DESIGN & IMPLEMENATION WORKSHOP. Conceptual Network Design For The Regional Cabled Observatory

Size: px
Start display at page:

Download "DESIGN & IMPLEMENATION WORKSHOP. Conceptual Network Design For The Regional Cabled Observatory"

Transcription

1 DESIGN & IMPLEMENATION WORKSHOP Conceptual Network Design For The Regional Cabled Observatory

2 50 N N4 N10 N11 N7 N8 N5 N9 N6 AN INTEGRATED RCO Maintain Integrity of a Plate-Scale Experiment & Future Expandability Optimize Early Return by Rapid Augmentation of Stage N N2 N1 N3 130 W 125 W

3 Potential for Integrating Climate, Biogeochemical and Marine Ecosystem Processes at Global to Coastal Scales Subarctic Current Alaska Gyre Alaska Current West Wind Drift Southern California Bight Central Pacific Gyre California Current

4 50 N ORION-RCO & West Coast N10 N11 N7 N8 N9 What linkages exist between carbon fluxes and climate forcing in adjacent coastal and regional regimes? West Wind Drift N5 N6 warm phase cool phase N4 45 N N2 N1 N3 California PDO &ENSO Coastal recommends surface moorings Ocean Biogeochemical, Climate Moorings 130 W 125 W

5 SEISMICITY & DEFORMATION A Plate-Scale Observatory For Seismology & Geodynamics of the Pacific Northwest Earthquakes, Physics, & Fault Mechanics Observatory on the Blanco Transform Fault Seismic and Geodetic Observations Along the Cascadia Continental Margin A Cabled Observatory on the Juan de Fuca Ridge Seismometers

6 Transformational Science with the Integrated OOI Subarctic Current West Wind Drift Alaska Gyre Alaska Current Tectonic plates are the fundamental building block of our planet. Central Pacific Gyre What are the interrelated processes that California control the formation, evolution and destruction of plates Currentand their interaction with the continents?

7 Papa

8 RCO and Earthscope Plate Boundary Observatory What is the structure and interaction between plate subduction and the over-riding continent? NA Plate

9 Crustal Strain, Hydrogeology, and the Biosphere Highest Density of ODP Holes thermistors, pressure sensors, ± seismometer packer ODP-IODP Corks microbial-fluid samplers

10 Plate-Scale Response to Seismic Events: Largest Fractured Aquifer 857D Davis et al., 2001 JGR Events/hr Pressure (kpa) Pressure transients ODP Observatories D Earthquakes from SOSUS M = Time (Days)

11 A. Fisher & N. Rager ORION RCO What is the magnitude and variability of plate-tectonically forced fluxes from the ocean crust into the overlying ocean? Hydrothermal Breathing Holes Ridge flanks account for 70-80% of the heat flux Chemical fluxes may be significant Ridge flanks 1-65 Ma make up 70% of ocean basins Potentially enormous habitable volume on a global scale Driving hypothesis: Where there is fluid circulation, there is microbial activity

12 METHANE HYDRATES Global Carbon Cycle, Biosphere, Climate Change, Hazards A Northeast Pacific Hydrate Observatory System (NEPHOS) at South Hydrate Ridge 1250 m Borehole Observations for Sustained Time-Series Observations: Hydrogeology, Geobiology, Plate-Scale Strain

13 Earths Carbon Reserves: Importance of methane hydrates Depth (m) BSR dissolved organic matter m terrestrial biosphere 830 Hydrate Ridge Leg 204 soils 1,400 detritial org. peat carbon fossil fuels (coal, oil, natural gas) 5,000 atmosphere3.6 marine biosphere gas hydrate (marine & terrestrial) 10,000 quantities in gigatons of carbon

14 Linkages Between Crustal Formation and Life

15 50 N 45 N N10 N11 N7 N8 N5 N4 N2 N3 N9 N6 N1 Priorities Maintain Integrity of a Plate-Scale Experiment & Future Expandability Node design optimizes largest component of interdisciplinary science Ideally include Gorda connection (strong water column and geophysical drivers), and Cleft (geophysical-hydrothermal) MARS is the test bed for Stage W 125 W Optimize early return by rapid augmentation of Stage 1. ~ 4X cheaper

16 DESIGN & IMPLEMENATION WORKSHOP Over All Recommendations Con t: Early mapping is critical for site characterization and route planning Engineering evaluate cost/reliability for connection of Stage 1 and 2 Prioritization of backbone cable, branching units, and primary nodes, secondary infrastructure Need for real estate management (cables, acoustic interaction etc) MARS and Stage 2 must be interoperable; goal for similar compatibility with Stage 1

17 DESIGN & IMPLEMENATION WORKSHOP ORION office establish mechanism for community interaction via the internet, updates, lists Maintain integrity of full plate scale experiment Investigate accommodation of cable route to southeast toward Gorda Plate Ridge community needs to evaluate Cleft site/phasing Core instrumentation for profiler moorings? - more mooring with no instruments and fewer moorings with core suite of instrumentation Establish close coordination with Coastal Group Engineering and CI needs to define interfaces and dependences between CI and the RCO

