114 Sentences With "tidal inlet" | Random Sentence Generator

Boaters can head out to Great Bay, a tidal inlet of the Atlantic.

As a tidal inlet, the waterway is comprised of a brackish mix of fresh and saltwater, which was thought to have been an automatic blockade for sharks.

Rather than embracing the shallow tidal inlet on its opposite side, the glider-shaped structure seems to soar toward it, its wings pointing inland as it rushes toward the water.

Cover image: Plastic bottles and other refuse lay washed up on the banks of a tidal inlet off the Delaware River at Pennypack On The Delaware Park in Philadelphia, PA, February 8, 2020.

With a bocce court, an abundance of outdoor seating overlooking a tidal inlet off Branford Harbor and a 2,500-square-foot taproom (complete with a granite-faced fireplace), Stony Creek has become one of the area's most popular destinations since its opening in March 2015.

The Deep Creek is a tidal inlet of the Bahamas.

The Starve Creek is a tidal inlet of the Bahamas.

Munlochy sits at the top of the tidal inlet of Munlochy Bay, that is itself an opening of the Moray Firth.

Matawan Creek is a creek and partially a tidal inlet of Raritan Bay. It lies in Monmouth County, New Jersey across from Staten Island, New York.

Early Cretaceous diorite stocks are exposed south of Tidal Inlet, and on Sebree and Sturgress Islands. Quartz diorite outcrops on Lemesurier Island. A granitic stock is exposed in Dundas Bay.

In 2017, storm surge from Hurricane Irma caused a new tidal inlet to breach the southern end of Blackbeard Island, and created a small island between Sapelo Island and Blackbeard Island.

Ophiomorpha burrows are common in the lower part. The Blood Reserve sandstones are interpreted as shoreline, barrier island and tidal inlet deposits.Lerand, M.M. 1983. Sedimentology of the Blood Reserve Sandstone in southern Alberta.

Warfleet Creek is a small triangular tidal inlet in the west side of the River Dart estuary in England. It is near Dartmouth, Devon. It has steep rocky sides. At low tide there is a stony beach with some small rockpools.

Knotts Creek is a U.S. Geological Survey. National Hydrography Dataset high- resolution flowline data. The National Map , accessed April 1, 2011 tidal inlet on the south shore of the Nansemond River in the city of Suffolk, Virginia, in the United States.

At the time of its founding, it was essentially laid out on a peninsula, and the pond was more of a tidal inlet of the Piscataqua River. Its present surroundings are the result of intensive development and redevelopment in the 19th and 20th centuries.

Potter Pond (formerly Fish Pond) is a saltwater pond in the town of South Kingstown, Washington County, Rhode Island, United States. Its tidal inlet connects to Point Judith Pond. It is one of nine coastal lagoons, referred to as "salt ponds" by locals, in southern Rhode Island.

Salt Marsh at Hoffler Creek Hoffler Creek is a U.S. Geological Survey. National Hydrography Dataset high-resolution flowline data. The National Map , accessed April 1, 2011 tidal inlet of the James River on its southern side in Hampton Roads. It forms the boundary between the cities of Portsmouth and Suffolk, Virginia.

Milepost 251.5, west of Saltash station. () A Class D viaduct high and long on 9 trestles. It was replaced by a stone viaduct on 19 October 1894. Because it crossed a deep, muddy tidal inlet, Brunel constructed this viaduct on timber piles and used timber trestles instead of stone piers.

The Glimmer Glass Bridge is a county owned bridge in Monmouth County, New Jersey, United States. It carries traffic from Brielle Road over the Glimmer Glass, a navigable tidal inlet of the Manasquan River, between Manasquan and Brielle. It has also been on the National Register of Historic Places, since 2008.

Aripeka is located at on both sides of Hammock Creek, a small tidal inlet to the Gulf of Mexico. Similar in geophysical structure to Hernando Beach, Bayport, and Pine Island, Florida, Aripeka is surrounded by marshland, mostly within Hernando County. The Pasco-Hernando county line is located at the South Hammock Creek Bridge.

View of Quaket River from Nanaquaket Bridge, Tiverton, Rhode Island The Quaket River is a tidal inlet, in the U.S. state of Rhode Island. It flows approximately 1 km (.6 mi) from the mouth of Nannaquaket Pond into the Sakonnet River. It is located entirely within the town of Tiverton, Rhode Island.

The Cray turns eastward through Crayford and Barnes Cray to join the Darent in Dartford Creek. The Creek is a well-watered partly tidal inlet (of the Tideway) between Crayford Marshes and Dartford Marshes by a slight projection of land, Crayford Ness. The villages through which the Cray flows are collectively known as "The Crays".

Engelhard is in eastern Hyde County along U.S. Route 264, which leads northeast to Manteo and west to Belhaven. According to the U.S. Census Bureau, the CDP has a total area of , all of it recorded as land. The community is at the head of Far Creek, a small tidal inlet of Pamlico Sound.

Ashlett is a small settlement in Hampshire, England. It is in the civil parish of Fawley. It is at the end of Ashlett Creek, a tidal inlet of Southampton Water. Ashlett is known for having a well-preserved tidal mill (currently a sailing club clubhouse), which is next to a free slipway and landing stage.

The Taylor River is a longNew Hampshire GRANIT state geographic information system river located in southeastern New Hampshire in the United States. It is a tributary of the Hampton River, a tidal inlet of the Atlantic Ocean. Approximately two miles of the Taylor River are tidal. The river rises on the border between Hampton Falls and Kensington, New Hampshire.

Portencross () is a hamlet near Farland Head in North Ayrshire, Scotland. Situated about west of Seamill and about south of Hunterston B nuclear power station, it is noted for Portencross Castle. It has two harbours and a pier. The "Old Harbour" is actually a small tidal inlet next to the castle, and is part of the castle property.

Bolsa Chica State Beach is a public ocean beach in Orange County, California, United States. It is located north of Huntington Beach and south of the community of Sunset Beach. This beach is used for surf fishing, especially in the tidal inlet channel at the southern end. Fish include perch, croaker, cabezon, California corbina, and shovelnose guitarfish.

