Chavez's legacy in Venezuela can be viewed in two totally contrasting ways, depending on who will be writing the history.
Explanation:
Hugo Chavez was one of the last communist leaders in the world, led by communism, which unlike the majority of the communist leaders, actually had a lot of support by the people. He was leader of Venezuela for long time, and his reign was only ended because he died. As a typical communist leader, Chavez wanted to have everything under control, including the resources of the country, eliminating and suppressing any opposition, and trying to make the country as self-sustaining as possible.
The majority of the people supported him, and one of the main reasons for that was that he openly opposed the United States and the corporations, and nationalized the oil and natural gas reserves. The people of Venezuela had very bad feelings for the United States because of their interference in their country, and Chavez used it to the maximum.
When future history books are written, how would Chavez be interpreted will depended mostly on who will write the history books, as well as the political climate in the country. It can range anywhere from portraying him as national hero that protected the country, its interest, and was beloved by the people, to a brutal tyrant that isolated the country, suppressed the people, and made Venezuela stagnate.
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Answer:
A. Multicultural
Explanation:
Montreal is a melting pot of people from all sorts of cultures
There military strength, there economy must be stable, and they must have a strong government
Answer:
well 8 x 25 = 200 so thats the volume
Explanation:
Answer:
A sediment deposit close to the continental rise having a coarse material overlaid by successively finer materials of non marine origin is called a turbidite.
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Explanation:
Turbidity current is the movement of sediment laden water . It is caused by the high density nature of sediments . The current is prevalent in oceans and lakes and it one process that transport sediments from coastal areas to deep sea.
The sediments in the current makes the flow denser and very rapid. The rapid nature of the movement of this sediment laden water causes a kind of selective deposition in deep sea. The more coarse sediments are deposited before less coarse sediments. The sediments deposited fines upward. The coarsest sediments are found at the bottom and it fine upward.
Turbidites are sediments deposited by turbidity currents which gradually change from coarse grain to fine grain sediments. The continental rise is the boundary between continents and the deep part of the oceans. This area is usually laden with sediment deposited by turbidity current. The sediments laden water moves downhill.
