Introduction to Manitoba Geology
|
|
- Allison Constance Jennings
- 6 years ago
- Views:
Transcription
1 Introduction to Manitoba Geology A journey through geological time Presentation to: Mining Matters 2010 By: Jim Bamburak Industrial Minerals Geologist Prepared by: Ric Syme Director Manitoba Geological Survey
2 Introduction to Manitoba Geology A journey through geological time
3 50 staff; 26 geologists Manitoba Geological Survey Visit us on the Internet (
4 50 staff; 26 geologists Mapping in northern Manitoba Manitoba Geological Survey 1. Regional and detailed geological investigations to support mineral and dhydrocarbon exploration in the province 2. Geoscience information for decision-making (e.g., land use planning, protected areas) 3. Outreach and education Mapping in southern Manitoba Working with First Nations
5 Geology of North America US Geological Survey PRECAMBRIAN
6 The third dimension Phanerozoic Usually, when we go down through the Earth's rock layers we are going back in time. Precambrian
7 Manitoba geology Churchill #S Precambrian Shield Sedimentary basins B #S Lynn Lake #S #S Leaf f Rapids p #S B Thompson Sherridon #S Snow Lake #S #S Wabowden Flin Flon Precambrian Shield Crystalline rocks >1.5 billion years old host of Manitoba s metallic mineral deposits Sedimentary basins Winnipeg #S Bissett #S#S Phanerozoic Sedimentary basins <500 million years old host of Manitoba s petroleum resources, aggregate and industrial minerals
8 Mineral production in Manitoba B #S Precambrian Shield Lynn Lake #S #S Leaf f Rapids p #S B Thompson Sherridon #S Snow Lake #S #S Wabowden Flin Flon Churchill #S Sedimentary basins Mine closed Nickel/Cobalt (Vale, Crowflight) Thompson Mine Birchtree Mine Bucko Mine 24% of fcanadian Ni production 16% of Canadian Co production Copper/Zinc (HudBay Minerals Inc.) Callinan and 777 mines Trout Lake Mine 10% of Canadian Cu production 11% of Canadian Zn production Sedimentary basins Winnipeg #S Bissett #S#S Tantalum/Cesium (Tantalum Mining Corp. of Canada Ltd.) Tanco Mine Gold (San Gold Corporation) Rice Lake Gold Mine
9 Lynn Lake Leaf Rapids Thom pson Manitoba through geological g time Flin Flon Snow L ake Lak e Win nipegos is Lake Winnipe g Formation of the Earth Present day Assiniboine River Lake Manitoba Red Riv er Bissett Winnipeg PRECAMBRIAN Hadean Archean Proterozoic Phanerozoic All of human history 4,600,000,000 years of earth history 4 periods or Eons Manitoba geology records significant portions of this extensive history Each Eon has a distinct mineral endowment Ma = million years (ago) y ( g ) 1000 million years = 1 billion years (e.g., 1500 Ma = 1.5 billion)
10 Zircons are tiny mineral crystals that occur in many rocks. Zircon contains trace amounts of uranium and thorium and can be dated by a variety of analytical techniques. Precambrian Time Hadean Eon: Formation of Earth Ma Assean Lake 3.9 billion year old zircons Greywacke The Earth formed as a solid planet Earth s interior organized into layers Early crust formed but was largely recycled or destroyed by rapid convection and numerous meteorite impacts
11 Archean Eon: Formation of Crust Ma Precambrian Time Earth's permanent e crust was formed First large continents formed Earliest life forms began The oceans and atmosphere resulted from volcanic out-gassing
12 Archean Eon in Manitoba Very early crust formed (3500 Ma). Locally contains indications of very old rocks (3900 Ma) Precambrian Time Seal River Remnants of early crust Granite gneiss 3.5 billion years old