The Gunpowder River is a U.S. Geological Survey. National Hydrography Dataset high-resolution flowline data. The National Map, accessed April 1, 2011 tidal inlet on the western side of Chesapeake Bay in Maryland, United States. It is formed by the joining of two freshwater rivers, Gunpowder Falls (often referred to locally as "Big Gunpowder Falls") and Little Gunpowder Falls.

The river's name is derived from the Anglo-Saxon "tidal inlet". In Anglo-Saxon times, the Fleet served as a dock for shipping. The lower reaches of the river were known as the Holbourne (or Oldbourne), whence Holborn derived its name. The river gives its name to Fleet Street which runs from Ludgate Circus to Temple Bar at the Strand.

Cariño is a municipality in the province of A Coruña, in the autonomous community of Galicia, northwestern Spain. It is situated in the north of the province and located on the Ría de Ortigueira y Ladrido (Ortigueira and Ladrido tidal inlet). Cariño has a population of 4,617 inhabitants (INE, 2008). Cariño and Cedeira's coast has some of the highest cliffs in Europe.

Prior to 1905, the only access across the Hillsborough River was by ferry.The Hillsborough River is a 30 km long and up to 1 km wide tidal inlet which empties into Charlottetown Harbour. During the 1800s, a seasonal passenger ferry service operated between the Charlottetown waterfront and Ferry Point on the opposite side. When the river was frozen in winter, horse-drawn sleighs would cross the ice.

The Little River is an east-west tidal inlet on the coast of Down East Maine, with the town of Cutler on its northern bank. At the mouth of the inlet stands Little River Island, near whose easternmost point the lighthouse stands. The station consists of a tower, keeper's house, oilhouse, and boathouse. The tower is an iron structure, with a supporting frame of steel and brick.

Barrow Harbour is a tidal inlet off Tralee Bay, County Kerry, Ireland. Once this was the major port for the region, servicing the monastic settlement of Ardfert and the general area of Tralee. Barrow is overlooked by Tralee Golf Club, from which there are views of Tralee Bay and Banna Strand. A narrow entrance to the harbour was protected by Fenit Castle on Fenit Island.

Retrieved on 2014-06-23. SeaLand expanded its operations into the newly developed container terminal. In 1958, the port authority dredged another shipping channel, which straightened the course of Bound Brook, the tidal inlet forming the boundary between Newark and Elizabeth. Dredged materials were used to create new upland south of the new Elizabeth Channel, where the port authority constructed the Elizabeth Marine Terminal.

Eastney Lake, also known by locals as 'Eastney Creek' or 'The Creek', is a natural tidal inlet of Langstone Harbour and is located on the northern side of the Eastney peninsular, with Milton on the northern side. A small enclosed lagoon nicknamed 'The Glory Hole' is located on the southern shore of Eastney Lake, and is refilled with Langstone Harbour's salt-water on high spring tides.

Mamaroneck Harbor is the name of a bay located in the village of Mamaroneck on the Long Island Sound, in Westchester County, New York. It is open to southerly winds but affords shelter against northerly winds for vessels drawing less than 10. The depth in the outer harbor is from 7 to 12 feet at low tide. Mamaroneck River is a shallow, and a stream or tidal inlet.

Lamprey River c. 1920, Epping, New Hampshire The Lamprey River is a NH GRANIT database river in southeastern New Hampshire, the United States. It rises in Meadow Lake in Northwood, and flows south, then generally east through Raymond, Epping, Lee, Durham and finally Newmarket. Here, it meets Great Bay, a tidal inlet of the Atlantic Ocean, to which it is connected by a tidal estuary, the Piscataqua River.

The bridge required four abutments, one on each shoreline and one on either side of the draw (or bascule) span.Arlington Memorial Bridge, HAER No. DC-7, p. 4. The abutments had to be erected on bedrock. The bridge was relatively low to the water,Originally, there was no land west of the Washington Monument grounds and south of Constitution Avenue NW; this area was a tidal inlet of the Potomac River.

Markt (market square) Bruges became important due to the tidal inlet that was important to local commerce, This inlet was then known as the "Golden Inlet". Bruges received its city charter on 27 July 1128, and new walls and canals were built. In 1089 Bruges became the capital of the County of Flanders. Since about 1050, gradual silting had caused the city to lose its direct access to the sea.

Each island in the chain is separated from the next by a tidal inlet. As a consequence of Corolla's development in the 1980s, horses on Currituck Banks came into contact with humans more frequently. By 1989, eleven Bankers had been killed by cars on the newly constructed Highway 12. That same year, the Corolla Wild Horse Fund, a nonprofit organization, was created to protect the horses from human interference.

Narrawallee is a coastal village in the South Coast region of New South Wales, Australia. At the , it had a population of 1,241. The village, along with its southern neighbours Mollymook and Mollymook Beach are generally considered part of the Milton-Ulladulla district within the City of Shoalhaven local government area. Narrawallee is predominantly a residential suburb, bordered by a tidal inlet to the north and Matron Porter Drive.

Map of Brooklyn in 1766, including Gowanus Creek The Gowanus neighborhood originally surrounded Gowanus Creek. It consisted of a tidal inlet of navigable creeks in original saltwater marshland and meadows that contained wildlife. The Dutch government issued the first land patents within Breukelen (modern-day Brooklyn), including the land of the Gowanus, from 1630 to 1664. In 1636, the leaders of New Netherland bought the area around the Gowanus Bay.

Ocean swimming is offered at Mile Beach and Half Mile Beach, while warmer waters are found at a tidal inlet, The Lagoon, where the quieter waters tend to be 10 to 15 degrees warmer. The park also has picnicking areas, fishing, and hiking trails. The beaches provide essential nesting areas for endangered least terns and piping plovers. Other wildlife commonly found along the beaches include various shorebirds, eider ducks, clams, and mussels.

