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Chapter 2 Notes I. The Structure of the Earth A. Three main layers of the earth 1. 2. 3. Core – center of the earth made up of iron and nickel Mantle – surrounds the core and has several layers Contains magma, which is molten rock Crust – thin layer of rock at the earth’s surface B. Four basic spheres found on and above the earth 1. Biosphere – where plants and animals live Consists of the atmosphere, lithosphere, hydrosphere 2. Atmosphere – layer of gases surrounding the earth 3. Lithosphere – solid rock portion of the earth’s surface 4. Hydrosphere – water elements on the earth C. Continental Drift Hypothesis States that the earth was once a supercontinent that divided and slowly drifted apart over millions of years. II. Bodies of Water A. B. C. Oceans and Seas Ocean covers 71% of our planet Ocean water circulates by currents, waves, and tides Water and air currents carry heat to other places. Hydrologic Cycle – Evaporation, Condensation, Precipitation, Collection Ground Water Water held in the pores of rock Water Table – level at which the rock is saturated III. Landforms A. B. Landforms – naturally formed features on the surface of the earth Oceanic Landforms Continental shelf – the earth’s surface from the edge of a continent to the deep part of the ocean. C. Continental Landforms Relief – difference in elevation of a landform from its lowest point to its highest point. o 4 Categories of Relief: 1. Mountains 3. Plains 2. Hills 4. Plateaus Topography – combination of the surface shape and composition of the landforms and their distribution in a region. INTERNAL FORCES SHAPING THE EARTH IV. Plate Tectonics A. B. C. D. Tectonic Plates – enormous moving pieces of the earth’s Lithosphere Plate Movement ( illustrated on pgs. 38 & 39) 1. spreading or moving apart 2. subduction, or diving under another plate 3. collision, or crashing into one another 4. sliding past each other in a shearing motion Three types of boundaries mark plate movements 1. Divergent boundary – plates move apart, spreading horizontally. 2. Convergent Boundary – plates collide 3. Transform Boundary – plates slide past one another Folds and Faults Folds – rock bends Faults – rock cracks V. Earthquakes A. Earthquakes – violent movement of the earth Caused by the grinding and slipping of plates along a fault Effects of earthquakes: o Landslides, displacement of land, fires, collapsed buildings, and tsunamis Seismograph – a device that measures the size of the waves created by an earthquake Richter Scale – scale that determines the relative strength of an earthquake VI. Volcanoes A. Volcanic Action Eruption – hot lava, gases, ash, dust, and rocks explode out of vents in the earth’s crust, often creating a hill or mountain. B. Ring of Fire A zone around the rim of the Pacific Ocean where 8 major tectonic plates meet. EXTERNAL FORCES SHAPING THE EARTH VII. Weathering A. Two Types of Weathering: 1. Mechanical Weathering – processes that break rock into smaller pieces. * Does not change the composition of the rock * Only changes its size 2. Chemical Weathering – rock is changed into a new substance VIII. Erosion - Occurs when weathered material is moved by the action of wind, water, ice, or gravity. A. Water Erosion – water flows in a stream or river picking up loose material and moving it downstream. When a river enters the ocean, the sediment is deposited in a fan-like landform called a delta. Waves reduce or increase beaches Sediment deposited by wave action may build up sandbars and islands. B. Wind Erosion – wind transports and deposits sediment in other locations. Landforms produced by wind erosion are: sand dunes, sculpted rocks, and loess deposits. C. Glacial Erosion – glaciers move downslope as a result of gravity. Glaciers change the land in the following ways: o Slice out valleys o Form hills called moraines o Leave ridges called eskers o Create depressions called kettles IV. Building Soil A. Weathering and erosion are a part of the process of forming soil. B. Soils Factors: Parent material Relief Organisms Climate Time C. Variety of soils, and the climate in which they are found, determine the types of vegetation that can grow in a location.