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Explore the theories of continental drift and plate tectonics, from Wegener's Pangaea to modern plate boundaries. Understand the evidence and mechanisms behind the movement of Earth's crust. Discover the dynamic forces shaping our planet.
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Warm-up #43 Mar. 26 • Brainstorming: • Will California eventually slide into the ocean? • Have continents really drifted apart over the centuries?
Unit 8 Plate Tectonics
Continental Drift • Alfred Wegener – German scientist proposed the theory of continental drift. • This hypothesis stated that the continents had once been joined to form a single supercontinent • Pangaea – all land
Pangaea • Part of Wegener’s theory was that Pangaea started splitting into smaller continents 200 million years before • Wegener collected lots of evidence to prove this theory
The Continental Puzzle • The shorelines of the continents nearly fit together to make a large land mass. • HOWEVER • The shorelines are constantly eroding and changing.
Matching Fossils • Fossil evidence for continental drift includes several fossil organisms found on different landmasses. • At one point the theory was that there were land bridges, however there is no evidence of this.
Rock Types and Structures • Several mountain belts that end at one coastline reappear on a landmass across the ocean
Ancient Climates • Wegener found glacial deposits showing that between 220 million and 300 million years ago ice sheets covered large areas of the S. Hemisphere
Rejecting Wegener’s Hypothesis • Many scientists questioned Wegener’s theory • He could not describe a mechanism that was capable of moving the continents • There was not enough evidence
A New Theory • In 1968 a new theory was proposed – PLATE TECTONICS
Plates • The lithosphere is broken up into segments called plates • The lithosphere is the uppermost layer of the mantle • Plates continuously move and change shape and size
Warm-up #44 Mar. 27 • Mesosaurus provided evidence that South America and Africa were once joined • On average, how much do you think the plates move a year? • 5 centimeters
Plate Boundaries • A plate boundary is where two plates meet. • There are three main types of boundaries: • Divergent • Convergent • Transform fault
Divergent • Also called spreading boundaries • Occurs when two plates move apart • Results in upwelling of material from the mantle to create new seafloor
Convergent • Form where two plates move together • Results in lithosphere plunging beneath an overriding plate and descending into the mantle
Transform fault • Margins where two plates grind past each other without the production or destruction of lithosphere
What happens at boundaries? • Divergent Boundaries • Seafloor spreading occurs along the boundary • Forms fractures on the ridge crests • Fractures fill with molten material • When the boundary occurs on a continent, rifts or rift valleys form
Convergent Boundaries • Oceanic-continental boundary • Forms a subduction zone within • Volcanic arcs form • Oceanic-oceanic boundary • Often forms volcanoes on the ocean floor • Island arc forms as volcanoes emerge
Convergent Boundaries • Continental-continental boundaries • Neither plate will subduct • Can produce mountains
Transform Fault Boundaries • No new crust created • No crust is destroyed • Most are in oceanic crust • Parallel the direction of plate movement • Aids movement of crustal material
Boundary Brochures • Needs to include: • 3 types: Divergent, Convergent, Transform • What each one is (use your notes) • A picture for each • An example for each • http://geology.com/plate-tectonics.shtml • Needs to be colored
Warm-up #45 Mar.28 Brainstorming: • Do you think it is possible for Earth’s magnetic poles to be reversed? • If so, what do you think could happen to the biosphere? • Also, how might geologist use that to support plate tectonics?
Evidence for Plate Tectonics • Paleomagnetism • Most persuasive piece of evidence. • Ancient magnetism preserved rocks. • Paleomagnetic records show: • Polar wandering • Earth’s magnetic field reversals
Evidence for Plate Tectonics • Earthquake patterns • Associated with plate boundaries • Deep-focus earthquakes along trenches provide a method for tracking the plate’s descent
Evidence for Plate Tectonics • Ocean Drilling • Deep Sea Drilling Project – Glomar Challenger • Age of deepest sediment • Youngest are near the ridges • Older are at a distance from the ridge • Ocean basins are geologically young
Evidence for Plate Tectonics • Hot Spots • Rising plumes of mantle material. • Volcanoes can form over
Driving Mechanism • No one model explains all plate motion • Earth’s heat is the driving force • Several models have been proposed • Convection currents in the mantle • Slab-pull and slab-push model • Hot plumes
Dynamic Earth • http://www.learner.org/interactives/dynamicearth/index.html
Ticket out the Door • What are the 3 main types of plate boundaries? • Name 2 pieces of evidence Wegener used to prove continental drift. • What is type of boundary is this?