Transcript Ch.4 Notes
Ch.4 Notes Plate Tectonics Continental Drift • • • • • • 400 years ago Magellan and Columbus mapping info Similar shoreline 1912 Alfred Wegener hypothesized Pangaea – 1 land mass Panthalassa – all seas World Map Evidence of Continental Drift • • • • • • • • • • Coastlines Fossils Mesosaurus – lived 270 million years ago They cannot swim well Age and type of rocks Brazil = Africa Mountain ranges Coal deposits Continents joined over South Pole No force making this happen? Still not accepted 1930’s Continental Drift Sea floor spreading • 1947 • Out of a ridge in the ocean floor magma flows creating new crust. • Pushing old crust outward. • Harry Hess – Princeton, MidAtlantic Ridge • Arthur Holmes hypothesis in 1930 to put Wegener hypothesis back on map Sea floor spreading Sea Floor Spreading Mid-Ocean Ridges • Go around the earth • 80,000 km long • Undersea mountain range with a valley in the middle. Mid Atlantic Ridge Iceland Paleomagnetism of the ocean floor • Magma has iron in it. • Iron aligns with the poles like a magnet • Reverse polarity in layers 1965 Paleomagnetism of the ocean floor 1960 • Hypothesis of continental drift and seafloor spreading turned into a theory. Assignment • Pg. 71 Questions 1-4 • • • • • • • • • • • • • • Assigned Due Explain how Sea Floor spreading occurs. You must include: - rift valley - magma - asthenosphere iron magnetism north and south poles use a diagram to help explain where the old rock and new rock is located why is this important to Alfred Wegeners idea of continental drift It should take at least 2 paragraphs to explain it in detail. The theory of Plate Tectonics • Explanation of how and why the continents broke apart. • Construction = tectonics • Crust • 1. oceanic • 2 continental • Lithosphere – upper mantle • Asthenosphere – solid rock that is under pressure • 30 different plates Plate Tectonics Lithospheric Plate Boundaries • • • • Boundaries can be anywhere Divergent – moving away Convergent – moving toward Transform Boundaries – moving across Divergent – moving away • • • • • Plates moving away from each other Asthenosphere flows upward to fill in Mid-ocean ridge Rift valley – center of plate boundary Red sea is one Sea floor spreading Convergent – moving toward • Opposite side of divergent • 1. Oceanic crust vs continental crust oceanic is denser so subduction – goes under, continental crust goes up • Forms deep ocean trenches • Often forms volcanoes on land • 2. If continental crust plates are even both crumple and go up (Himalayas) • 3. oceanic and oceanic crusts one is subducted • Deep trench and island arc of volcanoes Transform Boundaries – moving across • 2 plates grinding past each other • Not smooth so many spurts • San Andreas Fault in California Causes of Plate Motion • Movement of lithospheric plates by convection (transfer of heat) • Convectional current – boiling rice • Arthur Holmes Microplate Terranes • • • • • • Theory of plate tectonics refines continental drift theory Theory of microplate terranes Separate from other plates (neighbors) 1. Contains rock and fossils unique 2. major faults are the boundaries 3. magnetic properties differ • Palo Alto – fossils of coral reef • Ocean floor sediments in California mountains • Petosky stones Microplate Terranes Assignment • Page 77 • Sec. 4.2 Questions 1-5 • Page 78-79 • Question 1-14