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POS Unit 5: Planet Earth Topic 4 The Moving Crust Our earth is made up of different layers: 1. Atmosphere “vapour” (air) 2. Hydrosphere “water” (oceans, rivers, lakes) 3. Lithosphere “rocky” (land) 4. Asthenosphere “weak” (molten layer under lithosphere, the mantle) 5. Biosphere: living layer (plants/animals) *Although the earth may seem very large, the layers we inhabit, and require for our very survival are extremely thin. Our planet is more fragile (viewed from the moon) than we think. As small as we are, humans can bring about major environmental changes. How thin is the earth’s crust, the lithosphere? It is like the shell on an egg, or the skin of an apple …very thin relative to the rest Inside our planet Layers: Oceanic and Continental Crust (lithosphere) 5km-60 km deep Mantle (1000-4000oC) (asthenosphere) upper (more solid) and lower mantle (more liquid) layer of molten rock, reason for movement of tectonic plates, volcanoes, earthquakes Core (5500-6000oC) Outer-liquid iron Fe and nickel Ni (responsible for our magnetic field Inner-solid *relative temperatures Question: Why is the center of the earth solid? * The inner core should be a gas, seeing how the temperature is so high (materials expand as particles move farther apart) but the high pressure keeps the inner core solid Alfred Wegener Hmm… did they ever fit together? Movement The crust is moving, as it floats in pieces on the mantle Why is the crust moving? Convection currents! Movement: Continental drift Pieces: tectonic plates But why are they moving? Convection Currents The SUPERCONTINENT PANGAEA *Pick out the continents *Why is Asia mostly under water? Gondwanaland/Laurasia How old is the earth? 4.5 billion years When did the dinosaurs go extinct? 65 million years ago Continental Drift Evidence: 1-Shapes fit together supercontinent Pangaea -broke into Laurasia and Gondwanaland 2-still moving today measure distances, see the trenches, areas of sea floor spreading 3-common fossils Present day Three major types of movement Transform Fault  Slipping past eachother  The San Andreas Fault  California, US Converging Plates  Moving towards eachother  2 options:  Mountain building (continental crust crashing into continental crust)  Subduction (continental crust sliding on top of oceanic crust)  Results:  Earthquakes  Volcanic eruptions  Mountain formation Convergence of Tectonic Plates: Continental and Oceanic crust Ring of Fire (Pacific) The Pacific oceanic crust is subducting underneath the continental crust of surrounding plates This causes widespread earthquakes and volcanic activity Ex) Japan, Philippines, California, Seattle (Mt. St. Helens) *Convection Currents Hot gases/liquids rise, as the particles of that material become less dense, and float on the colder, more dense liquids/gases https://www.youtube.com/watch?v=ryrXA GY1dmE 1. Sea floor spreading 2. Subduction 3. Mountain formation *Convergent or divergent? Mid Atlantic Ridge Sea-floor spreading  Pushing apart North and South America from Africa and Europe at a rate of ~2cm a year Divergent boundaries Diverging plates Sea-floor spreading Summary Geysers-Old faithful Yellowstone National Park Deep Ocean Vents Activities  Activity pg 386 Give me a clue  Answer Q’s #1-4 in your journals  Glue map pieces in your journal “fitting together”  Activity pg 388 What do the rocks tell us?  Answer Q’s 1-3 and “What did you find out?” in your journal  Activity pg 389 The Spreading Sea Floor  Answer “What did you find out” questions #1-3 in your journals  Tape/staple the paper into your journal Assignments Vocabulary Update journals Topic 4 Evidence of plate tectonic movement Technologies Topic 4 Q’s pg 394 #1-5 Faces of Earth Video  Disc A, Episode 1: Building the planet  0:00-3:00 Intro  3:00 (skip)- Avaris camera- high altitude plane, lydar camera  START 8:20 Formation of earth in space 4.5 billion years ago  10:20 magnetic field + aurora, need it to keep the atmosphere/hydrosphere/biosphere  16:00- beginning of atmosphere/hydrologic cycle=hydrosphere  17:30=life 3 billion years ago, cyanobacteria’s waste product was oxygen (1st photosynthesis!) ozone  20:00-skip iron, other more complex life  26:00 extinctions Faces of Earth  cont. Disc A, Episode 1: Building the planet  26:00 PT permian extinction: 95% of all life!  Volcanism, Pangaea, altered atmosphere  Noah’s ark?  28:00 65 million years ago  KT Cretaceous/Tertiary extinction  Asteroid  Dinosaurs, 50% of all life  30:00 Fossil fuels  Coal formation by compressed peat (plant debris)  Natural Gas and Oil by microorganisms in the oceans  33:00 (stop) rocks for oil + gas research, seismic Faces of Earth  cont. Disc A, Episode 2: Shaping the planet  START 0:00 Intro: Divergent boundary in Ethiopia (Iceland only other one on land), plate tectonics  5:00-9:40 skip, tribe, monitoring, GPS  11:00 tectonic plates  13:00 mid Atlantic ridge  14:00 ice age  15:00-18:30 skip salt  18:30 convergent mountain building, subduction  23:00 volcanoes : Mt Vesuvius (Pompeii, Herculaneum)  27:00 normal fault  28:00 skip prediction  33:40 Himalayas, seismo, earthquakes  38:00 California, San Andreas Fault  42:00 P, S waves  44:00 END Faces of Earth  Disc B Episode 1: Assembling America  Mount Rainier erupts, Seattle WA  Subduction, water in volcanoes=explosive  Cascade range  Earthquake + seismograms  Ultralight aircraft over scab-land (monster flood)  Salt lake Utah  Yellowstone Geysers…some truth to supervolcano  Great Lakes  Appalachian mountains (Himalaya sized in Pangaea)  31:00 comet crashed Faces of Earth  Disc B Episode 2: A human world (boring!)  Weather, climates, ice ages  Ice cores  Caused by change in earth’s orbit around the sun, or wobble of the earth’s axis  Cultural evolution as part of environmental change  Metallurgy, mining  Global warming  … now it is us who are changing the face of earth by construction + demolition
 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
                                             
                                             
                                             
                                             
                                             
                                             
                                             
                                             
                                             
                                             
                                            