Transcript File
Evidence for Plate Tectonics Remember that Wegener proposed the theory of Continental drift in the early 1900’s. Evidence for continental drift: 1. 2. 3. 4. 5. Continental jigsaw fit Matching geological structures and rocks Matching fossils Paleoglaciation Coal deposits In 1960 (30 years after Wegener’s death), scientists proposed a mechanism to explain these observations called Plate Tectonic theory – plates can include continents, oceans or both. The scientist that is credited for explaining the evidence for plate tectonics is a Canadian Geologist J. Tuzo Wilson. Evidence for plate tectonic theory: 1. 2. 3. 4. 5. Earthquake and volcano zones Mountain formations Sea floor spreading Ridge sea floor age and sediment thickness Magnetic field reversal - Paleomagnetism Evidence for Plate Tectonics 1. Earthquake and volcano zones Notes: notice the distribution of Earthquakes and volcanoes along plate boundaries. Ring of Fire Evidence for Plate Tectonics 2. Mountain Range formations – like the Himalayas The Himalayas - referred to as the "roof of the world“ the highest peaks on earth - Mount Everest at 8,848 meters above sea level. Notes: Rocks on Mount Everest contain limestone, which forms at the bottom of warm, shallow seas These rocks contain fossilized marine creatures like plankton, clams and fish. Evidence for Plate Tectonics The Burgess Shale - Yoho National Park on the BC side of the Rockies. The town of Field, British Columbia is located between Lake Louise, AB and Golden Described as "the world's most significant fossil discovery" The Burgess Shale was discovered in 1909 and although it's high on a mountain now, at one time it was underwater on the continental edge of North America. The fossils embedded in the rock show a huge variety of species To protect from over-collection, the area became a World Heritage Site in 1981. Evidence for Plate Tectonics 3. Sea floor spreading - the mid Atlantic ridge forms a long mountain range running north to south down the length of the Atlantic ocean. Notes: Along spreading centers in the sea floor, melted rock rises through cracks, cools, and forms new crust that builds up mid-ocean ridges. Evidence for Plate Tectonics 4. Ridge sea floor age and thickness Notes: Youngest rocks found closest to the ridge. The further from the ridge centre the older the rocks and the thicker the sediments (silt and organic debris) deposited on the ocean floor. Evidence for Plate Tectonics 5. Magnetic field reversal - Paleomagnetism The Earth as a magnet Animation Notes: The Earth is like a large magnet. Notice the normal magnetic field can be reversed – called reverse polarity. Evidence for Plate Tectonics 5. Magnetic field reversal - Paleomagnetism Seafloor rock contains the magnetic mineral magnetite. When magma from the ridges rises and cools, it crystallizes, locking the magnetite crystals into alignment with the earth's magnetic field like the needle of a compass The Earth’s magnetic field fluctuates in intensity and occasionally even reverses itself. Notice the strongly patterned magnetic field reversals recorded on the seafloor provided the necessary proof of seafloor spreading. Specifically, they proved that new crust was continuously being generated at the mid-ocean ridges, where magma cooled and magnetite crystals "locked in" according to the orientation of the Earth's magnetic field at that time. Polarity of the Ocean Crust Evidence for Plate Tectonics 5. Magnetic field reversal - Paleomagnetism D = strong magnetic field at ridge (new rock being formed) – location of ridge C and E same distance on either side of D and same magnetic field strength – rock formed at same time on either side of ridge B and F same distance on either side of D and same magnetic field strength – rock formed at same time on either side of ridge Notice the magnetic field reversals