The Internal Energy of Earth

Slides:



Advertisements
Similar presentations
Chapter 9: Plate Tectonics Review Feb 11, What to study? Layers of the Earth Convection Currents Continental Drift Sea-floor Spreading Theory of.
Advertisements

Plate Tectonics Review
Shake, Rattle, and Roll the Earth
CONTINENTAL DRIFT, LAYERS OF THE EARTH, PLATE TECTONICS SI.
Earthquakes and Volcanoes Chapter 9 1 phsc001, chapter9, yuc.
Jeopardy!. Answer: Question: Volcanoes Plate Tectonics History Plate Tectonics Causes Earthquake Causes Earthquake Locations Inside the Earth
Integrated Science One
A Living Planet Chapter 2.
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.
Earth’s Interior Section1.
Unit D Vocabulary Howard Middle School 6 th grade Earth Science.
Plate Tectonics. Plate Tectonics What is Plate Tectonics The Earth’s crust and upper mantle are broken into sections called plates Plates move around.
1 Plate Tectonics Notes Geology – the study of the Earth and its processes.
Plate tectonics.
 Close examination of a globe results in the observation that most of the continents seem to fit together like a puzzle.  In 1912 Alfred Wegner.
Internal Structure of the Earth
Catalyst: Objectives Homework
Plate Tectonics. The Structure of the Earth A thin crust km thick A mantle – has the properties of a solid but it can also flow A core – made.
Earth’s Layers TheoriesBoundariesEarthquakesVolcanoesOther
Geology Vocabulary. A crack in the Earth’s crust along which the blocks of rock on either side have been pushed together or moved apart; they are created.
Topic Xii “Earth Dynamic Crust” I. Evidence of Crustal Movement: A. Original Horizontality: assumes that sedimentary rock is deposited in flat layers.
The Problem with Continental Drift While Wegener was able to find evidence of continental drift, there were 2 major problems with his ideas: – Wegener.
1 6.2 The Theory of Plate Tectonics. 2 How is water in a pot that is held over a flame become heated throughout, even though the flame touches only the.
List 1 fact about Earth. Agenda for Monday Nov 22 nd 1.Finish Movie 2.Layers of the Earth notes.
Tectonic Plates Large segments of the outer layer of Earth (lithosphere) which drift and float on the asthenosphere.
Plate Tectonics. Theory of Continental Drift The theory that continents drifted across the ocean to get their current spots on the globe. First suggested.
Plate Tectonics. Exploring Inside the Earth Geologists have used evidence from rock samples and evidence from seismic waves to learn about Earth’s interior.
The Dynamic Crust Topic 12. Principle of Original Horizontality: The assumption that sedimentary rocks form in horizontal layers. Drawing: Then how.
UNIT 1. THE EARTH’S STRUCTURE AND DYNAMICS. THE EARTH’S STRUCTURE.
Plate Tectonics, Earthquakes, and Volcanoes Study Guide
CGC1D PLATE TECTONICS. Theory that helps explain most geologic processes. Earth’s shell is made up of approximately 20 plates (made up of continents.
How our Earth changes By Rachel Williams.  What makes plates move?  Why do earthquakes happen?  How hot is lava?  Is there a need for earthquakes?
Geological Phenomena. The Continents Divide  It was long believed that the continents, mountains and oceans had not changed since the planet’s birth.
Plate tectonics What you need to know. Earth’s 3 Layers Earth can be divided into three layers based on chemical composition: the crust, the mantle, and.
LITHOSPHERE. The upper mantle and the crust together make up this part of the earth?
Section 1: Earth’s Interior and Plate Tectonics
Chapter 5 plate tectonics review
Earth’s Structure.
Chapter 9 Plate Tectonics.
6.2 The Theory of Plate Tectonics
LAYERS OF THE EARTH PLATE BOUNDARIES PLATE TECTONICS CONTINENTAL DRIFT
Earthquakes & Plate Tectonics
Plate Tectonics - Part A - Theory of Plate Tectonics
Theory of Plate Tectonics
Theory of Plate Tectonics
Geology Notes Part 6.
The Ocean floor and Coast
Plate Tectonics.
2 Plate Tectonics.
Plate Tectonics Theory that the outer rigid layer of the earth (the lithosphere) is divided into a couple of dozen "plates" that move around across the.
The Earth’s Crust in Motion…
Geology – the study of the Earth and its processes
Plate Tectonics Geography of Canada.
Geology – the study of the Earth and its processes
Geological Phenomena.
VIRTUAL EARTHQUAKE
Outer Core Liquid layer of Earth’s core Surrounds inner core.
Science Plate Tectonics
Chapter 8 Earth Systems Friedland and Relyea Environmental Science for AP®, second edition ©2015 W.H. Freeman and Company/BFW AP® is a trademark registered.
JEOPARDY !.
Geology – the study of the Earth and its processes
Geological Phenomena.
Plate Tectonics.
Theory of Plate Tectonics (Part 1)
QUICK REVIEW… Layers of the Earth
Earthquakes & Plate Tectonics
Theory of Plate Tectonics (Part 1)
Geology – the study of the Earth and its processes
Who proposed the theory of continental drift?
Earth’s Surface and Tectonic Processes: Part 2
Presentation transcript:

The Internal Energy of Earth 1

Main ideas Geothermal energy comes from the interior of Earth. The internal energy is the base of formation process of terrestrial relief. Geothermal energy is very badly exploitated nowadays.