A new location became available in 1890. When terrible floods hit the District of Columbia in 1881, Congress enacted legislation to have the channel of the Potomac River deepened to help prevent future flooding. The silt would be used to reclaim the Tiber Creek tidal inlet, building up the land south of B Street and west of the Washington Monument grounds to a height great enough to act as a levee.Tindall, p.

Chignik Lagoon is at (56.307535, -158.535023), on the southeast shore of the tidal inlet of the same name. It is bordered to the east by the city of Chignik. According to the United States Census Bureau, the CDP has an area of , all of it land. In 2009 the Marines of 4th Combat Engineer Battalion, 4th Marine Division, began work on an inter- village road system to link Chignik Lake to Chignik Lagoon.Sgt.

In the khor-lagoon-sabkha model, an initial rise in sea-level floods coastal areas and creates shallow water features. If the features silt up, or the land rises, or the sea level falls, then the trapped water evaporates, leaving a flat salt pan, or sabkha. If the coastal region has irregular topography, then the flooding creates large independent creeks, or khors. A khor is a shallow, subtidal flat or tidal inlet.

Dell Bridge is a footbridge in Port Sunlight, Wirral, England. It is recorded in the National Heritage List for England as a designated Grade II listed building. The bridge was built with sandstone in 1894 for Lever Brothers in their model village of Port Sunlight and was designed by the Chester architects' firm of Douglas and Fordham. It carries a pedestrian walkway over a landscaped hollow which had been formed from a former tidal inlet.

The city is on a strip of coastal lowland and extends up the lower alpine slopes of the Chugach Mountains. Point Campbell, the westernmost point of Anchorage on the mainland, juts out into Cook Inlet near its northern end, at which point it splits into two arms. To the south is Turnagain Arm, a fjord that has some of the world's highest tides. Knik Arm, another tidal inlet, lies to the west and north.

The Nyali Bridge is a concrete girder bridge connecting the city of Mombasa on Mombasa Island to the mainland of Kenya. The bridge crosses Tudor Creek (a tidal inlet) to the north-east of the island. The bridge is one of three road links out of Mombasa (the others being the Kipevu and Makupa Causeways). The Likoni Ferry provides a third transport link to the island, and is situated at the southern tip.

The name is an elision of "Pîl Gwynllyw" (or "Gwynllyw's Pîl" in English). 'Pîl' is a localised topographical element (found across the coast of South Wales, from Pembrokeshire and into Somerset) indicating a tidal inlet from the sea, suitable as a harbour. In local tradition, it is said that this name derives from the early part of Gwynllyw's life when he was an active pirate. The tradition states that Gwynllyw maintained his ships at Pillgwenlly.

Havelock is located in southern Craven County at (34.882736, -76.909230). The city limits encompass most of Marine Corps Air Station Cherry Point and extend as far north as the tidal Neuse River. Slocum Creek is a tidal inlet that extends south from the Neuse as far as the center of Havelock. According to the United States Census Bureau, the city has a total area of , of which is land and , or 4.56%, is water.

Retrieved on May 14, 2008. These were Peter, Richard, Osbert, and Umbald, with Peter becoming the first prior. The monks began the development of the marshes surrounding the abbey, cultivating the land and embanking the riverside into a Priory Close spanning 140 acres of meadow and digging dykes. They turned the adjacent tidal inlet at the mouth of the River Neckinger into the priory's dock, and named it St Saviour's Dock, after their abbey.

Handcrafted male figurine, 650–800 AD.Jaina Island is a pre-Columbian Maya archaeological site in the present-day Mexican state of Campeche. A small limestone island on the Yucatán Peninsula's Gulf coast with only a tidal inlet separating it from the mainland, Jaina served as an elite Maya burial site, and is notable for the high number of fine ceramic figurines excavated there.Coe. The term "Jaina" translates to "Temple in the Water".

Part of the south shore of Lituya Bay showing the trimline, with bare rock below Lituya Bay is a fjord located on the Fairweather Fault in the northeastern part of the Gulf of Alaska. It is a T-shaped bay with a width of and a length of . Lituya Bay is an ice-scoured tidal inlet with a maximum depth of . The narrow entrance of the bay has a depth of only .

Barra lies across the waters of North Bay. The headland of Rubha na Maighdein, Fuiay, on the left and the island of Flodaigh on the right The island had six households located along a "street" at Rubh' an Aiseig (English: "ferry headland") in the north west at some point, probably in the early 19th century. It has been uninhabited since about 1850. There is a tidal inlet here that may have been an effective fish-trap.

Carew Tidal Mill stands on the south end of a long causeway across the Carew River, a tidal inlet east of Milford Haven. Carew Castle, built in 1270, is to the east. The site of the now ruined castle was occupied by a fort in the Iron Age, and much later by an earth and wood fort built around 1100 by Gerald de Windsor, a Norman. The castle was in turn a military stronghold and a comfortable Elizabethan mansion.

Coney Island Creek is a Coney Island Creek Resiliency Study, New York City Economic Development Corporation (NYCEDC) - 2016.07.08, pages 14-15 tidal inlet in Brooklyn, New York City. It used to be a continual strait and a partial mudflat connecting Gravesend Bay and Sheepshead Bay, making Coney Island an actual island, but the eastern half of the creek was filled in by land owners and city construction projects during a period spanning the early to mid 20th century.

The power station is located on the north side of Field Street, an industrial area between Massachusetts Route 3A and the Town River, a tidal inlet of the Weymouth Fore River on Quincy's coast. It is a large brick structure, with three interior levels of work space. Its southern facade has three round-arch windows, set above recessed brick panels. The flat roof stands above a modillioned cornice, which is supported by brick pilasters at the building corners.

Tidal mill at 284x284px A tide mill is a water mill driven by tidal rise and fall. A dam with a sluice is created across a suitable tidal inlet, or a section of river estuary is made into a reservoir. As the tide comes in, it enters the mill pond through a one-way gate, and this gate closes automatically when the tide begins to fall. When the tide is low enough, the stored water can be released to turn a water wheel.

