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Continental Margins • • • Continental shelf: shallowest part of the margin Continental Slope: a steeper part Continental Rise: gently sloping region at the base of the of the continental slope; consists of sediment that piles up on the sea floor Deep Sea Basins 1. 2. 3. 4. 5. Abyssal plain: flat area Seamounts: old volcanos and islands Trenches: deepest part of the ocean Mid Oceanic Ridge: main feature of the ocean floor Central Rift Valley: great gap at the center where plates are pulling apart Structure of Earth • Earth Originated 4.5 billion years ago by the Big Bang • Earth’s materials were sorted by density – Densest is found at the center and the least on the outside Structure of Earth • Internal Structure – Inner Core: composed of Fe Ni, high pressure and temperatures reach 5,000oC; solid in nature – Outer Core: Same elements and temperature but less pressure so is a liquid – Mantle: Contains Si and O, semisolid state that moves like molasses • Asthenoshere-upper mantle – Crust: outermost layer, extremely thin, rigid skin floating on the mantle (Oceanic and Continental) • Lithosphere-uppermost mantle and crust Earth’s Crust • Continental Crust – Consist of granite – 3.8 byo – Not dense and thick •Oceanic Crust –Consist of Basalt –200 myo –Dense and thin Continental Drift • Proposed in 1920 by Alfred Wegener • Theory: states that all the continents had once been joined in a single super continent called Pangaea, 180 mya • Wegener was laughed at due his inability to proposed a mechanism for the movement of continents Continental Drift • Evidence – Coal deposits – geological formations – fossils match up on opposite sides of the Atlantic – Jigsaw puzzle like appearance of continents – Glacial rock deposits – Limestone and salt deposits Seafloor Spreading Evidence • Discovery of the Mid Ocean Ridge – Discovered using sonar – Interrupted by large geological fault called transform faults – EX: Mid-Atlantic Ridge and East Pacific Rise Seafloor Spreading Evidence • Magnetic Reversals – – – Discovered by the Glomar Challenger in 1968 Symmetric Pattern of Magnetic Bands in the seafloor from reversals of the magnetic poles Opposite matching bands on either side of mid-oceanic ridge Seafloor Spreading Evidence • Sediment Age and thickness – – Discovered by the Glomar Challenger Thickest and oldest sediments are found farthest from the Mid Ocean Ridge Seafloor Spreading • Proposed by Henry Hess in 1960’s • Theory: states that mantle rises up at the Mid Ocean Ridges is then cooled, placed on the seafloor and moved towards the continents • Mechanism was thought to be convection of the mantle beneath the seafloor Plate Tectonics • Combination of Continental Drift and Seafloor Spreading • Theory: earth’s surface is covered by a fairly rigid layer composed of the crust and the uppermost part of the mantle called the lithosphere that is broken into plates which move over the mantle Plate Collisions • Oceanic Plate to Oceanic Plate – Causes trenches, earthquakes, volcanoes and island arcs – EX: Aleutian Island in Alaska Plate Collisions • Oceanic Plate and Continental Plate – – Creates a trench, earthquakes, continental volcanoes Seafloor is destroyed at the trench which explains why the seafloor is so young Plate Collisions • Continental Plate and Continental Plate – – Create mountains EX: Himalayan Mountains Plate Movements • Apart: plates do move apart and create new crust – EX: mid ocean ridge and Iceland • Shear Boundary: plate are able to slide past each other – EX: California’s San Andreas Fault Marine Sediments • Hydrogenous – Result from chemical reactions within seawater • Cosmogenous – Result from outer space • Lithogenous Sediment – Formed from the weathering and erosion of rocks • Biogenous Sediment – Created from the skeleton or shells of marine organisms – Calcareous: made of calcium carbonate – Siliceous: made of silica Hot Spots • Stationary plume of magma under a moving plate • Creates volcanic islands in the middle of plates EX: Hawaiian Islands and the Emperor Seamount Chain