Postdoctoral Scholar Graduate Research Assistant Visiting Research Scientist

Size: px
Start display at page:

Download "Postdoctoral Scholar Graduate Research Assistant Visiting Research Scientist"

Transcription

1 Maryjo N. Brounce California Institute of Technology 363 Arms Laboratory, Mail code: California Institute of Technology, Pasadena CA phone: EDUCATION Ph.D. The University of Rhode Island Graduate School of Oceanography, 2014 Oceanography Thesis: A geochemical investigation of oxygen fugacity in the Marianas subduction zone Advisors: Katherine Kelley and Elizabeth Cottrell B.S. The Pennsylvania State University, Geosciences, as an EMSage Laureate 2009 Thesis: Co-variation of boron concentrations and isotope ratios in glasses from the Laki-Grimsvötn fissure eruption of Advisor: Maureen Feineman Minor The Pennsylvania State University, Chemistry 2009 POSITIONS HELD 2014-present Postdoctoral Scholar, Division of Geological and Planetary Sciences, California Institute of Technology Graduate Research Assistant, The Graduate School of Oceanography, University of Rhode Island Visiting Research Scientist, The National Museum of Natural History, Smithsonian Institution AWARDS RECEIVED 2015 University of Rhode Island Graduate School Excellence in Doctoral Research Award, University of Rhode Island 2013 Robert L. McMaster Scholarship in Marine Geology, The Graduate School of Oceanography, University of Rhode Island 2013 AGU Outstanding Student Paper Award: Tectonophysics. Fall 2012 Meeting 2013 GeoPRISMS AGU Student Prize for best oral presentation, Fall 2012 Meeting 2011 Distinction in Student Poster Presentation, GeoPRISMS Alaska Primary Site Planning Meeting 2011 Watkins Award: Distinction in geological oceanography graduate studies, The Graduate School of Oceanography, University of Rhode Island 2011 Honorable Mention, GeoPRISMS Student Poster Presentation, Fall 2010 AGU Meeting 2010, 2011 Honorable Mention, National Science Foundation Graduate Fellowship 2009 Excellent Research in Physical Sciences, Undergraduate Research Exhibition, The Pennsylvania State University 2009 Laureate, Earth and Mineral Sciences Academy for Global Experience (EMSage), The Pennsylvania State University 2008, 2009 Frank Dachille Award for Excellence in Geochemistry, The Pennsylvania State University

2 PEER REVIEWED JOURNAL PUBLICATIONS Brounce, M.N., Eiler, J., and Stolper, E. (in preparation) Redox variations in HSDP-2 Mauna Kea lavas and oxygen fugacity of the Hawaiian plume. Brounce, M.N., Stern, R.J., Kelley, K.A., Martinez, F., and Cottrell, E. (in preparation) The Fina Nagu Volcanic Complex: Unusual submarine arc volcanism in the rapidly deforming southern Mariana margin. Brounce, M.N., Kelley, K.A. and Cottrell, E. (in preparation) A review of transition element proxies for mantle source oxygen fugacity. Brounce, M.N., Kelley, K.A. and Cottrell, E. (in preparation) The redox budget of the Mariana subduction zone. Helz, R.T., Cottrell, E., Kelley, K.A., and Brounce, M.N. (in preparation) Redox history of the 1959 eruption of Kilauea volcano as defined by olivine-melt relationships and in situ XANES analyses. Ribeiro, J.M., Woodhead, J., Stern, R.J., Kelley, K.A., Ohara, Y., and Brounce, M.N. (in review) The dynamic interplay between Indian and Pacific mantle domains revealed in basalts from the southernmost Mariana convergent margin. Brounce, M.N., Kelley, K.A and Cottrell, E. (2015) Temporal evolution of mantle wedge oxygen fugacity during subduction initiation. Geology doi: /g Brounce, M.N., Kelley, K.A. and Cottrell, E. (2014) The Fe 3+ / Fe variations in Mariana Arc basalts and primary fo 2 of the mantle wedge. Journal of Petrology v. 55, pp Le Voyer, M., Cottrell, E., Kellley, K.A., Brounce, M.N., Hauri, E.H. (2014) The effect of primary versus secondary processes on the volatile content of MORB glasses: an example from the equatorial Mid-Atlantic Ridge (5N 3S) Journal of Geophysical Research: Solid Earth. Brounce, M.N., Feineman, M., LaFemina P., and Gurenko A. (2012) Insights into crustal assimilation from boron in melt inclusions: Lakagigar Eruption, Iceland. Geochimica et Cosmochimica Acta v. 94. pp O Hara, Y., Reagan, M.K., Fujikura, K., Watanabe, H., Martinez, F., Girard, G., Ribiero, J., Brounce M.N., Komori, N., and Kino, M. (2012) A serpentinite-hosted ecosystem in the Southern Mariana Forearc, PNAS v. 109, pp Jan 2016 May 2015 Feb 2015 Feb 2015 Jan 2015 Apr 2014 Nov 2013 INVITED PRESENTATIONS University of California, Los Angeles, Variations in magmatic redox caused by source and process Institut de Physique du Globe de Paris, The oxidation state of Fe in basalts from the Mariana subduction system Harvard University, The oxidation state of Fe in basalts from the Mariana subduction system and The redox budget of the Mariana subduction system California Institute of Technology, Constraints on the oxygen fugacity of the upper mantle Johns Hopkins University, The oxidation state of Fe in basalts from the Mariana subduction system. California Institute of Technology, A geochemical investigation of oxygen fugacity in the Marianas. Woods Hole Oceanographic Institution, A geochemical investigation of oxygen fugacity in the Marianas.

