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Pieces of a Puzzle O Law O Tells you exactly what to expect in certain situations O Newton’s Laws of Motion O Theory O An explanation that ties together many hypotheses and observations. O It is based on scientific evidence. Theory of Continental Drift O ***add to comparing and contrasting foldable** O Proposed by Alfred Wegener in 1915 O He suggested that the continents were once joined together as one “supercontinent.” The Theory of Plate Tectonics • the Earth’s lithosphere is divided into tectonic plates that move around on top of the asthenosphere • continents move at a rate of 2cm per year or about 1 inch year Comparing the Theories (“Both” on the foldable) O Continents move O Earth was once made up of one large continent O Same evidence proves the theories O fossils O puzzle pieces O glacial deposits O mountain ranges • Pangaea “all land” – The name of the one supercontinent – All continents joined together as one large land mass http://www.youtube.com/watch?v=q_IYQdKkWs U O Alfred Wegener O His studies were the 1st exhaustive research on the topic O He compiled evidence from many disciplines O His theory/hypothesis was not accepted by many scientists O What? – Theory of Plate Tectonics O It did not seem possible that the crust could move in that way O Finally accepted with discovery of sea floor spreading in the 1960s O When? O 245 mil yrs ago: Pangaea O 180 mil yrs ago: Laurasia & Gondwana O 65 mil yrs ago: continents continue to separate O 1620: Alfred Bacon – puzzle O 1858: Snider-Pellegrini - fossils O 1910: Frank Taylor - geological O 1915: Wegener – put it all together O 1960: seafloor spreading O Where? O continents and oceans O lithosphere and asthenosphere O Evidence of Continental Drift O Shapes of continents and the way they appear to fit together like pieces of a puzzle O Similar rock structures found on different continents O (highlight: locations of different types and ages of rock) More Evidence of Continental Drift O Fossils found on different continents O (highlight: matching fossil remains) O Glacial till deposits of same age and type found on different continents O (highlight: glacial deposits) O Matching mountain belts located on different continents O (highlight: matching mountain belts)