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91-599: (Redirected from Maritime Province ) Maritime province may refer to: Maritimes , a region of Canada on the Atlantic coast Maritime Province, another name for Primorsky Krai , Russia, sometimes used in English language texts Topics referred to by the same term [REDACTED] This disambiguation page lists articles associated with the title Maritime province . If an internal link led you here, you may wish to change

182-482: A Golden Age, but that was a myth created in the 1930s to lure tourists to a romantic era of tall ships and antiques. Recent historians using census data have shown that is a fallacy. In 1851–1871 there was an overall increase in per capita wealth holding. However most of the gains went to the urban elite class, especially businessmen and financiers living in Halifax. The wealth held by the top 10% rose considerably over

273-687: A booming agricultural and fishing export economy having led to that colony opting not to sign on. The major communities of the region include Halifax and Cape Breton in Nova Scotia, Moncton , Saint John , and Fredericton in New Brunswick, and Charlottetown in Prince Edward Island. In spite of its name, The Maritimes has a humid continental climate of the warm-summer subtype. Especially in coastal Nova Scotia, differences between summers and winters are narrow compared to

364-670: A great many potential culprits. In 1867 Nova Scotia and New Brunswick merged with the Canadas in Confederation , with Prince Edward Island joining them six years later in 1873. Canada was formed only a year after free trade with the United States (in the form of the Reciprocity Treaty ) had ended. In the 1870s John A. Macdonald 's National Policy was implemented, creating a system of protective tariffs around

455-416: A mean eustatic component of 0.07 mm/yr for the last 2000 years. Since 1880, the ocean began to rise briskly, climbing a total of 210 mm (8.3 in) through 2009 causing extensive erosion worldwide and costing billions. Sea level rose by 6 cm during the 19th century and 19 cm in the 20th century. Evidence for this includes geological observations, the longest instrumental records and

546-669: A portion of coastal Maine at one point. The most significant incident from this war which occurred in the Maritimes was the British capture and detention of USS Chesapeake , an American frigate in Halifax. In 1820, the Colony of Cape Breton Island was merged back into the Colony of Nova Scotia for the second time by the British government. British settlement of the Maritimes, as the colonies of Nova Scotia, New Brunswick and Prince Edward Island came to be known, accelerated throughout

637-486: A rise of 6.5 m in less than 140 years, such that sea levels 5000 years ago were around 3m lower than present day, as evidenced in many locations by fossil beaches. Such rapid rates of sea level rising during meltwater events clearly implicate major ice-loss events related to ice sheet collapse. The primary source may have been meltwater from the Antarctic ice sheet. Other studies suggest a Northern Hemisphere source for

728-450: A shorter timescale, the low level reached during the LGM rebounded in the early Holocene , between about 14,000 and 6,500 years ago, leading to a 110 m sea level rise. Sea levels have been comparatively stable over the past 6,500 years, ending with a 0.50 m sea level rise over the past 1,500 years. For example, about 10,200 years ago the last land bridge between mainland Europe and Great Britain

819-416: A similar view and provides considerable evidence that the early 1880s were in fact a booming period in Nova Scotia and this growth was only undermined towards the end of that decade. David Alexander argues that any earlier declines were simply part of the global Long Depression , and that the Maritimes first fell behind the rest of Canada when the great boom period of the early 20th century had little effect on

910-611: A smaller population of the Maliseet in western New Brunswick. Given the small population of the region (compared with the Central Canadian provinces or the New England states), the regional economy is a net exporter of natural resources, manufactured goods, and services. The regional economy has long been tied to natural resources such as fishing, logging, farming, and mining activities. Significant industrialization in

1001-554: Is a region of Eastern Canada consisting of three provinces : New Brunswick , Nova Scotia , and Prince Edward Island . The Maritimes had a population of 1,899,324 in 2021, which makes up 5.1% of Canada's population. Together with Canada's easternmost province, Newfoundland and Labrador , the Maritime provinces make up the region of Atlantic Canada . Located along the Atlantic coast, various aquatic sub-basins are located in

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1092-702: Is less prevalent today. During the American Civil War , a significant number of Maritimers volunteered to fight for the armies of the Union , while a small handful joined the Confederate Army . However, the majority of the conflict's impact was felt in the shipping industry. Maritime shipping boomed during the war due to large-scale Northern imports of war supplies which were often carried by Maritime ships as Union ships were vulnerable to Confederate naval raiders. Diplomatic tensions between Britain and

