The top documents tagged [liquid inner core]

Chapter 2
Technology Chapter 2

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Seismic Waves of Earthquakes By: Annette Miles. The location of the beginning of an earthquake is its ______. This is the ____________ point in the crust
Documents Seismic Waves of Earthquakes By: Annette Miles. The location of the beginning of an earthquake is its ______. This is the ____________ point in the crust

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Section 1: Earth’s Interior Who Studies Earth’s Interior? Geologists Scientists who study the forces that make and shape planet Earth. They study
Documents Section 1: Earth’s Interior Who Studies Earth’s Interior? Geologists Scientists who study the forces that make and shape planet Earth. They study

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Earthquakes Earth shaking. Basic Earthquake Words: The epicenter and focus Force pushing Force pushing Fault is a crack That forms Along the break An
Documents Earthquakes Earth shaking. Basic Earthquake Words: The epicenter and focus Force pushing Force pushing Fault is a crack That forms Along the break An

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Next Copyright © by Houghton Mifflin Harcourt Publishing Company Chapter 2 Geography A Living Planet Physical Geography The geography and structure of
Documents Next Copyright © by Houghton Mifflin Harcourt Publishing Company Chapter 2 Geography A Living Planet Physical Geography The geography and structure of

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Chapter 2 A Living Planet The geography and structure of the earth are continually being changed by internal forces, like plate tectonics, and external
Documents Chapter 2 A Living Planet The geography and structure of the earth are continually being changed by internal forces, like plate tectonics, and external

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Warm up 3 Facts learned yesterday 1. 2. 3. 1. A Living Planet The geography and structure of the earth are continually being changed by internal forces,
Documents Warm up 3 Facts learned yesterday 1. 2. 3. 1. A Living Planet The geography and structure of the earth are continually being changed by internal forces,

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TERRA FIRMA Plate interactions. EARTH’S INTERIOR crust under the oceans - basalt (more dense) crust under the continents - granite (less dense) mantle
Documents TERRA FIRMA Plate interactions. EARTH’S INTERIOR crust under the oceans - basalt (more dense) crust under the continents - granite (less dense) mantle

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Interior Structure of Earth Compositional Layering (Chemical) Crust - variable thickness and composition Continental 10 - 70 km thick Oceanic 8 - 10 km
Documents Interior Structure of Earth Compositional Layering (Chemical) Crust - variable thickness and composition Continental 10 - 70 km thick Oceanic 8 - 10 km

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Planets in The Solar System. Mercury cannot be imaged well from Earth; best pictures are from Mariner 10 Surface Features on Mercury
Documents Planets in The Solar System. Mercury cannot be imaged well from Earth; best pictures are from Mariner 10 Surface Features on Mercury

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Chapter 7 Earth. Mantle Two-part core Thin crust Hydrosphere (oceans) Atmosphere Magnetosphere Structure of Planet Earth
Documents Chapter 7 Earth. Mantle Two-part core Thin crust Hydrosphere (oceans) Atmosphere Magnetosphere Structure of Planet Earth

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Planets Planets orbit a star like our sun Planets do not give off light or heat energy
Documents Planets Planets orbit a star like our sun Planets do not give off light or heat energy

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