DESIGN & IMPLEMENATION WORKSHOP. Conceptual Network Design For The Regional Cabled Observatory

DESIGN & IMPLEMENATION WORKSHOP. Conceptual Network Design For The Regional Cabled Observatory DESIGN & IMPLEMENATION WORKSHOP Conceptual Network Design For The Regional Cabled Observatory DESIGN & IMPLEMENATION WORKSHOP Planning for a 30-year Experiment A design allowing future expansion is critical

More information

Fluid-Rock Interactions and the Sub-Seafloor Biosphere

Fluid-Rock Interactions and the Sub-Seafloor Biosphere Fluid-Rock Interactions and the Sub-Seafloor Biosphere BACKGROUND DATA Examples of Key Scientific Questions (OOI Science Plan) Scientific Priorities (San Juan Meeting) Example ORION Experiments (San Juan

More information

Ocean-Atmosphere Fluxes & Marine Meteorology

Ocean-Atmosphere Fluxes & Marine Meteorology Ocean-Atmosphere Fluxes & Marine Meteorology Breakout Group Questions How can the CND be enhanced to better address this science theme? What other approaches could be combined with the observatory elements

More information

Telepresence In The Ocean

Telepresence In The Ocean The Ocean Observatories Initiative: Establishing A Sustained And Adaptive Telepresence In The Ocean Shelby Walker (1) (1) National Oceanic and Atmospheric Administration, Office of Oceanic and Atmospheric

More information

Announcements. Manganese nodule distribution

Announcements. Manganese nodule distribution Announcements Lithospheric plates not as brittle as previously thought ESCI 322 Meet in Env. Studies Bldg Rm 60 at 1 PM on Tuesday One week (Thursday): Quiz on Booth 1994 and discussion. (Lots of odd terms

More information

CGSN Overview. GSN Sites CSN Sites Shore Facilities

CGSN Overview. GSN Sites CSN Sites Shore Facilities GSN Sites CSN Sites Shore Facilities CGSN Overview Coastal Pioneer Array Endurance Array Global Irminger Sea Southern Ocean Station Papa Fixed assets Surface mooring Subsurface mooring Mobile assets Ocean

More information

Earth s Magnetic Field Differential Rotation between the inner core and the outer core.

Earth s Magnetic Field Differential Rotation between the inner core and the outer core. Geology 15 Lecture 7 Schedule: Hazard Update: Review Lecture 6 Activity 2 cont: Plate Boundaries and Their Motions Cover Material/Objectives Plate Tectonics (continued) Earth s Structure Evidence for Continental

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

A Science Reader s Guide to CORKS

A Science Reader s Guide to CORKS A Science Reader s Guide to CORKS Readings from Ocean Drilling Program Highlights Teaching for Science Learning for Life TM www.deepearthacademy.org Introduction CORKS first caught my imagination because

More information

Ocean Observatories: Evolution and Future Directions Steven G. Ackleson Consortium for Ocean Leadership Washington, DC

Ocean Observatories: Evolution and Future Directions Steven G. Ackleson Consortium for Ocean Leadership Washington, DC Ocean Observatories Initiative Ocean Observatories: Evolution and Future Directions Steven G. Ackleson Consortium for Ocean Leadership Washington, DC sackleson@oceanleadership.org O cean Ob serv a to ry

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

SIO 226: Introduction to Marine Geophysics

SIO 226: Introduction to Marine Geophysics SIO 226: Introduction to Marine Geophysics Plate Tectonics Dave Chadwell Plate Tectonics, Sea-Floor Spreading and Continental Drift Main Parody Plate Geography Lineated Magnetic Anomalies in the Oceanic

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

COMPOSITION and PHYSICAL PROPERTIES GENERAL SUBJECTS. GEODESY and GRAVITY

COMPOSITION and PHYSICAL PROPERTIES GENERAL SUBJECTS. GEODESY and GRAVITY COMPOSITION and PHYSICAL PROPERTIES Composition and structure of the continental crust Composition and structure of the core Composition and structure of the mantle Composition and structure of the oceanic

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

Numerical modelling: The governing equation used in this study is: (K T ) c T H 0,

Numerical modelling: The governing equation used in this study is: (K T ) c T H 0, GSA DATA REPOSITORY 2012254 Cozzens and Spinelli Numerical modelling: The governing equation used in this study is: (K T ) c T H 0, where K is thermal conductivity, T is temperature, ρ is density, c is

More information

Seismological laboratory in Agua Negra tunnel

Seismological laboratory in Agua Negra tunnel Instituto Geofísico Sismológico Volponi Universidad Nacional de San Juan Seismological laboratory in Agua Negra tunnel Buenos Aires, Abril 2011 Why a Seismological laboratory in Agua Negra tunnel? Earthquake

More information

In 1912 Alfred Wegener proposed Continental Drift the continents have moved over time the continents were part of one giant landmass named Pangaea.

