Geography Study Guide Label Each of the Continents, Oceans, Equator

Total Page:16

File Type:pdf, Size:1020Kb

Geography Study Guide Label Each of the Continents, Oceans, Equator Geography Study Guide Label each of the continents, oceans, equator, and prime meridian Arctic Europ North Am. e Asia Atlantic Pacific Pacific South Am. Africa Aus Southern Ant. Label each of the bodies of water by using your notes. Columbia River St. Lawrence River Great Lakes Missouri River Ohio River Colorado River Mississippi River Rio Grande Gulf of Mexico Fill in the table below by using your notes or past quiz. Be sure to include all details for each body of water. Body of Water Details Ohio River Known as the “Gateway to the West.” Rio Grande Forms part of the boundary between the U.S. and Mexico. St. Lawrence River Was explored by the French and connects the Atlantic to the Great Lakes Mississippi River Transportation artery for farmers to ship goods. Connects to the gulf of Mexico Missouri River Transportation artery for farmers to ship goods. Connects to the Missouri River Colorado River was explored by the Spanish and is the home of the Grand Canyon Gulf of Mexico Explored by the French and Spanish, connects to the Atlantic Ocean Great Lakes French set up trading posts, inland port cities Columbia River Lewis and Clark sailed down this river on their way to the Pacific Lake Trib. Hill Mnt. Gulf Plateau River Peninsula Bay Island Plain Label the features of the map above: Hill Mountain Peninsula Plateau Lake River Tributary Island Plain Bay Gulf Using your notes label the map and draw at least 2 imagines that represent each region. Can. Shield Coastal Range Rocky Mts. Int. Lowlands Basin and Great Plains Range App. Mts. Coastal Plains Fill in the table below by using your notes. Geographic Region Full Description Coastal Plain Broad lowlands along the Atlantic with many excellent harbors Canadian Shield Thousands of lakes carved by glaciers; oldest rock formations in North America Coastal Range Rugged mountains and valleys along the coast with many vineyards Rocky Mtns Tall, rugged mountains from Alaska to Mexico; home of the Continental Divide Great Plains Flat grasslands that gradually rise in elevation towards the Rocky Mountains Appalachian Mtns Old, eroded mountains that stretch from Canada to Alabama Basin and Range Mountains and deserts, including Death Valley, the lowest and hottest place in the U.S. Interior Lowlands Rolling flatlands with broad rivers; excellent soil for farming; Breadbasket of America Mountains Which mountain range is located on the east coast and is the oldest mountain range in North America? Appalachian Mountains Which mountain range is the tallest mountain range in North America, home to the continental divide and located to the east of the Basin and Range? Rocky Mountains Which mountain range is located in the Coastal Range, and was a major obstacle for westward travelers? Sierra Navada Longitude and Latitude- Fill in the chart below by using the word bank. Word Bank: Parallels Meridians X Axis Y Axis Runs east to west Runs north to south Measures east or west of the PM Measures north or south of the equator Longitude Latitude Runs north to south Runs east to west Meridians Y axis X axis Parallels Measures east or west of the PM Measures north or south of the equator Give the coordinates for each location below and plot the coordinates given. 20S 50E 55N 5W 70N 40W 40S 175E 20N 155W .
Recommended publications
  • MUST KNOW Geography
    AP World History Ms. Avar File: Geography MUST KNOW Geography Description You must understand Geography to effectively study world history. Practice and learn the skills in your Geography 101 packet (given to you the first week of school), know the location of world regions and sub regions and be able to identify and locate key nations, landforms and bodies of water listed on this sheet. POLTICAL MAPS Instructions: Neatly locate, outline in color and label ALL of the following countries on your Continent Political maps. Use the world map at end of your textbook, Google Maps and/or worldatlas.com (search by continent) AFRICA North Africa Algeria Egypt East Ethiopia Kenya Libya Morocco Africa Madagascar Somalia Tunisia Sudan Tanzania West Africa Chad Benin Ghana Equatorial Cameroon Rwanda Mali Mauritania Senegal Africa Uganda Sudan Niger Nigeria Central African Republic Togo Cote D’Ivoire Democratic Republic of the Congo Southern Africa Angola Botswana Zimbabwe Zambia Republic of South Africa Mozambique ASIA East Asia Japan China SE Asia Cambodia Indonesia Vietnam North Korea South Korea Myanmar (Burma) Malaysia Thailand Taiwan Mongolia Philippines Singapore Laos South Asia Afghanistan Bangladesh SW Asia / Iran Iraq Turkey India Pakistan Middle East Jordan Israel Nepal Syria Saudi Arabia Central Asia Kazakhstan EUROPE Western France Germany Ireland Eastern Hungary Poland Europe Portugal Spain Switzerland Europe Romania Russia England/Great Britain/United Kingdom “U.K.” Ukraine Serbia Austria Czech Republic Northern Finland Norway Southern
    [Show full text]
  • Watersheds in New Mexico