13 Archean pillow lava, Cross Lake Modern pillow lava on the sea floor Archean Eon in Manitoba Formation of pillow lava Widespread volcanism ( Ma) Greenstone belts volcanic rocks Volcanic breccia, Knee Lake Volcanic eruption under the sea NOAA, courtesy of Richard Pyle at Lava Video Productions
14 Bissett Archean Eon in Manitoba Laurentian orogeny (mountain building) ( Ma) Granite plutonism and assembly of a large Archean Au continent (Superior craton ) Gold and quartz vein in metamorphic rock Many large gold deposits San Antonio Mine, Bissett On loan from the Royal Ontario Museum, Toronto, Canada, M38683 formed (e.g., Rice Lake AMNH / Craig Chesek mine in Bissett)
15 Ediacaran Fauna ( Ma) Proterozoic Eon: Modern Earth Processes Begin Ma National Museum of Natural History NOAA Mid-ocean rifting Subduction and island arc volcanoes Modern plate tectonics started Large mountain chains formed as the Archean continents collided Photosynthesis lead to iology/continental%20drift/tectonics.html oxygenated atmosphere around 2200 Ma Soft-bodied life forms proliferated (no skeletons)
16 Rifting Thompson Proterozoic Eon in Manitoba Ma opening of a large ocean basin subsequent (1885 Ma) with basin-margin shoreline sediments laid down emplacement on Archean of basement nickel deposits rocks Ni Ni Proterozoic >500 million-year time gap quartzite Rifting Archean gneiss /Continental%20Drift/Tectonics.html
17 Flin Flon Proterozoic Eon in Manitoba hers/rhamley/biology/continental %20Drift/Tectonics.html Lynn Lake Cu-Zn Thompson Nickel Belt Cu-Zn Trans-Hudson Orogen Leaf Rapids dary Z Hudson Bay Basin Ma active volcanism and deposition of copper-zinc deposits (e.g., Flin Flon, Lynn Lake) Snow Lake Flin Flon Ass siniboine Lak e Winnipegos is Superior Boundary Zone Lake Winnip pe g Western Canada Sedimentary Basin River Lake Manitoba Superior Province Red Riv er subduction The greenstone belts in the Trans-Hudson animation copyrighted by McGraw Orogen Hill as of Manitoba and Saskatchewan have part of PLUMMER MCGEARY produced AND more than $60 billion in metals (at CARLSON 11th edition 2010 prices) -making them some of the most productive greenstone belts in Canada.
18 Proterozoic Eon: copper-zinc-gold deposits hers/rhamley/biology/continental %20Drift/Tectonics.html Polished slab of basalt flow top breccia, Flin Flon Submarine eruption NOAA Underwater eruptions produce distinctive volcanic deposits that can be recognized in ancient greenstone belts
19 Proterozoic Eon: copper-zinc-gold deposits hers/rhamley/biology/continental %20Drift/Tectonics.html Dr. Robert Ballard Massive sulphide mound
20 Proterozoic Eon: copper-zinc-gold deposits Zinc ore, Snow Lake Copper ore, Flin Flon Massive sulphide mound
21 Proterozoic Eon in Manitoba Ma closing of ocean basin and formation of the Trans-Hudson Orogen (mountain belt)
22 Comparison of the Trans-Hudson Orogen with a modern orogen (mountain belt) Manitoba Trans-Hudson Orogen ( Ma) Superior Craton Alpine-Himalayan Orogen (< 50 Ma)
23 Phanerozoic Eon Lynn Lake Leaf Rapids Thom pson akepaleozoic Era Snow L Flin Flon Lake Winnipe g Mesozoic Era Era Cenozoic Phanerozoic Eon: Modern Earth and Life Forms Evolve Assiniboine Lak e Win nipegos is 542 Bissett Million of years ago Lake Manitoba River Red Riv er Winnipeg Precambrian Time Life forms with skeletons proliferate 8 major life extinction events Continents separated and then collided d again to form more mountain chains North America and Manitoba as we know it were formed.