In 1912 Alfred Wegener proposed Continental Drift the continents have moved over time the continents were part of one giant landmass named Pangaea. Plate Tectonics In 1912 Alfred Wegener proposed Continental Drift the continents have moved over time the continents were part of one giant landmass named Pangaea. Pangaea Landmass movements over millions

More information

Continental Drift. Wegener theory that the crustal plates are moving and once were a super continent called Pangaea.

Continental Drift. Wegener theory that the crustal plates are moving and once were a super continent called Pangaea. PLATE TECTONICS WHAT IS TECTONICS? Tectonism is the faulting or folding or other deformation of the outer layer of a planet. It happens very slowly, on the scale of millions of years. Tectonic activity

More information

Applications of Cabled Observatories to Earthquake and Tsunami Research and Early Detection: Experience from Canada and Europe.

Applications of Cabled Observatories to Earthquake and Tsunami Research and Early Detection: Experience from Canada and Europe. Applications of Cabled Observatories to Earthquake and Tsunami Research and Early Detection: Experience from Canada and Europe. Dr. Mairi Best, Founding Associate Director Science, NEPTUNE Canada Ocean

More information

Activity Pacific Northwest Tectonic Block Model

Activity Pacific Northwest Tectonic Block Model Activity Pacific Northwest Tectonic Block Model The Cascadia tectonic margin is caught between several tectonic forces, during the relentless motions of the giant Pacific Plate, the smaller subducting

More information

Earth s Tectonic Plates

Earth s Tectonic Plates MASTER 49 6.2 3.7 5.4 Philippine Pacific 5.4 North American Juan de Fuca Caribbean Cocos 10.0 9.2 2.3 2.5 2.3 1.8 3.0 Indian-Australian 10.5 7.1 17.2 16.8 6.0 Nazca South American 11.1 10.3 7.3 3.7 7.5

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

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

SM2.1/GD2.7/NH5.8/TS8.4, Large Earthquake and Tsunami Activity (co-organized), 13:30 17:00, Room B3

SM2.1/GD2.7/NH5.8/TS8.4, Large Earthquake and Tsunami Activity (co-organized), 13:30 17:00, Room B3 SM Seismology Orals and PICOs MO1, 08:30 10:00 MO2, 10:30 12:00 MOL, 12:15 13:15 MO3, 13:30 15:00 MO4, 15:30 17:00 TU1, 08:30 10:00 Monday, 08 April SM1.2/AS4.13, Research and Development in Nuclear Explosion

More information

Magnitude 7.9 SE of KODIAK, ALASKA

Magnitude 7.9 SE of KODIAK, ALASKA A magnitude 7.9 earthquake occurred at 12:31 am local time 181 miles southeast of Kodiak at a depth of 25 km (15.5 miles). There are no immediate reports of damage or fatalities. Light shaking from this

More information

Evidence from the Surface. Chapter 02. Continental Drift. Fossil Evidence for Pangaea. Seafloor Spreading. Seafloor Spreading 1/31/2012

Evidence from the Surface. Chapter 02. Continental Drift. Fossil Evidence for Pangaea. Seafloor Spreading. Seafloor Spreading 1/31/2012 Evidence from the Surface Surface landforms Continental shelf and slope Abyssal Plane Mid-oceanic ridge Oceanic Trenches Chapter 02 Continental Drift Continental Drift - a hypothesis that the continents

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

Earth and Space Science Semester 2 Exam Review. Part 1. - Convection currents circulate in the Asthenosphere located in the Upper Mantle.

Earth and Space Science Semester 2 Exam Review. Part 1. - Convection currents circulate in the Asthenosphere located in the Upper Mantle. Earth and Space Science 2015 Semester 2 Exam Review Part 1 Convection -A form of heat transfer. - Convection currents circulate in the Asthenosphere located in the Upper Mantle. - Source of heat is from

More information

RAYMOND SIEVER Harvard University

RAYMOND SIEVER Harvard University E A R T H FOURTH EDITION FRANK PRESS National Academy of Sciences RAYMOND SIEVER Harvard University W. H. Freeman and Company New York Preface xiii Acknowledgments xviii PART I PROLOGUE CHAPTER 1 HISTORY

More information

Continental Drift to Plate Tectonics: From Hypothesis to Theory

Continental Drift to Plate Tectonics: From Hypothesis to Theory Continental Drift to Plate Tectonics: From Hypothesis to Theory 1 Key Understandings Internal structure of the earth/structure of the crust. Difference between continental drift & plate tectonics. Evidence

More information

Overview of Geoscience Employers Workshop Outcomes

Overview of Geoscience Employers Workshop Outcomes Overview of Geoscience Employers Workshop Outcomes General thoughts on concepts: From Geoscience Employers Workshop Systems Thinking How systems work and interact Processes Atmosphere: Climate, Weather,

More information

Global Tectonics. Kearey, Philip. Table of Contents ISBN-13: Historical perspective. 2. The interior of the Earth.

