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Chapter 2 Lesson 1: Planet Earth
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The Solar System Sun is medium-sized star at edge of the Milky Way galaxy The solar system includes: sun and eight planets (Pluto just got voted out.) comets—icy spheres orbiting the sun asteroids—large chunks of rocky material orbiting the sun Earth is third planet in the solar system of the sun
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Size of Earth Circumference of the earth: about 24,900 miles
Diameter of the earth: about 7,900 miles
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On and Above the Earth Atmosphere is the layer of gasses surrounding the earth contains oxygen protects Earth from radiation, space debris Location of all weather and climate 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
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Continental Landforms
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
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Landforms 1. volcano 2. canyon 3. glacier 4. delta 5. oasis 6. swamp
7. bay/ gulf 8. prarie 9. mesa 10. valley 11. marsh 12. cape/ peninsula 13. straight 14. butte 15. cataract 16. steppe
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Continental Shelf the area of seabed around a large landmass where the sea is relatively shallow compared with the open ocean. The continental shelf is geologically part of the continental crust.
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Lesson 2: Forces of Change
Chapter 2 Lesson 2: Forces of Change
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Inside the Earth Core Mantle Crust Center of the earth
Made up of iron and nickel Outer core is liquid Inner core is solid Mantle Surrounds the core Contains most of Earth’s mass Made of molten rock called magma Crust Thin layer of rock at Earth’s surface
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Continental Drift Continents—landmasses above water on Earth
Continental Drift—Earth was once one supercontinent (Pangaea) The seven continents on earth fit together like a jigsaw puzzle Pangaea split into many plates that slowly drifted apart
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Plate Tectonics 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
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Plate Tectonics (continued)
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 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
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Folds and Faults Two plates meeting can cause folding and cracking of rock Fault occurs when pressure causes rock to fracture Fault line is the place where plates move past each other
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Earthquakes An earthquake occurs when plates grind or slip at a fault line A seismograph detects earthquakes and measures the waves they create 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 Richter Scale—numeric scale showing relative strength of earthquake
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Earthquake Damage Landslides Land displacement
Fires (broken gas lines) Collapsed buildings
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Tsunami Tsunami—a giant ocean wave
begins at epicenter of an earthquake travels at up to 450 mph waves of 50–100ft. or higher
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Volcanoes Volcano—underground materials pour from crack in the earth’s surface Most volcanoes occur at tectonic plate boundaries Eruption—lava, gases, ash, dust, explode from vent in Earth’s crust Lava—magma that has reached the earth’s surface; may create landform Ring of Fire—zone around rim of Pacific Ocean where most volcanoes are located
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Volcanoes (continued)
Hot springs, geysers indicate high temperatures in earth’s crust Some volcanic action is useful volcanic ash produces fertile soil for growing plants. hot springs are tapped for heat, energy
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Weathering 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
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Mechanical Weathering
Mechanical weathering—processes that break rock into smaller pieces Does not change rock’s composition, only size Examples: frosting, plant roots, road construction, mining
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Chemical Weathering Chemical weathering—interaction of elements creates new substance Example: when iron rusts it reacts to oxygen in air Warm, moist climates produce more chemical weathering than cool, dry
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Erosion Erosion—when weathered material moves by winds, water, ice, gravity Movement grinds rock into smaller pieces, carries to new location
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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
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Wind Erosion Wind transports sediment from one place to another
Loess—wind-blown silt and clay sediment; produces fertile soil
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Glacial Erosion Glacier—large, long-lasting mass of ice; forms in mountainous areas Glaciations—changing of landforms by slowly moving glaciers Example: cutting u-shaped valleys in land Moraine—hill or ridge formed by rocks deposited by glacier
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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
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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
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Chapter 2 Lesson 3: Earth’s Water
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Hydrosphere 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
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Hydrosphere Hydrologic Cycle—cycle of water between atmosphere, oceans, earth Water covers about three-fourths of the earth’s surface. 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
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Hydrosphere 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 Ground water—water held in the pores of rock Water table—level at which the rock is saturated
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Oceanic Landforms Landforms are naturally formed features on Earth’s surface Oceanic Landforms (naturally formed features on Earth’s surface) 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
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