Presentation on theme: "Earth’s Interior Section 1 Layers of the Earth Section 2"— Presentation transcript:
1 Earth’s Interior Section 1 Layers of the Earth Section 2 Plate Tectonics Ch 4Earth’s Interior Section 1 Layers of the Earth Section 2Drifting Continents Section 3 Plate Boundaries Section 4 The Theory of Plate Tectonics Section 5
2 Section 1: Earth’s Interior We know about the earth’s interior from indirect evidenceExample 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.Temperature and pressure change as you go deeper towards the coreTemperature increases towards the center of the earthPressure also increases towards the center
3 Cross-section of earth’s interior showing crust, mantle and the two parts of the core
4 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 waterThe mantle – 5-40 km down. Rock is of hotter temperatures. About 3,000 km thickThe outer core – liquid molten iron metalinner core – solid iron metal due to high pressure
5 This slide shows how temperature increases towards the center of the earth, as well as some of the elements found in each layer.
7 Seismic waves are a window to the interior of the earth Seismic waves are a window to the interior of the earth. S-waves do not travel through liquids. A shadow zone occurs on the opposite side of the earth from where the earth- quake occurred. All seismic stations in the shadow zone would record P-wavesbut not S-waves.
8 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.
10 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 asthensphere.
12 ConvectionConvection 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)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.
13 This slide shows the convection currents found in the asthenosphere. (Note the drawing is not drawn to scale)
14 These convection cells move sections of the crust 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!
15 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 tracesMost 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.
17 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
18 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.
19 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.
20 Sea-Floor Spreading Review of Evidence Molten material found erupting along mid-ocean ridgeIron within basaltic crust magnetized.Strips on either side of the mid-ocean ridge that match up
24 Crust and Lithosphere being thrust down at subduction zones. Notice the melting of the plate, forming the pockets of hot magma
25 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.
26 Location of earthquakes and volcanoes found along convergent and divergent plate boundaries (and over hot spots such as Hawaii and Yellowstone)