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The Pettaquamscutt River (pet-uh-KWAHM-skit; [1] also known as Narrow River) is a tidal extension of the Mattatuxet River in the U.S. state of Rhode Island. It flows approximately 6.3 miles (10.1 km). [ 2 ]
A bore in Morecambe Bay, in the United Kingdom Video of the Arnside Bore, in the United Kingdom The tidal bore in Upper Cook Inlet, in Alaska. A tidal bore, [1] often simply given as bore in context, is a tidal phenomenon in which the leading edge of the incoming tide forms a wave (or waves) of water that travels up a river or narrow bay, reversing the direction of the river or bay's current.
The river is navigable only by small boats below that, and the river below it is affected by the tides. It winds widely through marshes below that before emptying into Kingston Bay. The Elm Street Dam in Kingston on the Jones River was removed in Late-Summer/Fall 2019. Together with the Wapping Road Dam removal in 2011, the Jones River runs ...
The Little River is a 12.9-mile-long (20.8 km) river in New Hampshire and Massachusetts in the United States. It is a tributary of the Merrimack River , part of the Gulf of Maine watershed . The Little River rises in Kingston, New Hampshire , flows south through Plaistow , and enters the city of Haverhill, Massachusetts , where it joins the ...
Ed Lombardo, fly fishing expert, instructor and guide, said: “Fished the Narrow River [Narragansett] last week; was very slow landing four bass in three days. The water temperature on the upper ...
The town of Narragansett occupies a narrow strip of land running along the eastern bank of the Pettaquamscutt River (aka Narrow River) to the shore of Narragansett Bay on the Atlantic Ocean. It was separated from South Kingstown in 1888 and incorporated as a town in 1901. With several ocean beaches and a walkable strip along the ocean front ...
Head of tide, tidal limit [2] or tidehead [3] is the farthest point upstream where a river is affected by tidal fluctuations, [4] or where the fluctuations are less than a certain amount. [5] The river section influenced by tides and marine forces but without salinity is a tidal river, while downstream areas are brackish and termed estuaries. [6]
Great Pond is a 268-acre (1.08 km 2) [1] water body in Rockingham County in southeastern New Hampshire in the United States. The lake lies near the center of the town of Kingston.