1183-538: The Annapolis Basin . Acadians lived with uncertainty throughout the English constitutional crises under Oliver Cromwell , and it was not until the Treaty of Breda in 1667 that France's claim to the region was reaffirmed. Colonial administration by France throughout the history of Acadia was of low priority. France's priorities were in settling and strengthening its claim on the larger territory of New France and

1274-495: The Antarctica and Greenland ice sheets as snowfall . Slightly more water returns to the ocean in icebergs , from ice melting at the edges, and from rivers of meltwater flowing from ice sheets to the sea. The change in the total mass of ice on land, called the mass balance , is important because it causes changes in global sea level. High-precision gravimetry from satellites in low-noise flight has determined that in 2006,

1365-683: The Atlantic Ocean . The pre-history of the Canadian Maritimes begins after the northerly retreat of glaciers at the end of the Wisconsin glaciation over 10,000 years ago; human settlement by First Nations began in the Maritimes with Paleo-Indians during the Early Period , ending around 6,000 years ago. The Middle Period , starting 6,000 years ago, and ending 3,000 years ago, was dominated by rising sea levels from

1456-680: The Bay of Fundy being populated by French immigrants who called themselves Acadien . The Acadians eventually built small settlements throughout what is today mainland Nova Scotia and New Brunswick , as well as Île-Saint-Jean ( Prince Edward Island ), Île-Royale ( Cape Breton Island ), and other shorelines of the Gulf of St. Lawrence in present-day Newfoundland and Labrador , and Quebec . Acadian settlements had primarily agrarian economies. Early examples of Acadian fishing settlements developed in southwestern Nova Scotia and in Île-Royale, as well as along

1547-631: The Brittany , Normandie , and Vienne regions of France, continued to populate the colony of Acadia during the latter part of the 17th and early part of the 18th centuries. Important settlements also began in the Beaubassin region of the present-day Isthmus of Chignecto , and in the Saint John River valley, as well as smaller communities on Île-Saint-Jean and Île-Royale. In 1654, raiders from New England attacked Acadian settlements on

1638-566: The Caribbean , to being focused on commerce with the Canadian interior, enforced by the federal government's tariff policies. Coincident with the construction of railways in the region, the age of the wooden sailing ship began to come to an end, being replaced by larger and faster steel steamships . The Maritimes had long been a centre for shipbuilding , and this industry was hurt by the change. The larger ships were also less likely to call on

1729-585: The Confederation Bridge . There have been airport improvements at various centres providing improved connections to markets and destinations in the rest of North America and overseas. Improvements in infrastructure and the regional economy notwithstanding, the three provinces remain one of the poorer regions of Canada. While urban areas are growing and thriving, economic adjustments have been harsh in rural and resource-dependent communities, and emigration has been an ongoing phenomenon for some parts of

1820-542: The Laurentide Ice Sheet . Most of this had melted by about 10,000 years ago. Hundreds of similar glacial cycles have occurred throughout the Earth's history . Geologists who study the positions of coastal sediment deposits through time have noted dozens of similar basinward shifts of shorelines associated with a later recovery. This results in sedimentary cycles which in some cases can be correlated around

1911-784: The Raid on Chignecto , were conducted by Benjamin Church . In the second war, Queen Anne's War (the North American theatre of the War of the Spanish Succession ), the British conducted the Conquest of Acadia , while the region remained primarily in control of Maliseet militia , Acadia militia and Mi'kmaw militia . In 1719, to further protect strategic interests in the Gulf of St. Lawrence and St. Lawrence River , France began

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2002-592: The Siege of Louisbourg . The British returned control of Île-Royale to France with the fortress virtually intact three years later under the Treaty of Aix-la-Chapelle and the French reestablished their forces there. In 1749, to counter the rising threat of Louisbourg, Halifax was founded and the Royal Navy established a major naval base and citadel . The founding of Halifax sparked Father Le Loutre's War . During

2093-594: The Unionist North had deteriorated after some interests in Britain expressed support for the secessionist Confederate South . The Union Navy , although much smaller than the British Royal Navy and no threat to the Maritimes, did posture off Maritime coasts at times chasing Confederate naval ships which sought repairs and reprovisioning in Maritime ports, especially Halifax. The immense size of

