutes *Have students complete group work prior to going to the computer lab. 2.List of themes 3. Computer lab 4. Student
EARTH SYSTEM: HISTORY AND NATURAL VARIABILITY - Vol. IV - Epeiric Seas: A Continental Extension of Shelf Biotas - Harries P.J.
EPEIRIC SEAS: A CONTINENTAL EXTENSION OF SHELF BIOTAS Harries P.J. University of South Florida, Tampa, Florida USA Keywords: Epeiric seas, climate change, sea-level rise, biodiversity, endemism, sediments,
PLATE TECTONICS EXERCISE (Modified from North Seattle Community College online exercise)
PLATE TECTONICS EXERCISE (Modified from North Seattle Community College online exercise) Introduction: As discussed in our textbook, the speed at which tectonic plates move has been calculated in several
Investigation 6: What happens when plates collide?
Tectonics Investigation 6: Teacher Guide Investigation 6: What happens when plates collide? In this activity, students will use the distribution of earthquakes and volcanoes in a Web GIS to learn about
Plate Tectonics. Introduction. Boundaries between crustal plates
Plate Tectonics KEY WORDS: continental drift, seafloor spreading, plate tectonics, mid ocean ridge (MOR) system, spreading center, rise, divergent plate boundary, subduction zone, convergent plate boundary,
Plate Tectonics. Hi, I am Zed and I am going to take you on a trip learning about Plate Tectonics. And I am Buddy Zed s mascot
Plate Tectonics Hi, I am Zed and I am going to take you on a trip learning about Plate Tectonics And I am Buddy Zed s mascot Continental Drift Alfred Wegener proposed that continents were not always where
COASTAL DAMAGE INSPECTION SOUTHWEST VITI LEVU, FIJI AFTER CYCLONE SINA
COASTAL DAMAGE INSPECTION SOUTHWEST VITI LEVU, FIJI AFTER CYCLONE SINA Brendan J. Holden SOPAC Technical Secretariat July 1992 SOPAC Technical Report 148 Prepared for: South Pacific Applied Geoscience
Geologic time and dating. Geologic time refers to the ages relevant to Earth s history
Geologic time and dating Most figures and tables contained here are from course text: Understanding Earth Fourth Edition by Frank Press, Raymond Siever, John Grotzinger, and Thomas H. Jordan Geologic time
February 28 Earthquake: We got off easy
February 28 Earthquake: We got off easy State Geologist John Beaulieu Lucky may not be the first word that comes to mind after an earthquake that injured more than 200 and caused more than $1 billion damage,
NATURAL REGIONS OF KENTUCKY
NATURAL WONDERS As you travel around Kentucky taking pictures, you are excited by what you see. Kentucky offers diverse and amazing sights. The Six Regions In the West, you see the Mississippi River, the
Igneous rocks formed when hot molten material (magma) cools and hardens (crystallizes).
Objectives You will learn about how the land of North Dakota was formed. Introduction North Dakota is a wonderful place to live. Have you ever though about how it was formed? To answer that question, you
Ocean Floor Continental Slope Begins at the Continental Shelf Very sharp drop to depths over 2 miles Covered with thick layers of sand, mud, and rocks
Ocean Floor Continental Shelf Begins at the shoreline Gently slopes underwater Average depth of 430 feet Thick layers of sand, mud, and rocks The beach is part of the Continental Shelf Ocean Floor Continental
PLATE TECTONICS. Teacher Guide including Lesson Plans, Student Readers, and More Information
PLATE TECTONICS Teacher Guide including Lesson Plans, Student Readers, and More Information Lesson 1 - Evidence of Plate Tectonics Lesson 2 - Plotting Earthquakes and Volcanoes Lesson 3 - Case History
1. You are about to begin a unit on geology. Can anyone tell me what geology is? The study of the physical earth I.
PLATE TECTONICS ACTIVITY The purpose of this lab is to introduce the concept of plate tectonics and the formation of mountains. Students will discuss the properties of the earth s crust and plate tectonics.
Section 1 Earth s surface undergoes gradual and sudden changes
Section 1 Earth s surface undergoes gradual and sudden changes Student Class 1. Scientists estimate the age of the Earth to be about 4.6 billion years old, using evidence and theories. Then they construct
What are the controls for calcium carbonate distribution in marine sediments?
Lecture 14 Marine Sediments (1) The CCD is: (a) the depth at which no carbonate secreting organisms can live (b) the depth at which seawater is supersaturated with respect to calcite (c) the depth at which