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▼ The Gui River, The story of the world begins with geography—the study of the earth in all of its variety. Geography describes the earth’s land, water, and plant and animal life. It is the study of places and the complex relationships between people and their environment. The resources in this handbook will help you get the most out of your textbook—and provide you with skills you will use for the rest of your life. Guilin, China ▼ The Amazon, Brazil Geography Handbook ▼ Saharan sand dunes, Morocco Geography Handbook GH1 GH1 (t)Dallas and John Heaton/CORBIS, (c)Jamie Harron/CORBIS, (b)Owen Franken/CORBIS Places and Regions To understand how our world is connected, some geographers have broken down the study of geography into five themes. The Five Themes of Geography are (1) location, (2) place, (3) human/environment interaction, (4) movement, and (5) regions. You will see these themes highlighted in the Chapter Assessment Geography Skills of Journey Across Time: The Early Ages. Six Essential Elements Recently, geographers have begun to look at geography in a different way. They break down the study of geography into Six Essential Elements. Being aware of these elements will help you sort out what you are learning about geography. Place has a special meaning in geography. It means more than where a place is. It also describes what a place is like. It might describe physical characteristics such as landforms, climate, and plant or animal life. Or it might describe human characteristics, including language and way of life. To help organize their study, geographers often group places into regions. Regions are united by one or more common characteristics. The World in Spatial Terms Geographers first take a look at where a place is located. Location serves as a starting point by asking “Where is it?” Knowing the location of places helps you develop an awareness of the world around you. GH2 Getty Images Geography Handbook Physical Systems When studying places and regions, geographers analyze how physical systems—such as hurricanes, volcanoes, and glaciers—shape the earth’s surface. They also look at communities of plants and animals that depend upon one another and their surroundings for survival. Geography Handbook Human Systems Geographers also examine human systems, or how people have shaped our world. They look at how boundary lines are determined and analyze why people settle in certain places and not in others. A key theme in geography is the continual movement of people, ideas, and goods. Environment and Society How does the relationship between people and their natural surroundings influence the way people live? This is one of the questions that the theme of human/environment interaction investigates. It also shows how people use the environment and how their actions affect the environment. The Uses of Geography Knowledge of geography helps us understand the relationships among people, places, and environments over time. Understanding geography and knowing how to use the tools and technology available to study it prepares you for life in our modern society. Geography Handbook GH3 Getty Images Hemispheres To locate a place on the earth, geographers use a system of imaginary lines that crisscross the globe. One of these lines, the Equator, circles the middle of the earth like a belt. It divides the earth into “half spheres,” or hemispheres. Everything north of the Equator is in the Northern Hemisphere. Everything south of the Equator is in the Southern Hemisphere. Another imaginary line runs from north to south. It helps divide the earth into half spheres in the other direction. Find this line— called the Prime Meridian on a globe. Everything east of the Prime Meridian for 180 degrees is in the Eastern Hemisphere. Everything west of the Prime Meridian is in the Western Hemisphere. Hemispheres Northern Hemisphere Southern Hemisphere Indian Ocean Asia Australia Africa North Pole Africa Europe South Pole Atlantic Ocean Pacific Ocean Antarctica Atlantic Ocean South America North America Western Hemisphere North America Pacific Ocean Eastern Hemisphere Europe Asia Atlantic Ocean Africa Pacific Ocean South America Indian Ocean Australia GH4 Geography Handbook L ines on globes and maps provide information that can help you easily locate places on the earth. These lines—called latitude and longitude—cross one another, forming a pattern called a grid system. Latitude Lines of latitude, or parallels, circle the earth parallel to the Equator and measure the distance north or south of the Equator in degrees. The Equator is at 0° latitude, while the North Pole lies at latitude 90°N (north). Longitude Lines of longitude, or meridians, circle the earth from Pole to Pole. These lines measure distances east or west of the starting line, which is at 