In 1998, Canada's highest court declared that Quebec could not legally secede.
Explanation:
Canada is the second largest country in the world. In order for the vast territory to be easier for governing, Canada is divided into provinces and territories. Such provinces and territories in Canada are:
- Quebec
- Ontario
- Alberta
- Manitoba
- British Columbia
- Saskatchewan etc.
While most of the provinces and territories have nothing against being in the borders of Canada, there is one that opposes it, that being Quebec. Quebec is one of the provinces that contributes the most to the GDP of the country, is one of the most populous, and has an excellent location.
This province doesn't want to be in the borders of Canada though, but instead wants to be independent. The main reasons for that are that the majority of the people of Quebec have different ethnic and cultural background than the rest of the provinces and territories. While the people of Quebec already had several referendums about independence, with the majority of the population voting for it, the Canadian highest court declared any attempts for seceding of Quebec illegal in 1998.
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im super sure thats...C....sorry if im wronh
Well there's is frozen sea weed and there is plankton and hair grass
Hi there!
You will have already be known that the <em>sun's rays are closest to the equatorial regions</em> <em>than</em> the <em>polar regions</em>. So the stronger heat rays reach the equator first, heating it's water faster. Within the span of time when the rays reach the polar areas (poles), the sun rays become slanted, leading it into the ocean waters.
Also, the sharpness or intensity of the rays gets weakened, thereby heating the water of polar regions less.
Using this fact, we can say that the rays falling near the equator heats the water more than the rays heating the water at poles.
Hence, we can say that <u>D) </u><u>T</u><u>he sun heats earth and it ocean unevenly</u> will be your answer.
Thank you !
Answer:
transform
Explanation:
Is part of a transform plate boundary that disrupts the topography of an old subduction zone