The reason why the Midwestern United States have a very fertile soil, but Canada doesn't, despite both of them being covered by glaciers until relatively recently, and both having the same age of soil, is the climate and vegetation.
Canada is much colder than the Midwest, its winters are longer, and the summers mild, while the Midwest has higher temperatures, prolonged period of drought, and seasonal rainfall.
Because of this, Canada has been covered by coniferous forests. They leave relatively little biomass, and also the climate is making the decomposition of the biomass very slow, thus resulting in relatively poor soil quality.
In the Midwest, the climate is perfect for the development of the grasslands. The grasses grown and die each year. They live a lot of biomass, and the higher temperatures contribute that the biomass decomposes pretty quickly, thus resulting in good quality soil.
Answer:
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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.
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