The Wellington Dyke is an agricultural dyke in Kings County, Nova Scotia protecting over 3,000 acres (12 km2) of farmland along the Canard River between the communities of Starr's Point and Canard in Nova Scotia, Canada. Built by local farmers, it was begun in 1817 and completed in 1825. Today the dyke is owned by the Department of Agriculture of Nova Scotia in partnership with the farmers of the Wellington Marsh Body.
A levee, dike, dyke, embankment, floodbank or stopbank is an elongated naturally occurring ridge or artificially constructed fill or wall, which regulates water levels. It is usually earthen and often parallel to the course of a river in its floodplain or along low-lying coastlines.
Kings County is a county in the Canadian province of Nova Scotia. With a population of 60,600 in the 2016 Census,, Kings County is the third most populous county in the province. It is located in central Nova Scotia on the shore of the Bay of Fundy, with its northeastern part forming the western shore of the Minas Basin.
The Canard River is a river in Kings County, Nova Scotia, Canada which drains into the Minas Basin of the Bay of Fundy between the communities of Canard and Starr's Point. It is known for its fertile river banks and extensive dyke land agriculture.
The rich farmland along the river were originally dyked by the Acadians, who knew it as the Rivière-aux-Canards, to claim highly productive farmland from the Bay of Fundy tidal meadows of the Minas Basin. Beginning in the late 1600s, Acadians built progressively larger dykes across the Rivière-aux-Canards beginning first with its upper reaches at Upper Dyke, then the Middle Dyke and finally with the Grand Dyke near Port Williams. A sluice with a one-way valve, known to the Acadians as the "aboiteau", allowed the river to drain but shut out the incoming tide. After the Acadians were expelled in 1755, the New England Planters settled in the area, beginning in 1760. The Planters repaired the Acadian dykelands and gradually began to expand the dyked areas. The Planters carried out this work by forming "marsh bodies" which are elected associations of farmers owning dykeland fields who share the costs of building and maintaining dykes.
The Acadians are the descendants of French colonists who settled in Acadia during the 17th and 18th centuries, some of whom are also descended from the Indigenous peoples of the region. The colony was located in what is now Eastern Canada's Maritime provinces, as well as part of Quebec, and present-day Maine to the Kennebec River. Acadia was a distinctly separate colony of New France. It was geographically and administratively separate from the French colony of Canada. As a result, the Acadians and Québécois developed two distinct histories and cultures. They also developed a slightly different French language. France has one official language and to accomplish this they have an administration in charge of the language. Since the Acadians were separated from this council, their French language evolved independently, and Acadians retain several elements of 17th-century French that have disappeared in France. The settlers whose descendants became Acadians came from many areas in France, but especially regions such as Île-de-France, Normandy, Brittany, Poitou and Aquitaine. Acadian family names have come from many areas in France. For example, the Maillets are from Paris; the LeBlancs of Normandy; the surname Melançon is from Brittany, and those with the surnames Bastarache and Basque came from Aquitaine.
Rivière-aux-Canards was an Acadian village located at the west side of the Minas Basin from 1670 until 1755. The village was established in 1670 by the name of Saint-Joseph-de-la-Rivière-aux-Canards, later, it became Rivière-aux-Canards in short form.
The Bay of Fundy is a bay between the Canadian provinces of New Brunswick and Nova Scotia, with a small portion touching the US state of Maine. It has an extremely high tidal range.
Farmers in Starrs Point and Canard began to discuss building a large dyke at the mouth of the Canard River in 1809. They may have been inspired by the three mile long Wickwire Dyke completed near Wolfville in 1808. [1] The Planters at Canard had made steady additions to the Acadian dykes along the edges of the river but a dyke at near the mouth of the river would reclaim an additional 700 acres of farmland from the Minas Basin and save the maintenance of the many smaller dykes along the river which protected over 2,000 acres. A plan was organized in 1811. Materials were gathered and construction began in 1817. The dyke was named after the Duke of Wellington in honour of his decisive victory over Napoleon in 1815. [2] The new structure was a dramatic change from the Acadian dyke systems which were only a few feet high in most places. The Wellington Dyke would be 50 feet high, 120 feet at the base and over 300 feet long with additional embankments stretching over a mile just in from the mouth of the river. The aboiteau or sluice which allowed the river to drain was 100 feet and 14 feet wide. The work was financed and organized solely by the 70 farmers of the Wellington Marsh Body. It was built in stages seasonally, between high tides using only human and animal labour. At its peak over 100 teams of horses and oxen and 300 men worked on the dyke. Rum rations were issued as an incentive with extra shares for those who had to work in the water. [3] In some places the swift tidal currents swept away nine out of every ten cart loads of fill. [4]
Wolfville is a Canadian town in the Annapolis Valley, Kings County, Nova Scotia, located about 100 kilometres (62 mi) northwest of the provincial capital, Halifax. The town is home to Acadia University and Landmark East School.
