General Geology - GEOL 1113 Instructor: Dr. Glen S. Mattioli, Professor Office: Ozark Hall 27B Office Hours: MWF 10:30 - 11:30 AM Office Phone: 575-7295.

Slides:



Advertisements
Similar presentations
Theory of Plate Tectonics
Advertisements

Chapter 2 Section 2 Forces Of Change.
General Geology - GEOL 1113 Section 005 Instructor: Dr. Glen S. Mattioli, Professor Office: Ozark Hall 27B Office Hours: MW 10:30-12:00 & TR 11:00-12:00.
THE LANGUAGE OF THE EARTH – PART V PLATE TECTONIC THEORY.
Tsunami Great Sumatra Earthquake Tsunami Death Toll ~ 250,000 Tsunami Death Toll ~ 250,000.
The Tectonic Plates The Violent Earth. Types of Crust Continental Crust – 20 to 70 km (10 to 30 miles) thick. Oceanic Crust – 7 km (4 miles) thick.
Plate boundaries LO: to be able to explain what happens when plates meet.
Lesson 14: Plate Tectonics II Geological Oceanography.
Announcements 12/6 is the LAST day to turn in work for this Quarter. –Sea Floor (Due 11/26) –Relative dating problem set (Due 12/3) –Radiometric dating.
Plate Tectonics  Earth is a dynamic planet: its land masses and oceans are in constant motion. Continental blocks split to form new oceans.
Plate Tectonics Review Misc. Plate Tectonics Plate Evidence Earth's Interior Geologic Events Plate Boundaries.
I-5 Notes Dynamic Planet. The Nature of Earthquakes.
Chapter 8 Notes Place these notes into your Geology Notebooks.
Lecture Outlines Physical Geology, 14/e Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display. Plummer, Carlson &
Lecture Outlines Physical Geology, 13/e Plummer & Carlson Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display.
Physical Geology 1403 Chp. 1 Notes Introduction to Geology.
Dimensional Analysis  It is 93,000,000 miles to the sun. If a spaceship can travel 18,000 m/s how long would it take to get there?
An Introduction to Geology Chapter 1.  Geology is the science that pursues an understanding of planet Earth ▪ Physical geology – examines the materials.
The science of Geology Geology is the science that pursues an understanding of planet Earth Physical geology - examines the materials composing Earth.
Theory of Plate Tectonics Plate Tectonics Plate Boundaries Causes of Plate Tectonics.
Chapter 1 Introduction to Physical Geology IndexIndex  
Introducing Geology and an Overview of Important Concepts Physical Geology, Chapter 1 Tim Horner CSUS Geology Department (916)
CHAPTER 2 THE SEA FLOOR. OCEANIC & CONTINENTAL OCEAN ZONES & HABITATS.
Geology and Nonrenewable Minerals Chapter What Are the Earth’s Major Geological Processes and Hazards?  Concept 14-1A: Gigantic plates in the.
Lex Pritchett.  Plate tectonics are defined as the process and dynamics of tectonic plate movement  In the 1960s the theory of plate tectonics determined.
ENVIRONMENTAL SCIENCE Chapter 3 The Dynamic Earth 3.1 The Geosphere.
Lisa Wald USGS Pasadena U.S. Department of the Interior U.S. Geological Survey USGS Earthquake Hazards Program Earthquakes 101 (EQ101)
Geology 12 Plate Boundaries There are three types of plate boundaries 1. Divergent (or constructive) plate boundary 2. Convergent (or destructive) plate.
.. Plate Tectonics Theory that the Earth’s crust is made of rigid plates that float on the molten layer of the mantle. Comes from the Greek word meaning.
Changes Within the Earth Coach Parrish 7 th Grade History Oxford Middle School.
Theory of Plate Tectonics Plate Tectonics Plate Boundaries Causes of Plate Tectonics.
Changes Within The Earth Geography 8. Geology Study of earth’s physical structure and history 4.6 billion years old Geologists: –Learn about changes –Understand.
The Origins of Magma and Igneous Rocks
Integrated Coordinated Science End of Year Review.
Robert W. Christopherson Charlie Thomsen Chapter 11 The Dynamic Planet.
GEOS 112 Intro to Geology. Who Needs Geology Avoiding Geologic Hazards – Earthquakes – Volcanoes – Other geologic hazards.
The Earth’s Oceans and Plate Tectonics Oceanography Unit #1.
Continental Drift to Plate Tectonics: From hypothesis to theory Part C: The theory of plate tectonics 1.
Continental Drift to Plate Tectonics: From hypothesis to theory Part C: The theory of plate tectonics.
Unit 7 Mineral Resources.
Earthquakes 101 (EQ101) Lisa Wald USGS Earthquake Hazards Program
WELCOME TO PLANET EARTH ~4.6 BILLION YEARS OLD.
12. Tectonic landforms Introduction Introduction Major features of continents Major features of continents Major features of the oceans Major features.
Goal  to understand that geological forces are responsible for Canada’s varied landscape.  The various geological forces that caused our landscape are.
Geography of Canada Mr. J. Brazeau Plate Tectonics.
The Dynamic Crust Topic 12. Principle of Original Horizontality: The assumption that sedimentary rocks form in horizontal layers. Drawing: Then how.
CALIFORNIA Science Content Standards Grade 6-Focus on Earth Science As compiled by Mr. Holsinger.
Who Needs Geology?. Geology in Today’s World Geology - The scientific study of the Earth – Physical Geology is the study of Earth’s materials, changes.
Plate Tectonics Chapter 9. Theory of Plate Tectonics Plate Tectonics Plate Boundaries Causes of Plate Tectonics.
Earth History GEOL 2110 Theory of Plate Tectonics Part 2: Elements of Plate Tectonics.
Chapter 2 Plate Tectonics.
Dr.Souad Guernina Winter 2013
Plate Tectonics Not a form of Dubstep.
Plate Tectonics.
Plate Tectonics Evolution of the Earth.
Tectonic Plates Plate Boundaries
Quiz #3 Due Wednesday before Midnight
Plate Tectonics Evolution of the Earth.
Plate Tectonics, Earthquakes, and Volcanoes
Questions... What is the lithosphere? What is the asthenosphere?
Warm-Up: March 18, 2016 Write down everything you know about plate tectonics.
Theory of Plate Tectonics
Theory of Plate Tectonics
Plate Tectonics. Plate Tectonics Theory of Plate Tectonics Plate Boundaries Causes of Plate Tectonics.
Theory of Plate Tectonics
Place these notes into your Geology Notebooks.
Theory of Plate Tectonics
Warm up 9/24/18 Identify and describe two reasons that wetlands are ecologically important Farmer Keishi lives upstream from Freemont Creek which empties.
Plate Tectonics & Major Geological Events
Presentation transcript:

General Geology - GEOL 1113 Instructor: Dr. Glen S. Mattioli, Professor Office: Ozark Hall 27B Office Hours: MWF 10: :30 AM Office Phone: Class Web Page:

2006 Exams, Syllabus, and Grading Class Purpose: To introduce undergraduate students to physical geology, Earth’s internal structure and materials, and Geologic Time. Emphasis will be on developing close connections between Earth materials and processes within a Plate Tectonic framework. Four 1 Hour Examinations and Comprehensive Final Part I - Rocks and Minerals: Fri. Sept. 22nd Part II - Geologic Time and Surface Processes: Fri. Oct. 20th Part III - Deformation, Earthquakes, & Earth Structure: Mon. Nov. 13th Part IV - The Big Picture: Tectonics & Orogenesis: Fri. Dec. 1st FINAL - Saturday, December 9th, 7:30-9:30 AM

Grades and Grading

Physical Geology, 11/e Charles C. Plummer California State University at Sacramento Diane H. Carlson California State University at Sacramento The Late David McGeary Emeritus of California State University at Sacramento Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display. Required Text

Chapter 1 Introduction to Physical Geology

Why Study Geology? Mitigating Geologic Hazards –Earthquakes –Volcanoes Supplying Things We Need –Metals –Minerals –Petroleum Protecting the Environment –Water cycle –Global Change: Sea level rise Understanding Our Surroundings –The Earth’s relationship to other planets –Geological Time

Los Angeles Basin

Recent Southern California Earthquakes Northridge (94)San Fernando (71)Sierra Madre (91) Whitter Narrorws (87)Long Beach (33) From:

TIME: January 17, :30:55 am PST LOCATION: 34° 12.80' N, 118° 32.22'W; 20 miles west-northwest of Los Angeles 1 mile south-southwest of Northridge MAGNITUDE: M W 6.7 TYPE OF FAULTING: blind thrust FAULT INVOLVED: Northridge Thrust (also known as the Pico Thrust) DEPTH: 18.4 km Northridge Earthquake Facts

Northridge CA earthquake Jan. 17, 1994,

Northridge Earthquake

Northridge Aftershocks

Original AVS animation by Ian Sammis and Damien Sullivan.

Northridge Rupture Model Wald, David J., Heaton, Thomas H., and Hudnut, K.W. The Slip History of the 1994 Northridge, California, Earthquake Determined From Strong-Motion, Teleseismic, GPS, and Leveling Data, Special Northridge Earthquake Issue of the Bull. of the Seismo. Soc. of America

Convergent Margin Magma Genesis

Eruption of Mt. Pinatubo, June 15, 1991

Plymouth, Montserrat - Destroyed by pyroclastic flows in 1996/7 Photo credit: G. Mattioli

Automobiles - Always Thirsty for Gas!

Source:

Alaska Pipeline

An Overview of Physical Geology—Important Concepts Internal Processes: How the Earth’s Internal Heat Engine Works The Earth’s Interior The Theory of Plate Tectonics Surficial Processes: The Earth’s External Heat Engine

Convection Examples

Rayleigh-Benard Convection

Earth Structure

Convection in the Mantle

convection in the mantle models observed heat flow warm: near ridges cold: over cratons from: from:

From: "Dynamic models of Tectonic Plates and Convection" (1994) by S. Zhong and M. Gurnis

Earth’s Plates

obvious from space that Earth has two fundamentally different physiographic features: oceans (71%) and continents (29%) global topography from: crust

Convergent Margins and Magma Genesis

MORB Genesis

Submarine Pillow Basalt Formation

Ocean Crust Age-Depth Relations

Cross-cutting relationships

Simplified Geologic Time Scale