The Geographical Landscape Brazil’s Atlantic Coastal Plain

The settlers thereby came to search for alternative exports, in this case agriculture, especially sugarcane, cocoa, meadow (Kent 237). Throughout the rest of the colonial era, sugar agriculture became the backbone of the economy. Sugar planting brought Brazilian transformational transplantation system (Kent 236). Brazil moved from a popular remote location to a vibrant productive colony (Kent 238). This region is still the center of the people's economic, social, cultural and political life (Kent 236).

Coastal plains are low and flat areas near the coast. The coastal plains of South America are in the northeastern coast of Brazil, the Atlantic Ocean, Western Western Peru, the Pacific coast, Chile. The coastal plains in northeast Brazil are very dry. Brazilian highlands serve as wedges that expel moist sea breeze from coastal plains. The plain on the west coast is also very dry. They were trapped between the cold Peruvian stream in the West and the Andean in the east. Peru 's ocean current carries cold water to the Pacific coast of Peru and Chile. This cold surface water causes a reversal of heat. It is cold air at sea level, stable and warm air at high temperature. Thermal inversion creates thick clouds at low altitude. These lowland clouds cover most of the Pacific coast of South America. They can not form precipitation

The vast Atlantic coast plains are on the inland mountains in the middle. The narrow Pacific Coast Plain was blocked by the volcano and formed several wonderful landscapes. There are several volcanic lakes dotted in Nicaragua. The biggest of them is the boat shop of Lago de Nicaragua. The capital Managua is located on the contaminated Lago de Managua Coast. The highest point was 2,107 meters, Mogoton Nicaragua appeared by Spanish conquistadors in the early 16th century. Columbia's former Indian civilization was almost completely infected and the population's loss due to slavery and banishment was completely destroyed. Spain made Nicaragua colonized; Granada is one of America's oldest colonial cities. During the colonial period, Nicaragua was a member of General Capitania based in Guatemala.

The terrain of the southern colonies is located between latitudes 40 and 30 degrees and is usually divided into three regions. The Atlantic coastal plain (in two parts: the inner coastal plain and the tide water), Piedmont, Blue Ridge Mountains and Appalachian Mountains. The Atlantic coastal plain has developed over the past 6,000 years and has been flattened by global floods and sediment transport from the river system of the Appalachian Mountains. Ocean tide has a great influence on rivers passing through rivers, so these river systems cross each other and are therefore known as tidal waters.