Global Tectonics. Kearey, Philip. Table of Contents ISBN-13: Historical perspective. 2. The interior of the Earth. Global Tectonics Kearey, Philip ISBN-13: 9781405107778 Table of Contents Preface. Acknowledgments. 1. Historical perspective. 1.1 Continental drift. 1.2 Sea floor spreading and the birth of plate tectonics.

More information

Earth Systems Science Chapter 7. Earth Systems Science Chapter 7 11/11/2010. Seismology: study of earthquakes and related phenomena

Earth Systems Science Chapter 7. Earth Systems Science Chapter 7 11/11/2010. Seismology: study of earthquakes and related phenomena Earth Systems Science Chapter 7 I. Structure of the Earth II. Plate Tectonics The solid part of the earth system includes processes, just like the atmosphere and oceans. However, the time scales for processes

More information

The San Andreas Fault Observatory at Depth: Recent Site Characterization Studies and the 2.2-Km-Deep Pilot Hole

The San Andreas Fault Observatory at Depth: Recent Site Characterization Studies and the 2.2-Km-Deep Pilot Hole The San Andreas Fault Observatory at Depth: Recent Site Characterization Studies and the 2.2-Km-Deep Pilot Hole Steve Hickman and Bill Ellsworth (USGS) Mark Zoback (Stanford University) and the Pre-EarthScope

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

Tuesday, September 05, 2017 Planet Earth

Tuesday, September 05, 2017 Planet Earth Tuesday, September 05, 2017 Planet Earth Objective: Describe the solar system and Earth s location in it. Identify Earth s shape. Discuss Earth s structure. List Earth s landforms Do Now: What is a compass

More information

MAR110 Lecture #5 Plate Tectonics-Earthquakes

MAR110 Lecture #5 Plate Tectonics-Earthquakes 1 MAR110 Lecture #5 Plate Tectonics-Earthquakes Figure 5.0 Plate Formation & Subduction Destruction The formation of the ocean crust from magma that is upwelled into a pair of spreading centers. Pairs

More information

JAMSTEC Marine Geophysical Projects for Researches on Subduction Cycles and Deformation

JAMSTEC Marine Geophysical Projects for Researches on Subduction Cycles and Deformation JAMSTEC Marine Geophysical Projects for Researches on Subduction Cycles and Deformation Shuichi Kodaira Research Center for Earthquake and Tsunami JAMSTEC JAMSTEC Marine Geophysical Projects Motivation:

More information

The Two Types of Crust. Plate Tectonics. Physical Layers of the Earth. The Asthenosphere. The Lithosphere. Chemical Layers of the Earth

The Two Types of Crust. Plate Tectonics. Physical Layers of the Earth. The Asthenosphere. The Lithosphere. Chemical Layers of the Earth Plate Tectonics A Reminder of Earth s Structure Two physical units of Earth that are important too! How the Earth Works Plate Tectonics Plate Boundaries Chemical Layers of the Earth Crust - low density

More information

KECK REALTIME SEISMIC/GEODETIC BOREHOLE STATION. WHOI Ocean Bottom Seismograph Laboratory

KECK REALTIME SEISMIC/GEODETIC BOREHOLE STATION. WHOI Ocean Bottom Seismograph Laboratory KECK REALTIME SEISMIC/GEODETIC BOREHOLE STATION WHOI Ocean Bottom Seismograph Laboratory W.M. Keck Foundation Award to Design and Construct a Real-Time Borehole Seismic and Geodetic Observatory for Deployment

More information

RECONN. REgional Cabled Observatory Network (of Networks) Cabled Regional Observatory Workshop. Report of the. Held October 2003

RECONN. REgional Cabled Observatory Network (of Networks) Cabled Regional Observatory Workshop. Report of the. Held October 2003 RECONN REgional Cabled Observatory Network (of Networks) Report of the Cabled Regional Observatory Workshop Held October 2003 Ocean Observatories Initiative Ocean Observatories Initiative The National

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

SOCIAL STUDIES GENERAL

SOCIAL STUDIES GENERAL GEOGRAPHY, MILITARY Maps War - Greece and Turkey War - Greece and Turkey 1920-1922 (p1) 1920-1922 (p2) Dieppe (p1) Dieppe (p2) Dieppe (p3) Dieppe (p4) Dieppe (p5) 120 GEOGRAPHY, MILITARY Maps Allied advances

More information

BIOGEOCHEMICAL CYCLES

BIOGEOCHEMICAL CYCLES BIOGEOCHEMICAL CYCLES BASICS Biogeochemical Cycle: The complete path a chemical takes through the four major components, or reservoirs, of Earth s system (atmosphere, lithosphere, hydrosphere and biosphere)

More information

This is Planet Earth / Earth Story. Lecture 5 PLATE TECTONICS Drifting Continents, And Oceans That Open And Close

