1. Next Copyright © by Houghton Mifflin Harcourt Publishing Company Chapter 2 Geography A Living Planet Physical Geography The geography and structure of the earth are continually being changed by internal forces, like plate tectonics, and external forces, like the weather.

2. Copyright © by Houghton Mifflin Harcourt Publishing Company Next Previous Chapter 2 Geography Looking at the Earth Physical Geography SECTION 2 SECTION 4 SECTION 3 The Earth Inside and Out Bodies of Water and Landforms Internal Forces Shaping the Earth External Forces Shaping the Earth SECTION 5 SECTION 2 SECTION 1 SECTION 4 SECTION 3

3. Copyright © by Houghton Mifflin Harcourt Publishing Company Next Previous Chapter 2 Geography The Earth Inside and Out Section-1 The earth is the only habitable planet in the sun’s solar system. The drifting of the continents shaped the world we live in today.

4. Copyright © by Houghton Mifflin Harcourt Publishing Company Next Previous Chapter 2 Geography Section-1 Continental Puzzle Earth The Earth Inside and Out The seven continents on earth fit together like a jigsaw puzzle Continents—landmasses above water on Earth Francis Bacon (1620) first to suggest 7 continents were once one

5. Copyright © by Houghton Mifflin Harcourt Publishing Company Next Previous Chapter 2 Geography The Earth’s Neighborhood The Solar System Earth is third planet in the solar system of the sun Sun is medium-sized star at edge of the Milky Way galaxy The solar system includes: − sun and nine known planets − comets—icy spheres orbiting the sun − asteroids—large chunks of rocky material orbiting the sun

6. Copyright © by Houghton Mifflin Harcourt Publishing Company Next Previous Chapter 2 Geography 1 Inside the Earth The core is the center of the earth; made up of iron, nickel Outer core is liquid; inner core is solid The mantle surrounds the core: − has several layers − contains most of Earth’s mass Matters of Size The Structure of the Earth Circumference of the earth: about 24,900 miles Diameter of the earth: about 7,900 miles Continued…

7. Copyright © by Houghton Mifflin Harcourt Publishing Company Next Previous Chapter 2 Geography 1 On and Above the Earth Atmosphere is the layer of gasses surrounding the earth: − contains oxygen − protects Earth from radiation, space debris − is the medium for weather and climate Continued… Inside the Earth The Structure of the Earth {continued} Magma—molten rock that forms in the mantle Crust—thin layer of rock at Earth’s surface

8. Copyright © by Houghton Mifflin Harcourt Publishing Company Next Previous Chapter 2 Geography Continued… On and Above the Earth The Structure of the Earth {continued} Lithosphere—solid rock portion of Earth’s surface, forms ocean floor Hydrosphere—water elements on Earth including atmospheric water Biosphere—atmosphere, lithosphere, hydrosphere combined Plants and animals live within biosphere

9. Copyright © by Houghton Mifflin Harcourt Publishing Company Next Previous Chapter 2 Geography Continental Drift The Structure of the Earth {continued} Continental Drift—1912 hypothesis of Alfred Wegener: Earth once one supercontinent; Wegener calls it Pangaea, “all earth” Pangaea splits into many plates that slowly drift apart

10. Copyright © by Houghton Mifflin Harcourt Publishing Company Next Previous Chapter 2 Geography Bodies of Water and Landforms Section-2 Water covers about three-fourths of the earth’s surface. The earth’s surface displays a variety of landforms.

