EARTH STRUCTURE AND HEAT TRANSFER

Slides:

Advertisements

Similar presentations

The crust is the outermost part of the earth consisting of the continental crust and the oceanic crust. The continental crust forms continents that.

Advertisements

Earth Structure & Plate Tectonics Notes

Lesson 1 - Earth’s Interior

What Are Earth’s Layers Made Of?

 Understanding Earth’s Interior can be a complicated process.  It’s thick, hot and we don’t have the technology to dig to the core or even through.

Introduction to Earth’s Interior Layers Ms. Bridgeland 6 th Grade.

Unit 1, Section 3 1.  What are the layers of the Earth?  How do Earth’s internal forces change its surface? 2.

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 Starter Begin following Layers of the Earth Directions, skip #1 and begin with #2. Examples of how your cut out should look.

Heat and Plate Tectonics

Seismic Waves Vibrations that travel through the Earth carrying the energy released during an earthquake Pressure The force exerted on a surface divided.

Heat Transfer.  Earth’s molten outer core is nearly as hot as the surface of the sun.  Heat is transferred from the core to the surface of the Earth.

Earth’s Core By: Diego Gonzalez.

Basic Structure of the Earth

Layers of the Earth.

Journey to the Center of Earth

Earth on the Move Earth Structure & Plate Tectonics Notes.

Earth’s Interior Chapter-1 Section-1 By: Ms. Vigil Science P-1 9/6/04.

Earth Layers. Inner Core Made mostly of iron and nickel Dense ball of solid metal due to intense pressure Very hot and very dense 1,216 km thick.

LAYERS OF THE EARTH Structures of the EARTH By: Adreana Thompson & Victoria Wright.

Layers of the Earth.

What’s Inside?. The Earth’s Core – Almost as hot as the surface of the sun (due to radioactive decay) Escape of this inner heat drives geological activity.

Earth’s Internal Heat.

What happens to heat and pressure as you get closer to the center of the earth?

DO NOW FOR THURSDAY, FEB. 28 How do geologists know what the Earth is composed of?

Journey to the Center of Earth Layers of the Earth Crust Mantle Outer Core Inner Core.

The Cycling of Energy Key Concept: Various Heat-exchange systems work in the Earth system and affect phenomena on Earth’s surface.

6-70 km thick 6-70 km thick Very light; only 1% of Earth’s total mass Very light; only 1% of Earth’s total mass Made up of rock Made up of rock Two types.

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 5.1 Notes Earth’s Interior. Exploring the Earth Geologists use two types of evidence to learn about the Earth’s interior: -direct evidence from.

Earth’s Layers Geology Unit.

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.

Unit 3 Lesson 2 Energy Transfer Copyright © Houghton Mifflin Harcourt Publishing Company.

 Inner core, Outer core, Mantle asthenosphere, lithosphere, crust,

Explored through mines and wells Temperature and pressure increases with depth Earthquake (Seismic) Waves scientists are able to tell the density and.

Convection Currents.

Layers of Earth.

Ch 1A -Earth’s Layers.

The Earth’s Layers Scientists have spent many years determining what is inside the earth. Geologists can’t use x-rays to see inside the earth or.

Earth’s Inner Structure

Layers of Earth.

Earth’s Materials and Processes-Part 8 Investigating Earth’s Interior

Earth Structure & Plate Tectonics Notes

Earth Structure & Plate Tectonics Notes

Structure of the Earth.

Earth Structure & Plate Tectonics Notes

Convection Currents.

Earth Structure & Plate Tectonics Notes

Walk Around Notes!.

Layers of the Earth Foldable

Opening Activity What are the three states of matter and how does the molecular motion vary in each?

The Earth’s Layers Scientists have spent many years determining what is inside the earth. Geologists can’t use x-rays to see inside the earth or.

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 3 Section 1 The Earth System.

It may seem like the Earth is made up of one big solid rock, but it's really made up of a number of parts. Some of them constantly moving!

Earth’s Interior.

Crust! Thickness The crust is the thinnest and least dense layer.

Earth’s Layers.

Convection Currents and the Mantle

Earth's Interior Notes.

Write down some examples of this concept:

INSIDE EARTH CHAPTER 1: PLATE TECTONICS

Convection and the Mantle

Earth’s Internal Heat.

Energy Flow in the Earth System

Layers of the Earth.

Chapter 1 Science Review

The Sun is the source of energy for the Earth.

Inside the Earth.

Presentation transcript:

EARTH STRUCTURE AND HEAT TRANSFER

RADIATION Radiation is the transfer of heat transferred through electromagnetic waves. This type of heat transfer can be observed on sunny days. Most electromagnetic radiation form the sun is in the form of visible light. FUN FACT These frequencies are interpreted by our brain as colors.

CONDUCTION Is the transfer of heat from one molecule to another within a substance. When heat is transferred through conduction it flows from warmer to cooler regions and will transfer more rapidly with greater temperature differences.

CONVECTION Is the transfer of heat through the movement of a fluid. Convection transfers heat vertically into the atmosphere. HEAT RISES COLD FALLS

CONVECTION CONTINUED Convection is due to the sun heating Earth. The heat absorbs water shown by when there is a drought the water dries up and ground is cracked.

ENERGY BY THE SUN Energy from the sun will effect the ocean tide. Also the moon has an effect on the tide and gets its light from the sun.

EARTH LAYERS CRUST LITHOSPHERE ASTHENOSPHERE MANTLE OUTER CORE INNER CORE

CRUST The thin outer layer of the earth is where we live. The continental crust is made up of rocks that consist primarily of silica and alumina called the ‘sail”

MANTLE Mantle is much thicker than the Crust, it is three thousand kilometers deep. It is made up of slightly different rocks with a lot more magnesium and iron Magnesium has 12 protons and 12 neutrons Iron has 26 protons and 30 neutrons

Eleven thousand degrees fahrenheit OUTER CORE The earths outer core is made up of iron and nickel. it is very hot in the outer core. Ranging from 4400 to 5000+ degrees Celsius. In America that equals Eleven thousand degrees fahrenheit

INNER CORE The earths inner core is made up of iron and nickel. It is under immense pressure. So much pressure, that even though it is so hot, it is solid.

QUESTIONS CHRIS What is the very inside of the earth? What is the transfer of heat through electromagnetic waves?

QUESTIONS LIAM What is the definition of convection? How does the air transfer energy from one region to another?

Resources Google.com Google images Prentice hall Science explore inside earth Wikipedia.com