Arthur Wellesley, 1st Duke of Wellington, was a British soldier and Tory statesman who was one of the leading military and political figures of 19th-century Britain, serving twice as Prime Minister. His victory against Napoleon at the Battle of Waterloo in 1815 puts him in the first rank of Britain's military heroes.
The dyke was nearly complete in 1822 when storm at high tide found a leak on the south side of the dyke and created a breach allowing the Minas Basin to flood in and destroying much of the dyke and years of work. Work was renewed the next year with some assistance from the provincial government. Finally in September 1824 the dyke walls were largely complete. Finishing work on the facings and the addition of a road on top completed the dike in 1825. The total cost was over 21,000 pounds. Aside from 550 pounds from the province, all the costs were covered by the farmers along the river. [5] Many had mortgaged their farms to build the dyke and some faced foreclosure. However, with the dyke's completion, over 3,000 of acres were protected by the single dyke which gave farmers on the Canard River the lowest maintenance costs per acre of any dykelands in the Maritime Region. The road on top of the dyke provided a new connection between Starr's Point and Canard which became known as the Wellington Dyke Road. The dyke also provided protection for numerous roads and bridges further upriver. [6]
Once built, the dyke proved solid and enduring, surviving major storms such as the Saxby Gale of 1869. The dyke lands of the Canard River proved very rewarding. While average dyked marsh land produced two tons of hay per acre, the Canard fields yielded five tons per acre. Hay sales proved very rewarding in the boom years of the hay market in the late 19th century when eastern urban centres paid high prices for the rich marsh hay produced from dyke lands. [7]
However, after 1920 and the arrival of automobiles, the demand for marsh hay declined. By the 1940s, the dropping earnings of dyke lands, combined with the need for a new sluice posed a challenge for the dyke's owners. The Wellington Dyke received a major rebuild in 1947 with a new sluice and sidewalls constructed immediately behind the old dyke. The reconstruction was one of the first projects of a new federal-provincial partnership which was followed by 80 dyke repair projects across the Maritimes. The program came to be known as the Maritime Marshlands Rehabilitation Administration in 1948 with the federal government taking ownership and maintenance of the dykes, while the marsh bodies maintained the drainage ditches behind them. [8] In 1970, Nova Scotia's Department of Agriculture took ownership of the Wellington Dyke and other large agricultural dykes in the province. [9] The province installed a new three-box concrete sluice in the aboiteau in 1976. The 70 farmers of the Wellington Marsh Body continue to take care of the drainage network behind the dyke. An annual grant from the province to the Marsh body funds regular maintenance of the dyke wall itself. [10] A historic shipwreck is thought to lie just downstream of the Wellington Dyke, the wreck of the brigantine Montague, one of the ships which brought the New England Planters to the area but sank in the Canard River. An ongoing search led by the Kings County Museum has continued to search for traces of the wreck on the banks and bed of the river near the Wellington Dyke. [11]
Montague was an armed brigantine of the Nova Scotia government which patrolled Nova Scotian waters during the Seven Years' War as part Nova Scotia's Provincial Marine. Montague played a notable role in beginning New England Planter settlements until she was wrecked in the Canard River in Kings County, Nova Scotia in December 1760.
The Kings County Museum is a museum located in Kentville, Nova Scotia, Canada exploring the history of Kings County, Nova Scotia. It is housed in the restored 1903 Kings County Courthouse. The Museum hosts a variety of permanent and changing displays about Kings County. It is also home to the Parks Canada National Commemorative New England Planters Exhibit.