The Internal Energy of Earth How to exploit it What is it? Origen How it happens 3

What is the Internal Energy of Earth? It is the internal heat that our planet has since its creation. It originates, among others, the surface genesys relief. 4

Origen The earth was formed about 4600 million years ago. It was a glowing mass against which celestial bodies colliding  . The collision of that bodies raised the temperature In addition, the heat increased due to disintegration of radioactive atoms Later, the earth cooled and formed the different layers of the earth. 5

How it Happens Several ways: Earthquakes Volcans. Geysers. Plate Tectonics Genesys of rocks 6

Earthquakes Sudden release of energy caused by the clash between 2 plates. The place where it occurs is called the hypocenter. The location of the land area closest to the hypocenter is  called the epicenter.

The hypocenter released seismic waves that can be of several types: P or primary waves, the firstto spread. Longitudinal movement. Secondary or S waves, are second to propagate. Perpendicular motion. Surface waves. Longitudinal and perpendicular.The most destructive. L or Love Waves Rayleigh Waves. 8

The magnitude is the amount of energy liberated in the earthquake. The earthquakes are measured with machines called seismograph, and their graphs are called seismograms. The magnitude is the amount of energy liberated in the earthquake. The magnitude is measured according to Richter scale (1-10). The intensity is the effects which the earthquake produces. Different scales measure it (Mercalli, MSK...). 9

The 5 major earthquakes of the last century are: Valdivia (Chile), 1960. 9,5 on Richter scale. Sumatra (Indonesia), 2004. 9,3 on Richter scale. Alaska, 1964. 9,2 on Richter scale. Kamchatka (Rusia), 1952. on Richter scale. Chile, 2010. 8,8 on Richter scale. 10

Plate Tectonics The surface of the Earth is divided into plates. The Plates float on the  mantle and move by convection currents. Convection currents: Warming Ascension Cooling Decrease 11

The continents were not always separated. There was a supercontinent called Pangea.

According to the theory of plate tectonics, Pangaea was splitting up to stay in the world as we know today. This theory was first formulated by Alfred Wegener (continental drift theory). 13

Wegener provided evidences in his theory: Geographic: the edges of the continents fit. Paleontologic: there are fossils in both sides of the ocean of animals who aren´t able to cross it. Geologic and tectonic: if we match the continents we saw a physical continuity in the stones type, cronology and chain of mountains. Paleoclimatic: there are present areas with different climates with regard to the ones of their past. 14

Volcanoes This consists on cracks on the Earth’s surface where the magma, which comes from the interior of the Earth, goes up. This magma contains incandescent materials at a high temperature. The volcano can be on the Earth’s surface or under the oceans and seas.

Volcano Formation Basically, the volcanoes formation is due to a rise of the magma through the fractures in the Earth surface. This formation is produced by: Divergent plates Subduction zones Hot spots

Divergent plates When two oceanic plates move away, the magma rises, and when it gets in touch with the water, it gets cold and it solidifies.

Subduction zones When an oceanic or continental plate slides under other continental plate, it causes the rising of the magma through the crack between both plates.

Hot spots Inside the Earth there is a point which forces the way out to the surface. The magma rises in the same place but in different times. As the Earth surface is moving, the magma goes out in different places each time.

Structure

Rock Types Igneous or Magmatic Rocks: They are formed when the magma goes out to the surface.

Sedimentary Rocks: They are in the sedimentary basins, and they come from other rocks that have suffered the action of geological external processes.

Metamorphic Rocks: They originate from the transformation of other rocks, due to the high pressure and temperature.

Exploitation The inner power of earth allows the generation of Geothermal energy. It is based on the exploitation of the water that is a high temperature.

The bigger temperature, the bigger performance: If water extracted reaches 100ºC, it can be used for heating. From 300º C it can be used to generate electricity. The next step will be to exploit the own magma: more power and more performance (current studies in volcano Krafla).

Italy was pioneer in the exploitation of this kind of energy, but Iceland is the best example of performance and use: It generates 1/3 of electric power and 95% of heating and hot water. Since 1960, the power supply network covers all houses. Curiosity: there are no chims in iceland. Other advanced countries: Greece, Turkey, Japan, USA, Mexico and Italy.

The End Diego Burgos Roberto de la Calle

Bibliography http://www.cronosgea.es/?p=2039 http://www.phschool.com/science/science_news/articles/water_for_the_rock.html http://blopinion.com/epicentro http://ismael-lavidaylaciencia.blogspot.com/2009/01/el-interior-terrestre.html http://www2.funvisis.gob.ve/glosario_.php http://cerosentidocomun.wordpress.com/ http://www.blogalaxia.com/post/extincion+plantas/4 http://recursos.cnice.mec.es/biosfera/alumno/4ESO/MedioNatural1I/contenido2.htm http://recursostic.educacion.es/bancoimagenes/web/ http://recursos.cnice.mec.es/biosfera/alumno/2ESO/tierrin/contenidos12.htm