24 The Phanerozoic Mesozoic Paleozoic Precambrian Phanerozoic Eon Paleozoic Paleozoic Era Mesozoic Era Cenoz zoic Era Million of years ago
25 Crushed rock Tyndall Stone Paleozoic Era in Manitoba Ma Gillis quarry, Garson Preceded by a long period during which the Precambrian was eroded flat Manitoba was located near to the equator Shallow inland seas flooded North America V l bl d it f hi h l i Valuable deposits of high-calcium limestone, potash, building stone and oil
26 Trilobite diorama Maclurites (gastropod) Early Paleozoic diorama Paleozoic Era in Manitoba Receptaculites Bob Elias Solitary corals (Interlake) Graham Young World s largest trilobite from Churchill Gastropods and cephalopods Virgiana (brachipod)
27 Upper Devonian reef diorama images/upper-devonian-diorama.jpg Paleozoic Era in Manitoba Paleozoic Precambrian
28 Ma Mesozoic Era in Manitoba Mesozoic Phanerozoic Eon Paleozoic Era Ce enozoic Era Preceded Mesozoic by Era period of erosion Million of years ago
29 Mesozoic Era in Manitoba Periodically flooded by shallow inland seas Ended by a meteoric impact and major extinction event Cretaceous in Manitoba diorama Canadian Fossil Discovery Centre, Morden
30 Cenozoic Era 66 0Ma Phanerozoic Eon Paleozoic Era Glacial retreat In N America Mesozoic Era Cenozoic Era Quaternary Million of years ago Glacial retreat In Manitoba
31 Dr. Ron Blakey, NAU Geology - Cenozoic Era 66 0Ma Glacial retreat In N America Glacial retreat In Manitoba Present Ma Ma Cold Warm, Cool, Cooler, dry humid drier
32 Ice age diorama Cenozoic Era The Ice Age(s) Glacial retreat In N America Glacial retreat In Manitoba
33 Cenozoic Era The modern landscape p Esker, NE Manitoba Esker Rogan moraine Bedrock highs Rogan moraine, NE Manitoba Digital Elevation Model (NASA) The last glacial period resulted in the deposition or modification of the landscape features we see today.
34 Cenozoic Era The modern landscape p Digital topographic and surficial geology information is used by many government and non-government organizations Saskatchewan R. delta Bedrock Lake Agassiz Manitoba Conservation Digital Elevation Model (NASA)
35 Aerial photograph Iceberg scours, Lorette Cenozoic Era The modern landscape In the Red River Valley, it is still possible to see the scars left in the former lake bottom of Glacial Lake Agassiz Digital Elevation Model (NASA) Iceberg scours, in Red River valley (LIDAR imagery)
36 Conclusion Digital elevation model, oblique view looking north Vertical exaggeration: 30X Satellite image of the 1997 flood draped over DEM Gaywood Matile & Greg Keller, MGS Geological processes have shaped (and reshaped) Manitoba over nearly 4 billion years of Earth history Our geological heritage impacts our daily life o Resources we use (e.g., metals, oil, aggregate, groundwater) o Landscape we live in
37 Contact us The Manitoba Geological Survey is a public resource, available for anyone to use We can answer questions about rocks, minerals, how landscapes developed, and what exploration activity is going on in the province Call us at: Or minesinfo@gov.mb.ca i
GY 112 Lecture Notes Archean Geology
GY 112 Lecture Notes D. Haywick (2006) 1 GY 112 Lecture Notes Archean Geology Lecture Goals: A) Time frame (the Archean and earlier) B) Rocks and tectonic elements (shield/platform/craton) C) Tectonics
More informationThe Lithosphere and the Tectonic System. The Structure of the Earth. Temperature 3000º ºC. Mantle
The Lithosphere and the Tectonic System Objectives: Understand the structure of the planet Earth Review the geologic timescale as a point of reference for the history of the Earth Examine the major relief
More informationEarth s History. The principle of states that geologic processes that happened in the past can be explained by current geologic processes.
Earth s History Date: Been There, Done That What is the principle of uniformitarianism? The principle of states that geologic processes that happened in the past can be explained by current geologic processes.
More informationSocial Studies 9 UNIT 2 GEOGRAPHIC INFLUENCES ON IDENTITY: PLACE AND PEOPLE
Social Studies 9 UNIT 2 GEOGRAPHIC INFLUENCES ON IDENTITY: PLACE AND PEOPLE The Structure of the Earth To understand the forces that create Canada's physical landscape we must understand the structure
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 informationChapter Introduction. Chapter Wrap-Up. Explosion
Chapter Introduction Lesson 1 Lesson 2 Lesson 3 Chapter Wrap-Up Geologic Time Ancient Earth The Cambrian Explosion How have natural events changed Earth over time? What do you think? Before you begin,
More informationEarth s Evolution Through Time
1 2 3 4 5 6 7 8 9 10 11 12 13 14 Earth s Evolution Through Time Earth 9 th edition Chapter 22 Earth s evolution: summary in haiku form Super-continents have come and gone many times: giant bumper cars.
