Bay of Fundy - wikipedia Bay of Fundy The Bay of Fundy, shown on the east coast of North America The Bay of Fundy ( French : Baie de Fundy ) is a bay on the Atlantic coast of North America, on the northeast end of the Gulf of Maine between the Canadian provinces of New Brunswick and Nova Scotia, with a small portion touching the U.S. state of Maine. Some sources believe the name `` Fundy '' is a corruption of the French word Fendu, meaning `` split '', while others believe it comes from the Portuguese funda, meaning `` deep ''. The bay was also named Baie Française ( French Bay ) by explorer - cartographer Samuel de Champlain during a 1604 expedition led by Pierre Dugua, Sieur de Monts which resulted in a failed settlement attempt on St. Croix Island. The Bay of Fundy is known for having the highest tidal range in the world. Rivaled by Ungava Bay in northern Quebec, King Sound in Western Australia, Gulf of Khambhat in India, and the Severn Estuary in the UK, it has one of the highest vertical tidal ranges in the world. The Guinness Book of World Records ( 1975 ) declared that Burntcoat Head, Nova Scotia has the highest tides in the world : `` The Natural World, Greatest Tides : The greatest tides in the world occur in the Bay of Fundy... Burntcoat Head in the Minas Basin, Nova Scotia, has the greatest mean spring range with 14.5 metres ( 47.5 feet ) and an extreme range of 16.3 metres ( 53.5 feet ). '' Portions of the Bay of Fundy, Shepody Bay and Minas Basin, form one of six Canadian sites in the Western Hemisphere Shorebird Reserve Network, and are classified as a Hemispheric site. It is administered by the provinces of New Brunswick and Nova Scotia, and the Canadian Wildlife Service, and is managed in conjunction with Ducks Unlimited Canada and the Nature Conservancy of Canada. In July 2009, the Bay of Fundy was named as a finalist for the New 7 Wonders of Nature contest that ended in November 2011. It was not chosen as a wonder. The Hopewell Rocks at low tide, on the New Brunswick shore Contents 1 Extent 2 Tides 2.1 Tidal electrical power generation 3 Geology 3.1 Sub-basins 3.2 Rivers 3.3 Communities 4 History 5 Ports and shipping 6 Parks and protected areas 7 See also 8 References 9 External links Extent The International Hydrographic Organization defines the southwest limit of the Bay of Fundy as `` A line running northwesterly from Cape St. Mary ( 44 ° 05'N ) Nova Scotia, through Machias Seal Island ( 67 ° 06'W ) and on to Little River Head ( 44 ° 39'N ) in the State of Maine ''. Tides Alma, New Brunswick at high and low tide The Bay of Fundy is known for its high tidal range. The quest for world tidal dominance has led to a rivalry between the Minas Basin in the Bay of Fundy and the Leaf Basin in Ungava Bay, over which body of water lays claim to the highest tides in the world, with supporters in each region claiming the record. The Canadian Hydrographic Service finally declared it a statistical tie, with measurements of a 16.8 - metre ( 55 - foot ) tidal range in Leaf Basin for Ungava Bay and 17 meters ( 56 feet ) at Burntcoat Head for the Bay of Fundy. The highest water level ever recorded in the Bay of Fundy system occurred at the head of the Minas Basin on the night of October 4 -- 5, 1869 during a tropical cyclone named the `` Saxby Gale ''. The water level of 21.6 meters ( 71 feet ) resulted from the combination of high winds, abnormally low atmospheric pressure, and a spring tide. Leaf Basin has only been measured in recent years, whereas the Fundy system has been measured for many decades. The tide at Leaf Basin is higher on average than tides at Minas Basin ; however, the highest recorded tidal ranges ever measured are at Burntcoat Head and result from spring tides measured at the peak of the tidal cycle every 18 years. Traditional Mi'kmaq folklore states that the tides in the Bay of Fundy are caused by a giant whale splashing in the water. Oceanographers attribute it to tidal resonance resulting from a coincidence of timing : the time it takes a large wave to go from the mouth of the bay to the inner shore and back is practically