2184-627: The Vinland region around 1000 AD, which is when the L'Anse aux Meadows settlement in Newfoundland and Labrador has been dated. They may have made further exploration into the present-day Maritimes and northeastern United States. Both Giovanni Caboto (John Cabot) and Giovanni da Verrazzano are reported to have sailed in or near Maritime waters during their voyages of discovery for England and France, respectively. Several Portuguese explorers / cartographers have also documented various parts of

2275-467: The continental margin . Regional transportation networks have also changed significantly in recent decades with port modernizations, with new freeway and ongoing arterial highway construction, the abandonment of various low-capacity railway branch lines (including the entire railway system of Prince Edward Island and southwestern Nova Scotia), and the construction of the Canso Causeway and

2366-531: The 17th and 18th centuries brought Acadia to the centre of world-scale geopolitical forces. In 1613, Virginian raiders captured Port-Royal, and in 1621 France ceded Acadia to Scotland's Sir William Alexander , who renamed it Nova Scotia . By 1632, Acadia was returned from Scotland to France under the Treaty of Saint-Germain-en-Laye . The Port Royale settlement was moved to the site of nearby present-day Annapolis Royal . More French immigrant settlers, primarily from

2457-473: The 1950s, resulting in the need to draw upon equalization payments to provide nationally mandated social services. Since the 1990s the region has experienced an exceptionally tumultuous period in its regional economy with the collapse of large portions of the ground fishery throughout Atlantic Canada, the closing of coal mines and a steel mill on Cape Breton Island , and the closure of military bases in all three provinces. That being said, New Brunswick has one of

2548-540: The 20-year construction of a large fortress at Louisbourg on Île-Royale. Massachusetts was increasingly concerned over reports of the capabilities of this fortress, and of privateers staging out of its harbour to raid New England fishermen on the Grand Banks. In the fourth war, King George's War (the North American theatre of the War of the Austrian Succession ), the British engaged successfully in

2639-650: The British and maintained vital supply lines to the French Fortress of Louisbourg and Fort Beausejour. The British sought to neutralize any military threat Acadians posed and to interrupt the vital supply lines Acadians provided to Louisbourg by deporting Acadians from Acadia. The British began the Expulsion of the Acadians with the Bay of Fundy campaign in 1775. Over the next nine years over 12,000 Acadians of 15,000 were removed from Nova Scotia. In 1758,

2730-476: The Colony of Nova Scotia to create the new colony of New Brunswick in 1784. At the same time, another part of the Colony of Nova Scotia, Cape Breton Island, was split off to become the Colony of Cape Breton Island. The Colony of St. John's Island was renamed Prince Edward Island on November 29, 1798. The War of 1812 had some effect on the shipping industry in the Maritime colonies of New Brunswick, Nova Scotia, Prince Edward Island, and Cape Breton Island; however,

2821-588: The Earth. The depth of the ocean basins is a function of the age of oceanic lithosphere (the tectonic plates beneath the floors of the world's oceans). As older plates age, they become denser and sink, allowing newer plates to rise and take their place. Therefore, a configuration with many small oceanic plates that rapidly recycle the oceanic lithosphere would produce shallower ocean basins and (all other things being equal) higher sea levels. A configuration with fewer plates and more cold, dense oceanic lithosphere, on

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2912-544: The Greenland and Antarctic ice sheets experienced a combined mass loss of 475 ± 158 Gt/yr, equivalent to 1.3 ± 0.4 mm/yr sea level rise. Notably, the acceleration in ice sheet loss over the period 1988–2006 was 22 ± 1 Gt/yr² for Greenland and 14.5 ± 2 Gt/yr² for Antarctica, for a total of 36 ± 2 Gt/yr². By 2010 the acceleration had increased to over 50 Gt/yr². This acceleration is 3 times larger than for mountain glaciers and ice caps (12 ± 6 Gt/yr²). Ice shelves float on

3003-700: The Maritime regional economy has begun increased contributions from manufacturing again and the steady transition to a service economy. Important manufacturing centres in the region include Pictou County , Truro , the Annapolis Valley and the South Shore , and the Strait of Canso area in Nova Scotia, as well as Summerside in Prince Edward Island, and the Miramichi area, the North Shore and

3094-460: The Maritimes, namely Diogo Homem . However, it was French explorer Jacques Cartier who made the first detailed reconnaissance of the region for a European power and, in so doing, claimed the region for the King of France. Cartier was followed by nobleman Pierre Dugua, Sieur de Mons , who was accompanied by explorer / cartographer Samuel de Champlain in a 1604 expedition. During this they established