3 Oct 2013 University of Rhode Island, A geochemical investigation of oxygen fugacity in the Marianas. Jan 2012 Boston University. Fe 3+ /ΣFe variation in Mariana arc and back-arc magmas and primary fo 2 of the mantle wedge. Nov 2011 Brown University, The oxidation state of iron in arc basalts. PUBLIC SERVICE AND PROFESSIONAL ACTIVITIES Volunteer reviewer, National Science Foundation research proposal system Volunteer reviewer, German Research Foundation research proposal system Volunteer reviewer, for manuscript submissions to Contributions to Mineralogy and Petrology, Journal of the Geological Society, Geochemistry Geophysics Geosystems, Earth and Planetary Science Letters Co-convener, Geochemical and geophysical links between subduction zone dynamics and arc systems, The American Geophysical Union Joint Fall Meeting 2015 Co-mentor to Andrew Heard, (faculty mentor: Edward Stolper) Summer Undergraduate Research Fellows, California Institute of Technology 2015 Participant, alpha-melts workshop, California Institute of Technology 2014 Participant, isamples / C4P early career forum, EarthCube 2014 Participant, The Sulfur Cycle, Agouron Institute 2013, 2014 Judge, The American Geophysical Union student presentation competition, GeoPRISMS Student Representative, Educational Policy Committee, The Graduate School of Oceanography, University of Rhode Island Outreach Science Advisor, The Deep Carbon Observatory, University of Rhode Island Graduate School of Oceanography, Rensselaer Polytechnic Institute, and Carnegie Institution of Washington Outreach Scientist, The Office of Marine Programs, The Graduate School of Oceanography, University of Rhode Island 2013 Graduate mentor to Elizabeth Fisher, (faculty mentor: Katherine Kelley) Summer Undergraduate Research Fellows in Oceanography, University of Rhode Island 2013 Scribe/Participant, EarthCube planning workshop, Washington, D.C Scribe/Participant, ExTERRA Workshop, Goldschmidt Geochemistry meeting, Florence, Italy 2012 Scribe/Participant, East African Rift Focus site planning meeting, GeoPRISMS, Morristown, NJ 2011 Participant, Alaska focus site planning meeting, GeoPRISMS, Portland, Oregon Member, Women in Science and Engineering Pennsylvania Space Consortium Grant, The Pennsylvania State University BEAM TIME AWARDS AT DOE NATIONAL SYNCHROTRON FACILITIES Dec 2015 GSECARS GUP-46841: Determining links between magma redox heterogeneity and plate tectonic cycling, Advanced Photon Source, Argonne National Laboratory

4 Mar 2014 Score: 1.70 Total shifts awarded: 56 GSECARS GUP-38332: The effects of S speciation on volcanic S degassing and silicate magma evolution, Advanced Photon Source, Argonne National Laboratory Score: 1.60 Total shifts awarded: 27 ABSTRACTS Brounce, M.N., Stolper, E., and Eiler, J. (2015) Changes in magmatic oxidation state induced by degassing. AGU Fall Meet. Brounce, M.N., Kelley, K.A., Cottrell, E., Eiler, J., and Stolper, E. (2015) The relationship between slab fluids and oxidized arc basalts. INVITED, Goldschmidt Meet. Williams, H.M., Prytulak, J., Plank, T., Kelley, K.A., Brounce, M.N., and Woodhead, J. (2015) Iron stable isotopes, magmatic differentiation and the oxidation state of Mariana arc magmas. Goldschmidt Meet. Brounce, M.N., Cottrell, E., and Kelley, K.A. (2014) The redox budget of the Mariana subduction zone. AGU Fall Meet. Ohara, Y., Martinez, F., Brounce M.N., Pujana I., Ishii T., Stern R.J., Ribiero, J., Michibayashi, K., Kelley, K.A., Reagan, M.K., Watanabe, H., and Okumura, T. (2014) The first Shinkai dive study of the southwestern portion of the Mariana arc system. AGU Fall Meet. Kelley, K.A., Cottrell, E., Brounce, M.N., Gentes Z. (2014) Roles of magmatic oxygen fugacity and water content in generating signatures of continental crust in the Alaska- Aleutian arc. AGU Fall Meet. Helz, R., Cottrell, E., Kelley, K.A., and Brounce, M.N. (2014) Redox history of the 1959 Kilauea eruption determined by XANES analysis of glassy scoria. Goldschmidt Meet. Feineman, M., LaFemina, P., Brounce, M.N., Cappos, M., and Gurenko, A. (2014) Basaltic cannibalism in Iceland. Goldschmidt Meet. Brounce, M.N., Kelley, K.A. and Cottrell E. (2013) Temporal evolution of fo 2 in the Mariana mantle wedge. AGU Fall Meeting Abstracts, Abstract V43A Kelley, K.A., Cottrell, E. and Brounce, M.N. (2013) Links between oxygen fugacity, slab fluids, and calc-alkaline differentiation of arc magmas. AGU Fall Meeting Abstracts, Abstract V41E-06. Brounce, M.N., Kelley, K.A. and Cottrell E. (2013) Evaluating proxies for fo 2 in the Marianas. Goldschmidt Meet. Kelley, K.A., Cottrell, E., and Brounce M.N. (2013) The relationship between fo 2 and calcalkaline affinity of arc magmas. Goldschmidt Meet. Brounce, M.N., Kelley, K.A., and Cottrell E. (2012) Fe 3+ /ΣFe variation in Mariana arc and backarc magmas and primary fo 2 of the mantle wedge. AGU Fall Meeting Abstracts, Abstract T54A-05. Brounce, M.N., Kelley, K.A., and Cottrell E. (2011) Effect of differentiation on Fe oxidation in arc basalts. Goldschmidt Meet. Brounce, M.N., Kelley, K.A., and Cottrell E. (2010) Variations in Fe oxidation state at arc volcanoes driven by degassing and crystallization. AGU Fall Meeting Abstracts, Abstract V43A Kelley, K.A., Cottrell E., Brounce M.N., and Parks B. (2010) The influence of magmatic differentiation on the oxidation state of Fe in arc magmas. Goldschmidt Meet. Brounce, M.N., Feineman M., Gurenko A., and LaFemina P. (2009) Boron isotope variation in matrix glasses and inclusions from the Skaftar Fires eruption reflects