the same as the time from one high tide to the next. During the 12.4 - hour tidal period, 115 billion tonnes of water flow in and out of the bay. The tides in the Bay of Fundy are semidiurnal, which means that they have two highs and two lows each day. The height that the water rises and falls to each day during these tides are approximately equal. There are approximately six hours and thirteen minutes between each high and low tide. Tidal electrical power generation Alternative forms of energy are being explored in depth in a number of unique areas. Tidal energy harnesses the movement of ocean water to generate electricity through a number of mechanisms. Currently a process of gathering tidal energy called `` In - stream turbine technology '' is being tested in the Minas Passage, Nova Scotia. This project is being spearheaded by the Fundy Ocean Research Center for Energy or FORCE. In - stream tidal turbine technology is a relatively simple design. An elevated turbine is submerged under water in a location that enables its movement with tidal cycles. As the blades of the turbine move they create energy that powers an electric generator at the base. From here the power travels to a cable attached to the seafloor and back to an offsite facility where it can be added to the power grid. While this technology has shown to be successful in its early stages of testing, FORCE has not officially begun the process for energy collection. However, the installation of the undersea cable in December 2013 indicates that the project is moving along swiftly. A megawatt - scale turbine was installed at Cape Sharp near Partridge Island in November 2016. Project managers intend to install 16 MW by 2017, and 300 MW by 2020. Geology Basal contact of a lava flow section of Fundy basin The Bay of Fundy lies in a rift valley called the Fundy Basin ; as the rift began to separate from mainland North America, volcanic activity occurred, forming volcanoes and flood basalts. These flood basalts poured out over the landscape, covering much of southern Nova Scotia. Sections of the flood basalts have been eroded away, but still form a basaltic mountain range known as North Mountain. As a result, much of the basin floor is made of tholeiitic basalts giving its brown color. The rift valley eventually failed ( see aulacogen ) as the Mid-Atlantic Ridge continued to separate North America, Europe, and Africa. Sub-basins The upper part of the bay splits into Chignecto Bay in the northeast and the Minas Basin in the east. Chignecto Bay is further subdivided into Cumberland Basin and Shepody Bay and the extreme eastern portion of Minas Basin is called Cobequid Bay. Some of these upper reaches exhibit exposed red bay muds, for which the Bay of Fundy is noted ( for their appearance and biological productivity ). Cape Chignecto, as viewed from the Visitor Centre at Cape Chignecto Provincial Park. Cape Chignecto defines Chignecto Bay whereas Cape Split defines the Minas Channel, leading to the Minas Basin. The Minas Channel connects the Minas Basin with the main body of the bay. The channel is 5.6 kilometers across and approximately 106.7 meters deep. The tides that flow through the channel are very powerful. They are as powerful as 8000 train engines or 25 million horses. Facing Cape Split at the entrance to the Minas Channel are the basalt cliffs of Cape d'Or. The Minas Basin in early May. The lower part of the bay is also home to four important sub-basins : Passamaquoddy Bay and Back Bay on the New Brunswick shore, Cobscook Bay on the Maine shore, and the Annapolis Basin on the Nova Scotia shore. The bay is home to several islands, the largest of which is Grand Manan at the boundary with the Gulf of Maine. Other important islands on the north side of the bay include Campobello Island, Moose Island, and Deer Island in the Passamaquoddy Bay area. Brier Island and Long Island can be found on the south side of the bay while Isle Haute is in the upper bay off Cape Chignecto. Smaller islands and islets also exist in Passamaquoddy Bay, Back Bay, and Annapolis Basin. The Five Islands, in the