This is Planet Earth / Earth Story. Lecture 5 PLATE TECTONICS Drifting Continents, And Oceans That Open And Close This is Planet Earth / Earth Story Lecture 5 PLATE TECTONICS Drifting Continents, And Oceans That Open And Close Earth Structure The Lithosphere: Forms the outermost layer of the Earth. Consists of the

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

Dawn in the new millennium of oceanography: The Ocean Observatories Initiative

Dawn in the new millennium of oceanography: The Ocean Observatories Initiative Dawn in the new millennium of oceanography: The Ocean Observatories Initiative OOI will provide scientists an enduring in situ infrastructure to study episodic events in extreme ocean environments. Oceans

More information

General Oceanography Geology 105 Expedition 10 - Whole Lotta Shakin' Goin' On

General Oceanography Geology 105 Expedition 10 - Whole Lotta Shakin' Goin' On General Oceanography Geology 105 Expedition 10 - Whole Lotta Shakin' Goin' On Name Not attempting to answer questions on expeditions will result in point deductions on course workbook (two or more blank

More information

Moho (Mohorovicic discontinuity) - boundary between crust and mantle

Moho (Mohorovicic discontinuity) - boundary between crust and mantle Earth Layers Dynamic Crust Unit Notes Continental crust is thicker than oceanic crust Continental Crust Thicker Less Dense Made of Granite Oceanic Crust Thinner More Dense Made of Basalt Moho (Mohorovicic

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

THE DYNAMICS AND SIGNIFICANCE OF FLUIDS WITHIN THE SEAFLOOR

THE DYNAMICS AND SIGNIFICANCE OF FLUIDS WITHIN THE SEAFLOOR THE DYNMICS ND SIGNIFICNCE OF FLUIDS WITHIN THE SEFLOOR.T. Fisher Center for the Study of Imaging and Dynamics of the Earth, and Department of Earth Sciences University of California, Santa Cruz INTRODUCTION

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

DOWNLOAD OR READ : SHALLOW SUBDUCTION ZONES SEISMICITY MECHANICS AND SEISMIC POTENTIAL PDF EBOOK EPUB MOBI

DOWNLOAD OR READ : SHALLOW SUBDUCTION ZONES SEISMICITY MECHANICS AND SEISMIC POTENTIAL PDF EBOOK EPUB MOBI DOWNLOAD OR READ : SHALLOW SUBDUCTION ZONES SEISMICITY MECHANICS AND SEISMIC POTENTIAL PDF EBOOK EPUB MOBI Page 1 Page 2 shallow subduction zones seismicity mechanics and seismic potential shallow subduction

More information

is a unifying theme in modern geology that integrates the earlier ideas of

is a unifying theme in modern geology that integrates the earlier ideas of The concept of Global Plate Tectonics is a unifying theme in modern geology that integrates the earlier ideas of continental drift, sea-floor spread, and mountain building To explain why the present ocean

More information

Geology 101 Study Guide #4

Geology 101 Study Guide #4 Geology 101 Study Guide #4 Our last unit is the study of the earthquakes, the Earth s interior and plate tectonics. We live in a region which has been added on to North America through plate tectonics.

More information

Subject Classification

Subject Classification Istituto Nazionale di Geofisica e Vulcanologia earth-prints home page roma library bologna library catania library milano library napoli library palerm Subject Classification Earth-prints organize its

More information

Earth. Properties of Earth. Earth's Interior. Earth is the planet that we know best

Earth. Properties of Earth. Earth's Interior. Earth is the planet that we know best Earth Earth is the planet that we know best Our observations of the other planets are all compared to the conditions and properties of Earth Properties of Earth Semimajor Axis Orbital Eccentricity Orbital

More information

Plate Tectonics. 1)The plate tectonic system 2)A theory is born 3) Early evidence for continental drift 4) Continental drift and paleomagnetism

Plate Tectonics. 1)The plate tectonic system 2)A theory is born 3) Early evidence for continental drift 4) Continental drift and paleomagnetism Plate Tectonics Plate boundaries 1)The plate tectonic system 2)A theory is born 3) Early evidence for continental drift 4) Continental drift and paleomagnetism 6)History and future of plate motions system

More information

Earth/Space Honors EOC Pacing Guide

Earth/Space Honors EOC Pacing Guide Lesson Vocabulary NGSSS Minerals Understand the physical and chemical properties that define and identify a mineral. Chemical formula Luster Cleavage Fracture Hardness Streak Specific gravity Solid Inorganic

More information

Important information from Chapter 1

Important information from Chapter 1 Important information from Chapter 1 Distinguish between: Natural hazard // Disaster // Catastrophe What role does human population play in these categories? Know how to read a Hazard Map, such as Figure

More information

THE NEPTUNE CABLED OCEAN OBSERVATORY: OVERVIEW AND SCIENTIFIC OBJECTIVES

THE NEPTUNE CABLED OCEAN OBSERVATORY: OVERVIEW AND SCIENTIFIC OBJECTIVES THE NEPTUNE CABLED OCEAN OBSERVATORY: OVERVIEW AND SCIENTIFIC OBJECTIVES Adam Zielinski 1, Chris R. Barnes 2*, Mairi Best 2, Brian Bornhold 2, Kim Juniper 2, Peter Phibbs 2 and Benoit Pirenne 2 1 Department

More information

Lecture 26: Marine Geology Read: Chapter 21 Homework due December 3

Lecture 26: Marine Geology Read: Chapter 21 Homework due December 3 Learning Objectives (LO) Lecture 26: Marine Geology Read: Chapter 21 Homework due December 3 What we ll learn today:! 1. Describe the world s five oceans! 2. Understand patterns of ocean circulation! 3.