More informationHistory of Earth. Chapter 9: HISTORY OF EARTH. The Solar System. Early Earth: A Giant Impact! Early Earth. Formation of the Solar System
Chapter 9: HISTORY OF EARTH The Essential Earth, 2 nd Edition Thomas H. Jordan & John Grotzinger History of Earth Earth is 4.56 Billion Years Old Earth has experienced a rich and diverse history that we
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 informationPhys 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 informationThe Proterozoic Eon (2500 ma to 540 ma)
The Proterozoic Eon (2500 ma to 540 ma) December November October September August July June May April March February January 0 Ma Phanerozoic C M P 540 Ma oldest shelly fossils Proterozoic 2500 Ma first
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 of NYS. Definitions GEOLOGIC PROCESSES. Faulting. Folding 9/6/2012. TOPOGRAPHIC RELIEF MAP of NYS GRADATIONAL TECTONIC
TOPOGRAPHIC RELIEF MAP of NYS PALEOGEOGRAPHY of NYS Prof. Anthony Grande AFG 2012 Definitions GEOLOGIC PROCESSES Geography: study of people living on the surface of the earth. Geology: the scientific study
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 informationChapter 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 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 informationMichigan s Geology and Groundwater
Michigan s Geology and Groundwater Ralph J. Haefner Deputy Director U.S. Geological Survey Michigan-Ohio Water Science Center Lansing, Michigan Outline About the USGS Geology 101 Michigan s geology Bedrock
More informationCopyright McGraw-Hill Education. All rights reserved. No reproduction or distribution without the prior written consent of McGraw-Hill Education
Copyright McGraw-Hill Education. All rights reserved. No reproduction or distribution without the prior written consent of McGraw-Hill Education Tibetan Plateau and Himalaya -southern Asia 11.00.a VE 10X
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 informationReview participation point: The evidence for a fluid outer core is:
DDA1 Continental Drift to Plate Tectonics PS 100 Chapter 28 Review participation point: The evidence for a fluid outer core is: A. Average density of the earth is greater than the density of the crust.
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 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 information5. Compare the density of the oceanic crust to continental crust. 6. What kind of plate boundary is this? convergent
The youngest rock is in the middle (at ridge) and it gets older on either side as you move away in a symmetrical pattern. 1. How does the age of the seafloor compare on either side of the ridge? A = youngest
More informationGeology is the study of the structure and substance of the earth. The earth s physical features have been created by many geological events:
UNIT 1 NOTES : GEOLOGY & THE EARTH S PHYSICAL STRUCTURE GEOLOGY & THE EARTH S PHYSICAL STRUCTURE Geology is the study of the structure and substance of the earth. The earth s physical features have been
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 informationChapter Overview. Evidence for Continental Drift. Plate Tectonics. Evidence for Continental Drift. Evidence for Continental Drift 9/28/2010
Chapter Overview CHAPTER 2 Plate Tectonics and the Ocean Floor Much evidence supports plate tectonics theory. Different plate boundaries have different features. Tectonic plates continue to move today.
More informationThe Early Ages. Chapter 8. The Archean
Chapter 8 The Archean The formative phase of Earth and Moon took place 4.6 to 3.9 billion years ago. At the end of the formative phase, the Earth s first real geological epoch, the Archean, began. During
More informationPotential short answer questions: What is Pangea? Describe at least 4 pieces of evidence that led Wegener to suggest the theory of Continental Drift.