5 incorporation of altered materials in the Icelandic crust. AGU Fall Meeting Abstracts, Abstract V51E Brounce M.N., Feineman M., Gurenko A., and LaFemina P. (2008) Co-variation of boron concentrations and isotope ratios in glasses from the Laki-Grimsvötn fissure eruption of AGU Fall Meeting Abstracts, Abstract V21A July 2014 Jan 2011 Sept 2010 Sept 2010 August 2008 May 2008 FIELD/SHIPBOARD EXPERIENCE Shipboard Scientist aboard R/V Yokosuka, Shinkai 6500 submersible dives along the southern Mariana forearc, JAMSTEC Shipboard Scientist aboard R/V Thomas G. Thompson, dredging and geophysical investigation of the southern Mariana forearc, ONR UNOLS Observer aboard submersible Shinkai 6500, Dive 6K#1236; Investigation of seafloor geology in the western Marianas Trench, JAMSTEC Shipboard Scientist aboard R/V Yokosuka, Shinkai 6500 submersible dives and deep tow camera dives along the Southeast Marianas Forearc Rift, JAMSTEC Tephra mapping and collection at the Laki fissure in Iceland, The Pennsylvania State University Volcanic deposit mapping and glacial studies, introduction to LIDAR, seismic reflection, and continuous GPS monitoring in Iceland, The Pennsylvania State University TEACHING EXPERIENCE Teaching Assistant, The Graduate School of Oceanography, University of Rhode Island OCG 110: The Ocean Planet (Fall 2012) Primary responsibilities: grading, lecturer, design and lead inclass activities, design and administer homework assignments, tutor. OCG 131: Volcanoes (Fall 2010) Primary responsibilities: grading, lecturer Teaching Intern, The Pennsylvania State University Geosc 201: Earth Materials (Spring 2009) Primary responsibilities: lead laboratory exercises, grading Geosc 001: Physical Geology (Fall 2008) Primary responsibilities: lead laboratory exercises, grading Geosc 040: The Sea Around Us (Fall 2007, Spring 2008) Primary responsibilities: co-lead laboratory exercises, grading PROFESSIONAL SOCIETIES American Geophysical Union Geochemical Society Mineralogical Society of America

Magmatic Processes at Subduction Zones

Magmatic Processes at Subduction Zones Magmatic Processes at Subduction Zones Katherine A. Kelley Graduate School of Oceanography Univ. of Rhode Island Thanks to Terry Plank Erik Hauri GVP: Liz Cottrell Simon Carn Jennifer Jay Ed Venzke Subduction

More information

John Breier. CURRICULUM VITAE 28 August 2007 ADDRESS AND TELEPHONE

John Breier. CURRICULUM VITAE 28 August 2007 ADDRESS AND TELEPHONE CURRICULUM VITAE 28 August 2007 John Breier ADDRESS AND TELEPHONE Woods Hole Oceanographic Institution Applied Ocean Physics & Engineering 266 Woods Hole Road Blake Building, Room 200 Woods Hole, MA, 02543

More information

Crustal Boundaries. As they move across the asthenosphere and form plate boundaries they interact in various ways. Convergent Transform Divergent

Crustal Boundaries. As they move across the asthenosphere and form plate boundaries they interact in various ways. Convergent Transform Divergent Name: Date: Period: Plate Tectonics The Physical Setting: Earth Science CLASS NOTES Tectonic plates are constantly moving and interacting As they move across the asthenosphere and form plate boundaries

More information

The Lead 206/207 Dating Method

The Lead 206/207 Dating Method The Lead 206/207 Dating Method 1 U Pb Zircon Ages, Chemical Geology, Volume 211 (2004) Pages 87 109 2 Lead Isotope Planetary Profiling, Chemical Geology, Volume 233 (2006) Pages 1 45 3 U Pb Step-Leaching

More information

SUNYOUNG (SUNNY) PARK

SUNYOUNG (SUNNY) PARK SUNYOUNG (SUNNY) PARK Department of Earth and Planetary Sciences, Harvard University, 20 Oxford Street, Cambridge, MA 02138, USA +1 (617) 495-1172 sunyoungpark01@fas.harvard.edu http://seismology.harvard.edu/people/park.html

More information

Tieyuan Zhu Postdoctoral Fellow, Jackson School of Geosciences, the University of Texas at Austin Mail address: Telephone: Website:

Tieyuan Zhu Postdoctoral Fellow, Jackson School of Geosciences, the University of Texas at Austin Mail address: Telephone:   Website: Postdoctoral Fellow, Jackson School of Geosciences, the University of Texas at Austin Mail address: Telephone: Email: Website: 10100 Burnet Rd. #130, Austin TX 01-650- 308-6506 tzhu@jsg.utexas.edu http://www.jsg.utexas.edu/tyzhu/

More information

Plates Moving Apart Types of Boundaries

Plates Moving Apart Types of Boundaries Plates Moving Apart Types of Boundaries PLATE TECTONICS IS The theory that the Earth s crust is broken into slabs of rock that move around on top of the asthenosphere. How fast are plates moving? The Arctic

More information

How does the mantle beneath the Ring of Fire change through time?: a trace element

How does the mantle beneath the Ring of Fire change through time?: a trace element Page 1 How does the mantle beneath the Ring of Fire change through time?: a trace element study of primitive basalts erupted in a small area in the Southern Cascades Abstract I will test the hypothesis

More information

Electronic Appendix A: Supplementary material to accompany the manuscript, Fe 3+ / Fe in Mariana Arc basalts and primary fo 2.

