Cortez set the basis for social, economic, ethnic, religious, political changes in what is now Mexico, which was of great benefit for the Spanish, but devastating to the local populations.
Explanation:
Hernan Cortez was a Spanish conquistador. He was sent in what is now Mexico in order to gain territory for the Spanish crown, and get as much wealth as possible. In order to do so, Cortez was merciless, and that had devastating effects on the locals.
The Spanish conquistadors massacred the local populations. They destroyed their culture, their cities, and gave their best to assimilate them. On top of that, the diseases that spread out from the Spanish killed off much of the local populations.
Cortez, and the other conquistadors, took every piece of gold and silver they were able to get their hands on, robbing the region. For the Spanish that was of great benefit though, as they became very wealthy and powerful.
Some of the people that suffered from Cortez and the other conquistadors were:
- Aztecs
- Zapotecs
- Toltecs
- Maya
- Tlaxcala
- Mixtec
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A, in urban areas :)
Urban areas have bigger populations than rural ones and the Rocky Mountains have terrain that is difficult to settle on
Answer:
B. subsistence agriculture
Explanation:
Subsistence agriculture refers to that type of agriculture in which crops were grown in order to feed their own families. These crops were not grown for selling but for themselves in order to survive. At that time there were no markets where all food stuff available. They have plenty of lands where these people grow what they want to eat. They also hunt animals such as rabbit and deer etc in order to eat them.
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.
