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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 Class Web Page: http://comp.uark.edu/~mattioli/geol_1113.html Email: mattioli@uark.edu
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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
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Grades and Grading
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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
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Chapter 1 Introduction to Physical Geology
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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
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Los Angeles Basin
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Recent Southern California Earthquakes Northridge (94)San Fernando (71)Sierra Madre (91) Whitter Narrorws (87)Long Beach (33) From: http://www.scecdc.scec.org/labasin.html
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TIME: January 17, 1994 4:30:55 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
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Northridge CA earthquake Jan. 17, 1994,
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Northridge Earthquake
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Northridge Aftershocks
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Original AVS animation by Ian Sammis and Damien Sullivan.
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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
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Convergent Margin Magma Genesis
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Eruption of Mt. Pinatubo, June 15, 1991
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Plymouth, Montserrat - Destroyed by pyroclastic flows in 1996/7 Photo credit: G. Mattioli
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Automobiles - Always Thirsty for Gas!
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Source: http://www.wtrg.com/oil_graphs/oilprice1947.gif
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Alaska Pipeline
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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
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Convection Examples
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Rayleigh-Benard Convection
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Earth Structure
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Convection in the Mantle
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convection in the mantle models observed heat flow warm: near ridges cold: over cratons from: http://www.geo.lsa.umich.edu/~crlb/COURSES/270 from: http://www-personal.umich.edu/~vdpluijm/gs205.html
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From: "Dynamic models of Tectonic Plates and Convection" (1994) by S. Zhong and M. Gurnis
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Earth’s Plates
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obvious from space that Earth has two fundamentally different physiographic features: oceans (71%) and continents (29%) global topography from: http://www.personal.umich.edu/~vdpluijm/gs205.html crust
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Convergent Margins and Magma Genesis
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MORB Genesis
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Submarine Pillow Basalt Formation
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Ocean Crust Age-Depth Relations
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Cross-cutting relationships
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Simplified Geologic Time Scale
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