More information

Major Points in Introduction

Major Points in Introduction Near- Surface Processes and Resources John Louie - louie@seismo.unr.edu eismo. unr.edu Thomas Pratt tpratt@ocean.washington.edu ashington.edu Here is a Laundry List- With it, we can prioritize Major Points

More information

Lecture Outline Friday January 12 Friday January 19, 2018

Lecture Outline Friday January 12 Friday January 19, 2018 Lecture Outline Friday January 12 Friday January 19, 2018 Questions?? Key Points for today The structure of the Earth Introduction to Plate Tectonic Theory and Convection Chapter 2 Development of the Plate

More information

The Ocean Networks Canada Observatory Science, Industry and Society

The Ocean Networks Canada Observatory Science, Industry and Society The Ocean Networks Canada Observatory Science, Industry and Society S. Martin Taylor President and CEO, Ocean Networks Canada (www.oceannetworks.ca) May 31st, 2012 Global challenges of ocean events, processes

More information

Actual bathymetry (with vertical exaggeration) Geometry of the ocean 1/17/2018. Patterns and observations? Patterns and observations?

Actual bathymetry (with vertical exaggeration) Geometry of the ocean 1/17/2018. Patterns and observations? Patterns and observations? Patterns and observations? Patterns and observations? Observations? Patterns? Observations? Patterns? Geometry of the ocean Actual bathymetry (with vertical exaggeration) Continental Continental Basin

More information

Chapter 2: Plate Tectonics: A Unifying Theory

Chapter 2: Plate Tectonics: A Unifying Theory Chapter 2: Plate Tectonics: A Unifying Theory Chapter Outline 2.1 Introduction 2.2 Early Ideas About Continental Drift 2.3 What Is the Evidence for Continental Drift? 2.4 Features of the Seafloor 2.5 Earth

More information

Contents. Preface. IC. Introductory Chapter. 1. The Ocean in the Earth System. Ocean Studies and Pedagogy Acknowledgments

Contents. Preface. IC. Introductory Chapter. 1. The Ocean in the Earth System. Ocean Studies and Pedagogy Acknowledgments Contents Preface Ocean Studies and Pedagogy Acknowledgments IC. Introductory Chapter IC.1 Why the Ocean is Important to Us? IC.1.1 Biological Resources IC.1.1.1 Fisheries IC.1.1.2 Other Biological Resources

More information

Magnitude 6.5 OFFSHORE NORTHERN CALIFORNIA

Magnitude 6.5 OFFSHORE NORTHERN CALIFORNIA A powerful offshore earthquake that struck near the Northern California coast left a hodgepodge of debris for communities to sort through Sunday but spared residents any serious injury. After 25,000 people

More information

1. What is Wegener s theory of continental drift? 2. What were the 4 evidences supporting his theory? 3. Why wasn t Wegener s theory excepted?

1. What is Wegener s theory of continental drift? 2. What were the 4 evidences supporting his theory? 3. Why wasn t Wegener s theory excepted? Notebook 7a and 7b Objective (left-side): Students will be able to explain the theory of plate tectonics and be able to make predictions about plate interactions. Mapping Reflection 1. What is Wegener

More information

Grades 9-12: Earth Sciences

Grades 9-12: Earth Sciences Grades 9-12: Earth Sciences Earth Sciences...1 Earth s Place in the Universe...1 Dynamic Earth Processes...2 Energy in the Earth System...2 Biogeochemical cycles...4 Structure and Composition of the Atmosphere...4

More information

Subduction zones are complex plate boundaries in which variable geometry and structure can be

Subduction zones are complex plate boundaries in which variable geometry and structure can be 1 Chapter 1 Introduction Subduction zones are complex plate boundaries in which variable geometry and structure can be seismically observed. The along-strike transition from flat to normal subduction is

More information

UNIT SIX: Earth s Structure. Chapter 18 Earth s History and Rocks Chapter 19 Changing Earth Chapter 20 Earthquakes and Volcanoes

UNIT SIX: Earth s Structure. Chapter 18 Earth s History and Rocks Chapter 19 Changing Earth Chapter 20 Earthquakes and Volcanoes UNIT SIX: Earth s Structure Chapter 18 Earth s History and Rocks Chapter 19 Changing Earth Chapter 20 Earthquakes and Volcanoes Chapter Nineteen: Changing Earth 19.1 Inside Earth 19.2 Plate Tectonics

More information

The Basics The lithosphere is made up of numerous plates (14 major, 38 minor)

The Basics The lithosphere is made up of numerous plates (14 major, 38 minor) The Basics The lithosphere is made up of numerous plates (14 major, 38 minor) These plates float atop the asthenosphere, where they can move (albeit very slowly) Plate tectonics describes the formation,

More information

Activity #2 - Major Ocean Surface Currents

Activity #2 - Major Ocean Surface Currents Activity #2 - Major Ocean Surface Currents Concepts # 3 & 6 # 3 Atmospheric cells and ocean gyres redistribute heat from low to high latitudes, which influences climate, weather, and ocean temperature.