The Annapolis Valley is a valley and region in the Canadian province of Nova Scotia. It is located in the western part of the Nova Scotia peninsula, formed by a trough between two parallel mountain ranges along the shore of the Bay of Fundy. Statistics Canada defines the Annapolis Valley as an economic region, composed of Annapolis County, Kings County, and Hants County.
Kentville is a town in Kings County, Nova Scotia. It is one of the main towns in the Annapolis Valley, and it is the county seat of Kings County. As of 2016, the town's population was 6,271. Its census agglomeration is 26,222.
The Minas Basin is an inlet of the Bay of Fundy and a sub-basin of the Fundy Basin located in Nova Scotia, Canada. It is known for its extremely high tides.
Grand-Pré is a Canadian rural community in Kings County, Nova Scotia. Its French name translates to "Great/Large Meadow" and the community lies at the eastern edge of the Annapolis Valley several kilometres east of the town of Wolfville on a peninsula jutting into the Minas Basin surrounded by extensive dyked farm fields, framed by the Gaspereau and Cornwallis Rivers. The community was made famous by Henry Wadsworth Longfellow's poem Evangeline and is today home to the Grand-Pré National Historic Site. On June 30, 2012, the Landscape of Grand-Pré was named a World Heritage Site by UNESCO.
The New England Planters were settlers from the New England colonies who responded to invitations by the lieutenant governor of Nova Scotia, Charles Lawrence, to settle lands left vacant by the Bay of Fundy Campaign (1755) of the Acadian Expulsion.
Route 358 is a collector road in the Canadian province of Nova Scotia.
Tusket is a small fishing community located in Yarmouth County, Nova Scotia on route 308.
The Cornwallis River is in Kings County, Nova Scotia, Canada. It has a meander length of approximately 48 kilometres (30 mi) through eastern Kings County, from its source on the North Mountain at Grafton to its mouth near Wolfville on the Minas Basin. The lower portion of the river beginning at Kentville is tidal and there are extensive tidal marshes in the lower reaches. In its upper watershed at Berwick, the river draws on the Caribou Bog while a longer branch continues to the official source, a stream on the North Mountain at Grafton.
Canard is a rural community occupying a ridge to the north of the Canard River between the Canard and Habitant Rivers in Kings County in the Canadian province of Nova Scotia. The name comes from the French word for duck which was in turn derived from the Mi'kmaw name for the river which described the large numbers of black ducks once found there.
Scotch Village is an unincorporated community on the Kennetcook River in the Canadian province of Nova Scotia, located in the Municipality of West Hants. This area was part of Newport Township at the time of settlement primarily by Rhode Island Planters in the early 1760s. It was referred to as “Scotchman’s Dyke” or “Scotch Village”, due to settlement of early families of Scottish descent. Prior to the arrival of the Planters, Scotch Village had been the home of Mi'kmaq and Acadians.
Mount Denson is a small community in the Canadian province of Nova Scotia, located in The Municipality of the District of West Hants in Hants County. The community is named after Mount Denson; the mid-eighteenth-century estate of Henry Denny Denson.
Starr's Point is a community in the Canadian province of Nova Scotia, located in Kings County two miles west of Port Williams. Starr's point faces the Minas Basin to the east and separates the mouths of the Cornwallis River and the Canard River. It is an agricultural area noted for apple orchards.
Aboiteau farming on reclaimed marshland is a labor-intensive method in which earthen dykes are constructed to stop high tides from inundating marshland. A wooden sluice or aboiteau is then built into the dyke, with a hinged door that swings open at low tide to allow fresh water to drain from the farmland but swings shut at high tide to prevent salt water from inundating the fields.
Pisiguit is the pre-expulsion-period Acadian region located along the banks of the Pisiquit River from its confluence with the Minas Basin of Acadia, which is now Nova Scotia, including the St. Croix River drainage area. Settlement in the region commenced simultaneous to the establishment of Grand-Pré. Many villages spread rapidly eastward along the river banks. These settlements became known as Pisiguit or. The name is from the Mi'kmaq Pesaquid, meaning "Junction of Waters". In 1714, there were 351 people there.
Steam Mill Village is a rural community north of Kentville, Nova Scotia, Canada beside Camp Aldershot. It is named after an early steam-powered saw mill.
Coordinates: 45°7′36.7″N64°24′12.5″W / 45.126861°N 64.403472°W