Minas Basin, are particularly scenic. Eroded rock formations at the Bay of Fundy The Bay of Fundy is also home to another interesting geologic feature, the Hopewell Rocks formation. This formation is where the `` famous flower - pot rocks '' are located on a short, one kilometer long portion of Shepody Bay. These rocks are shaped by the tides, the strength of the rocks, and the presence of the joints in the rocks. The rock in the cliffs the stacks are being cut from are arkosic sandstone and coarse poorly sorted conglomerates. The tides that are eroding away the cliffs are between 10.7 meters and 14.7 meters high on average. Rivers The bay receives the waters of several rivers, including : Reversing Falls is where the Saint John River and Bay of Fundy meet New Brunswick Big Salmon River Little Salmon River Magaguadavic River Memramcook River Petitcodiac River Quiddy River Saint John River St. Croix River Shepody River Tantramar River Upper Salmon River Nova Scotia Annapolis River Avon River Cornwallis River Farrell River Salmon River Shubenacadie River Kennetcook River The Salmon River tidal bore October 22, 2009. The bay 's extreme tidal range causes several interesting phenomena in the various rivers which empty into it. Near the mouth of the Saint John River, where it passes through the city of Saint John, is the famous Reversing Falls. Here the changing tide causes alternating strong upriver and downriver flows several times a day as the tidal cycle changes. A narrow granite gorge and rocky bottom heavily restricts waterflow and creates strong rapids that flow upriver at high tide, and downriver at low tide. Rivers in the upper Bay of Fundy have a smaller flow - rate than the Saint John, and a shallower slope. As a result, extensive mud flats are deposited throughout the tidal range of the rivers. Tidal bore Another phenomenon which occurs in these rivers of the upper bay is a `` tidal bore '', where a wave front of water `` bores '' its way up a river against its normal flow. The narrow and shallow river estuaries around the upper Bay of Fundy regularly produce bores when the advancing tide is slowed by shallow waters creating a build - up with a steep surge of advancing water. Tidal bores are found on the Salmon River at Truro, the Petitcodiac River at Moncton as well as on the Shubenacadie River, the St. Croix River, the Maccan River, Kennetcook River and at River Herbert. One of the better examples of a tidal bore can be seen on the Shubenacadie River near the town of Truro and the village of Maitland, where local ecotourism operators offer the chance to experience rafting the bore upriver. Another good example of a tidal bore may be viewed on the Salmon River in the town of Truro. The once - famous tidal bores on the Petitcodiac and Avon rivers have been severely disrupted as a result of causeway construction in the 1960s -- 1970s which have caused excessive siltation. Communities The largest population centre on the bay is the New Brunswick city of Saint John. Saint John, New Brunswick The New Brunswick towns of St. Andrews, Blacks Harbour, St. Martins and Sackville as well as the Nova Scotia towns of Amherst, Parrsboro, Truro, Windsor, Wolfville, Annapolis Royal, and Digby are also on the bay. History Fort Edward ( built 1750 ), Windsor, Nova Scotia. The oldest blockhouse in North America. Major Benjamin Church : Led New England raids against Bay of Fundy Communities The Mi'kmaq fished in the Bay of Fundy and lived in communities around the bay for centuries before the first Europeans arrived and continue to live and work around the Bay. The first European settlement was at Île - Saint - Croix and then Port Royal was founded by Pierre Dugua, Sieur de Mons and Samuel de Champlain in 1605. The village was the first permanent European settlement north of St. Augustine, Florida. ( Two years later, the English made their first permanent settlement in Jamestown, Virginia. ) Approximately seventy - five years after Port Royal was founded, Acadians migrated from the capital and established what would become the other major Acadian settlements