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CHAPTER 2: THE EARTH The Earth’s Spheres Hydrosphere - part of the Earth made up of oceans, lakes, rivers, and other water bodies. About 70% of the Earth’s surface is water Lithosphere - part of the Earth made up of land, including ocean basins. About 30% of the Earth’s surface is land. Atmosphere - gases that cover the Earth and make up the air we breathe. Biosphere - part of the Earth that supports life (plants, animals, and humans). Landforms ~ Landforms are the natural or physical features of the Earth’s surface and have a particular shape or elevation. 1. Four major types of landforms a. Mountains b. Hills c. Plains d. Plateaus 2. The Earth’s most visible landforms are the large landmasses called a. Africa b. Antarctica c. Asia d. Australia e. Europe f. North America g. South America continents. Earth’s Heights and Depths 1. Mt. Everest - the Earth’s highest point located in Southwest Asia; its elevation is about 2. 29,035 feet above sea level. Dead Sea Shore - the Earth’s lowest point of dry land; it is about 1,349 feet below sea level. 3. Mariana Trench - the Earth’s deepest known depression; it is 35,827 feet deep (below sea level). Earth’s Structure ˜ The Earth’s surface is in slow but constant motion. ˜ Some forces that change the Earth occur at the surface, such as wind and water. ˜ Some forces that change the Earth originate (start) deep within the Earth’s interior, such as earthquakes and volcanic eruptions. A Layered Planet 1. Core a. Inner core - super hot, nickel and iron under great pressure b. Outer core - super hot, liquid nickel 2. Mantle - surrounds the core, thick layer of hot dense rock 3. Crust - thin rocky shell that covers the mantle; it is broken into slabs called plates, that hold and carry the Earth’s oceans and continents Plate Movement 1. Continental drift - theory of a “super continent” - Pangaea, which broke apart 2. Plate tectonics, or the movement of plates, is usually gradual; but, can change the face of the Earth. a. Plate tectonics can include plates crashing together, pulling apart, or sliding and grinding into one another b. Plate tectonics can create mountains, volcanoes, and earthquakes. Internal Forces of Change Folds and Faults 1. Folds are bends in layers of rock formed as moving plates squeeze the Earth’s surface. 2. Faults, or cracks in the Earth’s surface, are formed as plates grind against or slide past one another. The grinding of the two plates causes tremors. Earthquakes 1. Earthquakes are sudden, a. The violent movements of plates along a fault line. Ring of Fire is an area of high volcanic and earthquake activity along the Pacific Rim. Volcanic Eruptions 1. Volcanoes are mountains formed by lava or by magma that breaks through the Earth’s crust. a. Volcanoes often form plate boundaries where one plate plunges below another. The rocky plate melts as it dives downward into the hot mantle. b. Volcanoes also arise in various hot spots, where deep within the Earth the temperature is hotter than normal. The Hawaiian Islands were formed by this type of volcanic activity. c. Molten rock may also heat underground water to create geysers or hot springs, like those found in Yellowstone National Park in Wyoming. External Forces of Change A. Weathering - the process that breaks down rocks B. Erosion - the process that wears away the Earth’s surface 1. The movement of dust, sand, and soil from one place to another is called wind erosion. 2. Glacial erosion is the wearing away of the Earth by large bodies of ice that move slowly across the Earth’s surface. As they move they carry along rock and soil. 3. Water erosion is the wearing away of the Earth’s surface by moving water C. Deposition - the process of adding land or sediment to an area by moving water, wind or ice The Water Cycle ~ The hydrosphere is the part of the Earth’s surface covered by water including oceans, lakes, rivers, and other water bodies. ~ About 97% of the Earth’s water is saltwater ~ About 3% of the Earth’s water is freshwater, but about 2% of it is frozen * The total amount of water on the surface of the earth is unchanging, but the water is in constant motion The hydrologic/water cycle is the regular movement of the Earth’s water. 1. The Sun’s heat causes water in the oceans to evaporate, or to change from a liquid to a gas. The water vapor gathers in the air and rises with the warm air. 2. of As the air cools, water vapor changes back to a liquid through the process condensation. 3. When clouds gather more water than they can hold, they release the moisture. Water released from the clouds, in the form of rain, snow, or sleet is called precipitation. 4. Precipitation returns to the Earth. It sinks into the ground through or, as runoff, it returns to the Earth’s water bodies. infiltration; *The amount of water that evaporates is approximately the same as the amount that falls back to the Earth. The total volume of water in the Earth’s water cycle is geographers believe this is still true? constant. Do Bodies of Saltwater A. Oceans 1. About 97% of the Earth’s water is salt water. Most of the Earth’s water is contained in one of the five large water bodies, called the a. Atlantic b. Arctic c. Indian d. Pacific e. Southern oceans. B. Ocean Water to Drinking Water 1. Although 97% of the world’s water is found in oceans, it is too salty to drink or use for irrigation and manufacturing. 2. Scientists are developing ways to remove the salt from sea water. The process, known as desalination, is still in the early stages of development. Bodies of Freshwater ~ About 3% of the Earth’s total water supply is freshwater. ~ More than 2% of the Earth’s freshwater is frozen in glaciers and polar ice caps. Groundwater 1. Groundwater is fresh water found beneath the Earth’s surface. 2. This type of freshwater comes from rain and snow that has filtered through the soil and rock and accumulated below the Earth’s surface. Some water from lakes and rivers may also become part of the groundwater. 3. People often dig wells and use springs that tap into this type of freshwater. 4. An aquifer is a layer of porous rock below that Earth’s surface that traps and holds groundwater. 5. Aquifers and groundwater are important sources of freshwater.