Electronic Appendix A: Supplementary material to accompany the manuscript, Fe 3+ / Fe in Mariana Arc basalts and primary fo 2. Electronic Appendix A: Supplementary material to accompany the manuscript, Fe 3+ / Fe in Mariana Arc basalts and primary fo 2. Screening for olivine interference in Fe-µ-XANES spectra When collecting Fe-µ-XANES

More information

6. In the diagram below, letters A and B represent locations near the edge of a continent.

6. 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 information

Plate Tectonics. I. The Discovery of Plate Tectonics II. A Mosaic of Plates III. Types of Plate Boundaries IV. How Plates Move

Plate Tectonics. I. The Discovery of Plate Tectonics II. A Mosaic of Plates III. Types of Plate Boundaries IV. How Plates Move Plate Tectonics I. The Discovery of Plate Tectonics II. A Mosaic of Plates III. Types of Plate Boundaries IV. How Plates Move I. The Discovery of Plate Tectonics A. Continental Drift (Alfred Wegener) Proposed

More information

Captain s Tryouts 2017

Captain s Tryouts 2017 Captain s Tryouts 2017 Dynamic Planet Test Written by: Araneesh Pratap (Chattahoochee High School) Name: Date: Answer all questions on the answer sheet. Point values are given next to each question or

More information

Department of Meteorology, Penn State University NSF Research Experience for Undergraduate Internship,

Department of Meteorology, Penn State University NSF Research Experience for Undergraduate Internship, Kara Jo Sulia Curriculum Vita The University at Albany Atmospheric Science Research Center CESTM Building, 251 Fuller Road, Albany, NY 12222 Phone: (518) 437-8755 Email: ksulia@albany.edu Education: Ph.D.

More information

1.4 Notes: Plates Converge or Scrape Past Each Other Think About Tectonic Plates Push Together at Convergent Boundaries

1.4 Notes: Plates Converge or Scrape Past Each Other Think About Tectonic Plates Push Together at Convergent Boundaries 1.4 Notes: Plates Converge or Scrape Past Each Other Think About If new crust is created at divergent boundaries, why does the total amount of crust on Earth stay the same? Tectonic Plates Push Together

More information

Beneath our Feet: The 4 Layers of the Earty by Kelly Hashway

Beneath our Feet: The 4 Layers of the Earty by Kelly Hashway Beneath our Feet: The 4 Layers of the Earty by Kelly Hashway The Earth is more than a giant ball made up of dirt, rocks, and minerals. The Earth may look like a giant ball from when looking at it from

More information

Questions and Topics

Questions 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 information

Education. UNIVERSITY OF MISSOURI, Columbia, MO B.S., with honors in Geological Sciences, Cum Laude. Positions Held

Education. UNIVERSITY OF MISSOURI, Columbia, MO B.S., with honors in Geological Sciences, Cum Laude. Positions Held Fred A Davis University of Minnesota Duluth Department of Earth and Environmental Sciences 229 Heller Hall, 1114 Kirby Dr., Duluth, MN 55812 email: fdavis@d.umn.edu phone: (218) 726-8331 Education UNIVERSITY

More information

GENERAL GEOLOGY Fall Chapter 18: The Sea Floor. Partial Examination IV Study Guide Dr. Glen S. Mattioli

GENERAL GEOLOGY Fall Chapter 18: The Sea Floor. Partial Examination IV Study Guide Dr. Glen S. Mattioli GENERAL GEOLOGY 1113-005 Fall 2008 Partial Examination IV Study Guide Dr. Glen S. Mattioli Note that these are NOT questions, but rather are a list of topics that we have covered either in class or are

More information

A Plagioclase Analysis of the Thrihnukagigur Volcano in Southwest Iceland. Michael Cappos ABSTRACT

A Plagioclase Analysis of the Thrihnukagigur Volcano in Southwest Iceland. Michael Cappos ABSTRACT A Plagioclase Analysis of the Thrihnukagigur Volcano in Southwest Iceland Michael Cappos ABSTRACT The last eruption of the Thrihnukagigur volcano, located on the Reykjanes Peninsula in southwest Iceland,

More information

Plates & Boundaries The earth's continents are constantly moving due to the motions of the tectonic plates.

Plates & Boundaries The earth's continents are constantly moving due to the motions of the tectonic plates. Plates & Boundaries The earth's continents are constantly moving due to the motions of the tectonic plates. As you can see, some of the plates contain continents and others are mostly under the ocean.

More information

ESS103A Igneous Petrology

ESS103A Igneous Petrology Welcome to ESS103A Igneous Petrology Please pick up handouts Plan for today: Who are we? What is this class about? What is the structure of this course? How does the scientific method work? Who are we?

More information

Dynamic Crust Practice

Dynamic Crust Practice 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 information

Bathymetry Measures the vertical distance from the ocean surface to mountains, valleys, plains, and other sea floor features

Bathymetry Measures the vertical distance from the ocean surface to mountains, valleys, plains, and other sea floor features 1 2 3 4 5 6 7 8 9 10 11 CHAPTER 3 Marine Provinces Chapter Overview The study of bathymetry determines ocean depths and ocean floor topography. Echo sounding and satellites are efficient bathymetric tools.

More information

GSA Data Repository

GSA Data Repository GSA Data Repository 218145 Parolari et al., 218, A balancing act of crust creation and destruction along the western Mexican convergent margin: Geology, https://doi.org/1.113/g39972.1. 218145_Tables DR1-DR4.xls

More information

GD3.3/GM3.3/GMPV16/TS4.7

GD3.3/GM3.3/GMPV16/TS4.7 GD Geodynamics Orals and PICOs MO1, 08:30 10:00 MO2, 10:30 12:00 MO3, 13:30 15:00 MO4, 15:30 17:00 TU1, 08:30 10:00 TU2, 10:30 12:00 TU3, 13:30 15:00 Monday, 08 April Medal Lecture) (co-organized), 08:30

More information

1. I can describe evidence for continental drift theory (e.g., fossil evidence, mountain belts, paleoglaciation)

1. 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 information

Science 10 PROVINCIAL EXAM STUDY BOOKLET. Unit 4. Earth Science

Science 10 PROVINCIAL EXAM STUDY BOOKLET. Unit 4. Earth Science Science 10 PROVNCAL EXAM STUDY BOOKLET Unit 4 Earth Science Student nstructions 1. Ensure that you have blank paper and a Data Booklet. 2. Record all answers on a separate piece of paper. 3. Answer keys

More information

Map shows 3 main features of ocean floor

Map shows 3 main features of ocean floor Map shows 3 main features of ocean floor 2017 Pearson Education, Inc. Chapter 3 Marine Provinces 2017 Pearson Education, Inc. 1 Chapter 3 Overview The study of bathymetry determines ocean depths and ocean