6th Grade Earth Science Fall Semester Mid-Term Study Guide The mid-term may include: 4 short answer questions,1-2 sketches to draw and/or label, 4 partially filled charts which you should complete, 30
More informationGO ON. Directions: Use the diagram below to answer question 1.
d i a g n o s t i c t e s t : e a r t h a n d s p a c e s c i e n c e question 1. 1. What is the correct order (starting from the surface) of Earth s layers? A crust, outer core, inner core, mantle B mantle,
More informationName Date EARTH S HISTORY VOCABULARY
Name Date EARTH S HISTORY VOCABULARY Use Figure 2 to answer the following two questions. 10. Interpreting Graphics Which is older the sandstone layer or Dike A? Explain your answer. Conglomerate Sandstone
More informationIntroduction to Prospecting. Session Two Geology
Introduction to Prospecting Session Two Geology The Earth Earth is 4.6 billion years old (Ba). Bacteria & algae +3.5 Ba. Microscopic animals ~2 Ba. Animals ~600 million years (Ma) old. Mankind about 100,000
More informationComposition of the earth, Geologic Time, and Plate Tectonics
Composition of the earth, Geologic Time, and Plate Tectonics Layers of the earth Chemical vs. Mechanical Chemical : Mechanical: 1) Core: Ni and Fe 2) Mantle: Mostly Peridotite 3) Crust: Many different
More informationChapter 11. The Archean Era of Precambrian Time
Chapter 11 The Archean Era of Precambrian Time 1 Guiding Questions When and how did Earth and its moon come into being? How did the core, mantle, crust form? Where did Archean rocks form, and what is their
More informationEarth Science. Name Block. Unit 3 Review Worksheet. Circle the letter that corresponds to the correct answer
Earth Science Unit 3 Review Worksheet Name Block Circle the letter that corresponds to the correct answer 1. Which geologic principle is used when a geologist observes an outcrop or rocks and determines
More informationSocial Studies. Chapter 2 Canada s Physical Landscape
Social Studies Chapter 2 Canada s Physical Landscape Introduction Canada s geography its landforms and climate - has a great impact on Canadians sense of identity. Planet Earth The earth is divided into
More informationGeologic Trips San Francisco and the Bay Area
Excerpt from Geologic Trips San Francisco and the Bay Area by Ted Konigsmark ISBN 0-9661316-4-9 GeoPress All rights reserved. No part of this book may be reproduced without written permission in writing,
More informationContinental Landscapes
Continental Landscapes Landscape influenced by tectonics, climate & differential weathering Most landforms developed within the last 2 million years System moves toward an equilibrium Continental Landscapes
More informationUnit V: Earth s History
Rock Outcrop on Rte. 12 Depauville Unit V: Earth s History Review Book pp.97-112. Original photo taken by Mr. O on 8/11/10. Objective #1 Describe processes that formed the atmosphere and oceans of early
More 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 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 informationBlackline Masters Manitoba Education and Training 1999
Blackline Masters Manitoba Education and Training 1999 BLM 1 Scientific Inquiry Recording Sheet: Grades 1 and 2 What is the question? What do I think? What I used What I did What I observed What I found
More informationGeologic History of Texas: The Making of Texas Over 1.5 Billion Years
# 4 Geologic History of Texas: The Making of Texas Over 1.5 Billion Years Dr. Richard Kyle March 24, 2000 Produced by and for Hot Science - Cool Talks by the Environmental Science Institute. We request
More informationGeology of the Batemans Bay region. Geological evolution. The Lachlan Orogen
Australian Journal of Earth Sciences 1 The word orogen is derived from the ancient Greek language word for mountain building. The Lachlan Orogen The rocks exposed in the Batemans Bay are part of the geological
More informationThe Building of a Continent. Delving into Deep Time
The Building of a Continent Delving into Deep Time Methods for Studying the Past Identifying orogenies Mountain building events Mountains erode Can t study topography Study the evidence they leave behind