More information

Chapter. Graphics by Tasa Graphic Arts. Inc.

Chapter. Graphics by Tasa Graphic Arts. Inc. Earth Chapter Plate Science 9 Tectonics Graphics by Tasa Graphic Arts. Inc. 1 I. Earth s surface is made up of lithospheric plates. A. Lithospheric plates are composed of the crust and part of the upper

More information

Topic 5: The Dynamic Crust (workbook p ) Evidence that Earth s crust has shifted and changed in both the past and the present is shown by:

Topic 5: The Dynamic Crust (workbook p ) Evidence that Earth s crust has shifted and changed in both the past and the present is shown by: Topic 5: The Dynamic Crust (workbook p. 65-85) Evidence that Earth s crust has shifted and changed in both the past and the present is shown by: --sedimentary horizontal rock layers (strata) are found

More information

Welcome to GEO 101 Introduction to Geology

Welcome to GEO 101 Introduction to Geology Welcome to GEO 101 Introduction to Geology so what is Geology? not just rocks! Geology is... study of Earth and planetary bodies processes responsible for formation processes that modify all areas of geology

More information

Earth Science. Explain how Earth's biogeochemical cycles create a balance of materials. Examine the importance of biogeochemical cycles.

Earth Science. Explain how Earth's biogeochemical cycles create a balance of materials. Examine the importance of biogeochemical cycles. Unit 1: DYNAMIC STRUCTURE OF EARTH Introduction to Understand that earth science is based upon the four sciences of astronomy, geology, meteorology, and oceanography. Identify topics studied within the

More information

MCAS QUESTIONS: THE EARTH S INTERIOR, CONTINENTAL DRIFT, PLATE TECTONICS

MCAS QUESTIONS: THE EARTH S INTERIOR, CONTINENTAL DRIFT, PLATE TECTONICS NAME: PER: MCAS QUESTIONS: THE EARTH S INTERIOR, CONTINENTAL DRIFT, PLATE TECTONICS 1. Which of the following statements best explains why the lower mantle of Earth is much more rigid and dense than the

More information

Lecture 17: Earth s Interior. Extrasolar Planets. Extrasolar Planets. planet

Lecture 17: Earth s Interior. Extrasolar Planets. Extrasolar Planets. planet Lecture 17: Earth s Interior The appearance of life led to further profound changes in the atmosphere about 3.5 x 10 9 years ago Plants produce free oxygen and remove carbon dioxide The Earth s surface

More information

OOI Regional Scale Node. + bits on Coastal & CI

OOI Regional Scale Node. + bits on Coastal & CI OOI Regional Scale Node + bits on Coastal & CI Ron Johnson UW & Pacific Wave Trying to channel John Orcutt, John Delany, Matt Arrott et al Nov. 13, 2009 Ocean Sciences: Theory. Experiment. Observation.

More information

* If occurs, fossils that formed in shallow water may be found in water. Subsidence mean the crust is.

* If occurs, fossils that formed in shallow water may be found in water. Subsidence mean the crust is. Name Notes: Topic 5B Topic 5B: The Dynamic Crust A. What evidence exists that proves the Earth s Crust is and has moved? Earth Science 1. Tilted, folded or faulted strata Strata is a term that refers to.

More information

10/11/2010. Acceleration due to gravity, a. Bulk Properties Mass = 6 x kg Diameter = 12,756 km Density = 5515 kg/m 3 (mix of rock and iron)

10/11/2010. Acceleration due to gravity, a. Bulk Properties Mass = 6 x kg Diameter = 12,756 km Density = 5515 kg/m 3 (mix of rock and iron) Acceleration due to gravity, a Bulk Properties Mass = 6 x 10 24 kg Diameter = 12,756 km Density = 5515 kg/m 3 (mix of rock and iron) Escape Velocity, v e Albedo Amount of sunlight reflected back into space

More information

Earth s Interior. Theory of Tectonics. Tectonics & Landforms. Vocabulary

Earth s Interior. Theory of Tectonics. Tectonics & Landforms. Vocabulary Vocabulary Earth s Interior Theory of Tectonics Tectonics & Landforms Earthquake Volcano 100 100 100 100 100 100 200 200 200 200 200 200 300 300 300 300 300 300 400 400 400 400 400 400 500 500 500 500