More information

Geologic Evolution of Latin America. Plate Tectonics: General Concepts & Applications to Latin America

Geologic Evolution of Latin America. Plate Tectonics: General Concepts & Applications to Latin America Geologic Evolution of Latin America Plate Tectonics: General Concepts & Applications to Latin America Structure of Earth: 3 major divisions of Core, Mantle, and Crust Upper mantle differs in the way that

More information

Supplementary material to accompany the manuscript, Redox variations in HSDP2

Supplementary material to accompany the manuscript, Redox variations in HSDP2 Supplementary material to accompany the manuscript, Redox variations in HSDP2 Mauna Kea lavas, the oxygen fugacity of the Hawaiian plume, and the role of volcanic gases in Earth s oxygenation by M. Brounce,

More information

An Introduction of Aleutian Subduction Zone. Chuanmao Yang, Hong Yang, Meng Zhang, Wenzhong Wang 2016/04/29

An Introduction of Aleutian Subduction Zone. Chuanmao Yang, Hong Yang, Meng Zhang, Wenzhong Wang 2016/04/29 An Introduction of Aleutian Subduction Zone Chuanmao Yang, Hong Yang, Meng Zhang, Wenzhong Wang 2016/04/29 Outline General Introduction Formation history Structure from seismic study geochemical features

More information

Chapter Overview. Bathymetry. Measuring Bathymetry. Measuring Bathymetry

Chapter Overview. Bathymetry. Measuring Bathymetry. Measuring Bathymetry CHAPTER 3 Marine Provinces Chapter Overview The study of bathymetry determines ocean depths and ocean floor topography. Echo sounding and satellites are efficient bathymetric tools. Most ocean floor features

More information

Plate Tectonics Lab II: Background Information

Plate Tectonics Lab II: Background Information Plate Tectonics Lab II: Background Information This lab is based on a UW ESS101 Lab. Note: Hand in only the Answer Sheet at the back of this guide to your Instructor Introduction One of the more fundamental

More information

Citizenship Japan Status in Canada Permanent resident. Gender Female Languages English and Japanese

Citizenship Japan Status in Canada Permanent resident. Gender Female Languages English and Japanese Curriculum Vitae Ikuko Wada Postdoctoral Associate Department of Geosciences Virginia Polytechnic Institute and State University 4044 Derring Hall, Blacksburg VA 24060 USA Phone: 540.231.7855 E-mail: iwada@whoi.edu

More information

Plate Tectonics Tutoiral. Questions. Teacher: Mrs. Zimmerman. Plate Tectonics and Mountains Practice Test

Plate 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 information

Hydrothermal Vent Challenge

Hydrothermal Vent Challenge 2004 Ring of Fire Expedition Hydrothermal Vent Challenge FOCUS Chemistry of hydrothermal vents GRADE LEVEL 9-12 (Chemistry) FOCUS QUESTION What are common features of hydrothermal vent fluids, and how

More information

The Structure of the Earth and Plate Tectonics

The Structure of the Earth and Plate Tectonics The Structure of the Earth and Plate Tectonics Agree or Disagree? 1. The Earth if made up of 4 different layers. 2. The crust (where we live) can be made of either less dense continental crust or the more

More information

Plate Tectonics: A Scientific Revolution Unfolds

Plate Tectonics: A Scientific Revolution Unfolds Chapter 2 Lecture Earth: An Introduction to Physical Geology Eleventh Edition Plate Tectonics: A Scientific Revolution Unfolds Tarbuck and Lutgens From Continental Drift to Plate Tectonics Prior to the

More information

General Geology - GEOL 1113 Section 005

General Geology - GEOL 1113 Section 005 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 Office Phone: 575-7295 Class Web Page http://comp.uark.edu/~mattioli/geol_1113.html

More information

GEOLOGY MEDIA SUITE Chapter 12

GEOLOGY MEDIA SUITE Chapter 12 UNDERSTANDING EARTH, SIXTH EDITION GROTZINGER JORDAN GEOLOGY MEDIA SUITE Chapter 12 Volcanoes 2010 W.H. Freeman and Company Plate tectonics explains the global pattern of volcanism. Key Figure 12.20 (page

More information

Layer Composition Thickness State of Matter

Layer Composition Thickness State of Matter Unit 4.2 Test Review Earth and Its Layers 1. Label the layers of the earth. oceanic crust continental crust lithosphere asthenosphere mantle outer core inner core 2. Complete the Following Table about

More information

104 CEOAS Admin Bldg Corvallis, OR Oregon State University (Corvallis, OR)

104 CEOAS Admin Bldg Corvallis, OR Oregon State University (Corvallis, OR) ANDREA M. ALLAN 104 CEOAS Admin Bldg aallan@coas.oregonstate.edu Corvallis, OR 97331 541-737-3427 EDUCATION Ph.D., August 2012 M.S., June 2007 B.S., May 2005 Geography, (Corvallis, OR) Analyzing the present

More information

GRANTED PROPOSALS 2013 CIDER mini-project: Energy dissipation of melt squirt. Role: PI.

GRANTED PROPOSALS 2013 CIDER mini-project: Energy dissipation of melt squirt. Role: PI. SONGQIAO SHAWN WEI EDUCATION Ph.D., Geophysics, Washington University, St. Louis, MO, USA, 2016 Dissertation: Seismic Studies of the Tonga Subduction Zone and the Lau Back-arc Basin Advisor: Douglas A.