0° longitude and is called the Prime Meridian. The Prime Meridian runs through the Royal Observatory in Greenwich, England. Absolute Location The grid system formed by lines of latitude and longitude makes it possible to find the absolute location of a place. Only one place can be found at the point where a specific line of latitude crosses a specific line of longitude. By using degrees (°) and minutes (') (points between degrees), people can pinpoint the precise spot where one line of latitude crosses one line of longitude—an absolute location. Geography Handbook GH5 Mapmaking With Technology Technology has changed the way maps are made. Most cartographers use software programs called geographic information systems (GIS). This software layers map data from satellite images, printed text, and statistics. A Global Positioning System (GPS) helps consumers and mapmakers locate places based on coordinates broadcast by satellites. From Globes to Maps Maps, however, do have their limitations. As you can imagine, drawing a round object on a flat surface is very difficult. Cartographers, or mapmakers, use mathematical formulas to transfer information from the round globe to a flat map. However, when the curves of a globe become straight lines on a map, the size, shape, distance, or area can change or be distorted. Great Circle Route Map A 120°E S 60°N Great Circle Distance 5,450 mi. (8,769 km) True Direction Distance 5,795 mi. (9,324 km) 30°N 0° PACI F I C OCEAN 30°S 0 mi. 3,000 0 km 3,000 Mercator projection 0° Map B 60°E 60 °N 60°W N North Pole W 120°E Great Circle Route Tokyo 0 mi. PACI F I C True OCEAN ute D ir e cti o n R o 3,000 0 km 3,000 Polar Gnomonic projection GH6 Geography Handbook Los Angeles 40 °N Mapmakers have solved some problems of going from a globe to a map. A great circle is an imaginary line that follows the curve of the earth. Traveling along a great circle is called following a great circle route. Airplane pilots use great circle routes because they are the shortest routes. The idea of a great circle shows one important difference between a globe and a map. Because a globe is round, it accurately shows great circles. On a flat map, however, the great circle route between two points may not appear to be the shortest distance. Compare Maps A and B on the right. 120°W E W Tokyo Great Circle Routes N 180° E he most accurate way to depict the earth is as a globe, a round scale model of the earth. A globe gives a true picture of the continents’ relative sizes and the shapes of landmasses and bodies of water. Globes accurately represent distance and direction. A map is a flat drawing of all or part of the earth’s surface. Unlike globes, maps can show small areas in great detail. Maps can also display political boundaries, population densities, or even voting returns. 180° S T Los Angeles 120°W I Goode’s Interrupted Equal-Area Projection Winkel Tripel Projection A R C T IC EQUATOR N TROPIC OF CAPRICOR 30°S 60°S ANTARCTIC CIR ARCTIC CIRCLE 120°E MERIDIAN OF GREENWICH (LONDON) TROPIC OF CANCER 0° 60°E CIRCLE 30°N 60°N 30°N 0° 120°W 60°W 60°N ▼ magine taking the whole peel from an orange and trying to flatten it on a table. You would either have to cut it or stretch parts of it. Mapmakers face a similar problem in showing the surface of the round earth on a flat map. When the earth’s surface is flattened, big gaps open up. To fill in the gaps, mapmakers stretch parts of the earth. They choose to show either the correct shapes of places or their correct sizes. It is impossible to show both. As a result, mapmakers have developed different projections, or ways of showing the earth on a flat piece of paper. C LE The Winkel Tripel projection gives a good overall view of the continents’ shapes and sizes. Land areas in a Winkel Tripel projection are not as distorted near the Poles as they are in the Robinson projection. TROPIC OF CANCER EQUATOR 0° Mercator Projection TROPIC OF CAPRICORN 30°S 90°E 60°S 120°E 150°E 180° 150°W 120°W 90°W 60°W 30°W Take a second look at your peeled, flattened orange. You might have something that looks like a map based on Goode’s Interrupted Equal-Area projection. A map with this projection shows continents close to their true shapes and sizes. This projection is helpful to compare land areas among continents. 