The Drakes River is a longNew Hampshire GRANIT state geographic information system stream located in southeastern New Hampshire in the United States. It is a tributary of the Taylor River, a tidal inlet (via the Hampton River) of the Atlantic Ocean. The river rises in an office park just southeast of the Interstate 95/NH 101 interchange in Hampton, New Hampshire. It flows south, through Coffin Pond, and reaches the Taylor River just west of the Route 1 crossing of the Hampton saltmarsh.

Liverpool's first dock was the world's first enclosed commercial dock, the Old Dock, built in 1715. The Lyver Pool, a tidal inlet in the narrows of the estuary, which is now largely under the Liverpool One shopping centre, was converted into the enclosed dock. Further docks were added and eventually all were interconnected by lock gates, extending along the Liverpool bank of the River Mersey. From 1830 onwards, most of the building stone was granite from Kirkmabreck near Creetown, Scotland.

McClellanville is located in northeastern Charleston County at (33.088953,-79.467287). U.S. Route 17 passes along the northwestern edge of the town, leading northeast to Georgetown and southwest to Charleston. According to the United States Census Bureau, McClellanville has a total area of , of which is land and , or 5.02%, is water. Jeremy Creek, a tidal inlet, runs through the center of the town, and the town limits extend south to the Intracoastal Waterway, adjacent to Cape Romain National Wildlife Refuge.

Hamford Water is a biological Site of Special Scientific Interest between Walton-on-the-Naze and Harwich in Essex. The site is a tidal inlet which has marsh grasslands, creeks, mud and sand flats, salt marshes, islands and beaches. It is described by Natural England as "of international importance for breeding little terns and wintering dark-bellied brent geese, wildfowl and waders, and of national importance for many other bird species." Rare plants include hog's fennel and slender hare's-ear.

Wallasey Pool was a natural tidal inlet of water that separated the towns of Wallasey and Birkenhead on the Wirral Peninsula, England. Originally flowing directly into the River Mersey, it was converted into the sophisticated Birkenhead Dock system from the 1820s onwards by land reclamation, with the main portion of the pool becoming known as the Great Float. In 1933, with the exception of a small lake, the head of Wallasey Pool at Poulton was converted into Bidston Dock. By 2003, this dock had been filled in.

The Hampton River is a tidal inlet in the towns of Hampton and Hampton Falls, New Hampshire, the United States. It is surrounded by the largest salt marsh in New Hampshire, covering over .New Hampshire GRANIT database The river is formed by the confluence of the Taylor and Hampton Falls rivers. The Hampton River flows for one mile (1.6 km) before broadening into Hampton Harbor, an estuary which also receives flow from small tidal channels such as the Browns River and the Blackwater River.

Charlotte Harbor is located at (26.963897, -82.062267) on the north bank of the Peace River, the main tidal inlet to the Charlotte Harbor estuary, itself an arm of the Gulf of Mexico. U.S. Route 41, the Tamiami Trail, crosses the Peace River between Charlotte Harbor and Punta Gorda via the Barron Collier Bridge (northbound) and the Gilchrist Bridge (southbound). According to the United States Census Bureau, the Charlotte Harbor CDP has a total area of , of which is land and , or 53.95%, is water.

In the nineteenth century, Juhu was an island: a long, narrow sand bar rising above sea level by a metre or two, just off the west coast of Salsette. It could be reached during low tides by walking across the tidal inlet. Juhu was called "Juvem" by the Portuguese. At its north point, nestled the village of Juhu, inhabited by Bhandaris (toddy tappers), Agris (salt traders) and Kunbis (cultivators) and at its south point, opposite Bandra island, lived a small colony of fisherfolk and cultivators (Koliwada).

Other factors of importance to the shape of the delta are the local tectonic activities of the Peel Boundary Fault, the substrate and geomorphology, as inherited from the Last Glacial and the coastal-marine dynamics, such as barrier and tidal inlet formations.Cohen et al. (2002) Since ~3000 yr BP (= years Before Present), human impact is seen in the delta. As a result of increasing land clearance (Bronze Age agriculture), in the upland areas (central Germany), the sediment load of the Rhine has strongly increasedHoffmann et al.

The west side of the bay consists of a 26,000 feet thick sequence of Paleozoic sedimentary rocks, mainly massive limestones and argillite. The oldest rocks in this sequence are the Late Silurian Willoughby limestone and the youngest being the Middle Devonian Black Cap limestone. An outcrop west of Tidal Inlet includes a sandstone, graywacke and limestone of unknown age. Sedimentary rocks of unknown age on the east side of Muir Inlet include tuff interbedded with limestone. The rocks exposed on the 1,205 foot high hill called "The Nunatak" have been metamorphosed.

The Seabrook Nuclear Power Station, as seen across the Blackwater River in Seabrook The Blackwater River is a tidal inlet in northeastern Massachusetts and southeastern New Hampshire in the United States.New Hampshire GRANIT state geographic information system The river forms in a salt marsh in the northeastern corner of Salisbury, Massachusetts, by the convergence of the Little River and Dead Creek. Heading north, the river quickly enters Seabrook, New Hampshire and continues to flow through salt marsh until it reaches Hampton Harbor, northwest of Seabrook Beach, where it joins the Hampton River.

The Ouse valley in Sussex was almost certainly a tidal inlet in Norman times, for the Domesday book of 1086 lists several salt works, which produced salt by evapourating sea water. Some were quite far inland, and such works were recorded at Laughton and Ripe on the Glynde. Other activities around the edges of the water included fishing and agriculture. By the early 14th century, some reclamation of the flood plain had taken place, with the construction of embankments to create fertile meadows, but the process was not without risk.

In 1958, the Port Authority dredged another shipping channel which straightened the course of Bound Brook, the tidal inlet forming the boundary between Newark and Elizabeth. Dredged materials was used to create new upland south of the new Elizabeth Channel, where the Port Authority constructed the Elizabeth Marine Terminal. The first shipping facility to open upon the Elizabeth Channel was the new Sea-Land Container Terminal, which was the prototype for virtually every other container terminal constructed thereafter. The Ironbound is an industrial area along the bay which becomes residential farther inland near Downtown Newark.

