1. Chapter 3 When you see this symbol, copy the slide. We will just discuss the other slides.

2. Do-Now-Copy AND answer the following questions on a separate sheet of paper. 1.How do you think you did on the ch. 1 Test? 2.How long did you study? 3.Did you fully complete the review sheet? 4.What could YOU do to improve your grade? 5.What could WE do to help you?

3. Objectives Describe the composition and structure of the Earth. Describe the Earth’s tectonic plates. Explain the main cause of earthquakes and their effects. Identify the relationship between volcanic eruptions and climate change. Describe how wind and water alter the Earth’s surface.

4. Standards SCSh7a SEV1a SEV1e

5. The Earth as a System Earth is an integrated system made of rock, air, water, & living things that all interact. Four parts: Geosphere solid, rocky part from core to crust Atmosphere mixture of gases we breathe as air Hydrosphere water on or near Earth’s surface Biosphere Earth’s surface to 9km high, living things found here

7. Discovering Earth’s Interior Use seismic waves –The same waves that travel through Earth’s interior during an earthquake –A similar process would be you tapping on a melon to see if it is ripe. –A seismic wave is altered by the nature of the material through which it travels. –Measure changes in the speed and direction of seismic waves that penetrate the interior of the planet. We have learned that the Earth is made up of different layers & have inferred what substances make up each layer.

8. The Composition & Structure of Earth Scientists have classified Earth’s composition and structure two different ways. –Chemical make up –Physical structure

9. The (Chemical) Composition of the Earth 3 Layers of Earth: Crust Thin, outermost layer, <1% of Earth’s mass Mantle Rock between crust & core, 64% of Earth’s mass Core Central part of Earth, made of densest elements These layers are made up of progressively denser material toward the center of the Earth. **These layers are based on CHEMISTRY.

10. The (Physical) Structure of Earth 5 Layers of Earth –Lithosphere Outermost layer, made of crust and upper mantle, divided into tectonic plates –Asthenosphere made of mantle rock that slowly flows –Mesosphere “middle sphere,” lower mantle –Outer Core Outer shell of core, made of liquid nickel and iron –Inner Core Innermost, solid nickel and iron **These layers are based on PHYSICAL PROPERTIES.

12. Plate Tectonics Tectonic plates are blocks of lithosphere made of the crust and the rigid, outermost part of the mantle & glide across the asthenosphere. Major tectonic plates –Pacific, North America,South America, Africa, Eurasian, & Antarctic plates.

14. Plate Boundaries Much geological activity occurs here Enormous forces are generated with these actions causing mountains to form, earthquakes to shake the crust, & volcanoes to erupt along the plate boundaries.

15. Earthquakes A fault is a break in the Earth’s crust along which blocks of the crust slide relative to one another. –When rocks that are under stress suddenly break along a fault, a series of ground vibrations (earthquakes) is set off. Occurring all the time The measure of the energy released by an earthquake is called magnitude. –The smallest magnitude that can be felt is 2.0, and the largest magnitude ever recorded is 9.5. Magnitudes greater than 7.0 cause widespread damage.

16. Where do Earthquakes Occur? At or near tectonic plate boundaries because of the enormous stresses that are generated when tectonic plates separate, collide or slip past each other. –Over the past 15 million to 20 million years, large numbers of earthquakes have occurred along the San Andreas fault in California, where parts of the North America plate and the Pacific plate are slipping past one another.

18. Earthquake Hazard Can’t predict when earthquakes will take place Information about where earthquakes are likely to occur helps people prepare. An area’s earthquake-hazard level is determined by past and present seismic activity. Earthquake-resistant buildings, built in high risk areas, are slightly flexible so that they can sway with the ground motion preventing them from collapsing.

19. Volcanoes Mountains built from magma, or melted rock, that rises from the Earth’s interior to the surface, & can occur on land or in the sea. Often located near tectonic plate boundaries where they are colliding/separating –Most (active) are located along tectonic plate boundaries that surround the Pacific Ocean (Ring of Fire).

20. Remember this? Environmental problems are divided into three categories: –Local –Regional –Global

21. Local Effect of Volcanic Eruptions Clouds of host ash, dust, and gases can flow down the slope of a volcano at speeds of up to 200 km/hr and sear everything in their path. During an eruption, volcanic ash can mix with water and produce mudflow that runs downhill. In addition, ash that falls to the ground can cause buildings to collapse under its weight, bury crops, damage the engines of vehicles, and cause breathing difficulties.

22. Global Effects of Volcanic Eruptions Major volcanic eruptions can change Earth’s climate for several years. In large eruptions, clouds of volcanic ash and sulfur rich gases may reach the upper atmosphere, and spread across the planet reducing the amount of sunlight that reaches the Earth’s surface. The reduction in sunlight can cause a drop in the average global surface temperature.

23. Erosion Earth’s surface is continually battered by wind & scoured by running water. Is the process where Earth’s surface are loosened, dissolved, or worn away & transported by a natural agent, like wind, water, ice or gravity. –Wears down rocks & makes them smoother as times passes Older mountains are therefore smoother than younger ones.

24. Objectives Describe the composition of the Earth’s atmosphere. Describe the layers of the Earth’s atmosphere. Explain three mechanisms of heat transfer in Earth’s atmosphere. Explain the greenhouse effect.

