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Lecture 3  physiography, geography and climate of l.a
Lecture 3  physiography, geography and climate of l.a
Lecture 3  physiography, geography and climate of l.a
Lecture 3  physiography, geography and climate of l.a
Lecture 3  physiography, geography and climate of l.a
Lecture 3  physiography, geography and climate of l.a
Lecture 3  physiography, geography and climate of l.a
Lecture 3  physiography, geography and climate of l.a
Lecture 3  physiography, geography and climate of l.a
Lecture 3  physiography, geography and climate of l.a
Lecture 3  physiography, geography and climate of l.a
Lecture 3  physiography, geography and climate of l.a
Lecture 3  physiography, geography and climate of l.a
Lecture 3  physiography, geography and climate of l.a
Lecture 3  physiography, geography and climate of l.a
Lecture 3  physiography, geography and climate of l.a
Lecture 3  physiography, geography and climate of l.a
Lecture 3  physiography, geography and climate of l.a
Lecture 3  physiography, geography and climate of l.a
Lecture 3  physiography, geography and climate of l.a
Lecture 3  physiography, geography and climate of l.a
Lecture 3  physiography, geography and climate of l.a
Lecture 3  physiography, geography and climate of l.a
Lecture 3  physiography, geography and climate of l.a
Lecture 3  physiography, geography and climate of l.a
Lecture 3  physiography, geography and climate of l.a
Lecture 3  physiography, geography and climate of l.a
Lecture 3  physiography, geography and climate of l.a
Lecture 3  physiography, geography and climate of l.a
Lecture 3  physiography, geography and climate of l.a
Lecture 3  physiography, geography and climate of l.a
Lecture 3  physiography, geography and climate of l.a
Lecture 3  physiography, geography and climate of l.a
Lecture 3  physiography, geography and climate of l.a
Lecture 3  physiography, geography and climate of l.a
Lecture 3  physiography, geography and climate of l.a
Lecture 3  physiography, geography and climate of l.a
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Lecture 3 physiography, geography and climate of l.a

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  • 1. Physiography, Geographyand Climate ofLatin America (Lecture 3)
  • 2. Natural Landmarks in LatinAmerica Worlds longest and second highest mountain range, and the worlds highest active volcanoes. Biggest river in the world. Worlds driest desert. Worlds largest rainforest, and is the worlds greatest storehouse of species Worlds greatest reserve of potential agricultural land. It is a great storehouse of minerals, with enormous potential production.
  • 3. Landscape of Contrast: Patagonia: lakes, penguins, continental ice
  • 4. Andes, Macchu Pichu
  • 5. Pico de Orizaba (Volcano Citlaltépetl), Méxicos highest peak and NorthAmericas highest volcano.
  • 6. World’s Driest Desert:Atacama, Chile
  • 7. Rainforest canopy, and AmazonRiver Continuous Fields Tree Cover Project
  • 8. Climate Most of Latin America is located in the tropics – Land located between the Tropic of Cancer (23.5o N) and the Tropic of Capricorn (23.5o S) – In the tropics there is not much seasonal variation in temperature; seasonal differences are manifested in rainfall variations.
  • 9. Dallas USA 100 25 80 20Temperature (F) Precipitation (in) 60 40 15 The Tropical 20 10 Climate: Little 0 5 variation in annual -20 J F M A M J J A S O N D 0 temperature Annual Precip: 34.6 in. Max Temp. Ave. Temp. Ave. Precip. Rowntree, Lewis, and Price. Diversity and Globalization: World Regions, Environment, Development, 2nd edition (2002).
  • 10. Air temperature – yearly changes
  • 11. Precipitation annual variation
  • 12. Altitudinal Zonation– Much of the temperaturevariation in the tropics isseen with changes inelevation rather thanchanges in latitude As elevation increases, temperature decreases at an average rate of 3.5oF/1,000 ft. Five climate zones: Caliente (hot), Templada (warm), Fria (cold), Helada (frozen), and Paramos.
  • 13. 0 – 499 m 500 – 999 mTierra Caliente “Hot Land” below 900 meters - 3,000’ in elevation, coastal plains and foothills Hot days, warm nights Tropical agricultural products – sugar cane, tropical fruits (bananas), & lowland tubers
  • 14. 0 – 499 m 500 – 999 m 1000 – 1999 mTierra Templada Cloud Forest Nicaragua, coffee plantation–Temperate Land 900 m (3,000’)– 1800m (6,000’) in elevation, intermediate mountain slopes Mild days and cool nights Most populous zone Agricultural products include – Coffee, maize, vegetables, cut flowers.