    3 1 . Watersheds in New Mexico School-based Activities 371 Description: Students will color the different watersheds in the Southwest to learn which rivers drain out of each area of the state/region. Extensions include making a pie chart to show the area of each watershed in the state, researching the watersheds in teams and presenting fi ndings about the state’s watersheds to the class in a poster presentation. Objectives: Students will: • understand the concept of watersheds; and • be able to identify the watersheds in New Mexico and the Southwest and where they fl ow. Materials: colored pencils or highlighters a copy of the Defi ne Watershed Boundaries worksheet for each student a copy of the New Mexico Watersheds map for each student physical map of North America (for fi nding where New Mexico’s rivers fl ow) Background: Precipitation that falls to the ground can have one of several things happen to it—it can evaporate, soak into the soil to become ground water, or fl ow downhill as surface water in rivers and lakes. In this activity, we consider surface water movement as we look at the watersheds of New Mexico. Watersheds are identifi ed by surface water movement. Rivers, streams, creeks, and arroyos are formed where water fl ows when following gravity. A watershed, or drain- age basin, is an area of land drained by a river, river system or other body of water. Except in closed basins, which have no outfl ow, all watersheds eventually drain into an ocean or sea. Thus you can follow a river from its mouth up to its headwaters, including all of the tributaries that fl ow into it, to get an idea of the size of the watershed.
    [Show full text]
  • Regional Crustal Thickness and Precipitation in Young Mountain Chains
    Regional crustal thickness and precipitation in young mountain chains W. G. Ernst* Department of Geological and Environmental Sciences, Stanford University, Stanford, CA 94305-2115 Contributed by W. G. Ernst, September 7, 2004 Crustal thickness is related to climate through precipitation-induced erosion. Along the Andes, the highest mountains and thickest crust (Ϸ70 km) occur at 25° south, a region of low precipitation. Westerly winds warm passing over the Atacama Desert; precipita- tion is modest in the High Andes and eastward over the Altiplano. Severe aridity, hence low erosion rates, helps to account for the elevated volcanogenic contractional arc and high, internally draining plateau in its rain shadow. Weak erosion along the north- central arc provides scant amounts of sediment to the Chile–Peru Trench, starving the subduction channel. Subcrustal removal might be expected to reduce the crustal thickness, but is not a factor at 25° south. The thickness of the gravitationally compensated conti- nental crust cannot reflect underplating and͞or partial fusion of sediments, but must be caused chiefly by volcanism-plutonism and contraction. Contrasting climate typifies the terrane at 45° south where moisture-laden westerly winds encounter a cool margin, bringing abundant precipitation. The alpine landscape is of lower average elevation compared with the north-central Andes and is supported by thinner continental crust (Ϸ35 km). Intense erosion supplies voluminous clastic debris to the offshore trench, and vast quantities are subducted. However, the southern Andean crust is only about half as thick as that at 25° south, suggesting that ero- sion, not subcrustal sediment accretion or anatexis, is partly responsible for the thickness of the mountain belt.
    [Show full text]
  • The Population Bias of Severe Weather Reports West of the Continental Divide
    The Population Bias of Severe Weather Reports West of the Continental Divide Paul Frisbie National Weather Service Grand Junction, Colorado November 2005 1 Abstract Many severe storms in the West may go unreported or unobserved, and therefore the severe weather climatology is not fully understood. But as the population has increased in the West so has the number of severe weather reports. To check if a population bias exists, correlation coefficients are calculated with respect to population for tornadic and nontornadic severe storm activity. The sample size for tornadic storms is too small to draw any conclusion. To calculate the correlation coefficients for nontornadic severe storms, population and severe weather data are used for every county in each western state between the years 1986-1995 and 1996-2004. The calculated correlation coefficients reveal that population and the number of nontornadic severe storms are significantly correlated, and this indicates that a population bias does exist for several western states. 2 1. Introduction The number of severe weather reports for the western United States is considerably less than for other parts of the country. The lack of moisture, lift, and instability limits convective potential in the West; therefore, the number of severe storms is less than what occurs in other parts of the country. But there may be non-meteorological reasons that limit the number of severe weather reports. These reports may be limited to urban centers, and therefore severe weather data likely exhibit a population bias. Severe storms in rural areas may go unobserved, and hence unreported. Severe weather does occur in the west and occasionally grabs national media attention, like the 11 August 1999 Salt Lake City tornado that struck downtown.
