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American Falls with Goat Island to its right. The Niagara River (/ naɪˈæɡərə, - ɡrə / ny-AGG-ər-ə, -grə) flows north from Lake Erie to Lake Ontario, forming part of the border between Ontario, Canada, to the west, and New York, United States, to the east. The origin of the river's name is debated.
High water levels of the Neretva River. [7] Petexbatún River. Pasión River. Central America. Winter rain flooding of the Pasión River. [8] Qiantang River. Hangzhou Bay.
The Red River near Pembina, North Dakota, about 3 kilometres (2 mi) south of the Canada–U.S. border. The Pembina River can be seen flowing into the Red at the bottom. The Red River begins at the confluence of the Bois de Sioux and Otter Tail rivers, on the border of Wahpeton, North Dakota and Breckenridge, Minnesota.
The Mississippi River[ b ] is the primary river and second-longest river of the largest drainage basin in the United States. [ c ][ 15 ][ 16 ] From its traditional source of Lake Itasca in northern Minnesota, it flows generally south for 2,340 miles (3,766 km) [ 16 ] to the Mississippi River Delta in the Gulf of Mexico.
Starting in Brevard County and meeting the Atlantic Ocean at Duval County, the St. Johns is Florida's primary commercial and recreational waterway. It flows north from its headwaters, originating in the direction of the Lake Wales Ridge, which is only slightly elevated at 30 feet (9.1 m) above sea level.
The St. Lawrence River (French: Fleuve Saint-Laurent [flœv sɛ̃lɔʁɑ̃]) is a large international river in the middle latitudes of North America connecting the Great Lakes to the North Atlantic Ocean. Its waters flow in a northeasterly direction from Lake Ontario to the Gulf of St. Lawrence, traversing Ontario and Quebec in Canada and New ...
During the winter months as much as 75% of the flow in the North Branch is due to the discharge of treated sewage from the North Side Water Reclamation Plant into the North Shore Channel. [41] Flow on the main stem is measured at Columbus Drive; between 2000 and 2006 this averaged 136 cubic feet (3.9 m 3) per second. [42]
Under real-world conditions, the Coriolis force does not influence the direction of water flow perceptibly. Only if the water is so still that the effective rotation rate of the Earth is faster than that of the water relative to its container, and if externally applied torques (such as might be caused by flow over an uneven bottom surface) are ...