60°E ARCTIC CIRCLE 0° TROPIC OF CANCER EQUATOR TROPIC OF CAPRICORN 120°W ARCTIC CIRCLE 60°W 0° 60°E 120°E 30°S 60°N TROPIC OF CAPRICORN 30°S 60°S ANTARCTIC CIRCLE MERIDIAN OF GREENWICH (LONDON) EQUATOR 60°S A map using the Robinson projection has minor distortions. Land on the western and eastern sides of the Robinson map appears much as it does on a globe. The areas most distorted on this projection are near the North and South Poles. ANTARCTIC CIRCLE ▼ TROPIC OF CANCER MERIDIAN OF GREENWICH (LONDON) ▼ Robinson Projection 0° 30°E 60°N 30°N 30°N 0° ANTARCTIC CIRCLE The Mercator projection shows true direction and land shapes fairly accurately, but not size or distance. Areas that are located far from the Equator are quite distorted on this projection. Alaska, for example, appears much larger on a Mercator map than it does on a globe. Geography Handbook GH7 ▼ Map Key An important first step in reading a map is to note the map key. The map key explains the lines, symbols, and colors used on a map. For example, the map on this page shows the various climate regions of the United States and the different colors representing them. Cities are usually symbolized by a solid circle (•) and capitals by a (). On this map, you can see the capital of Texas and the cities of Los Angeles, Seattle, New Orleans, and Chicago. Climate Regions of the United States Desert Highland Humid continental Humid subtropical Marine Scale A measuring line, often called a scale bar, helps you figure distance on the map. The map scale tells you what distance on the earth is represented by the measurement on the scale bar. GH8 Geography Handbook Mediterranean Steppe Subarctic Tropical Tundra Compass Rose A map has a symbol that tells you where the cardinal directions—north, south, east, and west—are positioned. Spain: Political General Purpose Maps Maps are amazingly useful tools. Geographers use many different types of maps. Maps that show a wide range of general information about an area are called general purpose maps. Two of the most common general purpose maps are physical and political maps. 10°W FRANCE R. Do u r o R . PORTUGAL E W S S P A I N Seville 0 mi. 200 0 km 200 Lambert Azimuthal Equal-Area projection Jaffna Gulf of Mannar Bay of Bengal Kattankudi M´alaga d Me ATLANTIC O CE A N Point Pedro Valencia Balearic Islands ite rr e an an Se a GIBRALTAR U.K. S t r a i t o f G ib r a l t a r AFRICA Political Maps Political maps show the names and boundaries of countries, the location of cities and other humanmade features of a place, and often identify major physical features. The political map of Spain (above), for example, shows the boundaries between Spain and other countries. It also shows cities and rivers within Spain and bodies of water surrounding Spain. Matale Pidurutalagala 8,281 ft. (2,524 m) Colombo N W Barcelona uivir R. dalq ua G Sri Lanka: Physical Chilaw N 40°N Physical maps call out landforms and water features. The physical map of Sri Lanka (below) shows rivers and mountains. The colors used on physical maps include brown or green for land and blue for water. In addition, physical maps may use colors to show elevation—the height of an area above sea level. A key explains what each color and symbol stands for. SRI LANKA Zaragoza Madrid Tagus R. 8°S ANDORRA Eb ro Physical Maps Trincomalee 0° Bay o f Biscay INDIAN OCEAN E Matara S 0 mi. 0 km 80°E 100 100 Elevations Feet Meters 3,280 1,000 1,640 500 650 200 380 100 0 0 Mountain peak National capital Major city Geography Handbook GH9 Special Purpose Maps Egypt: Population Density Mediterranean Alexandria Se a Suez Cairo Canal 30°N El Giza N W EGYPT E S le Re Ni R. 300 Se 0 mi. d 0 km 300 Lambert Azimuthal Equal-Area projection a Some maps are made to present specific kinds of information. These are called thematic or special purpose maps. They usually show themes or patterns, often emphasizing one subject or theme. Special purpose maps may present climate, natural resources, and population density. They may also display historical information, such as battles or territorial changes. The map’s title tells what kind of special information it shows. Colors and symbols in the map key are especially important on these types of maps. Special purpose maps are often found in books of maps called atlases. One type of special purpose map uses colors to show population density, or the average number of people living in a square mile or square kilometer. As with other maps, it is important to first read the title and the key. The population density map of Egypt shows that the Nile River valley and delta are very densely populated. TROPIC OF CANCER Persons sq. mi. Uninhabited Under 2 2–60 60–125 125–250 Over 250 Some other special purpose maps such as the one of China’s Defenses are not presented in color. They are printed in black and white. This is an example of a map you might find on a standardized test or in a newspaper. per sq. km Uninhabited 20°N Boundary claimed by Sudan Under 1 1–25 25–50 50–100 Over 100 Cities City with more than 5,000,000 people City with 1,000,000 to 5,000,000 people 30°E China’s Defenses RUSSIA MONGOLIA G re a t W a ll o f C hina Yellow Sea East China Sea CHINA NEPAL Himalaya Gobi Taklimakan Manchurian Altay Mountains Plain GH10 Geography Handbook South China Sea Bar, Line, and Circle Graphs Comparing World Languages Chinese (Mandarin) 874 Languages A graph is a way of summarizing