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Science and Technology I Mid-Year Exam 2012 A Whole Lotta Shakin’ Going On Review EARTH’S STRUCTURE • The Earth has three main layers: – Crust (outer layer) – Mantle (middle layer) – Core (inner layer) • Inner core • Outer core QuickTime™ and a decompressor are needed to see this picture. TECTONIC PLATES • The lithosphere is made up of the crust and upper mantle. • The lithosphere is broken into pieces called tectonic plates. CONTINENTAL DRIFT • The tectonic plates are constantly moving because the mantle flows since it is partially melted. This moves the continents. • Alfred Wegener developed the theory after making two observations: 1. The continents looked like they fit together 2. Fossils of land animals found on both sides of the ocean on different continents. MOVEMENTS • The tectonic plates move in different directions: QuickTime™ and a decompressor are needed to see this picture. moving together QuickTime™ and a decompressor are needed to see this picture. moving apart QuickTime™ and a decompressor are needed to see this picture. sliding past each other OROGENESIS • Orogenesis means mountain formation QuickTime™ and a decompressor are needed to see this picture. • Mountains occur at convergence zones, when the tectonic plates have about the same weight. • Erosion changes the mountain over time. EARTHQUAKES • Usually occur at transform boundaries. • As the plates try to push past each other, they get stuck. When they finally manage to break free, a lot of energy is released and the ground shakes. That is an earthquake. • The location where the earthquake began is called the epicenter. Quick Time™ and a decompressor are needed to see this picture. EARTHQUAKES • Seismologists (people who study earthquakes) use a machine called a seismograph to detect and record earthquakes. • Earthquakes are measured on the Richter scale, which ranges from 0-10 (10 is the worst possible earthquake). VOLCANOES • Volcanoes usually occur at convergent or divergent boundaries. • At a convergent boundary, one tectonic plate is heavier than another, and so it slips underneath, melts, and the pressure inside the earth forces the magma to come out. • When the melted mantle is inside the Earth, it is called magma. When it is outside, it is called lava. QuickTime™ and a decompressor are needed to see this picture. VOLCANOES • The Ring of Fire is an area in the Pacific Ocean where the majority of volcanoes occur. QuickTime™ and a decompressor are needed to see this picture. TSUNAMIS • The word tsunami means giant wave. • Tsunamis are caused by an underwater earthquake or volcano, which makes waves. As the waves approach land, the become bigger and more powerful. QuickTime™ and a decompressor are needed to see this picture. SEISMOGRAPHS • A tsunami measures the intensity and duration of an earthquake. The ones we made in class looked like this: SEISMOGRAPHS • To make our seismographs, we used: – A cereal box – A cup – String – Sand – Paper – Pen SEISMOGRAPHS • When we simulated an earthquake, the box shook, but the sand kept the cup and the pen steady. • We pulled the paper through the slit in the box and saw how the pen made earthquake lines. SEISMOGRAPHS • A teacher could use this type of seismograph in class to demonstrate how a real seismograph works.