Global Shakes: Erica Rios, Angie Pettenato, and Shoua Yang How earthquakes help us understand plate tectonics and identify geohazardous regions of the.

Slides:



Advertisements
Similar presentations
Plate Tectonics What evidence do scientists have to support the fact that the Earth’s crust is continuously moving?
Advertisements

The Theory of Plate Tectonics
Plate Boundaries.
Types of Plate Boundaries
Plate Tectonics – Section 17.3
Guide to plate movement
PLATE TECTONICS. QUICK REVIEW: EARTH’S STRUCTURE CRUST MANTLE CORE.
Moving plates interact at divergent, convergent and transform fault boundaries.
Types of Plate Boundaries
 Scientists identify the boundaries between two plates by the plate movement.  There are three types of plate boundaries: 1. Divergent 2. Convergent.
Plate Tectonics. Earth’s Interior Earth is made of layers Crust Upper Mantle (asthenosphere ) Mantle Outer Core Inner Core Scientists discovered these.
Plate Tectonics Objective(s): SWBAT describe the layers of the Earth. SWBAT describe the plate tectonics theory including, how plate tectonics operating.
Factors that Cause Tectonic Plate Movement
Using Google Earth to See the World
Earth’s Geology – 3 primary layers Core, Mantle, and Crust Inner core is solid metal (iron and nickle) Outer Core is molten metal Rocky mantle (solid.
ISCI 2001 Chapters Plate Tectonics. Plate Activities – Divergent Plate Boundaries (1). Plates may ‘diverge’ Plates move apart Lava fills spaces.
Seafloor Spreading Theory Explains how ocean crust is formed at ocean ridges and destroyed at deep- sea trenches Supports Wagener’s continental drift.
We know the Earth is broken into 8 major lithospheric plates …. We know these plates move …. We know there are boundaries between the plates …. Now, let’s.
Plate Tectonics Why should you always forgive a Geologist? Because we all have “FAULTS”!
PLATE TECTONICS BY: Jamie Mosely. The History of Pangaea Alfred Wegner (German geologist) created the Pangaea theory and called it Pangaea or “all the.
Part 8: Fold Types. Tensional Stress Compressive Stress Shear Stress Orientation of stress leads to different folds.
Plate Tectonics. Plate Boundaries  There are 3 main plate boundaries:  1) Convergent Boundary  2) Divergent Boundary  3) Transform Boundary.
Plate Boundaries. Destructive Plate Boundaries Also known as convergent boundaries or compressional boundaries. These cause violent volcanoes and earthquakes,
Warm-Up Find the mistakes!
By: Cedric Gooch, Maria Paula Restrepo Giraldo, Peyton Henderson, and Phoebe Bosompem.
+ Plate Tectonics. + Aim & Learning Target Aim: How can we describe what causes the movement of the plates? Learning Target: I can describe what causes.
SLIP SLIDE Collide Lesson 2 Unless otherwise instructed, copy all questions in your science notebook and provide a complete answer.
Plate Tectonics. Overview: The Lithosphere and the Crust Basic Concepts of Plate Tectonics Plate Movements and Boundaries.
Plate Boundaries and Motion
These plates form, move, and subduct
How are oceans formed? Continents and ocean basins exist on lithospheric plates that move relative to each Other. Between their margins, new land is always.
Plate Tectonics Notes Notes
Earthquakes Vibrations of the earths crust Occur when rocks shift suddenly under a fault When friction prevents rocks from moving the fault is said to.
Chapter 17 Plate Tectonics Part 2. Plate Interactions  We have two different types of crust  Oceanic  Continental  We have three different types of.
Geology 12. Divergent Boundary /animations/basic_plate_boundari es.htm  Plates move apart.  The crust cracks and.
Starter/Practice: Connection : Application/ Notes 1/7/15 Plate Boundaries Notes How do you think the continents formed? Plate Boundaries Notes.
Plate Tectonics & Mountain Building
Plate Tectonics Plate Boundaries and Interactions.
Starter/Practice: Connection : Application/ Notes 1/6/16 Plate Boundaries Notes How do you think the continents formed? Plate Boundaries Notes.
Plate Tectonics. What is Plate Tectonics? Wikipedia defines Plate Tectonics as the large-scale movement of the Earth’s Lithosphere. Basically, the Earth’s.
Plate Boundaries. Divergent Plate Boundary Description of Plate Boundary & Motion at Boundary: ON LAND – two plates spread apart; crust separates and.
What is the following picture? Pacific Plate North American Plate.
Plate Tectonics. Plate Boundaries Causes of Plate Tectonics.
Plate Tectonics and the Theory of Continental Drift.
 The lithosphere is broken up into what are called tectonic plates. In the case of Earth, there are currently eight major and many minor plates  Earthquakes,
Tectonics Day 5 Notes Academic.
CL USB 6 Geography Yr 8 Place & Space MILLION YEARS AGO.
Plate Boundaries.
Convergent Boundaries
3 Movements at plate boundaries
Plate Tectonics.
Plate Tectonics.
Theory of Seafloor Spreading
DO NOW Pick up notes sheet..
9-3 Theory of Plate Tectonics
Plate Tectonics Evolution of the Earth.
Theory of Plate Tectonics
Plate Boundaries.
Continental Drift.
Plate Tectonics.
L.O: SWBAT explain the theory of plate tectonics
Plate Interactions How do tectonic plates interact with one another?
Plate Tectonics.
Plate Boundaries Foldable
Internal Forces Shaping the Earth Updated 8/21/12
Plate Tectonics Lab Discussion
Guide to plate movement
Ch. 13 Volcanoes Volcano: A vent or fissure in Earth’s surface through which magma and gases are expelled. Often volcanoes look like mountains.
Plate Tectonics.
Tectonic Plate Boundaries
Presentation transcript:

Global Shakes: Erica Rios, Angie Pettenato, and Shoua Yang How earthquakes help us understand plate tectonics and identify geohazardous regions of the world COSMOS 2006: Earthquakes in Action

Outline  What is an Earthquake?  Engdahl Centennial Catalog  Types of Boundaries  Major Trenches  Screen Shot  Conclusion  Acknowledgements  Demo

What is an Earthquake?  An earthquake is a trembling of the Earth's surface  Usually caused by stress that is released along the fault lines as pressure builds up over time  Shock waves will be generated by the movement of the masses of rock and crust.

Engdahl Centennial Earthquake Catalog  Contains information on earthquakes recorded around the world  Recently updated to include earthquakes from  Complete down to Mw 7.0 between and Mw 5.5 for

Transform Boundaries  Plates move horizontally against each other  Earthquakes tend to be shallow and small to moderate in magnitude  Example: San Andreas Fault in California  1906 San Francisco  1989 Loma Prieta /lic01ba.html

Divergent Boundaries  Where plates move apart and away from each other  Formation of new crust  Earthquakes tend to be shallow to medium depth with lesser magnitudes.  Ex) Mid-Atlantic Ridge  Ex) East African Rift Zone  Saudi Arabia, Red Sea, Horn of Africa net/geology100/IntroLecture1.htm

Convergent Boundaries  Plates move toward each other  One plate subducts under another  Earthquakes tend to be deep and range all magnitudes  Trenches & tsunamis  Earthquake struck northeast of La Paz, Bolivia on June 9, 1994  M 8.3  Depth of 636 km net/geology100/IntroLecture1.htm

Aleutian Trench  Pacific Plate is subducting under the North American Plate  Great earthquake hit Alaska on March 27, 1964  M 9.2  61.4°N, °W  Caused avalanches, landslides, tsunamis, and ground deformations eog3/concept_illus/691_ex.jpg

Peru-Chile Trench  Located along southeastern Pacific Ocean, about 160 km off the coast of Peru and Chile  Result of the eastern edge of the Nazca Plate subducting under the South American Plate  Extends 5,900 km and has a maximum depth of 8.1 km  Great earthquake struck south of Central Chile on May 22, 1960  M 8.6  Depth of 33 km ki/Oceanic_trench

Java Trench  Located in the northeastern part of the Indian Ocean  Trench is a seam between the Eurasian and Indian Plates  Extends 2,600 km and has a maximum depth of 7.7 km  Major earthquake resulted in the deadly tsunami of December _Trench

Visualization  Tectonic plate boundaries, colored by type  Earthquakes by magnitude  Major cities’ populations: 6 million to 12 million  Volcanic Hotspots

Conclusion  Engdahl Catalog: record of earthquakes from 1900 – 2002  Updated the catalog’s 3D scene file with tectonics, hotspots, major cities, undersea trenches  Geohazards of living in certain regions of the world

Acknowledgment We would like to thank the following people in helping us to complete this project: Allison Jacobs Bridget Smith Debi Kilb Jerry Lederman Benson Shing Andreas Stavridis Jon Deck

Works Cited html &archives=true