More information

MAR110 Lecture #4 Fundamentals of Plate Tectonics

MAR110 Lecture #4 Fundamentals of Plate Tectonics 1 MAR110 Lecture #4 Fundamentals of Plate Tectonics The Ocean Sea Floor is formed Along the Mid-Ocean Ridge Spreading Centers The Ocean Sea Floor is destroyed in the Subduction Zones Figure 4.2 Convection

More information

Marine Science and Oceanography

Marine 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 information

Plate Tectonics. entirely rock both and rock

Plate 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 information

Practice Questions: Plate Tectonics

Practice Questions: Plate Tectonics Practice Questions: Plate Tectonics 1. Base your answer to the following question on The block diagram below shows the boundary between two tectonic plates. Which type of plate boundary is shown? A) divergent

More information

Before Plate Tectonics: Theory of Continental Drift

Before 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 information

Introduction to Oceanography

Introduction to Oceanography Introduction to Oceanography Lecture 7: Plate Tectonics 3 Landers earthquake fault scarp, California, Photo by G. Peltzer (UCLA/JPL/NASA), courtesy JPL, http://www-radar.jpl.nasa.gov/sect323/insar4crust/landers_co_fig1.jpg

More information

Directed Reading. Section: Volcanoes and Plate Tectonics

Directed Reading. Section: Volcanoes and Plate Tectonics Skills Worksheet Directed Reading Section: Volcanoes and Plate Tectonics 1. What can cause some of the most dramatic changes to Earth s surface? a. solar activity b. tides c. geysers d. volcanic eruptions

More information

Remote Sensing of the Earth s Interior

Remote Sensing of the Earth s Interior Remote Sensing of the Earth s Interior Earth s interior is largely inaccessible Origin and Layering of the Earth: Geochemical Perspectives Composition of Earth cannot be understood in isolation Sun and

More information

General Oceanography Geology 105 Expedition 8 Plate Boundaries Beneath the Sea Complete by Thursday at 11:00 PM

General Oceanography Geology 105 Expedition 8 Plate Boundaries Beneath the Sea Complete by Thursday at 11:00 PM General Oceanography Geology 105 Expedition 8 Plate Boundaries Beneath the Sea Complete by Thursday at 11:00 PM Name Expedition Objectives Learn about the types of plate boundaries and their key characteristics

More information

ANOTHER MEXICAN EARTHQUAKE! Magnitude 7.1, Tuesday Sept. 19, 2017

ANOTHER MEXICAN EARTHQUAKE! Magnitude 7.1, Tuesday Sept. 19, 2017 ANOTHER MEXICAN EARTHQUAKE! Magnitude 7.1, Tuesday Sept. 19, 2017 Why is there no oceanic crust older than 200 million years? SUBDUCTION If new oceanic crust is being continuously created along the earth

More information

3. PLATE TECTONICS LAST NAME (ALL IN CAPS): FIRST NAME: PLATES

3. PLATE TECTONICS LAST NAME (ALL IN CAPS): FIRST NAME: PLATES LAST NAME (ALL IN CAPS): FIRST NAME: PLATES 3. PLATE TECTONICS The outer layers of the Earth are divided into the lithosphere and asthenosphere. The division is based on differences in mechanical properties

More information

The Ocean Floor Earth Science, 13e Chapter 13

The Ocean Floor Earth Science, 13e Chapter 13 The Ocean Floor Earth Science, 13e Chapter 13 Stanley C. Hatfield Southwestern Illinois College The vast world ocean Earth is often referred to as the blue planet Seventy-one percent of Earth s surface

More information

In order to study Plate Tectonics, we must first

In order to study Plate Tectonics, we must first TB Chapter 13 In order to study Plate Tectonics, we must first reorganize our layering system for the Earth: Old System 4 layers Crust (rigid) id) (rigid) Mantle (putty like) (semi rigid) Outer core (liquid)

More information

Plate Tectonics. By Destiny, Jarrek, Kaidence, and Autumn

Plate Tectonics. By Destiny, Jarrek, Kaidence, and Autumn Plate Tectonics By Destiny, Jarrek, Kaidence, and Autumn .The Denali Fault and San Andreas Fault - The San Andreas Fault is a continental transform fault that extends roughly 1300 km (810 miles) through

More information

Subduction zones 3 arc magmatism

Subduction zones 3 arc magmatism 5. 3 Subduction zones 3 arc magmatism Where can we observe magmatic/volcanic activities along subduction zones? Characteristics of arc magmatism (vs. mid-ocean ridge/intraplate magmatism) Structure of

More information

12/3/2014. Plate Tectonics: A Scientific Revolution Unfolds Earth Science, 13e Chapter 7. Continental drift: an idea before its time

12/3/2014. Plate Tectonics: A Scientific Revolution Unfolds Earth Science, 13e Chapter 7. Continental drift: an idea before its time Plate Tectonics: A Scientific Revolution Unfolds Earth Science, 13e Chapter 7 Stanley C. Hatfield Southwestern Illinois College Continental drift: an idea before its time Alfred Wegener First proposed

More information

Full file at

Full file at Essentials of Oceanography, 10e (Trujillo/Keller) Chapter 2 Plate Tectonics and the Ocean Floor Match the term with the appropriate phrase. You may use each answer once, more than once or not at all. A)

More information

Lecture 24 Hawaii. Hawaii

Lecture 24 Hawaii. Hawaii Lecture 24 Hawaii Friday, April 22 nd 2005 Hawaii The Hawaiian Islands, in the middle of the Pacific Ocean, are volcanic islands at the end of a long chain of submerged volcanoes. These volcanoes get progressively

More information

Mantle geochemistry: How geochemists see the deep Earth

Mantle geochemistry: How geochemists see the deep Earth Geochemistry: Overview: the geochemist's Earth (reservoirs, budgets and processes) Mantle geochemistry: How geochemists see the deep Earth Don DePaolo/Stan Hart CIDER - KITP Summer School Lecture #1, July

More information

The Nature of Igneous Rocks

The Nature of Igneous Rocks The Nature of Igneous Rocks Form from Magma Hot, partially molten mixture of solid liquid and gas Mineral crystals form in the magma making a crystal slush Gases - H 2 O, CO 2, etc. - are dissolved in

More information

FORCES ON EARTH. An investigation into how Newton s Laws of Motion are applied to the tectonic activity on Earth.