3185-585: The Maritimes, such as the Gulf of Maine and Gulf of St. Lawrence . The region is located northeast of New England in the United States, south and southeast of Quebec 's Gaspé Peninsula , and southwest of the island of Newfoundland . The notion of a Maritime Union has been proposed at various times in Canada's history; the first discussions in 1864 at the Charlottetown Conference contributed to Canadian Confederation . This movement formed

3276-411: The Maritimes. Growth was strong, and the region had one of British North America 's most extensive manufacturing sectors as well as a large international shipping industry. The question of why the Maritimes fell from being a centre of Canadian manufacturing to being an economic hinterland is thus a central one to the study of the region's pecuniary difficulties. The period in which the decline occurred had

3367-733: The Union Army (the largest on the planet toward the end of the Civil War), however, was viewed with increasing concern by Maritimers throughout the early 1860s. Another concern was the rising threat of Fenian raids on border communities in New Brunswick by the Fenian Brotherhood seeking to end British rule in Ireland . This combination of events, coupled with an ongoing decline in British military and economic support to

3458-593: The area of the Strait. Sea level has changed over geologic time . As the graph shows, sea level today is very near the lowest level ever attained (the lowest level occurred at the Permian - Triassic boundary about 250 million years ago). During the most recent ice age (at its maximum about 20,000 years ago) the world's sea level was about 130 m lower than today, due to the large amount of sea water that had evaporated and been deposited as snow and ice , mostly in

3549-478: The average ocean level was generally 200 metres above current levels. However, the largest known example of marine flooding was when the Atlantic breached the Strait of Gibraltar at the end of the Messinian Salinity Crisis about 5.2 million years ago. This restored Mediterranean Sea levels at the sudden end of the period when that basin had dried up, apparently due to geologic forces in

3640-721: The coming months, with Île-Saint-Jean falling in 1759 to British forces on their way to Quebec City for the first siege of Quebec and the ensuing Battle of the Plains of Abraham . The war ended and Britain had gained control over the entire Maritime region and the Indigenous people signed the Halifax Treaties . Following the Seven Years' War , empty Acadian lands were settled first by 8,000 New England Planters and then by immigrants brought from Yorkshire . Île-Royale

3731-499: The decline. The exact date that the Maritimes began to fall behind the rest of Canada is difficult to determine. Historian Kris Inwood places the date very early, at least in Nova Scotia, finding clear signs that the Maritimes "Golden Age" of the mid-19th century was over by 1870, before Confederation or the National Policy could have had any significant impact. Richard Caves places the date closer to 1885. T.W. Acheson takes

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3822-634: The early 2000s, the current rise in sea level observed from tide gauges, of about 3.4 mm/yr, is within the estimate range from the combination of factors above, but active research continues in this field. At times during Earth's long history , the configuration of the continents and sea floor has changed due to plate tectonics . This affects global sea level by altering the depths of various ocean basins and also by altering glacier distribution with resulting changes in glacial-interglacial cycles. Changes in glacial-interglacial cycles are at least partially affected by changes in glacier distributions across

3913-733: The entire territory of British North America into a united colony. The Charlottetown Conference ended with an agreement to meet the following month in Quebec City , where more formal discussions ensued, culminating with meetings in London and the signing of the British North America Act , 1867 (BNA Act). Of the Maritime provinces, only Nova Scotia and New Brunswick were initially party to the BNA Act: Prince Edward Island's reluctance, combined with

4004-450: The era was indeed a golden age but only for a small but powerful and highly visible elite. The cause of economic malaise in the Maritimes is an issue of great debate and controversy among historians, economists, and geographers. The differing opinions can approximately be divided into the "structuralists", who argue that poor policy decisions are to blame, and the others, who argue that unavoidable technological and geographical factors caused

4095-585: The exploration and settlement of interior North America and the Mississippi River valley. Over 74 years (1689–1763) there were six colonial wars, which involved continuous warfare between New England and Acadia (see the French and Indian Wars reflecting English and French tensions in Europe, as well as Father Rale's War (Dummer's War) and Father Le Loutre's War ). Throughout these wars, New England