before the Expulsion of the Acadians : Grand - Pré, Chignecto, Cobequid ( present - day Truro, Nova Scotia ) and Pisiguit ( present - day Windsor, Nova Scotia ). There were numerous naval battles as well as naval attacks on the settlements surrounding the Bay of Fundy. Port Royal was raided numerous times during the Acadian Civil War. There were also numerous battles and raids during six wars that engulfed the region over a period of 75 years : the four French and Indian Wars, Father Rale 's War and Father Le Loutre 's War. During King William 's War, there was the naval Action of July 14, 1696 off Saint John, New Brunswick and Major Benjamin Church arrived by sea from Boston and raided various Acadian communities around the Bay ( See Raid on Chignecto ( 1696 ) ). During Queen Anne 's War, Church attacked the Acadian communities around the Bay again ( See Raid on Grand Pré ). During Father Le Loutre 's War, there were naval assaults on the communities of Chignecto ( See Battle at Chignecto ) and the Acadian Exodus from the Cobequid. Finally, during the last French and Indian War, the British expelled the Acadians in the Bay of Fundy Campaign ( 1755 ), which was followed three years later with campaigns which targeted the Saint John River and the Petitcodiac River. During the American Revolution, the upper reaches of the Basin saw a significant rebellion and battle at the Siege of Fort Cumberland and American attacks at Saint John, New Brunswick as well as numerous privateering raids against towns like Annapolis Royal, Nova Scotia. After the War, the boundary between the United States and the newly created province of New Brunswick remained uncertain, resulting in a thriving smuggling trade in the region, especially on the waters of Passamaquoddy Bay. The Bay saw some action during the War of 1812 as well, mostly in the form of privateering and small patrol ships. After the War of 1812, the smuggling resumed and culminated in the so - called `` plaster war '' of 1820. The Bay of Fundy 's ports and basins became major shipbuilding and shipping centres in the 19th Century. Led at first by shipbuilders like James Moran of St. Martins, New Brunswick, shipbuilding to all shores of the Bay of Fundy and eventually included shipbuilders such as Joseph Salter in Moncton and William D. Lawrence of Maitland, Nova Scotia who build some of the larges sailing ships ever constructed in Canada. Among other accomplishments, Fundy ports produced the fastest ship in the world, the ship Marco Polo ; the largest wooden ship ever built in Canada, the ship William D. Lawrence ; and the first female sea captain in the western world, Molly Kool of Alma, New Brunswick. The fabled mystery ship the Mary Celeste was also built on the Bay. Ports and shipping The port of Saint John gives access to the pulp and paper industry and the Irving oil refinery. Hantsport, Nova Scotia, on the Avon River is also home to a pulp and paper mill and is the shipment point for raw gypsum exports to the United States. The ports of Bayside, Charlotte County, ( near St. Andrews ) and Eastport, Maine, are important local ports. A result of shipping traffic has been the potential for increased collisions between ships and the North Atlantic right whale. In 2003, the Canadian Coast Guard adjusted shipping lanes crossing prime whale feeding areas at the entrance to the Bay of Fundy to lessen the risk of collision. Grand Manan V ferry at North Head, Grand Manan Island The bay is also traversed by several passenger and automobile ferry services : Saint John, New Brunswick, to Digby, Nova Scotia. ( Operated by Bay Ferries Limited. ) Grand Manan Island to Blacks Harbour, New Brunswick and White Head Island, New Brunswick, to Grand Manan Island. ( Operated by Coastal Transport Limited. ) Deer Island to Letete, New Brunswick. ( The Letete to Deer Island Ferry, operated by the New Brunswick Department of Transportation. ) Campobello Island, New Brunswick, to Deer Island. Eastport, Maine, to Deer Island. ( Operated by East Coast Ferries Limited. ) Westport, Nova Scotia, ( Brier Island ) to Freeport, Nova