The word "estuary" is derived from the Latin word aestuarium meaning tidal inlet of the sea, which in itself is derived from the term aestus, meaning tide. There have been many definitions proposed to describe an estuary. The most widely accepted definition is: "a semi-enclosed coastal body of water, which has a free connection with the open sea, and within which seawater is measurably diluted with freshwater derived from land drainage". However, this definition excludes a number of coastal water bodies such as coastal lagoons and brackish seas.

Harborside Copper Mine in Brooksville first opened in the 1880s, but was acquired and reopened by Callahan Mining Corporation from New York in 1965. The company got permission from the state to drain the Goose Pond tidal inlet and opened an open pit copper mine that operated until reserves were depleted in 1972. The mine was equipped with a flotation mill and shipped zinc to Pennsylvania and copper to Quebec for smelting. A larger zinc, copper and lead mine was operated by Kerramerican next to Second Pond in Blue Hill.

Sirmach (, also Romanized as Sīrmach, Sīramoh, and Siramch; also known as Rāpch and Sīrāmach) is a village in Gabrik Rural District, in the Central District of Jask County, Hormozgan Province, Iran. At the 2006 census, its population was 282, in 57 families. The village is located near a tidal inlet known as Khowr Rapch or Lahūr-e Rāpch, a large and shallow inlet with a maximum depth of 8m,Red Sea and the Persian Gulf (ProStar Publications, 2007) page 208.George N. Curzon, Persia and the Persian Question.

The exhibition was held on reclaimed land at Logan Park, much of it reclaimed especially for the exhibition. A tidal inlet originally known as Pelichet Bay had been partly reclaimed, leaving a flat area and a lake, Lake Logan. In order to provide enough land for the exhibition, the lake was drained and the site cleared before construction of a series of magnificent exhibition buildings by architect Edmund Anscombe. The buildings consisted of a series of pavilions surrounding a central court area which was dominated by a domed festival hall, and covered an area of .

The area that would become Cogan was known as Cogan Pill for much of its history. The Pill (a tidal inlet, used as a harbour) lay within the commote of Dinas Powys and flowed into the river Ely near today's Pont y Werin footbridge but is no longer extant, having been developed into the Penarth Dock in the nineteenth century. The importance of the Cogan Pill is evident by its continued use in the local toponymy, with Pill Street, Cogan Pill Road and the Cogan Pill House all being named for it.

Glynde Reach and the River Ouse were almost certainly a tidal inlet at the time the Domesday book was produced in 1086. The main industry was the production of salt by the evaporation of sea water, and salt works were recorded at Ripe and Laughton. During the early 14th century, meadows were created on parts of the flood plain by building embankments, but conditions worsened later in the century. Meadows at Beddingham were flooded in the summer for five years in the 1360s and three in the 1380s, but not at all in the 1370s.

The English name "Pyle" is derived from the Welsh Pîl, meaning a tidal inlet of the sea, this localised toponym is found along the coast of South Wales, from Pembrokeshire and into Somerset. In this instance it may refer to the mouth of the River Kenfig, which is tidal for its first mile from the sea. A commonly stated, but erroneous derivation from the English word "pile" (a stake) is highly unlikely, with the only settlement in the United Kingdom known to have this derivation being a hamlet on the Isle of Wight.

The large tidal inlet of Langstone Harbour is east of the island. The Farlington Marshes, in the north off the coast of Farlington, is a 125-hectare (308-acre) grazing marsh and saline lagoon. One of the oldest local reserves in the county, built from reclaimed land in 1771, it provides habitat for migratory wildfowl and waders. alt=A high aerial view of Portsea Island (the island which Portsmouth is situated on), and neighbouring Hayling Island South of Portsmouth are Spithead, the Solent, and the Isle of Wight.

Pondwell is also the site of Seaview Wildlife Encounter -- formerly Flamingo Park, a small zoo and waterfowl park. There is also a pub called the "Wishing Well" (free house). It also offers holiday chalets at the Salterns and a nail technician, mortgage broker and the chair of the IOW Table Tennis Association. The beach at the bottom of the Salterns was formerly a thriving harbour for timber export; at that time the low-lying land at the foot of Pondwell Hill formed a tidal inlet of the sea known as Barnsley Creek.

It is clear from the Anglo-Saxon Chronicles that Maldon in Essex is the site of the battle, because of its proximity to Ipswich and because Byrhtnoth was an Ealdorman of Essex. (p. 18) More precise details come from The Battle of Maldon narrative, which describes how the Vikings established themselves on an island, separated from the mainland by a tidal inlet which could be crossed by a "bridge" or "ford" at low tide. The poem describes how the Vikings and Saxons negotiated by calling across the water while waiting for the tide to go out. Northey Island seems to fit this description.

The Slake was a tidal inlet which stretched south from the river, across the site of today's bus station, along the route of Beaconsfield Street, and on past Crofton Mill Pit. Before it was filled in, it almost entirely separated Blyth from Cowpen—Waterloo Bridge providing the only main link. Once it was removed, the two areas could combine and allow the town to begin to take its present form. The town continued to expand in the 20th century; much large-scale house building took place in the 1920s and 1930s, and from the 1950s to the 1970s.

The Lewes and Laughton Levels are an area of low-lying land bordering the River Ouse near Lewes and the Glynde Reach near Laughton in East Sussex, England. The area was probably a tidal inlet in Norman times, but by the early 14th century, some meadows had been created by building embankments. Conditions deteriorated later that century, and by 1537, most of the meadows were permanently flooded. Part of the problem was the buildup of shingle across the mouth of the Ouse, but in 1537 a scot tax was raised, and a new channel cut through the shingle.

Westchester Creek, looking north-east from Clason Point Park Westchester Creek (also known as Frenchman's Creek) is a tidal inlet of the East River located in the south eastern portion of the Bronx in New York City. It is 2.1 miles (3.39 km) in length. The creek formerly traveled further inland, to what is now Pelham Parkway, extending almost to Eastchester Bay and making Throggs Neck into an island during heavy storms. However, much of the route has been filled in, replaced by such structures as the New York City Subway's Westchester Yard and the Hutchinson Metro Center.

