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Evidence for Plate Tectonics • • • • • • • • Shape of Continents Rock Types Fossils Glaciers Mountain Chains Location of Earthquakes Mid-ocean ridges and ocean floor rock ages Magnetic Polarity Reversals Shape of the Continents • The edges of the continents appear to fit together like the pieces of a puzzle Alfred Wegener - Continental Drift • Noticed that continents appear to fit together • Hypothesized that continents were once together and had drifted apart • Idea was called “Continental Drift” Continental Drift Permian 225 m.y.a. Triassic 200 m.y.a. Jurassic 150 m.y.a. Cretaceous 65 m.y.a. Present Day Rock Type Evidence • Same sequence of rocks of same age can be found all over the world – Indicates that when these rocks formed all these places were connected Fossil Evidence • Same fossils found on many different continents – Fossils of organisms that could not fly or swim between continents – Continents were together when these animals lived, so they could walk from one continent to another Glacier Evidence • Glaciers leave marks on rocks called striations that show which direction they move Glacier Evidence • Striations have been found in places too warm to have glaciers now • Striations point in different directions • If all the continents were together at the south pole, striations point in the same direction Mountain Chains • Mountain ranges around the world appear similar to each other in composition and age. • If we reconstruct the past arrangement of the continents, these ranges formed as one mountain range and were later split Mountain Chains • This is true of mountain ranges all over the world Location of Earthquakes • Do earthquakes appear randomly on this map? • NO! Location of Earthquakes • Earthquakes form a definite pattern- we know now that these are the edges of “plates” of rock that fit together to form the earth’s crust Mid-Ocean Ridges • First discovered when scientists started to map the bathymetry of the oceanfloor • Long chain of underwater mountains that stretches around the entire earth Ocean Floor Rock Ages • Rocks all over the ocean floor were dated using absolute dating Ocean Floor Rock Ages • Rocks closest to the mid-ocean ridges were youngest • Rocks farthest from the mid-ocean ridges were oldest • Pattern of ages is the same on both sides of the ridges • Indicates that new rocks are forming at the mid-ocean ridges! The Theory of Plate Tectonics • Explains all evidence • Similar to continental drift, but more complex • Earth’s crust is composed of “plates” that make up the crust under the ocean and on the continents • Continents DO NOT float on the oceans • Plate boundaries do not always occur at the edges of continents • Earthquakes and volcanoes occur where two plates meet Plate Tectonics Today