Because the UK is the same distance from the equator as parts of Canada. The Gulf Stream keeps the UK warmer than Canada.
The St. Regis Mohawk Tribe is located in Northern New York State, on the border of Canada. The Reservation also lands between the Provinces of Ontario and Quebec. Mohawks of Kahnawake are located on the south shore of Montreal, Quebec. Mohawks of Kanesatake are located on Ottawa River, just up stream of Montreal, Quebec. Mohawks of Tyendinaga is located on the Bay of Quinte in southeastern Ontario, Canada. Wahta Mohawk Territory is a reserve in the District Municipality of Muskoka, Ontario, Canada. Six Nations of the Grand River is located on the Grand River which is just south of the City of Brantford, Ontario.
To measure the slope of a stream, you can use the formula: slope = (change in elevation) / (horizontal distance). First, determine the elevation difference between two points along the stream using a level or GPS. Then, measure the horizontal distance between those points on a map or with a measuring tool. The resulting slope will provide a ratio that indicates the steepness of the stream's gradient.
Yes, you can.
The vertical drop of a stream channel over distance is known as the Gradient.
The vertical drop of a stream channel over distance is known as the Gradient.
The St. Lawrence River of the Canadian provinces of Ontario and Quebec forms part of the international boundary line between Ontario and New York State. The Niagara River separates Canada & the U.S., from Buffalo to Niagara Falls.
WIth chinese skill :)
The vertical drop of a stream channel over distance is known as the Gradient.
A) the distance traveled by water in a channel times a drop in elevation b) the drop in elevation of a stream divided by the distance the water travels c) the water pressure at the bottom of the stream divided by the stream's width d) the increase in discharge of a stream per unit drop in elevation
13 miles
The term is known as stream gradient, which represents the steepness of a stream channel and is calculated as the vertical drop of a stream over a specific horizontal distance. It is expressed in feet per mile or meters per kilometer.