Earth’s Interior.

Slides:



Advertisements
Similar presentations
What are the three Chemical layers of the Earth?
Advertisements

PLATE TECHTONICS TEXT CH. 3..PG. 80. How do geologists study inside earth? Look at rock samples – Can determine conditions deep in the earth by looking.
Table of Contents Earth’s Interior Convection and the Mantle Classifying Rocks Igneous and Metamorphic Rock Sedimentary Rocks The Rock Cycle Earth’s Structure.
Earth: the home planet Earth’s Interior Earth’s Layered Structure Earth’s interior consists of layers Earth’s interior consists of layers Layers are.
Science Starter Turn to the next blank page in your ISN and cut and paste the handout that is located on the front desk. You will need colored pencils.
Science Questions By: Emma L.. 2a Defining What is a convection current? The movement of a fluid, caused by differences in temperature, that transfers.
Figure 1.CO2.
17-4 Causes of Plate Motion
Basic Structure of the Earth
Earth on the Move Earth Structure & Plate Tectonics Notes.
Layers of the Earth.
Earth’s Interior. The Earth’s Core Much of the information scientists have about the Earth’s interior has come not only from complex instruments but also.
Radiation – the transfer of energy through space. Heat transfer by radiation takes place with no direct contact between a heat source and an object. Example.
Ch5 Sec2 Convection and the Mantle. Key Concepts How is heat transferred? What causes convection currents? What causes convection currents in Earth’s.
What happens to heat and pressure as you get closer to the center of the earth?
Density and Mantle Convection Blue Type: Read, listen, and think Black Type: Take notes.
Earth’s Interior Chapter 5 Section 1.
The Earth’s Structure A Journey to the Center of the Earth.
Standard 2 Objective 1 Study Notes Plate Tectonics 1.
The Structure of the Earth
The Cycling of Energy Chapter 3-3 Study Guide. What is heat flow?  The transfer of energy from a warmer object to a cooler object.
CHAPTER 4.2 Convection and the Mantle. Standard  S.6.4.c Students know heat from Earth’s interior reaches the surface primarily through convection.
Heat and Thermal Energy Sources 14 Key Ideas Thermal energy influences temperature, density, pressure, and a substance’s physical state. Thermal energy.
 Gravitational Contraction ◦ Gravity pulled Earth’s center together causing friction that released heat energy. ◦ This thermal energy is left over.
EVIDENCE OF CONTINENTAL DRIFT - Similarities in coastlines of continents - same Fossils found on eastern S. America and west Africa - Rock type and age.
1.3 notes  There are 3 types of heat transfer: radiation, conduction, and convection.  The transfer of energy through space is radiation. Sunlight.
2 The Earth’s Structure series of layers or spheres which differ in density, chemistry (or composition) and physical properties.
DO NOW: Heat Transfer. What type of heat transfer is shown?
Thermal Energy & Heat.
Earth’s Layers G 103. General Information -Iron,Oxyge, Silicon, & Magnesium - Deepest drill 12 km -Radius of Earth 6371 km - How do we know about the.
Convection Currents Heat is always transferred from warmer substance to a cooler substance. Write down some examples of this concept:
Convection Currents and the Mantle. The Heat of the Earth Earth’s outer core is nearly as hot as the surface of the sun.
Earth’s Interior =mOSpRzW2i_4.
The Geosphere. Changes occur on the Earth constantly: Molten rock flows from volcanoes Hurricanes batter beaches and change coastline Earthquakes shake.
Welcome to Islands The Story: This unit is about both biological and geological evolution. Islands provide interesting, unusual examples of evolutionary.
Pop Quiz! 1.__ 2.__ 3.__ 4.__ 5.__ 6.__ 7.__ 8.__ Inner Core Mantle Mesosphere Outer Core Asthenosphere Ocean Crust Lithosphere Continental Crust.
Standard 2 Objective 1 Handout 2
Convection Currents.
Layers of the Earth.
Convection and the Mantle
Convection and the Mantle
Convection Currents and the Mantle
Chapter 2, Lesson 3, Earth’s Interior
Earth’s Materials and Processes-Part 8 Investigating Earth’s Interior
The Geosphere.
Earth’s Moving Surface
Essential Question: How does Earth's composition change the landscape
Convection Currents.
17.4 Cause of Plate Motions.
Inside the Earth.
Earth: Systems, Structures and Processes
Intro to Plate Tectonics
Section 4: Causes of Plate Motions
Section 4: Causes of Plate Motions
The Fiery Earth Earth’s Interior.
Eric Angat environmental science
What you Learned (L) (don’t fill out yet!)
Earth’s Interior.
What are the three Chemical layers of the Earth?
Convection and the Mantle
Science Starter Turn to the next blank page in your ISN and cut and paste the handout that is located on the front desk. You will need colored pencils.
Chapter 2, Lesson 3, Earth’s Interior
Earth’s Interior.
Chapter 7 Chapter 4 in Old Textbook – pg. 115
Convection Currents and the Mantle
Write down some examples of this concept:
What are the three Chemical layers of the Earth?
Earth’s Interior Chapter 5 Section 1.
Chapter 2, Lesson 3, Earth’s Interior
Part 1: Earth’s Dynamic Interior
Presentation transcript:

Earth’s Interior

Earth’s Structure

Earth’s Structure

Physical Properties

Physical Properties

Physical Properties

Seismic Waves Changes in seismic wave direction and speed indicate changes in chemical composition and the physical properties of density, temperature, pressure and state of matter.

Convection Convection is the transfer of energy by the flow of a heated substance (material moves from high heat, low density to low heat, high density) Convection currents in the mantle cause the overlying lithospheric plates to move.

How can our understanding of the earth’s interior help us better understand island formation?