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Viefleur [7K]
3 years ago
15

Which part of the election process helps political parties pick their candidates

History
2 answers:
Elina [12.6K]3 years ago
7 0
B. I hope this helps
melisa1 [442]3 years ago
6 0

Answer:

it is primary elections! dont put b or else your gonna fail it.

Explanation:

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Central America, southernmost region of North America, lying between Mexico and South America and comprising Panama, Costa Rica, Nicaragua, Honduras, El Salvador, Guatemala, and Belize. (Geologists and physical geographers sometimes extend the northern boundary to the Isthmus of Tehuantepec in Mexico.)

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Geography & Travel

Geographic Regions

Central America

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Professor Emeritus of Latin American History, Tulane University, New Orleans. Author of A Short History of Guatemala.

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Central America, southernmost region of North America, lying between Mexico and South America and comprising Panama, Costa Rica, Nicaragua, Honduras, El Salvador, Guatemala, and Belize. (Geologists and physical geographers sometimes extend the northern boundary to the Isthmus of Tehuantepec in Mexico.)

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BRITANNICA QUIZ

Quick Quiz: Central American Geography

Central America consists of seven countries (and sometimes part of an eighth), but this quiz includes only two questions. How quickly can you answer them?

Central America makes up most of the tapering isthmus that separates the Pacific Ocean, to the west, from the Caribbean Sea. It extends in an arc roughly 1,140 miles (1,835 km) long from the northwest to the southeast. At its narrowest point the isthmus is only about 30 miles (50 km) wide, and there is no location in Central America that is more distant than 125 miles (200 km) from the sea.

Humid swamps and lowlands extend along both the west and east coasts, but four-fifths of Central America is either hilly or mountainous. The western band of Pacific coastal lowland is narrow and overshadowed by mountain ranges, and, except in Nicaragua and Honduras, the eastern plains along the Caribbean are also narrow. Elevation steadily increases west of the Caribbean lowlands, until, toward the Pacific Coast, plateau highlands culminate in mountain ridges and some 40 volcanic cones, some of which attain elevations of more than 12,000 feet (3,700 metres). Some of Central America’s volcanoes erupt violently from time to time, and earthquakes frequently occur in the region. The weathered volcanic lavas produce a fertile soil, however, and the highlands of the volcanic zones have consequently become highly productive agricultural zones and areas of dense population.

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The eruption of Mount St. Helens 35 years ago provided an amazing opportunity for scientists to study the effects of catastrophe. The incredible lessons are as valuable as ever!

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May 18, 2015, marks the 35th anniversary of one of the most violent natural disasters of our modern time, the colossal 1980 eruption of Mount St. Helens in Washington state. Its explosive power shocked the world and made headline news. Fifty-seven people died, over $1 billion worth of property was destroyed, and over 230 square miles (600 km2) of forests were immediately flattened. Recent rumblings are again making news, raising fears that the volcano may be reawakening.

While the losses were tragic, the value to science has been inestimable. Geologists vastly improved their ability to predict eruptions, safely evacuating tens of thousands of Filipino people before Pinatubo erupted in 1991. Scientists began learning many other valuable lessons, some of which have challenged the foundations of evolutionary thinking.

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Harry R. Truman, who operated a lodge near Mount St. Helens for over fifty years, became a folk hero when he refused to evacuate. “The mountain is a mile away,” he told reporters. “The mountain ain’t gonna hurt me.” He and his lodge were later buried under 150 feet (46 m) of debris.

The eruption of Mount St. Helens is often regarded as the most significant geologic event of the twentieth century. Since the volcano was conveniently located in Washington state, only two hours’ drive from Portland, scientists could document the eruption in unprecedented detail. Although not the most powerful explosion on record, it provided a natural laboratory for understanding how quickly catastrophic processes can reshape the earth, and how rapidly wildlife can recover.

Within moments of eruption, the whole northern side of the mountain (two-thirds of a cubic mile of rock) slid away—the largest observed landslide on record. The eruption lasted nine hours, followed by more eruptions over the next six years. Geologists, who are accustomed to thinking about slow evolutionary processes shaping our world, were astounded by the scale of initial destruction and the speed at which new geologic features formed. Thirty-five years later, Mount St. Helens still teaches us lessons about the powerful forces the Creator used to shape the earth. These findings confront the underlying slow-and-gradual assumptions of modern geologic thinking, and they give us invaluable clues about the catastrophic potential of a global, cataclysmic Flood.

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