    [Show full text]
  • Steamboat Springs: Gateway to One of the World's Best Thru Hikes
    Steamboat Springs: Gateway to one of the world’s best thru hikes This welcoming western town is the newest Continental Divide Trail Gateway Community and the jumping off point for stunning wilderness areas; learn how you can support the wild places you love Steamboat Springs exudes a genuine, hospitable western spirit so palpable it’s no wonder this mountain destination was recently designated a Continental Divide Trail (CDT) Gateway Community. As one of just five gateway communities in Colorado, Steamboat Springs is committed to providing an inviting environment for hikers trekking the 3,100-mile CDT Scenic Trail, which runs between Mexico and Canada. Designated by Congress in 1978, the CDT is the highest, most challenging and most remote of the 11 National Scenic Trails. In short, it is a treasured national resource, one that is worth protecting and celebrating. CDT Gateway Communities are recognized for their part in promoting awareness and stewardship of the trail and creating a welcoming environment for people traveling along it. To that end, the Steamboat Springs Chamber is handing out welcome bags to thru-hikers passing through town on the CDT. The Chamber banded together with several local trail advocacy groups, the U.S. Forest Service and locally-based brands Big Agnes and Point6 to champion the designation and provide the goodie bag, which includes a pair of Point6 socks, Big Agnes swag, a free pint of beer at Mountain Tap, discounted entry to Old Town Hot Springs and more. CDT welcome bags are available at the Steamboat Springs Visitor Center from 8 a.m.
    [Show full text]
  • Continental Divide Trail Coalition February 2020
    CONTINENTAL DIVIDE TRAIL COALITION CONGRESSIONAL REPORT FEBRUARY 2020 CONTINENTAL DIVIDE NATIONAL SCENIC TRAIL Designated by Congress in 1978, the Continental Divide National Scenic Trail COMPLETING THE TRAIL stretches 3,100 miles from Mexico to Canada along the spine of the Rockies. The CDT is the highest, most challenging, and most remote of the 11 National The nature and purposes of the CDT are to provide for high-quality, primitive Scenic Trails. hiking and horseback riding opportunities and to conserve natural, historic, and cultural resources along the CDT corridor. Unfortunately, because the CDT remains incomplete, many segments of the CDT do not provide this experience The National Trails System Act creates a system of 1968 for visitors. National Scenic, Historic, and Recreational Trails. 1020 Miles in Idaho and Montana Congress passes the National Parks and Recreation Act, 1978 designating the CDT as the third National Scenic Trail and 612 miles of the CDT are still in making the Forest Service its lead administering agency. 510 Miles in Wyoming 26% Wilderness need of relocation off of roads The USFS amends the CDT Comprehensive Management 58% Other 2009 Plan, providing direction for local management of the Trail. Protected Land (Federal, State, or Public Easements) 11% Wilderness 172 miles of the CDT are still in 750 Study Areas Miles in need of protection as public land The Continental Divide Trail Coalition is founded to Colorado 2012 complete, promote, and protect the CDT. 820 USFS, BLM, CDTC, youth corps, and other stewardship Miles in 5% UNPROTECTED 2018 organizations partner to “Blaze the CDT,” marking the New Mexico trail in its entirety for the first time in history.