Scotia, ( Long Island ). Tiverton, Nova Scotia, ( Long Island ) to East Ferry, Nova Scotia. ( Operated by Nova Scotia Department of Transportation and Public Works. ) Parks and protected areas Point Wolfe at Fundy National Park. A number of parks preserve and interpret the Bay of Fundy 's coastal ecosystem. They include Fundy National Park in New Brunswick and Cape Chignecto Provincial Park and Five Islands Provincial Park and Blomidon Provincial Park in Nova Scotia. The Canadian Wildlife Service maintains a number of National Wildlife Areas in the Bay of Fundy including a proposed designation of Isle Haute in the middle of the Bay. See also Central Nova Tourist Association -- Tourism Association Representing Cumberland and Colchester County. Tidal power References Jump up ^ `` Canadian Encyclopedia ''. Archived from the original on January 13, 2010. Jump up ^ Slocum, Victor ( 1950 ). Capt. Joshua Slocum. New York : Sheridan House. pp. 27 -- 28. ISBN 0 - 924486 - 52 - X. Jump up ^ `` Description ''. Western Hemisphere Shorebird Reserve Network. Retrieved February 18, 2008. Jump up ^ `` New 7 Wonders omit Bay of Fundy ''. CBC News. CBC. November 11, 2011. Retrieved November 12, 2011. Jump up ^ `` Limits of Oceans and Seas, 3rd edition '' ( PDF ). International Hydrographic Organization. 1953. Retrieved February 7, 2010. Jump up ^ `` Teaching & Learning about Canada ''. Archived from the original on August 20, 2007. Retrieved September 26, 2007. Jump up ^ `` World 's Highest Tides -- Town of Parrsboro, Nova Scotia ''. Retrieved April 27, 2016. Jump up ^ Yeo, R.K, Risk, M.J., 1981, The sedimentology, stratigraphy, and preservation of intertidal deposits in the Minas Basin System, Bay of Fundy : Journal of Sedimentary Petrology, v. 51, pp. 245 -- 260. ^ Jump up to : Klein, G.D., 1963, Bay of Fundy intertidal zone sediments : Journal of Sedimentary Petrology, v. 33, pp. 844 -- 854. Jump up ^ The Official Site of the Bay of Fundy, 2010, Tides in the Bay of Fundy ( WWW document ). URL : `` Archived copy ''. Archived from the original on April 9, 2010. Retrieved 2010 - 04 - 15. Accessed April 4, 2010. Jump up ^ `` Annual Report 2012. '' Fundy Ocean Research Center for Energy ( 2012 ) : 1 - 25. Web. 8 December 2013. Jump up ^ `` The Fundy Ocean Research Center for Energy '' ( PDF ). FORCE ( Brochure ). Bay of Fundy, Nova Scotia, Canada : The Fundy Ocean Research Center for Energy. May 2012. Retrieved 9 December 2013. Imagine the power of the highest tides in the world. Imagine the technology to harness it. Jump up ^ `` Tidal Energy. '' National Oceanic and Atmospheric Administration ( 2010 ) : 1 -- 162. Web. 8 December 2013. Jump up ^ `` Massive new tidal turbine has been deployed on the coast of Nova Scotia and now produces electricity - first in North America ''. Electrek. 23 November 2016. Retrieved 23 November 2016. Jump up ^ Bay of Fundy, 2010, Fundy Geology ( WWW document ). URL : http://www.bayoffundy.com/geology.aspx Accessed April 4, 2010. ^ Jump up to : Trenhaile, A.S., Pepper, D.A., Trenhaile, R.W., and Dalimonte, M., 1998, Stacks and notches at Hopewell Rocks, New Brunswick, Canada : Earth Surface Processes and Landforms, v. 23, pp. 975 -- 988. Jump up ^ Dalton, F.K. ( 1951 ). `` Fundy 's prodigious tides and Petitcodiac 's tidal bore ''. Journal of the Royal Astronomical Society of Canada. XLV : 225 -- 231. Jump up ^ Natural History of Nova Scotia Vol. I, Chap. T6. 1 : `` Ocean Currents '', p. 109 ^ Jump up to : Faragher, John Mack, A Great and Noble Scheme New York ; W.W. Norton & Company, 2005. pp. 110 -- 112 ISBN 0 - 393 - 05135 - 8 Jump up ^ John Grenier. The Far Reaches of Empire : War in Nova Scotia, 1710 -- 1760. Oklahoma University Press. 