11. Copyright © by Houghton Mifflin Harcourt Publishing Company Next Previous Chapter 2 Geography Continued… Ocean Motion Bodies of Water Bodies of Water and Landforms Section-2 The ocean circulates through currents, waves, tides Currents act like rivers flowing through the ocean Waves are swells or ridges produced by winds Tides are the regular rising and falling of the ocean − created by gravitational pull of the moon or sun Motion of ocean helps distribute heat on the planet − winds are heated and cooled by ocean water

12. Copyright © by Houghton Mifflin Harcourt Publishing Company Next Previous Chapter 2 Geography Lakes, Rivers, and Streams Lakes hold more than 95% of the earth’s fresh water Freshwater lakes, like the Great Lakes, are result of glacial action Saltwater lakes form when outlet to sea is cut off: − streams and rivers carry salts into lake − salts build up with nowhere to go Continued… Bodies of Water {continued} Hydrologic Cycle Hydrologic Cycle—cycle of water between atmosphere, oceans, earth

13. Copyright © by Houghton Mifflin Harcourt Publishing Company Next Previous Chapter 2 Geography Ground Water Ground water—water held in the pores of rock Water table—level at which the rock is saturated Bodies of Water {continued} Lakes, Rivers, and Streams Rivers and streams carry water to and from larger bodies of water Tributaries are smaller rivers, streams that feed into larger ones Drainage basin—area drained by river and its tributaries

14. Copyright © by Houghton Mifflin Harcourt Publishing Company Next Previous Chapter 2 Geography 2 Oceanic Landforms Continental shelf—sea floor from continent’s edge to deep ocean Sea floor has ridges, valleys, canyons, plains, mountain ranges Islands are formed by volcanoes, sand, or coral deposits Landforms Landforms are naturally formed features on Earth’s surface

15. Copyright © by Houghton Mifflin Harcourt Publishing Company Next Previous Chapter 2 Geography Section-3 Internal forces reshape the earth’s surface. Internal forces shaping the earth often radically alter the lives of people as well. Internal Forces Shaping the Earth

16. Copyright © by Houghton Mifflin Harcourt Publishing Company Next Previous Chapter 2 Geography Continental Landforms Landforms Internal Forces Shaping the Earth Section-3 Relief—difference in landform elevation from lowest to highest point Four categories of relief—mountains, hills, plains, plateaus Topography—the configurations and distribution of landforms Topographic map shows vertical dimensions, relationship of landforms

17. Copyright © by Houghton Mifflin Harcourt Publishing Company Next Previous Chapter 2 Geography Continued… Plate Tectonics The Earth Moves Tectonic plates are massive, moving pieces of Earth’s lithosphere Plates ride above circulating, heated rock Geographers study plate movements to understand: − how the earth is reshaped − how earthquakes and volcanoes are formed Plate Movement Plates move in one of four ways: − by spreading, or moving apart − subduction, or diving under another plate − collision, or crashing together − sliding past each other in a shearing motion

18. Copyright © by Houghton Mifflin Harcourt Publishing Company Next Previous Chapter 2 Geography Continued… Plate Tectonics {continued} Plate Movement Movement of plates effects surface of the earth Saudi Arabia–Egypt’s plates are spreading apart, widening Red Sea India’s plate is crashing into Asian continent, building up Himalayas Three types of boundaries mark plate movement: − divergent boundary − convergent boundary − transform boundary

19. Copyright © by Houghton Mifflin Harcourt Publishing Company Next Previous Chapter 2 Geography 3 Two plates meeting can cause folding, cracking of rock Fault occurs when pressure causes rock to fracture, or crack Fault line is place where plates move past each other Plate Tectonics {continued} Folds and Faults

20. Copyright © by Houghton Mifflin Harcourt Publishing Company Next Previous Chapter 2 Geography 3 Earthquake Locations Location in the earth where an earthquake begins is called the focus Epicenter—the point directly above focus on the earth’s surface Nearly 95% of earthquakes occur at tectonic plate boundaries Continued… An earthquake occurs when plates grind or slip at a fault line A seismograph detects earthquakes and measures the waves they create Earthquakes The Earth Trembles

21. Copyright © by Houghton Mifflin Harcourt Publishing Company Next Previous Chapter 2 Geography Tsunami Tsunami, a giant ocean wave, begins at epicenter of an earthquake: − travels at up to 450 mph − waves of 50–100 ft. or higher Earthquakes {continued} Earthquake Damage Earthquakes release energy in the form of motion, causing: − landslides − land displacement − fires (broken gas lines) − collapsed buildings Richter Scale—numeric scale showing relative strength of earthquake