    [Show full text]
  • Level One Level Two Level Three Land Compass Rose Equator North
    BROWN'S WORLD OUTLINE Level One Level Two Level Three Level Four Level Five September Land Compass Rose Equator North Pole Tropic of Capricorn Maps and Globes Water North South Latitude (Parallel) South Pole Tropic of Cancer Mountain East West Northern Hemisphere Longitude (Meridian) Arctic Circle River Scale Southern Hemisphere Prime Meridian Antarctic Circle Tropical Zone October North America Pacific Ocean Gulf of Mexico Panama Canal Hudson Bay The World South America Atlantic Ocean Great Lakes Bering Sea St. Lawrence River Continents Europe Indian Ocean Greenland Caribbean Sea Mediterranean Sea And Oceans Asia Arctic Ocean PugetSound Great Salt Lake New Zealand Africa Montana Australia Washington Idaho North Dakota Antarctica Oregon Wyoming South Dakota November Canada Cuba Haiti Jamaica Costa Rica North America United States Guatemala Dominican Republic Bahamas Puerto Rico Central America Mexico Belize West Indies Vancouver Island EISalvador Mississippi River Honduras Olympic Peninsula North American Nicaragua Rocky Mountains Panama Continental Divide Yucatan Peninsula California Washington. DC Nevada Alaska Nebraska Utah Hawaii Kansas Colorado January Ecuador Colombia Peru Paraguay Galapagos Islands South America Brazil Venezuela Bolivia Uruguay Guyana Chile Andes Mountains Amazon River Cape Horn French Guiana Argentina louisiana Iowa Suriname Oklahoma Missouri Arizona Texas Arkansas New Mexico February United Kingdom Spain Poland Portugal Ireland Europe France Germany Denmark Switzerland Belgium Norway Sweden Netherlands Alps Adriatic
    [Show full text]
  • World Geography
    World Geography Ch. 7, 8, & 9 North America United States & Canada United States • 50 U.S. States • Shares a northern border with Canada & southern border with Mexico • Fourth in the World in land area & third in Population • U.S & Canada Make up 80% of the Continent of North America Chap. 7, 8, & 9 (North America) Chap. 7, 8, & 9 (North America) Chap. 7, 8, & 9 (North America) Chap. 7, 8, & 9 (North America) Chap. 7, 8, & 9 (North America) Landforms of United States • Coastal Plain – stretches along the Atlantic Ocean & the Gulf of Mexico. • Piedmont – area at or near the foot of a mountain region. • Appalachian Mts. – stretch from Alabama to Southeastern Canada. • Interior Plains – between the Appalachian and Rocky Mountains. • Great Plains – part of Interior Plains • Rocky Mountains – Run from Canada to New Mexico • Intermountain Region – between the Rockies and the Coastal Mountain Ranges. • Sierra Nevada & Cascade Mountain ranges – Located on the Pacific Coast Chap. 7, 8, & 9 (North America) Rocky Mountains Chap. 7, 8, & 9 (North America) Smoky Mountains (Appalachians) Chap. 7, 8, & 9 (North America) Continental Divide • The Continental Divide is located at the crest of the Rocky Mountains. • It divides North America’s major river systems into: – Those flowing eastward (Mississippi, Missouri, and Ohio Rivers) – Those flowing westward (Colorado, Columbia, Fraser, and Yukon Rivers). • North America also has more lakes than any other Continent. Chap. 7, 8, & 9 (North America) Climactic Influences • Four major factors influence climate in the United States – Middle Latitude Locations – Prevailing Winds – Ocean Currents – High Mountain Ranges • All Climates of the world are found in North America.
    [Show full text]
  • Simulation of the Diurnal Cycle in Tropical Rainfall and Circulation During Boreal Summer with a High-Resolution GCM
    3434 MONTHLY WEATHER REVIEW VOLUME 138 Simulation of the Diurnal Cycle in Tropical Rainfall and Circulation during Boreal Summer with a High-Resolution GCM JEFFREY J. PLOSHAY AND NGAR-CHEUNG LAU NOAA/Geophysical Fluid Dynamics Laboratory, Princeton, New Jersey (Manuscript received 24 November 2009, in final form 9 March 2010) ABSTRACT The simulation of the diurnal cycle (DC) of precipitation and surface wind pattern by a general circulation model (GCM) with a uniform horizontal resolution of 50 km over the global domain is evaluated. The model output is compared with observational counterparts based on datasets provided by the Tropical Rainfall Measuring Mission and reanalysis products of the European Centre for Medium-Range Weather Forecasts. The summertime diurnal characteristics over tropical regions in Asia, the Americas, and Africa are portrayed using the amplitude and phase of the first harmonic of the 24-h cycle, departures of data fields during selected hours from the daily mean, and differences between extreme phases of the DC. There is general agreement between the model and observations with respect to the large-scale land–sea contrasts in the DC. Maximum land precipitation, onshore flows, and landward migration of rainfall signals from the coasts occur in the afternoon, whereas peak maritime rainfall and offshore flows prevail in the morning. Seaward migration of precipitation is discernible over the western Bay of Bengal and South China Sea during nocturnal and morning hours. The evolution from low-intensity rainfall in the morning/early afternoon to heavier precipitation several hours later is also evident over selected continental sites. However, the ob- served incidence of rainfall with very high intensity in midafternoon is not reproduced in the model atmosphere.