Hindi 366 and presenting information visually. English 341 Each part of a graph gives useful Spanish 322 information. First read the graph’s title to find out its subject. Then read Bengali 207 the labels along the graph’s axes— Portuguese 176 the vertical line along the left side of Russian 167 the graph and the horizontal line Japanese 125 along the bottom. One axis will tell you what is being measured. The German 100 other axis tells what units of measKorean 78 urement are being used. Number of Native Speakers (in millions) Graphs that use bars or wide lines Source: The World Almanac, 2003. to compare data visually are called Bar graph bar graphs. Look carefully at the bar graph (right) which compares world lanA line graph is a useful tool for showing guages. The vertical axis lists the languages. changes over a period of time. The amounts The horizontal axis gives speakers of the lanbeing measured are plotted on the grid above guage in millions. By comparing the lengths of each year and then are connected by a line. the bars, you can quickly tell which language Line graphs sometimes have two or more lines is spoken by the most people. Bar graphs are plotted on them. The line graph (below) shows especially useful for comparing quantities. that the number of farms in the United States has decreased since 1940. Number of farms (in millions) U.S. Farms, 1940–2000 7 6 5 4 3 2 1 0 1940 1950 Source: The World Almanac, 2003. 1960 1970 1980 1990 2000 Year Line graph Geography Handbook GH11 Using Graphs, Charts, and Diagrams You can use circle graphs when you want to show how the whole of something is divided into its parts. Because of their shape, circle graphs are often called pie graphs. Each “slice” represents a part or percentage of the whole “pie.” On the circle graph at right, the whole circle (100 percent) represents the world’s population in 2002. The slices show how this population is divided among some of the most heavily populated areas of the world. World Population* Latin America 9% North America 5% Europe 12% Charts Charts present facts and numbers in an organized way. They arrange data, especially numbers, in rows and columns for easy reference. To interpret the chart, first read the title. Look at the chart on page 91. It tells you what information the chart contains. Next, read the labels at the top of each column and on the left side of the chart. They explain what the numbers or data on the chart are measuring. Africa 13% Asia 61% Source: World Population Data Sheet, 2003. Circle graph Production figures for five major auto-producing countries Major AutomobileProducing Countries, 2001 Japan Germany United States France South Korea = 1,000,000 passenger cars Pictograph GH12 Geography Handbook *Excluding Australia Source: The World Almanac, 2003. Pictographs Like bar and circle graphs, pictographs are good for making comparisons. Pictographs use rows of small pictures or symbols, with each picture or symbol representing an amount. Look at the pictograph (left) showing the number of automobiles produced in the world’s five major automobile-producing countries. The key tells you that one car symbol stands for 1 million automobiles. The total number of car symbols in a row adds up to the auto production in each selected country. Geography Handbook Climographs Average monthly temperature Climograph: Moscow, Russia °F °C in. mm 100 37.8 20 508 90 32.2 18 457.2 80 26.7 16 406.4 70 21.1 14 355.6 60 15.6 12 304.8 50 10.0 10 254 4.4 8 203.2 30 –1.1 6 152.4 20 –6.7 4 101.6 10 –12.2 2 50.8 0 –17.8 0 0 40 Average monthly precipitation A climograph, or climate graph, combines a line graph and a bar graph. It gives an overall picture of the long-term weather patterns in a specific place. Climographs include several kinds of information. The green vertical bars on the climograph of Moscow (right) show average monthly amounts of precipitation (rain, snow, and sleet). These bars are measured against the axis on the right side of the graph. The red line plotted above the bars represents changes in the average monthly temperature. You measure this line against the axis on the left side. Jan. Feb. Mar. April May June July Aug. Sept. Oct. Nov. Dec. Source: World Weather Guide. Climograph Diagrams Diagrams are drawings that show steps in a process, point out the parts of an object, or explain how something works. An elevation profile is a type of diagram that can be helpful when comparing the elevations—or height—of an area. It shows an exaggerated side view of the land as if it were sliced and you were viewing it from the side. The elevation profile of Africa (below) clearly shows sea level, low areas, and mountains. Africa: Elevation Profile Mt. Kenya 17,058 ft. (5,199 m) 16,404 ft. 0 mi. 13,123 ft. 0 km 300 300 5,000 m Margherita Peak 16,763 ft. (5,109 m) 4,000 m Lake Victoria 9,842 ft. 