More informationGeologic History. Earth is very, very old
Geologic History Earth is very, very old Earth s History The history of Earth and the ages of rocks can be investigated and understood by studying rocks and fossils. Evidence of ancient, often extinct
More 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 informationScience 20. Unit C: The Changing Earth. Assignment Booklet C3
Science 20 Unit C: The Changing Earth Assignment Booklet C3 FOR TEACHER S USE ONLY Summary Teacher s Comments Chapter 3 Assignment Total Possible Marks 45 Your Mark Science 20 Unit C: The Changing Earth
More informationCOURSE OUTLINE GEOLOGY 101, Sec 002 Fall 2008, Diecchio Text: Lutgens, Tarbuck and Tasa, Essentials of Geology, 10 th edition
COURSE OUTLINE GEOLOGY 101, Sec 002 Fall 2008, Diecchio Text: Lutgens, Tarbuck and Tasa, Essentials of Geology, 10 th edition Overview Of Earth ch 1 Earth's place in solar system, galaxy, universe Atmosphere,
More informationThe Earth s Structure. The Lithosphere and Tectonic. The Lithosphere and Tectonic. System. Chapter 12. The Earth s Interior
The Lithosphere and Tectonic System Chapter 12 The Lithosphere and Tectonic System The theory describing the changing configuration of the continents through time is called plate tectonics. Plate tectonic
More informationThe Proterozoic Part 1
UNIVERSITY OF SOUTH ALABAMA GY 112: Earth History The Proterozoic Part 1 Lectures 18/19: Tectonics Instructor: Dr. Douglas W. Haywick Last Time 1) The Early Atmosphere 2) The Oceans and Hydrosphere 3)
More informationChapter 2 Plate Tectonics and the Ocean Floor
Chapter 2 Plate Tectonics and the Ocean Floor Chapter Overview Much evidence supports plate tectonics theory. The plate tectonics model describes features and processes on Earth. Plate tectonic science
More informationLIGO sees binary neutron star merger on August 17, 2017
LIGO sees binary neutron star merger on August 17, 2017 Laser Interferometer Gravitational-Wave Observatory (LIGO) Laser Interferometer Gravitational-Wave Observatory (LIGO) Multi-Messenger Astronomy This
More informationWhy does the Earth have volcanoes? Why is there Earthquakes?
Why does the Earth have volcanoes? Why is there Earthquakes? Turn to your neighbor and review: How and when did the Earth form? How old are the first traces of life on Earth? Logical? * 1.5Ga (1 st multicellular
More informationContinental Drift and Plate Tectonics
Continental Drift and Plate Tectonics Continental Drift Wegener s continental drift hypothesis stated that the continents had once been joined to form a single supercontinent. Wegener proposed that the
More informationObjectives. Vocabulary. Describe the geologic time scale. Distinguish among the following geologic time scale divisions: eon, era, period, and epoch.
The Geologic Time Scale Objectives Describe the geologic time scale. Distinguish among the following geologic time scale divisions: eon, era, period, and epoch. Vocabulary geologic time scale eon era period
More informationEARTH S HISTORY. What is Geology? logy: science. Geology is the scientific study of the Earth, including its:
EARTH S HISTORY 1 What is Geology? Geo: earth logy: science Geology is the scientific study of the Earth, including its: composition, structure, and physical properties. 2 1 Geologists study: the origin
More informationGossan s Industrial Mineral Opportunities in Manitoba
Gossan s Industrial Mineral Opportunities in Manitoba Presentation to: Gossan Resources Limited James Bamburak, M.Sc., P.Geo. July 2003 Manitoba Industry, Trade and Mines Industrial Mineral Opportunities
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 informationGeologic Time. Early Earth History
chapter 10 3 Geologic Time section 2 Early Earth History Before You Read Think of a picture of a volcano you have seen. Describe what Earth would be like if the land were almost completely covered with
More informationEarth, the Lively* Planet. * not counting the life on the planet!