    [Show full text]
  • 2017-CDTC-Congressio
    CONTINENTAL DIVIDE TRAIL COALITION CONGRESSIONAL REPORT FEBRUARY 2017 www.continentaldividetrail.org CONTINENTAL DIVIDE NATIONAL SCENIC TRAIL THE HARDEST. THE HIGHEST. THE CDT. The Continental Divide Trail climbs and descends along the Rocky Mountains from Canada to Mexico, traversing 3,100 miles of America’s most dramatic and wild backcountry across the Continental Divide, the backbone of America. For more information visit www.continentaldividetrail.org THE FACTS: COMPLETING THE TRAIL 1978 2016 The trail is to be managed as non- The Continental Divide Trail is Proposed to Congress. Approximately 95% of the trail is 980 Miles in 1966 located within public ownership. Land motorized. Approximately 24% of the Idaho and Montana acquisitions or easements are needed to 76% trail exists on routes open to motor 95% protect the remaining 5% (172 miles) of NON vehicle use, and should be relocated in PROTECTED MOTORIZED Designated as a National Scenic Trail by the National Parks and the trail corridor. the coming years. 730 MILES on MOTORIZED Routes 1978 Recreation Act, which amended National Trails System Act. 2350 MILES on NON-MOTORIZED Trail 550 Miles in Wyoming Continental Divide Trail Comprehensive Management Plan is Once the trail is “complete”, the work is never done. Agency staff, partners and volunteers will continue to work tirelessly to ensure the trail is well-maintained, passable, and re-aligned as necessary in the years to come. 2009 amended. 800 Miles in 3100 Miles in total Colorado 2150 Miles across 20 National Forests HIKING THE CDT Since 1978, there have been 10-25 attempted thru hikes every year. In 2011, approximately 50 people attempted thru 770 381 Miles across 13 BLM Field Offices hikes.
    [Show full text]
  • Catchment Boundaries of Ocean Drainage Basins
    Catchment Boundaries of Ocean Drainage Basins Philip Craig February 27, 2019 Contents 1 Introduction1 2 Terminology2 3 Method 2 4 Datasets 3 4.1 HydroSHEDS.....................................3 4.2 ETOPO05.......................................3 4.3 Geofabric.......................................4 4.4 Natural Resources Canada..............................5 4.5 Ice Sheet Mass Balance Inter-Comparison Exercise (IMBIE)............6 5 Catchment boundaries7 5.1 Americas.......................................8 5.2 Africa and the Middle-East..............................9 5.3 South-East Asia.................................... 10 5.4 The Arctic....................................... 11 5.5 Southern Ocean.................................... 13 6 The Ocean Drainage Basins 14 References 16 1 Introduction This document describes the data and method used to construct the boundaries between the drainage basins of each ocean basin. These will be used primarily as the release points for trajectories in chapter 5 and also to evaluate moisture fluxes in chapter 4 of Craig(2018) - this documentation is also adapted from chapter 2 of Craig(2018). Figure1 shows the drainage basins for the major oceans and seas. The aim is to use topographic datasets (section4) to approximate the catchment boundaries and the ocean drainage basins they surround. These will not precisely match Figure1 as they are approximated and also because different extents of the ocean drainage basins will be used to suit this study. 1 Figure 1: Depiction of the major ocean drainage basins from www.radicalcartography.net. Light green regions drain into the Atlantic Ocean, dark green into the Arctic Ocean, purple into the Pacific Ocean, red into the Indian Ocean, brown into the Southern Ocean, blue into the Caribbean Sea and turquoise into the Mediterranean Sea.
    [Show full text]
  • Physical & Man-Made Features
    United States Geography Physical & Man-Made Features You might be wondering… What are physical features? Physical Features of a place include things like: We will learn about the following physical features: •Atlantic Coastal Plain •Continental Divide •The Great Basin •Death Valley •Great Lakes •St. Lawrence River •Gulf of Mexico •Great Plains Atlantic Coastal Plain • Located along the East Coast • Borders the Atlantic Ocean • Lowland area • Great for agriculture or farming • Contains many rivers, swamps, and marshes Great Plains • Located in the Central United States, east of the Rocky Mountains • Grassy flatlands • No trees • Easy to see for miles Continental Divide •Imaginary line located in the peaks of the Rocky Mountains •Rivers on the eastern side of the Continental Divide flow to the Atlantic Ocean or Gulf of Mexico •Rivers on the western side flow toward the Pacific Ocean The Great Basin •Located west of the Rocky Mountains •Has many different elevations: mountains, valleys, & low lying areas. •Water does not drain out of this region. It holds rainwater and precipitation like a basin or Click here for a bowl, because water is unable short video on to drain to the sea. the Great Basin Death Valley •Located within The Great Basin Region •Home of the lowest point in North America •282 feet below sea level •Temperatures up to 120 degrees are common here Click here to watch a short video about Death Valley. Great Lakes •Located in the northern United States, between the U.S. and Canada •Largest fresh water lakes in the world •Includes 5 lakes: Superior, Michigan, Huron, Erie, and Ontario Click here to watch a short video about the Great Lakes .
    [Show full text]