4186-431: The first commercial production field for oil beginning in the 1980s. Natural gas was also discovered in the 1980s during exploration work, and this is being commercially recovered, beginning in the late 1990s. Initial optimism in Nova Scotia about the potential of off-shore resources appears to have diminished with the lack of new discoveries, although exploration work continues and is moving farther off-shore into waters on

4277-430: The fortress of Louisbourg was laid siege for a second time within 15 years, this time by more than 27,000 British soldiers and sailors with over 150 warships. After the French surrender, Louisbourg was thoroughly destroyed by British engineers to ensure it would never be reclaimed. With the fall of Louisbourg, French and Mi'kmaw resistance in the region crumbled. British forces seized remaining French control over Acadia in

4368-621: The industry in Central Canada. The policies in the early years of Confederation were designed by Central Canadian interests, and they reflected the needs of that region. The unified Canadian market and the introduction of railroads created a relative weakness in the Maritime economies. Central to this concept, according to Acheson, was the lack of metropolises in the Maritimes. Past sea level Over geologic time sea level has fluctuated by more than 300 metres, possibly more than 400 metres. The main reasons for sea level fluctuations in

4459-530: The larger Dominion of Canada . The Mi'kmaq , Maliseet and Passamaquoddy people are indigenous to the Maritimes, while Acadian and British settlements date to the 17th century. The word maritime is an adjective that means of the sea ; from Latin maritimus "of the sea, near the sea", from mare "sea". Thus any land adjacent to the sea can be considered maritime. But the term Maritimes has historically been collectively applied to New Brunswick, Nova Scotia and Prince Edward Island, all of which border

4550-461: The largest military bases in the Commonwealth of Nations ( CFB Gagetown ), which plays a significant role in the cultural and economic spheres of Fredericton, the province's capital city. While the economic underperformance of the Maritime economy has been long lasting, it has not always been present. The mid-19th century, especially the 1850s and 1860s, has long been seen as a "Golden Age" in

4641-585: The last 15 million years are the Antarctic ice sheet and Antarctic post-glacial rebound during warm periods. The current sea level is about 130 metres higher than the historical minimum. Historically low levels were reached during the Last Glacial Maximum (LGM), about 20,000 years ago. The last time the sea level was higher than today was during the Eemian , about 130,000 years ago. Over

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4732-646: The late 18th century and into the 19th century with significant immigration to the region as a result of Scottish migrants displaced by the Highland Clearances and Irish escaping the Great Irish Famine (1845–1849). As a result, significant portions of the three provinces are influenced by Celtic heritages, with Scottish Gaelic (and to a lesser degree, Irish Gaelic ) having been widely spoken, particularly in Cape Breton, although it

4823-477: The link to point directly to the intended article. Retrieved from " https://en.wikipedia.org/w/index.php?title=Maritime_province&oldid=932981419 " Category : Disambiguation pages Hidden categories: Short description is different from Wikidata All article disambiguation pages All disambiguation pages Maritimes The Maritimes , also called the Maritime provinces ,

4914-421: The long-term mean sea level has been higher than today (see graph above). Only at the Permian - Triassic boundary ~250 million years ago was the long-term mean sea level lower than today. Long term changes in the mean sea level are the result of changes in the oceanic crust , with a downward trend expected to continue in the very long term. During the glacial-interglacial cycles over the past few million years,

5005-406: The mean sea level has varied by somewhat more than a hundred metres . This is primarily due to the growth and decay of ice sheets (mostly in the northern hemisphere) with water evaporated from the sea. The Mediterranean Basin 's gradual growth as the Neotethys basin, begun in the Jurassic , did not suddenly affect ocean levels. While the Mediterranean was forming during the past 100 million years,

5096-417: The melting glaciers in polar regions. This is when what is called the Laurentian tradition started among Archaic Indians , the term used for First Nations peoples of the time. Evidence of Archaic Indian burial mounds and other ceremonial sites existing in the Saint John River valley has been uncovered. The Late Period extended from 3,000 years ago until first contact with European settlers. This period

5187-620: The meltwater in the Laurentide Ice Sheet. Recently, it has become widely accepted that late Holocene, 3,000 calendar years ago to present, sea level was nearly stable prior to an acceleration of rate of rise that is variously dated between 1850 and 1900 AD. Late Holocene rates of sea level rise have been estimated using evidence from archaeological sites and late Holocene tidal marsh sediments, combined with tide gauge and satellite records and geophysical modeling. For example, this research included studies of Roman wells in Caesarea and of Roman piscinae in Italy. These methods in combination suggest