Earth, the Lively* Planet * not counting the life on the planet! What We Will Learn Today What are planet Earth s features? What processes shape planetary surfaces? How does Earth s surface move? How did
More informationThe Official CA State Science Education Standards for Earth Science K 8
The Official CA State Science Education Standards for Earth Science K 8 Kindergarten The Earth is composed of land, air and water. As a basis for understanding this concept, students know: a. characteristics
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 informationLandforms in Canada. Canada is made up of three dis;nct types of landforms: Canadian Shield Highlands Lowlands
Canada s Landforms What is a Landform? A landform is any physical feature of the Earth s surface having a characteris;c, recognizable shape, produced by natural causes. Landforms include major features
More informationUnit 6: The Sea Floor
Unit 6: The Sea Floor Turn to Page 62 in Introduction to the World s Oceans Study the bathymetric chart What features do you see? How do the Atlantic and Pacific Oceans differ? What do you think accounts
More informationSAMPLE PAGE. pulses. The Ice Age By: Sue Peterson
Page 61 Objective sight words (pulses, intermittent, isotopes, chronicle, methane, tectonic plates, volcanism, configurations, land-locked, erratic); concepts (geological evidence and specific terminology
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 informationName 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 informationGrade 9 Social Studies Canadian Identity. Chapter 2 Review Canada s Physical Landscape
Grade 9 Social Studies Canadian Identity Chapter 2 Review Canada s Physical Landscape Name: Unit 1: Empowerment Terms (notes or textbook) 1. Core 2. Crust 3. Mantle 4. Magma 5. Continental drift 6. Plate
More informationName: Date: Period: Page 1
Name: Date: Period: Base your answers to questions 1 through 4 on the three bedrock outcrops below and on your knowledge of Earth science. The outcrops, labeled I, II, and III, are located within 15 kilometers
More informationEarth s Continents and Seafloors. GEOL100 Physical Geology Ray Rector - Instructor
Earth s Continents and Seafloors GEOL100 Physical Geology Ray Rector - Instructor OCEAN BASINS and CONTINENTAL PLATFORMS Key Concepts I. Earth s rocky surface covered by of two types of crust Dense, thin,
More informationMARINE GEOLOGY & GEOGRAPHY
MARINE GEOLOGY MARINE GEOLOGY & GEOGRAPHY Marine Geology 4 LAYERS OF THE EARTH CRUST THICKNESS: VARIES BETWEEN OCEAN & CONTINENTS 5-40 KM STATE: SOLID ELEMENTS: SILICON, ALUMINUM, CALCIUM, SODIUM, POTASSIUM
More informationThe Geology of Sebago Lake State Park
Maine Geologic Facts and Localities September, 2002 43 55 17.46 N, 70 34 13.07 W Text by Robert Johnston, Department of Agriculture, Conservation & Forestry 1 Map by Robert Johnston Introduction Sebago
More informationLANDFORM REGIONS IN CANADA. Classroom Notes and Descriptions
LANDFORM REGIONS IN CANADA Classroom Notes and Descriptions Landform Regions in Canada There are eight distinct landforms in Canada: Western Cordillera Region Interior Plains Canadian Shield Hudson Bay
More informationEssentials of Oceanography Eleventh Edition
Chapter Chapter 1 2 Clickers Lecture Essentials of Oceanography Eleventh Edition Plate Tectonics and the Ocean Floor Alan P. Trujillo Harold V. Thurman Chapter Overview Much evidence supports plate tectonics
More informationChapter 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 informationSection 1: Earth s Interior and Plate Tectonics Section 2: Earthquakes and Volcanoes Section 3: Minerals and Rocks Section 4: Weathering and Erosion
Section 1: Earth s Interior and Plate Tectonics Section 2: Earthquakes and Volcanoes Section 3: Minerals and Rocks Section 4: Weathering and Erosion Key Terms Crust Mantle Core Lithosphere Plate Tectonics
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 informationUnit 4 - Water. Earth s Interior. Earth s Interior. Continental Drift. Continental Drift. Continental Drift. Crust. Mantle. Core.
Unit 4 - Water How did the oceans form? What special adaptations do saltwater organisms have? Where does our water come from? How do humans affect the Earth s water? Crust Rigid outer shell of Earth Oceanic
More informationSTATION #1 Compaction and Cementation
STATION #1 Compaction and Cementation STATION #2 High Temperature and Pressure STATION #3 Sediments Examples: Glacial deposits: gravel, sand, clay River and lake deposits: gravel, sand, mud Sand dunes
More informationAlfred Wegener gave us Continental Drift. Fifty years later...
CHAPTER 2 Plate Tectonics and the Ocean Floor Plate Tectonics: summary in haiku form Alfred Wegener gave us Continental Drift. Fifty years later... Words Chapter Overview Much evidence supports plate tectonics
More informationThere are numerous seams on the surface of the Earth
Plate Tectonics and Continental Drift There are numerous seams on the surface of the Earth Questions and Topics 1. What are the theories of Plate Tectonics and Continental Drift? 2. What is the evidence
More information6. In the diagram below, letters A and B represent locations near the edge of a continent.
