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Chapter 5: Plate Tectonics Section 4: Sea-Floor Spreading 1. Mid-Ocean Ridges: an undersea mountain chain where new ocean floor is produced a. Scientists mapped the mid-ocean ridges using sonar in the 1900’s i. Sonar: a device that bounces sound waves off underwater objects and then records the echoes of these sound waves 1. The time it takes for the echo to arrive indicates the distance to the object ii. Most of the mountains in the mid-ocean ridge system lie hidden under hundreds of meters of water iii. In a few places, the ridge pokes above the surface 1. Ex: The island of Iceland is a part of the mid-ocean ridge 2. What is Sea-Floor Spreading? a. Harry Hess, an American geologist, carefully examined maps of the midocean ridge system i. He began to think Wegener was right about Pangaea ii. In 1960, he proposed sea-floor spreading 1. Sea-floor spreading: a process that continually adds new material to the ocean floor a. The sea floor spreads apart along both sides of a mid-ocean ridge as new crust is added. b. The ocean floors move like conveyor belts, carrying the continents along with them c. Begins at a mid-ocean ridge, which forms along a crack in the oceanic crust d. Molten material beneath the surface rises and erupts along the ridge e. Older rock moves outward on both sides of the ridge f. As the molten material cools, it forms a strip of solid rock in the center of the ridge g. It forms a new strip of rock 3. Evidence for Sea-Floor Spreading a. Supporting Evidence: eruptions of molten material, magnetic stripes in the rock of the ocean floor, and the ages of the rocks themselves i. Evidence from Molten Material 1. Scientists proved that new material is erupting along mid-ocean ridges 2. They took a submarine, Alvin, to a ridge valley where they found pillow shaped rocks, or like toothpaste squeezed from a tube a. Rocks like this only form when molten material hardens quickly after erupting under water ii. Evidence from Magnetic Stripes 1. While studying the ocean floors, scientists found that the Earth’s magnetic poles have reversed themselves many times. a. The last reversal happened 780,000 years ago 2. The rock that makes up the ocean floor lies in a pattern of magnetized “stripes” 3. The rock contains iron a. As the rock cooled, the iron bits lined up in the direction of Earth’s magnetic poles iii. Evidence from Drilling Samples 1. The Glomar Challenger, a drilling ship built in 1968, gathered samples from the ocean floor 2. This showed scientists that the newest rocks were always in the center of the ridges a. Made scientists assured that sea-floor spreading really has taken place 4. Subduction at Trenches a. Deep-ocean trenches: a deep valley along the ocean floor beneath which oceanic crust slowly sinks toward the mantle i. The oceanic crust bends downward ii. Part of the ocean floor sinks back into the mantle at deep-ocean trenches b. The Process of Subduction i. Subduction: the process by which ocean floor sinks beneath a deepocean trench and back into the mantle ii. Crust closer to a mid-ocean ridge moves away from the ridge and toward a deep-ocean trench iii.Sea-floor spreading and subduction work together 1. They move as if the ocean floor were a giant conveyor belt c. Subduction and Earth’s Oceans i. Subduction and sea-floor spreading can change the size and shape of the oceans ii. The ocean floor is renewed about every 200 million years iii.The Pacific Ocean covers almost 1/3 of Earth 1. It is shrinking 2. Sometimes a deep ocean trench swallows more oceanic crust than a mid-ocean ridge can produce 3. If the ridge does not add new crust fast enough, the width of the ocean will shrink iv. The Atlantic Ocean is expanding 1. It has only a few short trenches 2. The ocean floor has nowhere to go a. As the ocean floor spreads, the continents along its edges also move b. The whole ocean gets wider Review • What device is used to map the ocean floor? Review • How does new oceanic crust form? Review • Why does the rock of the ocean floor have a pattern of magnetic stripes? Review • Why is the Pacific Ocean shrinking?