Contacts between sedentary and nomad peoples<span> resulted in trade, tribute payments</span>
Answer:
The climate and vegetation of Latin America have made many people move out, certain areas to be highly populated while some lack population, with the way of life, is very vibrant, with a lot of interaction, music, and spending time outside.
Explanation:
The majority of Latin America has tropical types of climate, with smaller patches having Mediterranean, temperate, or mountainous climates. Being dominated by tropical climates, this region is not the best when it comes to equal distribution of population, as the tropical rainforests have too much vegetation, heat, humidity, and precipitation, while the deserts and semi-deserts lack vegetation and water resources.
This has led to people being concentrated heavily along the coastlines, but also at relatively flat area high on the mountains and plateaus near the Equator. A lot of people have decided to migrate to other regions though, as their environment has not been the best for living. The ways of life can be said that are similar in many ways to the cultures from the Mediterranean region, vibrant, loud, lot of interaction and music, spending a lot of time outside.
The lithosphere, which is the rigid outermost shell of a planet (the crust and upper mantle), is broken up into tectonic plates. The Earth's lithosphere is composed of seven or eight major plates (depending on how they are defined) and many minor plates. Where the plates meet, their relative motion determines the type of boundary: convergent, divergent, or transform. Earthquakes, volcanic activity, mountain-building, and oceanic trench formation occur along these plate boundaries. The relative movement of the plates typically ranges from zero to 100 mm annually.[2]
Tectonic plates are composed of oceanic lithosphere and thicker continental lithosphere, each topped by its own kind of crust. Along convergent boundaries, subduction carries plates into the mantle; the material lost is roughly balanced by the formation of new (oceanic) crust along divergent margins by seafloor spreading. In this way, the total surface of the lithosphere remains the same. This prediction of plate tectonics is also referred to as the conveyor belt principle. Earlier theories, since disproven, proposed gradual shrinking (contraction) or gradual expansion of the globe.[3]
Tectonic plates are able to move because the Earth's lithosphere has greater strength than the underlying asthenosphere. Lateral density variations in the mantle result in convection. Plate movement is thought to be driven by a combination of the motion of the seafloor away from the spreading ridge (due to variations in topography and density of the crust, which result in differences in gravitational forces) and drag, with downward suction, at the subduction zones. Another explanation lies in the different forces generated by tidal forces of the Sun and Moon. The relative importance of each of these factors and their relationship to each other is unclear, and still the subject of much debate.
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