More information

Continental Drift and Plate Tectonics

Continental 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 information

Week: 4 5 Dates: 9/8 9/12 Unit: Plate Tectonics

Week: 4 5 Dates: 9/8 9/12 Unit: Plate Tectonics clementaged.weebly.com Name: ODD Period: Week: 4 5 Dates: 9/8 9/12 Unit: Plate Tectonics Monday Tuesday Wednesday Thursday Friday 7 No School 8 E 9 O *Vocabulary *Frayer Vocab *Continental Drift Notes

More information

Directed Reading. Section: The Theory of Plate Tectonics. to the development of plate tectonics, developed? HOW CONTINENTS MOVE

Directed Reading. Section: The Theory of Plate Tectonics. to the development of plate tectonics, developed? HOW CONTINENTS MOVE Skills Worksheet Directed Reading Section: The Theory of Plate Tectonics 1. The theory that explains why and how continents move is called. 2. By what time period was evidence supporting continental drift,

More information

CONTENT. A. Changes in the Crust Facts Changes Construction and Destruction. B. Continental Drift What is it? Evidence

CONTENT. A. Changes in the Crust Facts Changes Construction and Destruction. B. Continental Drift What is it? Evidence Name Earth Science Date Period TOPIC THE DYNAMIC EARTH CONTENT A. Changes in the Crust Facts Changes Construction and Destruction B. Continental Drift What is it? Evidence C. Theory of Plate Tectonics

More information

Drilling into the Memory of the Earth An Introduction to International Ocean Discovery Program

Drilling into the Memory of the Earth An Introduction to International Ocean Discovery Program Drilling into the Memory of the Earth An Introduction to International Ocean Discovery Program Y. Tatsumi (Dept. Earth & Planetary Sciences) Why is this planet to be the Earth? This is a fundamental question

More information

The Mega-Earthquakes of Chile: Seismology and the Sounds of the Earth

The Mega-Earthquakes of Chile: Seismology and the Sounds of the Earth The Mega-Earthquakes of Chile: Seismology and the Sounds of the Earth Michael Wysession Department of Earth and Planetary Sciences Washington University, St. Louis, MO Puerto Montt, Chile, November 6,

More information

THE INTERNAL STRUCTURE OF THE EARTH

THE INTERNAL STRUCTURE OF THE EARTH UNIT 1 THE INTERNAL STRUCTURE OF THE EARTH 1.1.Earth s interior layers The interior of the Earth can be divided into layers according to: -Composition layers ( organized in order of increasing density

More information

General Oceanography Geology 105 Expedition 8 Plate Boundaries Beneath the Sea

General Oceanography Geology 105 Expedition 8 Plate Boundaries Beneath the Sea General Oceanography Geology 105 Expedition 8 Plate Boundaries Beneath the Sea Name Not attempting to answer questions on expeditions will result in point deductions on course workbook (two or more blank

More information

2016 PLED 576 Earth and Space Science Correlation to Next Generation Science Standards (NGSS) High School Earth and Space Science

2016 PLED 576 Earth and Space Science Correlation to Next Generation Science Standards (NGSS) High School Earth and Space Science 2016 PLED 576 Earth and Space Science Correlation to Next Generation Science Standards () High School Earth and Space Science Course Objectives 1. Evaluate the differing theories that explain the structure,

More information

Laboratory #7: Plate Tectonics

Laboratory #7: Plate Tectonics Materials Needed: 1. Pencil 2. Colored Pencils 3. Metric/Standard Ruler 4. Calculator 5. Tracing Paper Laboratory #7: Plate Tectonics Plate Tectonics The Earth is composed of layers. At the center is a

More information

Earth Science 14 th Edition, 2015 Tarbuck Lutgens - Tasa

Earth Science 14 th Edition, 2015 Tarbuck Lutgens - Tasa A Correlation of Tarbuck Lutgens - Tasa To the Oklahoma Academic Standards for Earth & Space Science A Correlation of, EARTH & SPACE SCIENCE HS-ESS1 Earth s Place in the Universe HS-ESS1-1 Students who

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

Earth Science, (Tarbuck/Lutgens) Chapter 10: Mountain Building

Earth Science, (Tarbuck/Lutgens) Chapter 10: Mountain Building Earth Science, (Tarbuck/Lutgens) Chapter 10: Mountain Building 1) A(n) fault has little or no vertical movements of the two blocks. A) stick slip B) oblique slip C) strike slip D) dip slip 2) In a(n) fault,

More information

MAGMATIC, ERUPTIVE AND TECTONIC PROCESSES IN THE ALEUTIAN ARC, ALASKA

MAGMATIC, ERUPTIVE AND TECTONIC PROCESSES IN THE ALEUTIAN ARC, ALASKA MAGMATIC, ERUPTIVE AND TECTONIC PROCESSES IN THE ALEUTIAN ARC, ALASKA Introduction The Aleutian Arc contains roughly ten percent of the world s active volcanoes. Hardly a year goes by without a major eruption

More information