How does colonization still affect us today?

1 answer:

5 0

Colonization caused a major cultural shift and merge. For example, the English left a footprint on the United States, which is why Americans speak English. Another example is the country of Haiti in the Caribbean. They were a colony of France and now today their population speaks Haitian French. Traditions of colonizers were also passed down. Mexico was a colony of Spain and at the time of the colonization of the New World Spain was highly Catholic, now the Mexican population are also highly Catholic due to the spreading of Catholicism during Mexicos colonial days. The merge of Settlers and Natives also created a new mix of population and a more diverse community. Even Japan during WW2 had colonized Indochina (Vietnam, Cambodia, Laos) which in the short period all the Vietnamese learned Jungle War tactics from the Japanese that were used in The Vietnam War.

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Where a mid-ocean ridge is offset, the linear feature connecting and between the crests of the ridge segments is called a?

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When a mid-ocean ridge is offset, the linear feature connecting and between the crests of the ridge segments is called a Transform Fault.

As the Earth's tectonic plates separate, new ocean bottom is generated along divergent plate borders, which are known as mid-ocean ridges. Massive basalt volcanic eruptions result from molten rock rising to the seafloor as the plates divide. A ridge's shape is influenced by how quickly it spreads; slower spreading rates produce steep, erratic topography, while faster spreading rates result in much wider profiles and kinder slopes.

In geology and oceanography, a transform fault is a type of fault when two tectonic plates slide past one another. A transform fault may develop in the area of a fracture zone that connects spreading centres to deep-sea trenches in subduction zones or that lies between various offset spreading centres.

In the 1960s, Morgan postulated that spreading centres and transform faults separate opposing plates along an oceanic ridge crest that is offset by fracture zones.

The direction of motion on the transform faults was predicted by Morgan's hypothesis to be opposite to the offsets of the ridge crests, which was a rather dramatic assertion.

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