 Composition: Silicon, Oxygen, and Aluminum  Types: › Continental Crust: solid & rocky outer layer › Oceanic Crust: thin & dense material.

Slides:



Advertisements
Similar presentations
Plate Tectonics 6.E.2.2 Explain how crustal plates and ocean basins are formed, move and interact using earthquakes, heat flow and volcanoes.
Advertisements

Plate Tectonics Review
Earth’s Interior By Aimee Chavez.
Chapter 17 Plate Tectonics
Major Geological Events Caused by Plate Tectonics
Plate Tectonics. Earth’s Interior Earth is made of layers Crust Upper Mantle (asthenosphere ) Mantle Outer Core Inner Core Scientists discovered these.
Pangea, Plate Tectonics. Alfred Wegener argued that, 200 million years ago, all of earth’s continents existed as one supercontinent called Pangaea. Wegener’s.
Seismic Waves Vibrations that travel through the Earth carrying the energy released during an earthquake Pressure The force exerted on a surface divided.
The Structure of the Earth and Plate Tectonics. 2 Structure of the Earth The Earth is made up of 3 main layers: –Core –Mantle –Crust Inner core Outer.
Chapter One Section 1 Plate Tectonics
Inside the Earth Why does the earth look the way it does today? 3PYh4http:// 3PYh4.
Planet EarthSection 1 What is Earth’s Interior Like? 〉 How is Earth’s interior structured? 〉 Earth’s interior is made up of several distinct compositional.
Plate Tectonics. Layers of the Earth Lithosphere – the crust and uppermost part of the mantle The lithosphere is broken into plates that can move around.
Review. a. They both decrease. b. They both stay the same. c. They both increase. d. Temperature increases and pressure decreases.
Crustal Movement.
Plate Tectonics. Plate Tectonics What is Plate Tectonics The Earth’s crust and upper mantle are broken into sections called plates Plates move around.
What type of boundary is represented here?
The Changing Earth Chapter 9: Plate Tectonics. Review Earth Has Several Layers.
The Earth’s Interior & Plate Tectonics. The Earth’s Interior The Earth’s Interior can be broken up into 4 major zones Crust Mantle Outer core Inner core.
Journey to the Center of Earth
The Theory of Plate Tectonics. Earth’s Internal Layers The crust varies in thickness (4-60 km) oxygen, silicon, magnesium and iron The mantle (2885 km)
Processes that shape the planet.. Earth’s Internal Layers The crust (oxygen, silicon, magnesium and iron) The mantle (silicon & oxygen) Outer core (iron.
“Continental Drift” I. Early Evidence of Continental Movement: A. Continental Drift: 1. Continental Drift -A hypothesis, which states that continents.
UNIT 3 EARTH SCIENCE RI_Z2Kgs&safety_mode=true&persist_s afety_mode=1&safe=active.
Our Amazing Planet. Planet Earth Earth’s Layers Crust Earth’s thin outermost layer. – Continental Crust (land) - thick low density rock (granite). –
Our Amazing Planet.
Internal Structure of the Earth
What provides the force that moves the tectonic plates?
The Earth. Layers of the Earth CRUST MANTLE OUTER CORE INNER CORE.
Day 1.
Theory of Plate Tectonics. How do we know the plates exist?  Earthquake and Volcano Zones  Ocean floor features (Trenches and Mid-Oceanic ridges)
Plate Tectonics. What is Plate Tectonics? The Earth’s crust and upper mantle are broken into sections called plates Plates move around on top of the mantle.
What is it? And what makes it work?.  Our Earth  Not a solid ball of rock  Composed of distinct layers  Three main layers based on composition: 
The Earth’s Interior & Plate Tectonics Physical Science Chapter 17 Section 1.
Plate Tectonics. The Earth’s 4 Layers 1.Inner Core: Center, made of solid iron and nickel km 2.Outer Core: Made of liquid iron and nickel
Plate Tectonics.
Main ??? Plates converge Plates move Continents change Earth layers
Ch. 6 Plate Tectonics.
The Earth and it’s layers
The Theory of Plate Tectonics Earth’s crust is made of many ________ These plates move as a result of ______________ in the mantle Earth’s surface is.
Theory of Continental Drift (pg ) The Theory of Continental Drift states that all continents on Earth were once joined together as Pangaea, but.
Warm-up What are the phases of the moon starting with the New Moon? Draw them.
Plate Tectonics 8 th Grade Science. Earth’s Composition.
Our Amazing Planet. Engage Assignment Make a 3 slide power point on each of the three types of plate boundaries – Convergent boundaries – Divergent boundaries.
Forces that act on the Earth. The Inner Core The deepest layer in Earth is the inner core. It is located at the center of Earth because it contains.
Forces that Shape the Earth
Science 8 th Grade Geology Part 3 Rocks Standard A.
Plate Tectonics Plate Boundaries Causes of Plate Tectonics.
Plate Tectonics Test Review
Plate Tectonics Chapter 6. Earth is made up of materials with different densities. Scientists theorize that Earth began as a spinning mass of rocks and.
Bell Ringer 2/8/2016 Which plate is thicker and less dense? Continental Plate or Oceanic Plate.
Planet EarthSection 1 SECTION 1: EARTH’S INTERIOR AND PLATE TECTONICS Topics of section: KEY IDEAS 〉 How is Earth’s interior structured? 〉 How has the.
Earth’s Layers The three main layers of Earth are the crust, mantle, and the core. These layers vary greatly in size, composition (what they are made of),
Earth’s interior. Geologist have used evidence to learn about the Earth’s interior: Direct evidence and indirect evidence. Geologist have used evidence.
Plate Tectonics 8 th Grade Science. Earth’s Composition.
Planet EarthSection 1 Section 1: Earth’s Interior and Plate Tectonics Preview Key Ideas Bellringer What is Earth’s Interior Like? Plate Tectonics Plate.
Plate Tectonics the movement of Earth.
Plate Tectonics Ocean Floor Earth Layers Potpourri
Good Afternoon! Please get your science notebook and get out your plate boundaries map and worksheet from Friday.
 From the surface of the Earth the layers are the crust, mantle, outer core, and inner core.
Journey to the Center of Earth
Earth’s Structure.
Plate Tectonics.
Plate Tectonics.
Earth’s Layers The three main layers of Earth are the crust, mantle, and the core. These layers vary greatly in size, composition (what they are made of),
Earth’s Interior Inner Core Solid Metal
Plate Tectonics 8th Grade Science.
Section 3: Earth’s Interior
Plate Tectonics 10/22/12 *Take out your Continental Drift summary for me to check* Earth’s Insides Plate boundaries Do Now [journal] How do plate tectonics.
Plate Tectonics v3 JEOPARDY.
Presentation transcript:

 Composition: Silicon, Oxygen, and Aluminum  Types: › Continental Crust: solid & rocky outer layer › Oceanic Crust: thin & dense material

 Includes the Earth’s Crust & Upper Mantle  Divided into small and large tectonic plates that help move the continental and oceanic crust

 Composition: Silicon, Oxygen, and Magnesium  Thickest layer  Convection currents are located here

 Composition: Molten (liquid) Iron & Nickle

 Composition: Solid Iron & Nickle  Solid because of the pressure from the layers above  Solid inner core spins in the molten (liquid) outer core › Creates the Earth’s Magnetic Field  Hottest layer

 Happens in the Middle Mantle › Has hot, dense rock that slowly flows  Movement created moves the tectonic plates in the Lithosphere  Caused by hot material, deep in the Mantle, being heated by the Core to rise then cool and sink again

 Molten rock found beneath the Earth’s surface

 Molten rock found on the Earth’s surface

 Large pieces of Earth’s crust (lithosphere) that can move, collide, or slide past each other  Causes: › Continental drifting › Earthquakes › Volcanoes › Mountains › Ocean trenches

 States pieces of Earth’s lithosphere are in constant, slow motion, driven by convection currents in the Mantle  Explains: › Plate formation › Plate movement › Subduction of plates

 Two tectonic plates moving toward each other and collide  Types = Creates: › Continental-continental = Mountains & their ranges › Oceanic-oceanic = Island Arcs › Continental-oceanic = Subduction Zone & Trenches

 Two tectonic plates moving away from each other  Creates: › Volcanoes › Mid-Ocean Ridge › New Ocean Floor › Rift Valley

 Two tectonic plates that move or slide past one another › Opposite or same direction at different rates  Creates: › Earthquakes › Fault lines

 Continents have shifted their position over geologic time  One time, all land masses were connected to form Pangaea  Evidence: › Continents look to fit together › Minerals, fossils, and mountains now on different continents would match if they were together

 Magma and molten material rises from the convection currents to create a divergent boundary, separating plates  Helps move the continents  Oceans are spreading ~2 cm per year  Creates: › New Ocean Floor Crust › Mid-Ocean Ridges

 Process where the ocean floor sinks beneath an ocean trench and melts back into the Mantle