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Mexico
| Term Paper Title |
Mexico |
| # of Words |
3769 |
| # of Pages (250 words per page double spaced) |
15.08 |
Mexico
Mexico
Southward from its 1,500 mile long border with the United States lies
the Estados Unidos Mexicanos. A country with slightly more than 750,000 square
miles in area, Mexico has a vast array of mineral resources, limited
agricultural land, and a rapidly growing population. These factors are the basis
for many of the country's present problems as well as opportunities for future
development. The nation is struggling to modernize its economy. With more than
80 million people in the mid-1980s, Mexico's overall population density exceeds
110 per square mile. More than half of its inhabitants live in the country's
central core, while the arid north and the tropical south are sparsely settled.
The stereotype of Mexico is that it is a country with a population
consisting mainly of subsistence farmers has little validity. Petroleum and
tourism dominate the economy, and industrialization is increasing in many parts
of the nation. Internal migration from the countryside has caused urban centers
to grow dramatically: more than two thirds of all Mexicans now live in cities.
Mexico City, with a metropolitan area population of approximately 16 million
people, is the largest city in the world. While still low by United States
standards, the nation's gross national product per capita rose significantly
during the 1970s. Despite impressive social and economic gains, since 1981
Mexico has been wracked by severe inflation and an enormous foreign debt brought
on in large part by precipitous declines in the value of petroleum products.
Geologically, Mexico is located in one of the Earth's most dynamic areas.
It is a part of the "Ring of Fire," a region around the Pacific Ocean
highlighted by active volcanism and frequent seismic activity. Within the
context of plate tectonics, a theory developed to explain the creation of major
landform features around the world, Mexico is situated on the western, or
leading, edge of the huge North American Plate. Its interaction with the Pacific,
Cocos, and Caribbean plates has given rise over geologic time to the Earth-
building processes that created most of Mexico. Towering peaks, like
Citlaltepetl at some 18,000 feet, are extremely young in geologic terms and are
examples of the volcanic forces that built much of central Mexico. The
spectacular eruption of the volcano Chinchon in 1981 was more powerful than that
of Mount St. Helens in the United States a year earlier and led to widespread
devastation.
Much of the complex
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