Answer:
The independence processes of the United States and Canada were very different from each other.
The United States obtained its independence from Great Britain after a war of independence that lasted from 1775 to 1783. That is, it was a violent and convulsive process, in which both nations faced each other to settle their directly opposed interests.
On the other hand, Canada walked its way towards independence in a peaceful way. In 1867 the Constitution Act was approved, which created the Dominion of Canada, with an autonomous government but subject to the laws of the British Parliament. Years later, in 1931, the Statute of Westminster was approved, establishing the legislative equality of the British and Canadian Parliament. Finally, in 1982, the Constitution of Canada eliminated dependence on the British Parliament.
It was Great Britain. You can see it through the fact that English is still spoken there. Southern Rhodesia is today's Zimbabwe and Northern Rhodesia is today's Zambia.
Answer:
Mineral industry
Explanation:
The most important industry in the American industrial development process is the mineral industry. In industrialization in general, the use of energy and mineral resources is essential.
The U.S. has a large diversity of mineral deposits, such as coal and iron, which are abundant. However, there is a dependence on petroleum due to the decrease in oil reserves and other minerals, making it the largest importer of minerals in the world.
We can see this because the U.S. is the nation that most consumes these resources. The proof of this is the American's cars, with their majority having powerful engines of 8, 10, and 12 cylinders, which consume much fuel.
Rigaudon is in duple meter
Answer: The December 26, 2004 Indian Ocean tsunami was caused by an earthquake that is thought to have had the energy of 23,000 Hiroshima-type atomic bombs. ... Within hours of the earthquake, killer waves radiating from the epicenter slammed into the coastlines of 11 countries, damaging countries from east Africa to Thailand.
The high of the wave in 2004 tsunami was 100 feet
Explanation: For an earthquake-generated tsunami, the wavelength generally reaches a few hundred kilometres if the concerned fault is long. For the 2004 Sumatra earthquake, the wavelength is estimated, from the first wave measured by the Jason-1 satellite altimeter, as around 500–600 km (Gower 2005).