3,000 m 6,562 ft. Indian Ocean 2,000 m Atlantic Ocean 3,281 ft. Congo River 1,000 m Sea level 0˚ latitude (Equator) Diagram Geography Handbook GH13 Volcano Mountain peak Strait Sound Island Valley Cape Ocean Cliff Isthmus As you read about world history, you will encounter the terms listed below. Many of the terms are pictured in the diagram. Bay Harbor Gulf Delta Peninsula st Seacoa absolute location exact location of a place on the earth described by global coordinates basin area of land drained by a given river and its branches; area of land surrounded by lands of higher elevation bay part of a large body of water that extends into a shoreline, generally smaller than a gulf canyon deep and narrow valley with steep walls cape point of land that extends into a river, lake, or ocean channel wide strait or waterway between two landmasses that lie close to each other; deep part of a river or other waterway cliff steep, high wall of rock, earth, or ice continent one of the seven large landmasses on the earth cultural feature characteristic that humans have created in a place, such as language, religion, housing, and settlement pattern delta flat, low-lying land built up from soil carried downstream by a river and deposited at its mouth divide stretch of high land that separates river systems downstream direction in which a river or stream flows from its source to its mouth elevation height of land above sea level Equator imaginary line that runs around the earth halfway between the North and South Poles; used as the starting point to measure degrees of north and south latitude GH14 Geography Handbook glacier large, thick body of slowly moving ice gulf part of a large body of water that extends into a shoreline, generally larger and more deeply indented than a bay harbor a sheltered place along a shoreline where ships can anchor safely highland elevated land area such as a hill, mountain, or plateau hill elevated land with sloping sides and rounded summit; generally smaller than a mountain island land area, smaller than a continent, completely surrounded by water isthmus narrow stretch of land connecting two larger land areas lake a sizable inland body of water latitude distance north or south of the Equator, measured in degrees longitude distance east or west of the Prime Meridian, measured in degrees lowland land, usually level, at a low elevation map drawing of the earth shown on a flat surface meridian one of many lines on the global grid running from the North Pole to the South Pole; used to measure degrees of longitude mesa broad, flat-topped landform with steep sides; smaller than a plateau Geography Handbook Mountain range Glacier Source of river Channel Highland Lake Plateau Hills Canyon Mouth of river River Desert Upstream Downstream Plain Lowland Basin Tributary mountain land with steep sides that rises sharply (1,000 feet [305 m] or more) from surrounding land; generally larger and more rugged than a hill mountain peak pointed top of a mountain mountain range a series of connected mountains mouth (of a river) place where a stream or river flows into a larger body of water ocean one of the four major bodies of salt water that surround the continents ocean current stream of either cold or warm water that moves in a definite direction through an ocean parallel one of many lines on the global grid that circle the earth north or south of the Equator; used to measure degrees of latitude peninsula body of land jutting into a lake or ocean, surrounded on three sides by water physical feature characteristic of a place occurring naturally, such as a landform, body of water, climate pattern, or resource plain area of level land, usually at a low elevation and often covered with grasses plateau area of flat or rolling land at a high elevation, about 300–3,000 feet (91–914 m) high Prime Meridian line of the global grid running from the North Pole to the South Pole through Greenwich, England; starting point for measuring degrees of east and west longitude relief changes in elevation over a given area of land river large natural stream of water that runs through the land sea large body of water completely or partly surrounded by land seacoast land lying next to a sea or ocean sea level position on land level with surface of nearby ocean or sea sound body of water between a coastline and one or more islands off the coast source (of a river) place where a river or stream begins, often in highlands strait narrow stretch of water joining two larger bodies of water tributary small river or stream that flows into a larger river or stream; a branch of the river upstream direction opposite the flow of a river; toward the source of a river or stream valley area of low land between hills or mountains volcano mountain created as liquid rock or ash erupts from inside the earth Geography Handbook GH15