5278-437: The more successful English settlement at Jamestown in present-day Virginia by three years. Champlain was considered the founder of New France 's province of Canada, which comprises much of the present-day lower St. Lawrence River valley in the province of Quebec . Champlain's success in the region, which came to be called Acadie , led to the fertile tidal marshes surrounding the southeastern and northeastern reaches of

5369-481: The most important changes, and one that almost certainly had an effect, was the revolution in transportation that occurred at this time. The Maritimes were connected to central Canada by the Intercolonial Railway in the 1870s, removing a longstanding barrier to trade. For the first time this placed the Maritime manufacturers in direct competition with those of Central Canada. Maritime trading patterns shifted considerably from mainly trading with New England , Britain, and

5460-425: The new nation. Throughout the period there was also significant technological change both in the production and transportation of goods. Several scholars have explored the so-called "Golden Age" of the Maritimes in the years just before Confederation. In Nova Scotia , the population grew steadily from 277,000 in 1851 to 388,000 in 1871, mostly from natural increase since immigration was slight. The era has been called

5551-440: The northwestern coastal regions of the present-day Bay of Fundy . The Mi'kmaq Nation is also believed to have crossed the present-day Cabot Strait at around this time to settle on the south coast of Newfoundland , but they were a minority compared to the Beothuk Nation. After Newfoundland, the Maritimes were the second area in Canada to be settled by Europeans. There is evidence that Viking explorers discovered and settled in

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5642-495: The observed rate of 20th century sea level rise. For example, geological observations indicate that during the last 2,000 years, sea level change was small, with an average rate of only 0.0–0.2 mm per year. This compares to an average rate of 1.7 ± 0.5 mm per year for the 20th century. Baart et al. (2012) show that it is important to account for the effect of the 18.6-year lunar nodal cycle before acceleration in sea level rise should be concluded. Based on tide gauge data,

5733-412: The other hand, would result in deeper ocean basins and lower sea levels. When there was much continental crust near the poles, the rock record shows unusually low sea levels during ice ages, because there was much polar land mass on which snow and ice could accumulate. During times when the land masses clustered around the equator, ice ages had much less effect on sea level. Over most of geologic time,

5824-480: The other two Maritime provinces in that it has a much higher Francophone population . There was once a significant Canadian Gaelic speaking population. Helen Creighton recorded Celtic traditions of rural Nova Scotia in the mid-1900s. There are Black Canadians who are mostly descendants of Black Loyalists or black refugees from the War of 1812 . This Maritime population is mainly among Black Nova Scotians . There are Mi'kmaq reserves in all three provinces, and

5915-408: The rapid melting of the British-Irish Sea, Fennoscandian, Laurentide , Barents-Kara , Patagonian , Innuitian ice sheets and parts of the Antarctic ice sheet . At the onset of deglaciation about 19,000 years ago, a brief, at most 500-year long, glacio-eustatic event may have contributed as much as 10 m to sea level with an average rate of about 20 mm/yr. During the rest of the early Holocene,

6006-582: The rate of sea level rise varied from a low of about 6.0–9.9  mm/yr to as high as 30–60  mm/yr during brief periods of accelerated sea level rise. Solid geological evidence, based largely upon analysis of deep cores of coral reefs , exists only for 3 major periods of accelerated sea level rise, called meltwater pulses , during the last deglaciation. They are Meltwater pulse 1A between circa 14,600 and 14,300 years ago; Meltwater pulse 1B between circa 11,400 and 11,100 years ago; and Meltwater pulse 1C between 8,200 and 7,600 years ago. Meltwater pulse 1A

6097-447: The region as the Home Office favoured newer colonial endeavours in Africa and elsewhere, led to a call among Maritime politicians for a conference on Maritime Union , to be held in early September 1864 in Charlottetown – chosen in part because of Prince Edward Island's reluctance to give up its jurisdictional sovereignty in favour of uniting with New Brunswick and Nova Scotia into a single colony. New Brunswick and Nova Scotia felt that if

6188-459: The region's finances. T.W. Acheson is one of the main proponents of this theory. He notes the growth that was occurring during the early years of the National Policy in Nova Scotia demonstrates how the effects of railway fares and the tariff structure helped undermine this growth. Capitalists from Central Canada purchased the factories and industries of the Maritimes from their bankrupt local owners and proceeded to close down many of them, consolidating

