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Plate Tectonics. Plate Tectonics Ch 4. Earth’s Interior Section 1 Layers of the Earth Section 2 Drifting Continents Section 3 Plate Boundaries Section 4 The Theory of Plate Tectonics Section 5. Section 1: The Earth’s Interior What you will learn:.
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Plate Tectonics Ch 4 Earth’s Interior Section 1Layers of the Earth Section 2 Drifting Continents Section 3 Plate Boundaries Section 4The Theory of Plate Tectonics Section 5
Section 1: The Earth’s InteriorWhat you will learn: • How do we know what the earth’s interior is really like? • What are the characteristics of the Earth’s crust, mantle and core? • Could we really journey to the center of the earth? • Why does the earth have a magnetic field?
Section 1: Earth’s Interior We know about the earth’s interior from indirect evidence Example of indirect evidence: How would you know where to hang a picture so that it stays hung solidly? You can’t see inside the wall.
Section 1: Earth’s Interior • Seismic Waves provide indirect evidence and give us an idea of the earth’s interior-Three kinds of seismic wavesP, S and surface • Speed of these wavesP-waves are faster than S-waves • Path of these waves • Seismic stations all over the worldpick up most seismic waves
Seismic waves are a window to the interior of the earth. P-waves can travel through the entire earth, solid or liquid layers. S-waves do not travel through liquids.A shadow zone occurs on the opposite side of the earth from where the earthquake occurred. All seismic stations in the shadow zone would record P-waves but not S-waves.
What Would it Be Like if You Could Travel to the Center of the Earth? Temperature and pressure change as you go deeper towards the core • Temperature increases towards the center of the earth • Pressure also increases towards the center
This slide shows how temperature increases towards the center of the earth, as well as some of the elements found in each layer.
Four Main Layers of the Earth’s Interior • The crust – the layer of rock that forms the earth’s outer skin, includes rocks, mountains, soil and water • The mantle – 5-40 km down. Rock is of hotter temperatures. About 3,000 km thick • The outer core – liquid molten iron metal • inner core – solid iron metal due to high pressure
Cross-section of earth’s interior showing crust, mantle and the two parts of the core
Earth’s Magnetic Field Currents in the liquid outer core force the solid inner core to spin at a slightly faster rate than the rest of the planet. These currents in the outer core create the magnetic field causing the earth to act like a giant bar magnet. The magnetic field protects living things from dangerous solar radiation.
Section 2:Convection Currents and the MantleWhat you will learn • How is heat transferred? • What causes convection currents? • What are some everyday examples of convection currents that we can use to describe what is happening within the earth’s mantle? • How to draw convection cells that are found in the earth’s mantle.
Convection Convection is heat transfer by movement of heated fluid (gas or liquid).
Radiation The transfer of energy through empty space. Sunlight is radiation that warms Earth’s surface. Also the heat you feel around a flame or open fire is radiation.
Conduction Heat transfer by direct contact (molecules transfer energy directly to neighboring molecules)
Heat Transfer • Conduction • Radiation • Convection
Convection Convection is heat transfer by movement of heated fluid (gas or liquid). Heat transfer by convection is caused by differences of temperature and density within that fluid (for example, how this room is heated)
Convection The heating and cooling of the fluid, changes in the fluid’s density, and the force of gravity all combine to set convection going in the earth’s mantle.
Section 2:Convection Currents and the Mantle • In the upper-most part of the Mantle is a rigid layer called the lithosphere. Litho means rocky or stone. • Below the lithosphere is the asthenosphere, which means weak, but it is actually semi-molten and the semi-melted rock is moving in slow currents! • The lithosphere rides on top of the slow moving asthenosphere.
This slide shows the convection currents found in the asthenosphere. (Note the drawing is not drawn to scale)
These convection cells move sections of the crust. Hot, less dense molten lava rises to the surface creating new crustal sections. Old crust is “subducted” or forced down in the earth, melting and recycling!
Section 3:Drifting Continents • 1910 Alfred Wegener hypothesized that all the continents had once been joined together in a single landmass and have since drifted apart. • Evidence includes mountain ranges that line up, fossils that were similar, mineral deposits that also lined up, as well as climate evidence and traces • Most scientists at the time did not believe in this theory of drifting continents, as Wegener could not explain what force was actually moving the continents.
Section 4: Sea-Floor Spreading • Mapping the Mid-Ocean Ridge – the longest chain of mountains in the world! (and they are underwater) • Sonar mapping(begun in 1959) revealed the location of these Mountains
Evidence of Sea-Floor Spreading • Ocean floors move like conveyor belt, carrying the continents along with them. • At the mid-ocean ridge, molten material rises from the mantle and erupts. The molten material then spreads out, pushing older rock to both sides of the ridge.
This little animation shows molten lava coming to the surface at the mid-oceanic ridge. As it reaches the surface, the lava cools, hardens and is pushed aside by new magma coming to the surface.
Sea-Floor SpreadingReview of Evidence • Molten material found erupting along mid-ocean ridge • Iron within basaltic crust magnetized. • Strips on either side of the mid-ocean ridge that match up
Subduction at Deep-Ocean Trenches Trenches – forms where the oceanic crust is thrust back down into the mantle and begins cracking and melting
Crust and Lithosphere being thrust down at subduction zones. Notice the melting of the plate, forming the pockets of hot magma
Section 5:The Theory of Plate Tectonics • The Theory of Plate Tectonics explains the formation, movement, and subduction of Earth’s plates. • There are three types of plate boundaries: convergent, divergent, and transform. • Plate converge in three different way: Two ocean crusts colliding, two continental crusts colliding, and a continental crust colliding with an ocean crust.
Location of earthquakes and volcanoes found along convergent and divergent plate boundaries (and over hot spots such as Hawaii and Yellowstone)
Convergent Plate Boundaries Two plates “coming together” Ocean crust | Ocean crust (Japan, Taiwan) Ocean crust | Continent crust (Andes Mts.) Continent crust | Continent crust (Himalaya Mts.)
Folded Mountain Belts occur when continents are involved (similar to “rug” analogy)
Divergent Plate Boundaries Two plates “moving apart” Plates are created and move apart at the mid-oceanic mountain range in the Atlantic Ocean
Transform Faults Two plates “slide” past each other. San Andreas Fault in Southern California
Review of Terms Locate: Trench, folded mountain belts, mid-oceanic ridge, volcanoes, hot spots, crust, subduction zones, transform fault, lithosphere, convergent plate boundary, divergent plate boundary, asthenosphere
Motion of India’s plate The formation of a rift valley Convergent Boundary
Can you identify and describe each type of convergent plate boundary?
How islands are formed: Hot spots in the crust allow melted magma to form little cones on the ocean floor that build higher and higher to create islands.
What is happening to the Red Sea? Will we need to someday rename Lake Victoria to Victoria Ocean?