1. Base your answer to the following question on the cross section below and on your knowledge of Earth science. The cross section represents the distance and age of ocean-floor bedrock found on both sides
More informationRelative Dating. How do we determine a rocks age by the surrounding rocks?
Relative Dating How do we determine a rocks age by the surrounding rocks? 1 Geologic History 2 Relative Dating Uniformitarianism - the idea that forces working on our planet today worked on our planet
More 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 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 informationChapter 2. The Planet Oceanus
Chapter 2 The Planet Oceanus Composition of the Earth The Earth consists of a series of concentric layers or spheres which differ in chemistry and physical properties. There are two different ways to describe
More informationPlate Tectonics. entirely rock both and rock
Plate Tectonics I. Tectonics A. Tectonic Forces are forces generated from within Earth causing rock to become. B. 1. The study of the origin and arrangement of Earth surface including mountain belts, continents,
More informationEarth s Structure and Surface
Earth s Structure and Surface Structure of the Earth The earth is thought have originated about 4.5 billion years ago from a cloud or clouds of dust. The dust was the remains of a huge cosmic explosion
More informationCHAPTER 2 Plate Tectonics and the Ocean Floor Pearson Education, Inc.
CHAPTER 2 Plate Tectonics and the Ocean Floor Plate Tectonics Alfred Wegener first proposed in 1912 Called it Continental Drift Evidence for Continental Drift 1. Noted puzzle-like fit of modern continents
More informationCycles in the Phanerozoic
Cycles in the Phanerozoic Evolutionary trends: extinctions, adaptive radiations, diversity over time Glaciations Sea level change Ocean chemistry Atmospheric CO 2 biosphere Mass extinctions in the..you
More informationGeology Test Review Answers
Name: Geology Test Review Answers Core: Fill in the blanks: 1. Sediments get compacted and cemented into sedimentary rock. 2. Igneous rocks can be intrusive or extrusive from a volcano. 3. Adding heat
More 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 informationModule 10: Resources and Virginia Geology Topic 4 Content: Virginia Geology Notes
Virginia is composed of a very diverse landscape that extends from the beaches and barrier islands all of the way to the highly elevated Appalachian Plateau. Geologists have discovered ancient shallow
More informationThe Building of the NYC Region
The Building of the NYC Region Definitions Fall Line marks the area where an upland region (continental bedrock) and a coastal plain meet Piedmont the plateau region of the eastern United States which
More informationATOC OUR CHANGING ENVIRONMENT Lecture 21 (Chp 12) Objectives of Today s Class The long-term climate record
ATOC 1060-002 OUR CHANGING ENVIRONMENT Lecture 21 (Chp 12) Objectives of Today s Class The long-term climate record Announcements: 1. The Project; HW3; 2. Review session for the final exam: Dec 7 th. Sean
More informationGeologic Time Essentials of Geology, 11th edition, Chapter 18 Geologic Time: summary in haiku form Key Concepts Determining geological ages
1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 Geologic Time Essentials of Geology, 11 th edition, Chapter 18 Geologic Time: summary in haiku form Superposition and horizontality tell stories in rocks. Key
More informationGeologic Time. Decoding the Age of our Planet & North Carolina
Geologic Time Decoding the Age of our Planet & North Carolina The Geologic Time Scale Objectives Describe the geologic time scale. Distinguish among the following geologic time scale divisions: eon, era,
More 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 informationRock cycle diagram. Principle of Original Horizontality. Sediment is deposited horizontally
Geologic Time Rock cycle diagram Leaves of History Chapter 21 Lateral Continuity Principle of Original Horizontality Sediment is deposited horizontally Principle of Superposition Oldest rock A Younger
More informationGeology 15 West Valley College. Exam IV: Sierra Nevada
Geology 15 West Valley College Name Exam IV: Sierra Nevada 1) On the diagram above, where is the Arc- Trench Gap? a. 1 and 3 c. 7 and 8 d. 6 e. 5 and 10 2) On the diagram above, where is the subduction
More information