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Ch. 3 The Dynamic Earth
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Earth is a system with 4 parts Geosphere – rock Atmosphere – air Hydrosphere – water Biosphere – living things These 4 parts are constantly causing the earth to change.
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Composition of the earth – 3 layers Crust – outer layer, thin, made of lighter elements Mantle – middle layer, medium density rocks Lithosphere – rigid outer layer made of tectonic plates Asthenosphere – layer of rock that flows very slowly allowing the tectonic plates to move on top Core – innermost layer of dense elements Outer core – liquid nickel and iron Inner core – solid nickel and iron
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Lithosphere divided into pieces called plates Plates float on top of the asthenosphere Continents are on top of plates and move with them Plate boundaries – site of geological activity when plates collide, move away from or slide along each other Causes mountain building, earthquakes, and volcanoes
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Fault – break in the earth’s crust where blocks of the crust slide along each other Rocks (blocks) slip due to stress sending out vibrations of energy through the earth’s crust causing an earthquake Magnitude – measure of energy released by an earthquake Richter scale – 1 to 14 – measure of 7 = widespread damage Where? – along plate boundaries Can’t predict when, but can label hazard areas
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Volcano – mountains built by magma, rises from inside the earth to the surface Located along plate boundaries Ring of Fire – around pacific ocean Effects: human loss, building destruction, crop destruction, mudflows, breathing difficulties, can cause climate changes
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Erosion – removal and transport of surface materials Caused by wind and water Changes the shape of rocks and landscape – softer rocks erode more quickly Applachian mtns = rounded tops = older Rocky mtns = jagged = younger
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Mixture of gases surrounding the earth Keeps the earth warm so living things can survive Gases constantly put in and taken out Composition Nitrogen 78% Oxygen 21% Other 1% Atmospheric dust Air Pressure – atmosphere more dense near surface due to gravity
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Based on temp changes Troposphere – nearest to the surface, where all the weather occurs, temp ↓ as altitude ↑ Stratosphere – temp ↑ as altitude ↑ because ozone is absorbing uv rays from the sun Mesosphere – coldest layer Thermosphere - contains the auroras
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Energy comes from the sun Transferred in 3 ways Radiation – rays through space Conduction – objects touching Convection – by air currents – circulates heat through atmosphere Energy comes into atmosphere from sun Some is reflected by earth’s surface Some is absorbed by earth’s surface (1/2) Some is scattered by clouds and air Some is absorbed by clouds Earth’s surface radiates heat back into atmosphere Heat absorbed by greenhouse gases keeping the earth warm
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Process in which gases trap heat near the earth Life could not exist on earth without GE
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All water on or near the earth’s surface Required for life The water cycle – continuous movement of water into the air, onto land and back to water sources Evaporation – liquid to gas – ground to air Condensation – gas to liquid – water forms droplet on dust particle – forms clouds Precipitation – water falling from clouds
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World ocean – interconnected body of all the oceans Covers 70% of earth’s surface Made of: Pacific, Atlantic, Indian, Arctic Ocean water: contains more salts than freshwater Salinity – concentration of salts (avg. = 3.5%), different for different parts of the ocean Temperature zones – warmer at the surface, colder in deep water Function of world ocean – regulates temperatures in the atmosphere Ocean water absorbs radiation from the sun and releases heat (more slowly than land) Temp of atmosphere changes more slowly because of the ocean
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Ocean currents – stream like movements of water through the ocean, can be warm or cold, at the surface or deep Warm water won’t mix with cold so the currents can travel a great distance where they influence local climates on land
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30% of hydrosphere – most is frozen in glaciers and icecaps, the rest is in rivers, lakes, wetlands, and the ground River system – network of streams that drain an area of land Groundwater – water stored underground in rock or soil (aquifers)
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Narrow layer around the earth’s surface in which life can exist Includes uppermost part of geosphere, most of the hydrosphere, and the lower part of the atmosphere Fulfills 3 requirements for life: Liquid water, moderate temps, energy source Energy flow Closed system – energy comes in and goes out so it must be constantly supplied Matter is recycled through the system
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