The Shinnecock Canal and Dismal Swamp Canal are both near which ocean?
4e3bf05ec2072b1e220f6f26d8444529
Shinnecock Canal The Shinnecock Canal (also known as the Shinnecock and Peconic Canal) is a canal that cuts across the South Fork of Long Island at Hampton Bays, New York. At 4700 ft long, it connects Great Peconic Bay and the north fork of Long Island with Shinnecock Bay and the Atlantic Ocean. The canal opened to traffic in 1892.
70b030c42e62122889b7ef70b0595003
Dismal Swamp Canal The Dismal Swamp Canal is located along the eastern edge of the Great Dismal Swamp in Virginia and North Carolina in the United States. It is the oldest continually operating man-made canal in the United States, opened in 1805, and closed in October 2016. It is part of the Intracoastal Waterway, an inland route, which parallels the east coast and offers boaters shelter from the Atlantic Ocean from Manasquan Inlet, New Jersey, to Brownsville, Texas. The route runs through bays, lakes, rivers, streams, and canals, and includes the Intracoastal Waterway running from Norfolk, Virginia, to the Florida Keys.
dcb4515d5f95eb9e91f8100f229f6cad
Dalcahue Channel Dalcahue Channel (Spanish: ""Canal de Dalcahue"") is a body of water of the Sea of Chiloé that separates Quinchao Island from Chiloé Island, both part of the Chiloé Archipelago in southern Chile. The town of Dalcahue is located close to the narrowest part.
c5fd6aefe4a4f81e7ecfa36293ef13ac
Mozambique Channel The Mozambique Channel (French: "Canal du Mozambique" , Malagasy: "Lakandranon'i Mozambika" , Portuguese: "Canal de Moçambique" ) is an arm of the Indian Ocean located between Madagascar and Mozambique. The channel is about 1600 km long and 419 km across at its narrowest point, and reaches a depth of 3292 m about 230 km off the coast of Mozambique. A warm current, the Mozambique Current, flows in a southward direction in the channel, leading into the Agulhas Current off the east coast of South Africa.
83a992d866a553ae2af751824c182476
Panama Bight The Panama Bight is a marine ecoregion on the Pacific coast of the Americas.
c8709818c17ebd7fbc20344f907199a0
Dismal Swamp, South Australia Dismal Swamp is a locality in the Australian state of South Australia located about 361 km south-east of the state capital of Adelaide and about 19 km north-west of the municipal seat of Mount Gambier.
6a22911e25924506a2be61c0324a9a79
North Channel (Great Britain and Ireland) The North Channel (known in Irish and Scottish Gaelic as "Sruth na Maoile", in Scots as the "Sheuch" and alternatively in English as the Straits of Moyle or Sea of Moyle) is the strait between north-eastern Ireland and south-western Scotland. It connects the Irish Sea with the Atlantic Ocean, and is part of the marine area officially classified as the "Inner Seas off the West Coast of Scotland" by the International Hydrographic Organization (IHO).
01d248531f2ab6f3e93e14f88838e80d
Great Bay (New Hampshire) Great Bay is a tidal estuary located in Strafford and Rockingham counties in eastern New Hampshire, United States. The bay occupies over 6000 acre , not including its several tidal river tributaries. Its outlet is at Hilton Point in Dover, New Hampshire, where waters from the bay flow into the Piscataqua River, thence proceeding southeast to the Atlantic Ocean near Portsmouth. The northern end of the bay, near its outlet, is referred to as Little Bay.
d5fce36d3040bd9d026411b2987448b7
Newichawannock Canal The Newichawannock Canal is a man-made canal which drains Great East Lake into Horn Pond at the border between Wakefield, New Hampshire, and Acton, Maine, in the northeastern United States. It is at the head of the Salmon Falls River, which the Abenaki called "Newichawannock", meaning "river with many falls". Begun in 1850 by the Great Falls Company to increase the water available for its mills in Somersworth, New Hampshire, the 0.75 mi canal is unusual as it was built for strictly industrial purposes in an area remote from the actual industrial site. The canal forms the boundary between the states of New Hampshire and Maine, and is spanned by a stone bridge built at the same time. The canal and bridge, along with related artifacts, were listed on the National Register of Historic Places in 2014.
1f4da19520cfda50640878407594f8a7
Hampton Beach, New Hampshire Hampton Beach is a village district, census-designated place, and beach resort in the town of Hampton, New Hampshire, United States, along the Atlantic Ocean. Its population at the 2010 census was 2,275. Hampton Beach is in Rockingham County, about 15 mi south of Portsmouth. The community is a popular tourist destination and the busiest beach community in New Hampshire. Ocean Boulevard, the main street along the beach, includes a boardwalk, many shops and businesses, several seasonal hotels, and the Hampton Beach Casino Ballroom, which hosts national acts in the summer. Hampton Beach State Park was named one of four "Superstar" beaches in the United States in 2011, for having had perfect water-quality testing results in each of the previous three years.