22. Copyright © by Houghton Mifflin Harcourt Publishing Company Next Previous Chapter 2 Geography Continued… Volcanoes The Explosive Earth Volcano—underground materials pour from crack in the earth’s surface Most volcanoes occur at tectonic plate boundaries Volcanic Action Eruption—lava, gases, ash, dust, explode from vent in Earth’s crust Lava—magma that has reached the earth’s surface; may create landform

23. Copyright © by Houghton Mifflin Harcourt Publishing Company Next Previous Chapter 2 Geography Volcanoes {continued} Ring of Fire Ring of Fire—zone around rim of Pacific Ocean: − meeting point of eight tectonic plates − vast majority of the earth’s active volcanoes located here “Hot spots” are where magma rises to surface from mantle Hot springs, geysers indicate high temperatures in earth’s crust Some volcanic action is useful: − volcanic ash produces fertile soil − hot springs are tapped for heat, energy

24. Copyright © by Houghton Mifflin Harcourt Publishing Company Next Previous Chapter 2 Geography Section-4 External Forces Shaping the Earth Wind, heat, cold, glaciers, rivers, and floods alter the surface of the earth. The results of weathering and erosion change the way humans interact with the environment.

25. Copyright © by Houghton Mifflin Harcourt Publishing Company Next Previous Chapter 2 Geography Mechanical Weathering Mechanical weathering—processes that break rock into smaller pieces Does not change rock’s composition, only size Examples: frost, plant roots, road construction, mining Continued… Weathering Section-4 External Forces Shaping the Earth Altering the Landscape Weathering—processes that alter rock on or near the earth’s surface Can change landscapes over time and create soil for plant life Sediment—mud, sand, silt created by weathering processes

26. Copyright © by Houghton Mifflin Harcourt Publishing Company Next Previous Chapter 2 Geography 4 Weathering {continued} Chemical Weathering Chemical weathering—interaction of elements creates new substance Example: when iron rusts it reacts to oxygen in air and crumbles Warm, moist climates produce more chemical weathering than cool, dry

27. Copyright © by Houghton Mifflin Harcourt Publishing Company Next Previous Chapter 2 Geography 4 Water Erosion Most streams erode vertically and horizontally − a valley cut by a stream gets deeper, wider; forms v-shaped valley − a river deposits sediment at ocean, creates delta—fan-like landform Continued… Erosion Weathered Material Moves Erosion—when weathered material moves by winds, water, ice, gravity − movement grinds rock into smaller pieces, carries to new location Example: water carries topsoil from hill to river, river narrows

28. Copyright © by Houghton Mifflin Harcourt Publishing Company Next Previous Chapter 2 Geography Erosion {continued} Wind Erosion Wind transports sediment from one place to another Loess—wind-blown silt and clay sediment; produces fertile soil Glacial Erosion Glacier—large, long-lasting mass of ice; forms in mountainous areas Glaciation—changing of landforms by slowly moving glaciers Example: cutting u-shaped valleys in land Moraine—hill or ridge formed by rocks deposited by glacier

29. Copyright © by Houghton Mifflin Harcourt Publishing Company Next Previous Chapter 2 Geography 4 Continued… Building Soil Soil Formation Soil—loose mix of weathered rock, organic matter, air, water Soil supports plant growth; fertility is dependent on three factors: − texture − amount of humus, which is organic material in soil − amount of air and water

30. Copyright © by Houghton Mifflin Harcourt Publishing Company Next Previous Chapter 2 Geography Building Soil {continued} Soil Factors When geographers study soil, they look at five factors: − parent material—the chemical composition of the original rock − relief—the steeper the slope, the greater erosion; less soil made − organisms—plants, worms, ants, bacteria loosen soil; supply nutrients − climate—hot, cold, wet, dry climates produce different soils − time—about 2.5 cubic cm. of soil produced each century

31. Copyright © by Houghton Mifflin Harcourt Publishing Company Next Previous Chapter 2 Geography This is the end of the chapter presentation of lecture notes. Click the HOME or EXIT button.HOMEEXIT

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