2008 ISBN 978 - 0 - 8061 - 3876 - 3 Jump up ^ Smith, Joshua ( 2007 ). Borderland Smuggling : Patriots, Loyalists, and Illicit Trade in the Northeast, 1780 -- 1820. Gainesville, FL : UPF. pp. passim. ISBN 0 - 8130 - 2986 - 4. Jump up ^ Smith, Joshua ( 2011 ). Battle for the Bay : The Naval War of 1812. Fredericton, NB : Goose Lane Editions. pp. passim. ISBN 978 - 0 - 86492 - 644 - 9. External links Wikimedia Commons has media related to Bay of Fundy. Wikivoyage has a travel guide for Bay of Fundy. Wikisource has the text of the 1911 Encyclopædia Britannica article Fundy, Bay of. Travel and Science Information on Bay of Fundy region Bay of Fundy NASA Earth Observatory Official Bay of Fundy Tourist Site Central Nova Tourist Association The Quoddy Loop around Passamaquoddy Bay, in the Bay of Fundy Where the Bay Becomes the Sea, a documentary on the Bay of Fundy ecosystem Bay of Fundy Ecosystem Partnership -- scientific and popular information about the Bay The Official Tourism Site for Campobello Island, New Brunswick Tourism New Brunswick 's Bay of Fundy Earth 's oceans and seas Arctic Ocean Amundsen Gulf Barents Sea Beaufort Sea Chukchi Sea East Siberian Sea Greenland Sea Gulf of Boothia Kara Sea Laptev Sea Lincoln Sea Prince Gustav Adolf Sea Pechora Sea Queen Victoria Sea Wandel Sea White Sea Atlantic Ocean Adriatic Sea Aegean Sea Alboran Sea Archipelago Sea Argentine Sea Baffin Bay Balearic Sea Baltic Sea Bay of Biscay Bay of Bothnia Bay of Campeche Bay of Fundy Black Sea Bothnian Sea Caribbean Sea Celtic Sea English Channel Foxe Basin Greenland Sea Gulf of Bothnia Gulf of Finland Gulf of Lion Gulf of Guinea Gulf of Maine Gulf of Mexico Gulf of Saint Lawrence Gulf of Sidra Gulf of Venezuela Hudson Bay Ionian Sea Irish Sea Irminger Sea James Bay Labrador Sea Levantine Sea Libyan Sea Ligurian Sea Marmara Sea Mediterranean Sea Myrtoan Sea North Sea Norwegian Sea Sargasso Sea Sea of Åland Sea of Azov Sea of Crete Sea of the Hebrides Thracian Sea Tyrrhenian Sea Wadden Sea Indian Ocean Andaman Sea Arabian Sea Bali Sea Bay of Bengal Flores Sea Great Australian Bight Gulf of Aden Gulf of Aqaba Gulf of Khambhat Gulf of Kutch Gulf of Oman Gulf of Suez Java Sea Laccadive Sea Mozambique Channel Persian Gulf Red Sea Timor Sea Pacific Ocean Arafura Sea Banda Sea Bering Sea Bismarck Sea Bohai Sea Bohol Sea Camotes Sea Celebes Sea Ceram Sea Chilean Sea Coral Sea East China Sea Gulf of Alaska Gulf of Anadyr Gulf of California Gulf of Carpentaria Gulf of Fonseca Gulf of Panama Gulf of Thailand Gulf of Tonkin Halmahera Sea Koro Sea Mar de Grau Molucca Sea Moro Gulf Philippine Sea Salish Sea Savu Sea Sea of Japan Sea of Okhotsk Seto Inland Sea Shantar Sea Sibuyan Sea Solomon Sea South China Sea Sulu Sea Tasman Sea Visayan Sea Yellow Sea Southern Ocean Amundsen Sea Bellingshausen Sea Cooperation Sea Cosmonauts Sea Davis Sea D'Urville Sea King Haakon VII Sea Lazarev Sea Mawson Sea Riiser - Larsen Sea Ross Sea Scotia Sea Somov Sea Weddell Sea Endorheic basins Aral Sea Caspian Sea Dead Sea Sea of Galilee Salton Sea Book Coordinates : 45 ° 00 ′ N 65 ° 45 ′ W ﻿ / ﻿ 45.000 ° N 65.750 ° W ﻿ / 45.000 ; - 65.750 VIAF : 315125002 GND : 4134099 - 1 Retrieved from `` https://en.wikipedia.org/w/index.php?title=Bay_of_Fundy&oldid=796014836 '' Categories : Bays of New Brunswick Bays of Nova Scotia Bays of Maine Bays of the Atlantic Ocean Borders of New Brunswick Borders of Nova Scotia Canada -- United States border Hidden categories : Use mdy dates from June 2012 Articles containing French - language text Coordinates on Wikidata Wikipedia articles with VIAF identifiers Wikipedia articles with GND identifiers Talk Contents About Wikipedia Wikivoyage Azərbaycanca Bân - lâm - gú Беларуская Беларуская ( тарашкевіца ) ‎ Bosanski Català Cebuano Čeština Dansk Deutsch ދިވެހިބަސް Español Esperanto Euskara فارسی Français Gaeilge Galego 한국어 Ilokano Bahasa Indonesia Íslenska Italiano עברית ქართული Қазақша Kurdî Latviešu Lietuvių Lumbaart मराठी Nederlands 日本 語 Norsk ਪੰਜਾਬੀ پنجابی Polski Português Română Русский Scots Slovenčina Српски / srpski Suomi Svenska Türkçe Українська اردو Tiếng Việt Winaray 中文 Edit links This page was last edited on 17 August 2017, at 23 : 00. 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Question: why are the tides so extreme in the bay of fundy
Answer: tidal resonance resulting from a coincidence of timing: the time it takes a large wave to go from the mouth of the bay to the inner shore and back is practically the same as the time from one high tide to the next