25. Standards SCSh7a SEV1e SEV3a

26. The Atmosphere The atmosphere is a mixture of gases that surrounds a planet. –Nitrogen, oxygen, carbon dioxide, and other gases Gases are added to & removed from the atmosphere. –For example: –Animals remove oxygen when they breathe in & add carbon dioxide when they breath out. –Volcanic eruptions also add gases to the atmosphere, while vehicles both add & remove gases. Insulates Earth’s surface

27. Composition of the Atmosphere Nitrogen makes up 78% of Earth’s atmosphere –enters when volcanoes erupt & dead plants/animals decay Oxygen is the 2 nd most abundant gas & is primarily produced by plants. Other gases such as argon, carbon dioxide, methane, & water vapor make up the rest. Many types of tiny, solid particles, or atmospheric dust

28. Air Pressure Earth’s atmosphere is pulled toward our surface by gravity, so the atmosphere is denser near the Earth’s surface. Air becomes less dense with elevation, so breathing at higher elevations is more difficult.

29. Layers of the Atmosphere 4 layers based on temperature changes that occur at different distances above the Earth’s surface: The Troposphere The Stratosphere The Mesosphere The Thermosphere

30. Troposhere Lowest layer Temperature drops at a constant rate as altitude increases Where weather conditions exist Densest atmospheric layer & extends to 18 km above Earth’s surface

31. Stratosphere Lies immediately above the troposphere & extends from about 10 to 50 km above the Earth’s surface Temperature rises as altitude increases because ozone in the stratosphere absorbs the sun’s ultraviolet (UV) energy & warms the air. Because ozone absorbs UV radiation, it reduces the amount of UV radiation that reaches the Earth. UV radiation that does reach Earth can damage living cells.

32. Mesosphere Above the stratosphere Extends to an altitude of about 80 km. Coldest layer of the atmosphere where temperatures have been measured as low as –93ºC.

33. Thermosphere Farthest from Earth’s surface Nitrogen & oxygen absorb solar radiation resulting in temperatures measuring above 2,000 ºC. Air is so thin that air particles rarely collide, so little heat is transferred, & wouldn’t feel hot to us The absorption of X rays & gamma rays by N & O causes atoms to become electrically charged (IONS). The lower thermosphere is called the ionosphere. –Ions can radiate energy as light, & these lights often glow in spectacular colors in the night skies near the Earth’s North & South Poles.

34. Energy Transfer in the Atmosphere Radiation is the energy that is transferred as electromagnetic waves, such as visible light & infrared waves. Conduction is the transfer of energy as heat through a material. Convection is the movement of matter due to differences in density that are caused by temperature variations an can result in the transfer of energy as heat.

36. Heating of the Atmosphere Solar energy reaches the Earth as electromagnetic radiation –visible light, infrared radiation, & ultraviolet light About 1/2 the solar energy that enters the atmosphere passes through it and reaches the Earth’s surface, while the rest of the energy is absorbed or reflected in the atmosphere by clouds, gases, & dust or it is reflected by Earth’s surface. The Earth does not continue to get warmer because the oceans & the land radiate the absorbed energy back into the atmosphere.

37. The Movement of Energy in the Atmosphere As a current of air rises it cools, & eventually becomes more dense than the air around it & sinks. It then moves back toward the Earth until heated & less dense & then begins to rise again. The continual process of warm air rising & cool air sinking & moving air in a circular motion is called a convection current.

38. The Greenhouse Effect Warming of the surface & lower atmosphere of Earth that occurs when carbon dioxide, water vapor, & other gases in the air absorb & reradiate infrared radiation The gases in the atmosphere that trap & radiate heat are called greenhouse gases. Most abundant greenhouse gases: –water vapor, carbon dioxide, methane, and nitrous oxide The quantities of carbon dioxide & methane in the atmosphere vary considerably as a result of natural & industrial processes.

40. Objectives Name the three major processes in the water cycle. Describe the properties of ocean water. Describe the two types of ocean currents. Explain how the ocean regulates Earth’s temperature. Discuss the factors that confine life to the biosphere. Explain the difference between open and closed systems.

41. Standards SCSh7a SEV1d SEV2b SEV2d SEV3a

42. The Hydrosphere Includes all of the water on or near Earth’s surface –oceans, lakes, rivers, wetlands, polar ice caps, soil, rock layers beneath Earth’s surface, & clouds

43. The Water Cycle Continuous movement of water from the ocean to the atmosphere to the land & back to the ocean Water continually evaporates (liquid to a gas) from the Earth’s oceans, lakes, streams, & soil. Water vapor forms water droplets (condensation=gas to liquid) on dust particles which then form clouds in which the droplets collide to create larger, heavier drops that then fall as precipitation (rain, snow, sleet, hail).

44. Earth’s Oceans Play important roles in the regulation of the planet’s environment & temperature.

45. Ocean Water The difference between ocean water & fresh water is that ocean water contains more salts. Salinity is a measure of the amount of dissolved salts in a given amount of liquid. –Lower in places that get a lot of rain or where fresh water flows in to the sea –Higher where water evaporates rapidly & leaves the salts behind –Most salt is sodium chloride –Many other elements present

46. Fresh Water and River Systems Fresh water is water that contains insignificant amounts of salts. Most is in icecaps & glaciers Also in lakes, rivers, wetlands, the soil, & atmosphere

47. Remember The Biosphere? The only part of Earth where life exists Extending about 11 km into the ocean & about 9 km into the atmosphere The biosphere is located near Earth’s surface because most of the sunlight is available near the surface. The materials that organisms require must be continually recycled. Gravity allows a planet to maintain an atmosphere & to cycle materials.

48. Energy Flow in the Biosphere The energy used by organisms must be obtained in the biosphere & must be constantly supplied for life to continue. When an organism dies, its body is broken down & the nutrients in it are used by other organisms (flow of energy). Closed systems=can’t exchange matter or energy with surroundings Open systems=can exchange both matter & energy with surroundings Earth is… –A closed system with respect to matter –An open system for energy as energy travels from plant to animal which is eaten by other animals. Some energy is lost as heat to the environment.