1821-1903
They both involved Canada and Britain. In the Boer war, Britain wanted Canada to send troops to help them out. Wilfred Laurier, the prime minister of Canada, as a compromise to the imperialists and the nationalists in the country, decided to send one thousand volunteer troops. In the Alaska Boundary Dispute between Canada and the United States, Britain chose two Canadians and one British judge. The deciding voter, the British Lord Alverstone, chose to move the US border closer to the coastline, but not close enough for Canada to have control over the Lynn canal. Canadians were unhappy with the result.
An example is the Alaska Boundary Dispute. This was between Canada and the United States. In the end, the Canadians were unhappy because the US had control over the Lynn canal. This issue was brought to light due to the gold in the Klondike region.
Thomas Hodgins has written: 'The Alaska-Canada boundary dispute'
The assassination of President McKinley made the Alaska boundary negotiations easier for America to deal with. Teddy Roosevelt, who took over for McKinley, was prepared to use force to settle disputes over Alaska and the Canadians backed down and let the United States set most of the boundaries.
CANADA
Russian and Canadians both make good neighbors.
The U.S. President who based his campaign slogan on the Oregon boundary dispute with Britain was James K. Polk. His campaign slogan was "Fifty-four Forty or Fight!", which referred to the latitude line of 54°40' north as the desired northern boundary of the Oregon Territory, extending all the way to the southernmost tip of Alaska.
the nile
The Mount Redoubt, like the other volcanoes of southern Alaska, is the result of a convergent plate boundary, specifically a subduction zone.
Seattle The folks is Alaska would like to dispute that. Barrow Alaska is the northern most incorporated area, but only has a population of 4000. Fairbanks Alaska is the most northern US City with a population over 20,000.
The plate boundary associated with earthquakes in Alaska is primarily a transform boundary, where the Pacific Plate slides horizontally past the North American Plate along the Aleutian Trench. This movement causes frequent seismic activity in the region.