FORCES ON EARTH. An investigation into how Newton s Laws of Motion are applied to the tectonic activity on Earth. FORCES ON EARTH An investigation into how Newton s Laws of Motion are applied to the tectonic activity on Earth. GEOLOGY Geologists scientists who study the forces that make and shape the Earth Geologists

More information

12. The diagram below shows the collision of an oceanic plate and a continental plate.

12. The diagram below shows the collision of an oceanic plate and a continental plate. Review 1. Base your answer to the following question on the cross section below, which shows the boundary between two lithospheric plates. Point X is a location in the continental lithosphere. The depth

More information

Earth Science Lesson 3 Dynamic Earth Processes (Grades 8-12 ) Instruction 3-3 Plate Boundaries

Earth Science Lesson 3 Dynamic Earth Processes (Grades 8-12 ) Instruction 3-3 Plate Boundaries As we told you in a recent Instruction, much of the Earth's lithosphere (its Crust and the top layer of its Outer Mantle) is made up of moving masses of rock called tectonic plates (tectonic means moving).

More information

Early Career Scientists/Student Introduction. Part II

Early Career Scientists/Student Introduction. Part II Early Career Scientists/Student Introduction Part II Jeffrey Marlow // 4 th year (already?) grad student // Caltech Anaerobic Methane Oxidation Endolithic Activity & Community Diversity Methane Seep Proteomics

More information

A) 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?

A) 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 information

Tectonic Forces Simulation: Volcanoes Activity One

Tectonic Forces Simulation: Volcanoes Activity One Tectonic Forces Simulation: Volcanoes Activity One Introduction Volcanoes form above vents or cracks in the earth's crust. When a volcano erupts, magma is forced up through the cracks - sending lava, ash,

More information

Lecture 4.1 Continental Drift

Lecture 4.1 Continental Drift Plate Tectonics Chapter 4 California Science Content Standards Covered: Big Ideas 3A: Students know the features of the ocean floor that provide evidence of plate tectonics Mid Ocean Ridges (ex. Mid Atlantic

More information

An Introduction to the Seafloor and Plate Tectonics 1

An Introduction to the Seafloor and Plate Tectonics 1 An Introduction to the Seafloor and Plate Tectonics 1 Objectives 1) Investigate the components of the lithosphere and lithospheric plates. 2) Identify the associations among various seafloor features,

More information

Mantle Wedge Oxygen Fugacity Katherine A. Kelley Graduate School of Oceanography, Univ. of Rhode Island

Mantle Wedge Oxygen Fugacity Katherine A. Kelley Graduate School of Oceanography, Univ. of Rhode Island Mantle Wedge Oxygen Fugacity Katherine A. Kelley Graduate School of Oceanography, Univ. of Rhode Island With contributions from: M. Brounce GSO/URI E. Cottrell & O. Lopez Smithsonian Inst. J. Warren &

More information

5. Convergent boundaries produce a relatively low number of earthquakes compared to other boundaries. a. True

5. Convergent boundaries produce a relatively low number of earthquakes compared to other boundaries. a. True 1. Earth s crust is thinner than its mantle. ANSWER: True 2. The concept of isostacy states that high-density rock will stand higher than low-density rock, which explains the formation of subduction zones.

More information

FORCES ON EARTH UNIT 3.2. An investigation into how Newton s Laws of Motion are applied to the tectonic activity on Earth.

FORCES ON EARTH UNIT 3.2. An investigation into how Newton s Laws of Motion are applied to the tectonic activity on Earth. FORCES ON EARTH UNIT 3.2 An investigation into how Newton s Laws of Motion are applied to the tectonic activity on Earth. USE THESE NOTES: OUR HOME PLANET EARTH: What do you know about our planet? SO.HOW

More information

BS degrees awarded by race/ethnicity 2014

BS degrees awarded by race/ethnicity 2014 BS degrees awarded by race/ethnicity 2014 Race or Ethnicity % of population Ocean Science BS (%) Earth Science BS (%) White 62.1 80 80 Hispanic 17.4 6.8 7.7 Black 12.4 3.2 2.1 Asian 5.3 6.8 3.3 Am. Indian/

More information

Review participation point: The evidence for a fluid outer core is:

Review 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 information

Continental Drift. & Plate Tectonics

Continental Drift. & Plate Tectonics Continental Drift & Plate Tectonics Alfred Wegener, a German scientist, proposed the hypothesis of CONTINENTAL DRIFT, in 1912. Hypothesis stated: All Earth s continents were once a single landmass (Pangaea)

More information

Geology 300, Physical Geology Spring 2019 Quiz Ch 19, Plate Tectonics Name

Geology 300, Physical Geology Spring 2019 Quiz Ch 19, Plate Tectonics Name Geology 300, Physical Geology Spring 2019 Quiz Ch 19, Plate Tectonics Name MULTIPLE CHOICE. Choose the one alternative that best completes the statement or answers the question. 1) The portion of a fracture

More information

Bradford Scott Barrett

Bradford Scott Barrett Bradford Scott Barrett ADDRESSES: United States Austria School of Meteorology Wegener Center for Climate Change University of Oklahoma 25 Leechgasse 120 David L. Boren Blvd. #5900 A-8010 Graz AUSTRIA Norman,

More information

Yanbu University College. General Studies Department. PHSC001 Course. Chapter9 (Basic Geology: Earthquakes and volcanoes ) Worksheet Solutions

Yanbu University College. General Studies Department. PHSC001 Course. Chapter9 (Basic Geology: Earthquakes and volcanoes ) Worksheet Solutions Yanbu University College General Studies Department PHSC001 Course Chapter9 (Basic Geology: Earthquakes and volcanoes ) Worksheet Solutions Phsc001 worksheet9 solutions, yuc Page 1-6 Chapter 9 worksheet

More information

Chapter 2 Plate Tectonics and the Ocean Floor

Chapter 2 Plate Tectonics and the Ocean Floor Chapter 2 Plate Tectonics and the Ocean Floor Matching. Match the term or person with the appropriate phrase. You may use each answer once, more than once or not at all. 1. hydrothermal vents A. convergent

More information

Plate Tectonics: The New Paradigm

Plate Tectonics: The New Paradigm Earth s major plates Plate Tectonics: The New Paradigm Associated with Earth's strong, rigid outer layer: Known as the lithosphere Consists of uppermost mantle and overlying crust Overlies a weaker region

