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Published byHollie Merritt Modified over 8 years ago
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EARTH’S INTERIOR Chapter 1 – Section 1
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A. Exploring inside the Earth 1. Direct evidence a. Rock samples 2. Indirect evidence a. Seismic waves
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B. Journey to the Center of Earth 1. Temperature a. Increases with depth (after 20 meters) b. Results from- a. formation of the earth b. decay of radioactive materials 2. Pressure a. Increases with depth b. Results from weight of rocks above
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C. The Crust 1. The skin of the earth 2. Oceanic a. Thin b. Dense c. Rock - basalt 3. Continental a. Thick b. Less dense c. Rock - granite
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D. Mantle 1. Layer of hot solid rock 2. Lithosphere a. Upper mantle and crust 3. Asthenosphere a. Softer part of mantle b. Bends/flows like plastic 4. Lower Mantle a. Solid b. Extends to core
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E. The Core 1. Made of iron and nickel 2. Outer Core a. Molten (liquid) metal b. Cause of Earth’s magnetic field 3. Inner Core a. Solid metal
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Answer in your Notebook Questions 1-3 on page 13 AND Questions 1-4 on page 12 Use complete sentences when answering the questions. Be sure to indicate what page number your questions are from in your notebook.
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Chapter 1 – Section 2 Convection and the Mantle
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A. Types of Heat Transfer 1. Radiation a. Transfer of energy through space b. No direct contact c. Sunlight, fire
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2. Conduction a. Heat transfer within a material or between materials b. Some of the heat transfer within the earth
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3. Convection a. Heat transfer by the movement of fluids b. Caused by the differences of temperature and density of a fluid Hotter = particles farther apart = less dense Colder = particles closer together = more dense
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B. Convection Currents 1. Flow that transfers heat within a fluid
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C. Convection Currents in Earth 1. Heat from core and mantle cause convection currents within the mantle 2. Very Slowly within the solid mantle Mantle simulation
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Answer in your Notebook Questions 1-3 on page 17 Use complete sentences for all questions! Be sure to indicate what page number your questions are from in your notebook.
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Chapter 1 – Section 3 Drifting Continents
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A. Continental Drift 1. Alfred Wegener – 1910 a. Studied land features, fossils, and evidence of climate change b. Continental drift - all continents were once together in a single landmass and have since drifted apart c. Pangaea – “all lands” i. 300 million years ago
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B. Evidence for Continental Drift 1. Land Features a. Mountain ranges b. Coal fields 2. Fossils a. Similar organisms found on continents separated by oceans i. Glossopteris – Fernlike plant ii. Mesosaurus and Lystrosaurus – freshwater reptile
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3. Climate a. Fossils of organisms from warmer climates support movement of continents i. Equator = warm climate ii. Poles = colder climate b. Evidence of glaciers indicate colder climate
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C. Wegener’s Hypothesis Rejected 1. Idea rejected because he could not identify the cause of continental drift 2. Continued his work and died in 1930 exploring Greenland’s glacier
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