6279-424: The region's numerous universities and colleges—are significant economic contributors. Another important contribution to Nova Scotia's provincial economy is through spin-offs and royalties relating to off-shore petroleum exploration and development. Mostly concentrated on the continental shelf of the province's Atlantic coast in the vicinity of Sable Island , exploration activities began in the 1960s and resulted in

6370-405: The region. Another problem is seen in the lower average wages and family incomes within the region. Property values are depressed, resulting in a smaller tax base for these three provinces, particularly when compared with the national average which benefits from central and western Canadian economic growth. This has been particularly problematic with the growth of the welfare state in Canada since

6461-495: The region. E.R. Forbes, however, emphasizes that the precipitous decline did not occur until after the First World War during the 1920s when new railway policies were implemented. Forbes also contends that significant Canadian defence spending during the Second World War favoured powerful political interests in Central Canada such as C. D. Howe , when major Maritime shipyards and factories, as well as Canada's largest steel mill, located in Cape Breton Island, fared poorly. One of

6552-897: The rest of Canada. The inland climate of New Brunswick is in stark contrast during winter, resembling more continental areas. Summers are somewhat tempered by the marine influence throughout the provinces, but due to the southerly parallels still remain similar to more continental areas further west. Yarmouth in Nova Scotia has significant marine influence to have a borderline oceanic microclimate , but winter nights are still cold even in all coastal areas. The northernmost areas of New Brunswick are only just above subarctic with very cold continental winters. The Maritimes were predominantly rural until recent decades, having resource-based economies of fishing, agriculture, forestry, and coal mining. Maritimers are predominantly of west European origin: Scottish Canadians , Irish Canadians , English Canadians , and Acadians . New Brunswick, in general, differs from

6643-410: The second half of the 19th century brought steel to Trenton, Nova Scotia , and subsequent creation of a widespread industrial base to take advantage of the region's large underground coal deposits. After Confederation, however, this industrial base withered with technological change, and trading links to Europe and the U.S. were reduced in favour of those with Ontario and Quebec. In recent years, however,

6734-489: The second permanent European settlement in what is now the United States and Canada, following Spain's settlement at St. Augustine in present-day Florida in the American South. Champlain's settlement at Saint Croix Island , later moved to Port Royal ( Annapolis Royal ), survived. By contrast, the ill-fated English settlement at Roanoke Colony off the southern American coast did not. The French settlement pre-dated

6825-464: The significant Royal Navy presence in Halifax and other ports in the region prevented any serious attempts by American raiders. Maritime and American privateers targeted unprotected shipping of both the United States and Britain respectively, further reducing trade. New Brunswick's section of the Canada–US border did not have any significant action during this conflict, although British forces did occupy

6916-410: The sixth and final colonial war, the French and Indian War (the North American theatre of the Seven Years' War ), the military conflicts in Nova Scotia continued. The British Conquest of Acadia happened in 1710. Over the next forty-five years, the Acadians refused to sign an unconditional oath of allegiance to Britain. During this time period Acadians participated in various militia operations against

7007-473: The smaller population centres such as Saint John and Halifax, preferring to travel to cities like New York and Montreal . Even the Cunard Line , founded by Maritime-born Samuel Cunard , stopped making more than a single ceremonial voyage to Halifax each year. More controversial than the role of technology is the argument over the role of politics in the origins of the region's decline. Confederation and

7098-618: The south and west coasts of Newfoundland, the Gaspé Peninsula , and the present-day Côte-Nord region of Quebec. Most Acadian fishing activities were overshadowed by the much larger seasonal European fishing fleets that were based out of Newfoundland and took advantage of proximity to the Grand Banks . The growing English colonies along the American seaboard to the south and various European wars between England and France during

7189-424: The surface of the sea and, if they melt, to first order they do not change sea level. Likewise, the melting of the northern polar ice cap which is composed of floating pack ice would not significantly contribute to rising sea levels. However, because floating ice pack is lower in salinity than seawater, their melting would cause a very small increase in sea levels, so small that it is generally neglected. As of

7280-466: The targets of American raiders. Charlottetown, the capital of the new colony of St. John's Island, was ransacked in 1775 with the provincial secretary kidnapped and the Great Seal stolen. The largest military action in the Maritimes during the revolutionary war was the attack on Fort Cumberland (the renamed Fort Beauséjour ) in 1776 by a force of American sympathizers led by Jonathan Eddy . The fort