More information

Lab 1: Plate Tectonics April 2, 2009

Lab 1: Plate Tectonics April 2, 2009 Name: Lab 1: Plate Tectonics April 2, 2009 Objective: Students will be introduced to the theory of plate tectonics and different styles of plate margins and interactions. Introduction The planet can be

More information

Ocean Dynamics Marine Ecosystem Dynamics Climate Nonlinear Science

Ocean Dynamics Marine Ecosystem Dynamics Climate Nonlinear Science François Ascani University of Hawaii at Manoa Department of Oceanography 1000 Pope Rd Honolulu, HI 96822 French and US citizenship (808) 956-9505 (Work) (808) 225-1719 (Cell) fascani@hawaii.edu Research

More information

Endogene processes and landforms NGEA01, 2018

Endogene processes and landforms NGEA01, 2018 Endogene processes and landforms NGEA01, 2018 Cecilia Akselsson Department of Physical Geography and Ecosystem Science Lund University Endogene and exogene processes () Endogene/Internal/Constructive/Ulifting

More information

The Structure of the Earth and Plate Tectonics

The Structure of the Earth and Plate Tectonics The Structure of the Earth and Plate Tectonics Structure of the Earth The Earth is made up of 4 main layers: Inner Core Outer Core Mantle Crust Crust Mantle Outer core Inner core The Crust This is where

More information

Structure of the Earth and the Origin of Magmas

Structure of the Earth and the Origin of Magmas Page 1 of 12 EENS 2120 Petrology Tulane University Prof. Stephen A. Nelson Structure of the Earth and the Origin of Magmas This document last updated on 23-Jan-2015 Magmas do not form everywhere beneath

More information

Modified by E. Schauble, from image at

Modified by E. Schauble, from image at Introduction to Oceanography Lecture 7: Plate Tectonics 3 Introduction to Oceanography Incipient divergent plate boundary, Afar, Ethiopia/Eritrea Landers earthquake fault scarp, California, Photo by G.

More information

Crustal Activity. Plate Tectonics - Plates - Lithosphere - Asthenosphere - Earth s surface consists of a major plates and some minor ones

Crustal 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 information

Plate Boundaries & Resulting Landforms

Plate Boundaries & Resulting Landforms Plate Boundaries & Resulting Landforms Divergent Plate Boundaries (plates being pulled apart) Type: oceanic plates Description: rising magma gently lifts the crust creating a ridge. The flow of convection

More information

Geology of the Hawaiian Islands

Geology of the Hawaiian Islands Geology of the Hawaiian Islands Class 4 22 January 2004 Turn in Homework #1 Any Questions? IMPORTANT Big Island Field Trip We need a $162 payment for airfare BEFORE January 29 th Description of logistics,

More information

SEA-FLOOR SPREADING. In the 1950 s and early 1960 s detailed study of the oceans revealed the following surprising information:-

SEA-FLOOR SPREADING. In the 1950 s and early 1960 s detailed study of the oceans revealed the following surprising information:- SEA-FLOOR SPREADING In the 1950 s and early 1960 s detailed study of the oceans revealed the following surprising information:- Detailed bathymetric (depth) studies showed that there was an extensive submarine

More information

TRACE ELEMENTS IN MAGMAS

TRACE ELEMENTS IN MAGMAS TRACE ELEMENTS IN MAGMAS A Theoretical Treatment Studying the distribution of certain elements, present in very low concentrations in igneous and metamorphic rocks, can yield important clues about the

More information

Anne-Sofie Crüger Ahm

Anne-Sofie Crüger Ahm Anne-Sofie Crüger Ahm Carlsberg Foundation Postdoctoral Fellow ascahm@gmail.com Princeton University aahm@princeton.edu Department of Geosciences, Guyot Hall ORCID: 0000-0002-5142-0326 Princeton, NJ 08544,

More information

Lecture 25 Subduction Related Magmatism

Lecture 25 Subduction Related Magmatism Lecture 25 Subduction Related Magmatism Monday, May 2 nd 2005 Subduction Related Magmatism Activity along arcuate volcanic chains along subduction zones Distinctly different from the mainly basaltic provinces

More information

Do NOT open the test until instructed to do so.

Do NOT open the test until instructed to do so. Raw Score: Rank: School: Team Number: Names: Boyceville Invitational, December 2, 2017 Dynamic Planet Plate Tectonics and Geographical Impacts Do NOT open the test until instructed to do so. 2011 Tohoku

More information

Full file at

Full file at Chapter 2 PLATE TECTONICS AND PHYSICAL HAZARDS MULTIPLE-CHOICE QUESTIONS 1. What direction is the Pacific Plate currently moving, based on the chain of Hawaiian Islands with only the easternmost island

More information

APPLICATIONS OF ISOTOPES TO IGNEOUS PETROGENESIS

APPLICATIONS OF ISOTOPES TO IGNEOUS PETROGENESIS APPLICATIONS OF ISOTOPES TO IGNEOUS PETROGENESIS Elisabeth Widom Miami University, Oxford, Ohio, USA Keywords: cosmogenic nuclides, crustal recycling, decay series, fractionation, igneous petrology, isochron,

More information

OBJECTIVE: For each boundary type, give an example of where they occur on Earth.

OBJECTIVE: For each boundary type, give an example of where they occur on Earth. OBJECTIVE: Explain the theory of Plate Tectonics. COMPARE AND CONTRAST DIVERGENT, CONVERGENT AND TRANSFORM BOUNDARIES. ***very important. Describe what geologic features form at each of the three CONVERGENT

More information

GEOSCIENCE 105 THE DYNAMIC EARTH FIRST ONE-HOUR EXAMINATION. Tuesday, October 20, 1998 NAME STUDENT #

GEOSCIENCE 105 THE DYNAMIC EARTH FIRST ONE-HOUR EXAMINATION. Tuesday, October 20, 1998 NAME STUDENT # GEOSCIENCE 105 THE DYNAMIC EARTH FIRST ONE-HOUR EXAMINATION Tuesday, October 20, 1998 NAME STUDENT # Instructions: 1. Answer all questions legibly. 2. Put your name and student number on this front page.

More information