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EARTH’S INTERIOR Chapter 1 – Section 1. A. Exploring inside the Earth 1. Direct evidence a. Rock samples 2. Indirect evidence a. Seismic waves.

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Presentation on theme: "EARTH’S INTERIOR Chapter 1 – Section 1. A. Exploring inside the Earth 1. Direct evidence a. Rock samples 2. Indirect evidence a. Seismic waves."— Presentation transcript:

1 EARTH’S INTERIOR Chapter 1 – Section 1

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3 A. Exploring inside the Earth 1. Direct evidence a. Rock samples 2. Indirect evidence a. Seismic waves

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5 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

6 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

7 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

8 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

9 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.

10 Chapter 1 – Section 2 Convection and the Mantle

11 A. Types of Heat Transfer 1. Radiation a. Transfer of energy through space b. No direct contact c. Sunlight, fire

12 2. Conduction a. Heat transfer within a material or between materials b. Some of the heat transfer within the earth

13 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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15 B. Convection Currents 1. Flow that transfers heat within a fluid

16 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

17 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.

18 Chapter 1 – Section 3 Drifting Continents

19 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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21 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

22 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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26 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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