The name ‘Hook’ refers to the hook shaped spit of land at the mouth of the River Hamble. In medieval times this protected the entrance to a tidal inlet known as the fleet, hence the local name ‘Fleet End’. The medieval hamlet and port of Hook occupied the southern shore of the inlet, situated some distance west of the present settlement. Even at its height the settlement was probably little more than a scatter of cottages and a chapel but its significance as a port is indicated by records of the conflict with France in 1345.

Until 1949 East Huntspill was part of the ancient parish and civil parish of Huntspill. The first mention of Huntspill is around 796 AD, when the area was granted to Glastonbury Abbey by Aethelmund, a nobleman under King Offa of Mercia. Huntspill was listed in the Domesday Book of 1086 as Honspil, meaning 'Huna's creek' possibly from the Old English personal name Huna and from the Celtic pwll as used in Welsh, e.g. Pwllheli. An alternative origin is from Hun's Pill in Old English, meaning a port on a tidal inlet, or pill, belonging to a Saxon lord, or hun.

Sunset over the Braakman The Braakman was a large tidal inlet in the middle of the Dutch region of Zeelandic Flanders, on the south bank of the Westerschelde west of Terneuzen. It was created by a succession of storm surges in the 14th and 15th centuries, including the St. Elizabeth's flood (1404) and the St. Elizabeth's flood (1421). For a long time the Braakman was a natural barrier between east and west Zeelandic Flanders, and also access to the ports of Boekhoute, Philippine, Axel and Sas van Gent. Over the centuries it steadily spread, drowning at least 15 villages between 1200 and 1601.

Barker Inlet is a shallow tidal inlet which, with the adjacent Port River Estuary, formed during the Holocene by the progressive extension of the Lefevre Peninsula by northward littoral drift of sand carried by wave action along the eastern shore of Gulf St Vincent.Bowman, G. & Harvey, N. (1986): Geomorphic Evolution of a Holocene Beach-Ridge Complex, LeFevre Peninsula, South Australia. Journal of Coastal Research 2(3):345-362 It has a narrow central channel used for boating. Spring tides are over 2½ metres and at low tide much of the inlet is mudflats that are above water level.

A community of Cluniac monks resided at elevated Bermondsey Abbey south-east of the site from 1082 onwards. The community began the development of the marshes surrounding their abbey at Bermondsey, cultivating the land and embanking the riverside into a Priory Close spanning 140 acres of meadow and digging dykes. They turned the adjacent tidal inlet at the mouth of the River Neckinger into the priory's dock, and named it Saint Saviour's Dock after their abbey's patron. This provided a safe landing for Bishops and goods below the traditional first land crossing, the congested stone arches of London Bridge.

Their travel routes have been identified as along the easy tracks such as along beaches, stream beds and river valleys. The most commonly identified locations for sighting bears in the Glacier Bay are: The Bartlett Cove, the Bartlett River, the Beardslee Islands and North and South Sandy Cove locations for black bears, while brown bears are seen to the north of Tidal Inlet in the west arm of glacier and north of Adams Inlet in the east arm. They are also seen swimming in the Bay, crossing from one bank to the other. Salmon are their favorite food, apart from bumblebees, sand fleas, bird eggs, birds, voles and marine mammal carcasses.

Using pulped straw from the local farmers and esparto (imported from Algeria and Southern Spain) as a replacement for expensive cotton rag which was becoming more expensive; the output supplied newsprint his mills in Bow. To speed production, in 1904 Lloyd built a wharf on the tidal inlet at Milton Creek, and a horse-drawn tramway to carry materials to the mill. On what is now known as the Sittingbourne & Kemsley Light Railway, in 1906 the first of three steam locomotives, Premier, came into service, all 0-4-2 Brazil type tank engines sourced from Kerr Stuart. In 1913 the railway was extended to the new dock built at Ridham.

Penpol Creek, an inlet on the north bank of Restronguet Creek Houses on the shore at Point near Chycoose Chycoose (, meaning house of the wood), Point and Penpol (, meaning head of a creek) form a coastal settlement around Penpol Creek in Cornwall, England, United Kingdom. The creek is a ria, a tidal inlet on the north side of Restronguet Creek. It is situated approximately three- quarters of a mile (1 km) west of Feock village which is four miles (6.5 km) south of Truro.Ordnance Survey: Landranger map sheet 204 Truro & Falmouth Chycoose is on the west bank of Penpol Creek and Penpol hamlet is at the north end of the creek.

Fronting the beach along the southern shore is the promenade road of Eastney, which includes is punctuated by three forts, small Eastney Fort West (dismantled), Eastney Fort East and large Fort Cumberland, which occupies a modest peninsula. Eastney is the most south- eastern area of Portsea island and forms part of the entrance into Langstone Harbour. Eastney offers a marina (confusingly named as "Southsea Marina") and also a foot-passenger ferry service across Langstone Harbour to neighbouring Hayling Island. Eastney Lake, a natural tidal inlet of Langstone Harbour is located on the northern side of the Eastney peninsular, with Milton on the opposite northern side of Eastney Lake.

The conservation park has an area of and lies immediately to the south of the town of American River, about southeast by south of Kingscote and southwest by west of Penneshaw. It consists of land on the peninsula of the north side of the tidal inlet of Pelican Lagoon as well as five islets within the inlet itself. It includes woodland, scrub and heath formations as well as wetland vegetation and adjoins samphire mudflats, providing habitat for several species of woodland and wetland birds and other animals. The conservation park is located within the boundaries of the gazetted locality of Pelican Lagoon with exception to the islets located within the lagoon.