85091148f5a0eb9897b355ad3f43d2c4
Case Inlet Case Inlet, in southern Puget Sound in the U.S. state of Washington, is an arm of water between Key Peninsula on the east and Hartstine Island on the west. Its northern end, called North Bay, reaches nearly to Hood Canal, creating the defining isthmus of Kitsap Peninsula. Case Inlet is the boundary between Pierce County and Mason County. The southern end of Case Inlet is connected to Nisqually Reach, part of the southern basin of Puget Sound. Herron Island lies in Case Inlet.
02884b0bf550498bda828ba13aa145a3
Blake Plateau The Blake Plateau lies in the western Atlantic Ocean off the southeastern United States coasts of North Carolina, South Carolina, Georgia and Florida. The Blake Plateau lies between the North American continental shelf and the deep ocean basin extending about 145 kilometers (90 miles) east and west by 170 kilometers (106 miles) north and south, with a depth of about 500 meters (1,640 feet) inshore sloping to about 1,000 meters (3,281 feet) about 375 kilometers (233 miles) off shore, where the Blake Escarpment drops steeply to the deep basin. The Blake Plateau, associated Blake Ridge and Blake Basin are named for the U.S. Coast and Geodetic Survey steamer George S. Blake, in service 1874-1905, that first used steel cable for oceanographic operations and pioneered deep ocean and Gulf Stream exploration. Survey lines of the steamer "Blake" first defined the plateau that now bears the ship's name.
b535cd342ae9fb770dd0a5fa79108fdd
Chemung Canal The Chemung Canal is a former canal in New York, United States. The canal connected Seneca Lake at Watkins Glen to the Chemung River at Elmira, New York. It was planned to connect the Finger Lakes region and Pennsylvania's Susquehanna River watershed with New York's Erie Canal system. The latter connected the Great Lakes with the Hudson River and ultimately the Atlantic port of New York City.
3b9ffa1cb91b033d9139c7b1c728fe5c
Gardiners Bay Gardiners Bay is a small arm of the Atlantic Ocean, approximately 10 mi (16 km) long and 8 mi (13 km) wide in the U.S. state of New York between the two flukelike peninsulas at the eastern end of Long Island. It is bounded on its eastern end, where it connects to Block Island Sound, by Gardiners Island and Promised Land.
cacbd247be199f62d9ae53da3bfdbb00
Kennebunk River The Kennebunk River is a 17.6 mi river in southern Maine in the United States. It drains a settled rural area southwest of Portland, emptying into the Atlantic Ocean.
67ae76df2267e189628aaee8c72c20d0
Northwest Passage The Northwest Passage (abbreviated as NWP) is, from the European and northern Atlantic point of view, the sea route to the Pacific Ocean through the Arctic Ocean, along the northern coast of North America via waterways through the Canadian Arctic Archipelago. The eastern route along the Arctic coasts of Norway and Siberia is accordingly called Northeast Passage (NEP).
91b9c547a2a2887fc6a97db2c1c2a2de
Supply, North Carolina Supply is a small unincorporated community in Brunswick County, North Carolina, United States located around the intersection of US 17 (Ocean Highway) and NC 211 (Southport-Supply Road/Green Swamp Road). Its name is derived from the use of the Lockwoods Folly River as a trade route in the 18th and 19th centuries. Residents of the nearby beach communities of Holden Beach, Oak Island, Ocean Isle, Caswell Beach, and Sunset Beach often used to commute to Supply for goods and other materials. This practice is still common, but development in the town of Southport and in the Intracoastal Waterway commercial districts has made traveling to Supply unnecessary.
a61323873cd83c7f264411e9843bc956
Broad Canal Broad Canal is a short canal in East Cambridge, Massachusetts, previously larger and part of the now-vanished canal system that made Cambridge an active seaport.
6c90ad50123dbcafad2eca32094516fa
Sea of Japan The Sea of Japan (see below for other names) is a marginal sea between the Japanese archipelago, Sakhalin, the Korean Peninsula and Russia. The Japanese archipelago separates the sea from the Pacific Ocean. It is bordered by Japan, Korea (North and South) and Russia. Like the Mediterranean Sea, it has almost no tides due to its nearly complete enclosure from the Pacific Ocean. This isolation also reflects in the fauna species and in the water salinity, which is lower than in the ocean. The sea has no large islands, bays or capes. Its water balance is mostly determined by the inflow and outflow through the straits connecting it to the neighboring seas and Pacific Ocean. Few rivers discharge into the sea and their total contribution to the water exchange is within 1%.
5ab72a2ac65a36f32ef6587f8fe2c1c2
Washington Canal (New Jersey) The Washington Canal, in Sayreville, New Jersey, is a waterway connecting the South River with the Raritan River, bypassing several loops at the mouth of the former.
480a8e0eb7c0ca35fe5b634780e96980
Dismal Swamp (New Jersey) The Dismal Swamp is a marshy area in
66873b7ac08ee9e74388577c3c0fb66d
Miami River (Florida) The Miami River is a river in the United States state of Florida that drains out of the Everglades and runs through the city of Miami, including Downtown. The 5.5 mi long river flows from the terminus of the Miami Canal at Miami International Airport to Biscayne Bay. It was originally a natural river inhabited at its mouth by the Tequesta Indians, but it was dredged and is now polluted because of its route through Miami-Dade County. The mouth of the river is now home to the Port of Miami and many other businesses whose pressure to maintain it has helped to improve the river's condition.