7371-492: The tariff and railway freight policies that followed have often been blamed for having a deleterious effect on the Maritime economies. Arguments have been made that the Maritimes' poverty was caused by control over policy by Central Canada which used the national structures for its own enrichment. This was the central view of the Maritime Rights Movement of the 1920s, which advocated greater local control over

7462-489: The two decades, but there was little improvement in the wealth levels in rural areas, which comprised the great majority of the population. Likewise Gwyn reports that gentlemen, merchants, bankers, colliery owners, shipowners, shipbuilders, and master mariners flourished. However the great majority of families were headed by farmers, fishermen, craftsmen and labourer. Most of them—and many widows as well—lived in poverty. Out migration became an increasingly necessary option. Thus

7553-577: The union conference were held in Charlottetown, they might be able to convince Island politicians to support the proposal. The Charlottetown Conference , as it came to be called, was also attended by a slew of visiting delegates from the neighbouring Crown colony , the Province of Canada , who had largely arrived at their own invitation with their own agenda. This agenda saw the conference dominated by discussions of creating an even larger union of

7644-507: The upper Saint John River valley of New Brunswick. Some predominantly coastal areas have become major tourist centres, such as parts of Prince Edward Island, Cape Breton Island, the South Shore of Nova Scotia and the Gulf of St. Lawrence and Bay of Fundy coasts of New Brunswick. Additional service-related industries in information technology , pharmaceuticals, insurance and financial sectors—as well as research-related spin-offs from

7735-459: The world with great confidence. This relatively new branch of geological science linking eustatic sea level to sedimentary deposits is called sequence stratigraphy . The most up-to-date chronology of sea level change through the Phanerozoic shows the following long-term trends: During deglaciation between about 19– 8  ka , sea level rose at extremely high rates as the result of

7826-468: Was a 13.5 m rise over about 290 years centered at 14,200 years ago and Meltwater pulse 1B was a 7.5 m rise over about 160 years centered at 11,000 years ago. In sharp contrast, the period between 14,300 and 11,100 years ago, which includes the Younger Dryas interval, was an interval of reduced sea level rise at about 6.0–9.9  mm/yr. Meltwater pulse 1C was centered at 8,000 years ago and produced

7917-799: Was allied with the Iroquois Confederacy based around the southern Great Lakes and west of the Hudson River . Acadian settlers were allied with the Wabanaki Confederacy . In the first war, King William's War (the North American theatre of the Nine Years' War ), natives from the Maritime region participated in numerous attacks with the French on the Acadia / New England border in southern Maine (e.g., Raid on Salmon Falls ). New England retaliatory raids on Acadia, such as

8008-695: Was dominated by the organization of First Nations peoples into the Algonquian -speaking Abenaki Nation, which occupied territory largely in present-day interior Vermont , New Hampshire , and Maine , and the Mi'kmaq Nation, which inhabited all of Nova Scotia, Prince Edward Island, eastern New Brunswick and the southern Gaspé . The primarily agrarian Maliseet Nation settled throughout the Saint John River and Allagash River valleys of present-day New Brunswick and Maine. The Passamaquoddy Nation inhabited

8099-555: Was partially overrun after a month-long siege, but the attackers were ultimately repelled after the arrival of British reinforcements from Halifax. The most significant impact from this war was the settling of large numbers of Loyalist refugees in the region (34,000 to the 17,000 settlers already there), especially in Shelburne and Parrtown (Saint John). Following the Treaty of Paris in 1783, Loyalist settlers in what would become New Brunswick persuaded British administrators to split

8190-528: Was renamed Cape Breton Island and incorporated into the Colony of Nova Scotia. Some of the Acadians who had been deported came back but went to the eastern coasts of New Brunswick. Both the colonies of Nova Scotia (present-day Nova Scotia and New Brunswick) and St. John's Island (Prince Edward Island) were affected by the American Revolutionary War , largely by privateering against American shipping, but several coastal communities were also

8281-414: Was submerged, leaving behind a salt marsh. By 8000 years ago the marshes were drowned by the sea, leaving no trace of any former dry land connection. Observational and modeling studies of mass loss from glaciers and ice caps indicate a contribution to a sea-level rise of 2 to 4 cm over the 20th century. Each year about 8 mm (0.3 inches) of water from the entire surface of the oceans falls onto

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