Fratton Park is south of the railway line, and thus is in Milton. This fact can also be proven further as Fratton Park has a Milton based PO4 8RA postal code address (Fratton and Portsmouth city centre has a "PO1" postal code). A further fact is that Fratton Park lies within the Milton Ward electoral district for Portsmouth City Council and national level parliamentary elections. On the eastern edge of Portsea Island bordering Langstone Harbour, is an area now known as Milton Common, formerly a tidal inlet known as Milton Lake (and even earlier, "Felder Lake" from which the current Velder Avenue's name is derived).

Porth Hellick is a tidal inlet on the south coast of St Mary’s, the largest island in the Isles of Scilly. The bay is delineated to the south by a headland known as the Giant’s Castle, which is an Iron Age cliff fort, and Porth Hellick Down and Porth Hellick Point to the north.Ordnance Survey: Landranger map sheet 203 Land's End At low tide a wide expanse of sand and rocks are exposed and a bar of fine shingle provides a barrier from the sea to form the largest area of (usually) fresh water on St Mary’s. A stream rises in Holy Vale and flows south through Higher Moors to the sea at Porth Hellick.

Farm Cove looking towards the City of Sydney Farm Cove is a tidal inlet and shallow bay in Sydney Harbour, separated from Sydney Cove by Bennelong Point, New South Wales, Australia (site of the Sydney Opera House). Known to the indigenous inhabitants of Sydney as Woccanmagully, Farm Cove was used by them as an initiation ground and for the "Kangaroo and Dog Dance". The land immediately adjacent to Farm Cove was set aside soon after first European settlement in 1788 by Governor Arthur Phillip for the Government House Domain, a private reserve for the NSW Governor. The first farm for the colony was thereafter established in the area, subsequently lending its name to the cove.

The Barker Inlet is a tidal inlet of the Gulf St Vincent in Adelaide, South Australia, named after Captain Collet Barker who first sighted it in 1831. It contains one of the southernmost mangrove forests in the world, a dolphin sanctuary, seagrass meadows and is an important fish and shellfish breeding ground. The inlet separates Torrens Island and Garden Island from the mainland to the East and is characterized by a network of tidal creeks, artificially deepened channels, and wide mudflats. The extensive belt of mangroves are bordered by samphire saltmarsh flats and low-lying sand dunes, there are two boardwalks (at Garden Island and St Kilda), and ships graveyards in Broad Creek, Angas Inlet and the North Arm.

Brave Boat Harbor Farm is located on the north side of Brave Boat Harbor, a tidal inlet on the coast of southern Maine, and on the southeast coast facing the Gulf of Maine. The developed portion of the farm consists of of rolling fields, grass meadows, developed garden areas, and a pond; most of the remainder of the property (which is over ) consists of undeveloped woodland. At the center of developed area are a house, cottage, and cluster of farm buildings, in whose immediate area is a designed garden landscape. All except the cottage were built between 1951 and 1954 in a deliberate homage to colonial-era farmsteads, by Calvin and Marion Hosmer.

Katikati is a town in New Zealand (North Island) located on the Uretara Stream near a tidal inlet towards the northern end of Tauranga Harbour, 28 kilometres south of Waihi and 40 kilometres northwest of Tauranga. State Highway 2 passes through the town; a bypass scheduled to have begun construction in 2008 is on hold.NZTA: Katikati Bypass Katikati has become known for its many murals painted on walls of commercial buildings. These were started in the 1990s to regenerate tourist interest in the town and district, and led to the town being recognised New Zealand's 'Most Beautiful Small Town' award for towns of less than 8,000 population in 2005 by the Keep New Zealand Beautiful Society.

Wave swash and currents can impact significantly on the sediment budget, although it is difficult to measure. Swash can be either an erosive or accretion process depending on many factors such as the sand texture and the individual wave itself. Although during fair weather the impact of swash is negligible, during storms the sea level can rise high enough to erode dunes and cliffs, dumping large quantities of sediment into the littoral cell, which can only be given back to the dune by aeolian transport. Where storm surge causes sediments to be deposited on the land from the littoral cell, they can form washover fans or open a new tidal inlet which transports sediment away from the littoral cell.

The Pettengill Farm occupies a significant portion of land at the head of the Harraseeket River, a tidal inlet that extends southwest to Casco Bay. The farm property is bounded on the south and west by the river, the north by Flying Point Road, and the east by Kelsey Brook, which empties into the river near the point where it opens into the wide channel. The farmstead is located on a terrace overlooking a bend in the narrow portion of the river, near the southern end of the property, and is about a walk down the access road from the public trailhead. The property, which is now no longer in agricultural use, has a combination of open fields and woods, with public trails now crossing them.

Lake Macquarie Airport (formerly Belmont Airport) is an airfield located in the Lake Macquarie suburb of Marks Point, south of Newcastle, New South Wales, Australia. The airport is located on a narrow peninsula between the Pacific Highway and a shallow tidal inlet that forms the entrance to Lake Macquarie. For most of its history, the airfield functioned as the base for Aeropelican Air Services, who operated commuter flights to and from Sydney using DHC-6 Twin Otters, however services were withdrawn in 2006 and the airfield was sold to the Mirvac Group for $5.5 million in 2008. NSW Ambulance and Westpac Life Saver Rescue Helicopter Service operate a base from the airport, performing aeromedical retrieval services for northern New South Wales.

SR 103 begins in the west at an intersection with SR 236 (which is itself a former alignment of SR 103 there) west of Eliot, near its intersection with SR 101 just southwest of the border between South Berwick and Dover, New Hampshire. For its first mile SR 103 heads south-southwest, until crosses Sturgeon Creek, a tidal inlet of the Piscataqua River, the state border with New Hampshire. There it turns southeast to parallel the river, meandering slightly inland southeast through Eliot and into Kittery, which it enters on the causeway over Spinney Creek, which divides the two towns there. SR 103's first intersection is two-thirds of a mile later at Dennett Road, where it T's right and passes underneath U.S. Route 1 Bypass.

