Answer: is best known for conquering the Aztecs and claiming Mexico on behalf of Spain. ... Cortés ignored the order and traveled to Mexico anyway, setting his sights on overthrowing ruler Montezuma II in the Aztec capital of Tenochtitlan.
Explanation:
The correct answer is the following.
The correct matches are:
Western nations grew richer by exploiting colonized nations: effect.
Locals suffered in poverty: effect.
Western nations wanted to profit from weaker, resource-rich nations: cause.
Internal conflicts arose because of diverse communities living in a single nation: effect.
European countries expansionist goals and imperialist ideas affected South Asia. These nations wanted to expand their territories and used their military force to impose its will in South Asia. The Netherlands, England, Spain, and France were the European countries that had political and economic interests in this region. France invaded Saigon in 1859, Great Britain controlled Burma until 1948. Spain colonized the Philippines in 1565 until 1898. The Netherlands colonized the Indonesian Archipelago in 1605.
Answer:
Texas is the correct answer.
Explanation:
Answer:
Three causes of the War of 1812 were maritime problems, Manifest Destiny, and national pride. One of the three main causes of the War of 1812 was maritime problems between the United States and Great Britain. The seeds of these maritime problems were planted nine years before the War of 1812 even began.
Explanation:
Answer: Twentieth century.
Plate tectonics is a scientific theory that describes the movement of plates of the Earth’s lithosphere. The model builds on the concept of continental drift, which proposed that continents had “drifted” relative to each other across the ocean bed. The speculation was first put forward by Abraham Ortelius in 1596. The concept was developed independently by Alfred Wegener in 1912, but the theory was generally rejected.
It was only with the discovery of mid-oceanic ridges in 1947 that the theory began acquiring evidence. Scientists also used devices developed during WWII to study odd magnetic variations across the ocean floor. By 1967, plate tectonics were fully accepted in modern geophysics.