  • 15. 0 – 499 m 500 – 999 m 1000 – 1999 m 2000 – 2999 mTierra Fria Potato harvest, Bolivia “Cold Land” 1800m (6,000’) – 3600m (12,000’) in elevation, mountainous areas More common in South America Warm days and cold nights Wheat, barley, maize, tubers (Peruvian Andes), sheep, guinea pigs, Llama, Alpaca (hardier or highland crops and animals
  • 16. 0 – 499 m 500 – 999 m 1000 – 1999 m 2000 – 2999 m 3000 – 3999 mTierra Helada 4000 – 4999 m –“Frozen Land” Above 3600m (12,000’) in elevation, highest mountain peaks Cool days and cold nights Highland grains and tubers, sheep, guinea pigs, Llama, Alpaca
  • 17. 0 – 499 m 500 – 999 m 1000 – 1999 m 2000 – 2999 m 3000 – 3999 mParamos 4000 – 4999 m 5000 – 5999 m – Above 4600 m (15,000’) in elevation, highest mountain peaks Just below snow line characterized by tussock grasses, shrubs and cushion plants
  • 18. Glaciers and the Snowline:LA has glaciers near the equator Latin America
  • 19. Physical GeographyLatin America and the Caribbean can be divided in three topographic zones: Lowlands ( less than 500 meters) Highlands (500-2000 meters) – Plateaus: flat top highland regions Mountain (greater than 2000 meters)
  • 20. Plateaus or highlands Mountains lowlands 1000 2000 30000m >5000 m
  • 21. The Mighty AndesNorthern, Central and Southern Andes– Run from northwestern Venezuela to the southern tip of Tierra del Fuego. Mountain chain formed by the subduction of the Pacific plate beneath South America.– Approximately 30 peaks that are over 20,000 feet high– The Andes are divided into three sub-regions Northern – Venezuela, Columbia, and Ecuador Central – Ecuador, Peru and Bolivia – high altitude plateaus (Altiplano) Southern – defines the border between Chile & Argentina – South of Santiago the mountains are lower.
  • 22. TopographicProfiles
  • 23. Relief of S. America
  • 24. Highlands of Mexico and CentralAmerica – Mexican plateau and the Central American volcanic arc – This area is home to the major cities of Mexico and Central America – Mexican Plateau lower (4,000’) in the north (near Juarez) and higher (8,000’) in the south (near Mexico City) This region is home to rich deposits of silver, copper & zinc – Central American Highlands Volcanic chain runs from Tehuantepec Isthmus, southern Guatemala, Costa Rica to Panama The volcanic eruptions has resulted in rich volcanic soil throughout much of Central America
  • 25. Physiography of Mexico
  • 26. Middle America Physiography Mexico to TehuantepecCordilleran system of North Americacontinues in Mexico with Sierra MadreOriental and Occidental forming anintermontane plateau of 4,000 to 8,000feet. Tehuantepec to PanamaHighlands of volcanic origin containinghigh plateaus.Narrow coastal lowlands.The intermontane basins may containlakes as Lake Nicaragua
  • 27. Andes Mountains Flyover VideoThis computer animation simulates a high-altitude flight along the Andes.
  • 28. South America Flyover the Andes http://www.jpl.nasa.gov/srtm/images/movies/AndesFlt_3201.MPG
  • 29. Plateaus of South America Brazilian Plateau Largest and more important in terms of natural resources and settlement Runs from the southern edge of the Amazon Basin to the Rio de la Plata Major population centers of Brazil are located along the coastal fringe of the Brazilian plateau. Patagonian Plateau Much of this area is steppe (dry grasslands) Guiana Plateau A sparsely settled region
  • 30. River Basins and Lowlands Within the major river basins there are vast interior lowlands Most of these lowlands are sparsely settled and offer little agricultural activity, with the exception of grazing livestock
  • 31. Amazonlowlands Rio de la Plata lowlands
  • 32. Rivers ofLatinAmerica:All of theMajor Riversare in SouthAmerica
  • 33. Continental Orinoco system Divide in S. Amazon system America is close to the Pacific Rio de la Plata system The Continental divide North America in a more central positionContinental divide
  • 34. Run off / Water Surplus
  • 35. 3 Major Rivers in S. America 1. Amazon 3 – Drains an area of approx. 2.4 million sq. miles – the 1 largest river in the world 2. Rio de La Plata – S. America’s second largest watershed 3. Orinoco River 2 – Third largest river basin in South America –
  • 36. Natural Resources Because of its tropical location, there is a high degree of biodiversity in the region – Many varieties of plants and animals found nowhere else on earth – The region is home to the world’s largest rain forest There are also massive reserves of natural resources – natural gas and oil (South America as well as Mexico) – copper (Chile), silver (Mexico and Peru), Iron (Brazil).

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