Thus the possibility arose of goods from the Brookmerland being transported by water to the Münsterland. The Wadden mudflats of Leybucht and Kuipersand in front of Marienhafe take their name from the old three-aisle Marienhafe mother church. Its roof was covered on its north side with copper (Kuiper = Frisian-Dutch for copper) and on the south side with slate (Ley = old German for slate), so that, from the sea, the changing view of the church with its copper and slate sides acted as a seamark to guide the experienced sailor along the permanently navigable tidal inlet and other stretches of waterway, even at low tide. Without this local knowledge, the place and its tide-dependent harbour were virtually unapproachable from the sea.

Sea lavender blossoms in August–September The Zwin is a nature reserve at the North Sea coast, on the Belgian-Dutch border. It consists of the entrance area of a former tidal inlet which during the Middle Ages connected the North Sea with the ports of Sluis and Bruges inland. The Zwin inlet was formed originally by a storm that broke through the Flemish coast in 1134, creating a tidal channel that reached some 15 km inland and was also connected, through another channel, to the mouth of the Scheldt further north-east. The new waterway offered access to the sea to the inland city of Bruges, which consequently rose to become one of the foremost medieval port cities of Europe.

When the Domesday book was produced in 1086, the Ouse valley was probably a tidal inlet with a string of settlements located at its margins. In later centuries the river was draining the valley sufficiently well for some of the marshland to be reclaimed, by building embankments to create highly prized meadow land. However, by the 14th century the Ouse valley was regularly flooding in winter, and frequently the waters remained on the lower meadows through the summer. In 1422 a Commission of Sewers was appointed to restore the banks and drainage between the coast and Fletching, around inland, which may indicate that the Ouse was affected by the same storm that devastated the Netherlands in the St Elizabeth's flood of 1421.

They turned an adjacent tidal inlet at the mouth of the River Neckinger into a dock, named St Saviour's Dock after their abbey. But Bermondsey then was little more than a high street ribbon (the modern Bermondsey Street), leading from the southern bank of the Thames, at Tooley Street, up to the abbey close. The Knights Templar also owned land here and gave their names to one of the most distinctive streets in London, Shad Thames (a corruption of "St John at Thames"). Other ecclesiastical properties stood nearby at Tooley (a corruption of "St Olave's") Street, located in the Archbishop of Canterbury's manor of Southwark, where wealthy citizens and clerics had their houses, including the priors of Lewes and St Augustine's, Canterbury, and the abbot of Battle.

The Riverlife project aims to engage the community to actively appreciate Cooks River in Sydney, Australia. It usually more a tidal inlet then a River although is capable of flooding and receives the stormwater from 100 square kilometers of a highly urbanised part of the Sydney Metropolitan area. Other major waterways of Sydney include the Hawkesbury, Sydney Harbour, Georges River, and Port Hacking, all of which are Rias, but Cooks River shows more signs of slow weathering and development as a river than of being a flooded river valley. The River was an important part of the life of local aborigines for tens of thousands of years, and was a beautiful recreation facility for Sydney Siders during the early years of the development of the City.

As it nears the coast it passes through the Lewes and Laughton Levels, an area of flat, low-lying land that borders the river and another tributary, the Glynde Reach. It was a large tidal inlet at the time of the Domesday book in 1086, but over the following centuries, some attempts were made to reclaim some of the valley floor for agriculture, by building embankments, but the drainage was hampered by the buildup of a large shingle bar which formed across the mouth of the river by longshore drift. In 1539, a new channel for the entrance to the river was cut through the shingle bar, and meadows flourished for a time, but flooding returned and meadows reverted to marshland. The engineer John Smeaton proposed a solution for the drainage of the valley in 1767, but it was only partly implemented.

Squamscott River in 1908, Exeter, New Hampshire Route 108, Newfields, New Hampshire The Squamscott River is a tidal river in Rockingham County, southeastern New Hampshire, in the United States.New Hampshire GRANIT state geographic information system It rises at Exeter, fed by the Exeter River. The Squamscott runs north between Newfields and Stratham to Great Bay, a tidal estuary, which is connected to the Piscataqua River, a tidal inlet of the Atlantic Ocean. More specifically, after rising at the Great Bridge (actually a very modest Works Progress Administration project) adjacent to the former "Loaf & Ladle" restaurant in downtown Exeter, the Squamscott River passes the "Wooden Wave" (an interesting architectural statement next to the Phillips Exeter Academy boathouse), then tends north alongside the Swasey Parkway, through the haymarshes, passing by the town's water purification plant and then under State Route 101, a major east–west arterial road in New Hampshire.

Somers is perhaps best known for its yacht club and sailing facilities. The waters offshore from Somers, neighbouring Balnarring and Merricks Beaches, Flinders and Shoreham, and the body of water between the Mornington Peninsula and Philip Island are some of the most ideal and safest regions for sailing of all types in Australia. On most days many sailboats, mainly catamarans, can be seen in the waters of Western Port Bay participating in several races that are held during good sailing conditions, usually on weekends. The tidal inlet of Merricks Creek at low tide is one of the best places around Melbourne and the Mornington Peninsula for skiffle boarding, while the South Beach (actually to the east of the main beach) is tucked away behind the belt of foreshore bushland that is Somers Foreshore Reserve, and is enjoyed mainly by local residents, while the main beach, Somers Beach, is home to one of the major yacht clubs in Western Port, Somers Yacht Club.

Location of Castlepark within Kinsale harbour The marina at Castlepark in 2002, looking south-eastwards from Compass Hill on the Kinsale side of the Bandon River. The image also shows the village which straddles the neck of land joining the James's Fort townland to the main body of the peninsula. James's Fort, which is not pictured, is off to the left The Castlepark peninsula in Kinsale harbour on the coast of County Cork, on the south coast of Ireland is really more a presque-isle than a peninsula, being joined to the mainland only by an extremely narrow neck at its north-western corner. Thus, the Castlepark peninsula is almost surrounded by water: the River Bandon, flowing from the north-west, bounds the peninsula on the north; the entrance to Kinsale harbour bounds the peninsula on the east; the Atlantic Ocean bounds it to the south; and the tidal inlet known as Sandycove Creek bounds the peninsula on the west.