Tuesday, March 31, 2009
Boston
Boston is the capital and largest city of the Commonwealth of Massachusetts, and is one of the oldest cities in the United States. The largest city in New England, Boston is considered the economic and cultural center of the region, and is sometimes regarded as the unofficial "Capital of New England." Boston city proper had a 2007 estimated population of 608,352, making it the twenty-first largest in the country. Boston is also the anchor of a substantially larger metropolitan area called Greater Boston, home to 4.4 million people and the tenth-largest metropolitan area in the country. Greater Boston as a commuting region includes parts of Rhode Island, New Hampshire and Maine; it includes 7.4 million people, making it the fifth-largest Combined Statistical Area in the United States.
In 1630, Puritan colonists from England founded the city on the Shawmut Peninsula. During the late 18th century Boston was the location of several major events during the American Revolution, including the Boston Massacre and the Boston Tea Party. Several early battles of the American Revolution, such as the Battle of Bunker Hill and the Siege of Boston, occurred within the city and surrounding areas. Through land reclamation and municipal annexation, Boston has expanded beyond the peninsula. After American independence was attained Boston became a major shipping port and manufacturing center, and its rich history now attracts 16.3 million visitors annually. The city was the site of several firsts, including America's first public school, Boston Latin School (1635), and first college, Harvard College (1636), in neighboring Cambridge. Boston was also home to the first subway system in the United States.
With many colleges and universities within the city and surrounding area, Boston is a center of higher education[10] and a center for medicine. The city's economy is also based on research, finance, and technology – principally biotechnology. Boston ranks first in the country in jobs per square mile ahead of New York City and Washington, DC. The city has been experiencing gentrification and has one of the highest costs of living in the United States, though it remains high on world livability rankings.
Owing to its early founding, Boston is very compact. According to the United States Census Bureau, the city has a total area of 89.6 square miles (232.1 km²)—48.4 square miles (125.4 km²) (54.0%) of land and 41.2 square miles (106.7 km²) (46.0%) of water. Boston is the country's fourth most densely populated city that is not a part of a larger city's metropolitan area. Of United States cities with more than 600,000 people, only San Francisco is smaller in land area.
Boston is surrounded by the "Greater Boston" region and is bordered by the cities and towns of Winthrop, Revere, Chelsea, Everett, Somerville, Cambridge, Watertown, Newton, Brookline, Needham, Dedham, Canton, Milton, and Quincy.
Boston's official elevation, as measured at Logan International Airport, is 19 ft (5.8 m) above sea level. The highest point in Boston is Bellevue Hill at 330 ft (101 m) above sea level, and the lowest point is at sea level.
Much of the Back Bay and South End neighborhoods are built on reclaimed land—all of the earth from two of Boston's three original hills, the "trimount," was used as landfill material. Only Beacon Hill—the smallest of the three original hills—remains partially intact; only half of its height was cut down for landfill. The downtown area and immediate surroundings consist mostly of low-rise brick or stone buildings, with many older buildings in the Federal style. Several of these buildings mix in with modern high-rises, notably in the Financial District, Government Center, the South Boston waterfront, and Back Bay, which includes many prominent landmarks such as the Boston Public Library, Christian Science Center, Copley Square, Newbury Street, and New England's two tallest buildings—the John Hancock Tower and the Prudential Center. Near the John Hancock Tower is the old John Hancock Building with its prominent weather forecast beacon—the color of the illuminated light gives an indication of weather to come: "steady blue, clear view; flashing blue, clouds are due; steady red, rain ahead; flashing red, snow instead." (In the summer, flashing red indicates instead that a Red Sox game has been rained out.) Smaller commercial areas are interspersed among single-family homes and wooden/brick multi-family row houses. Currently, the South End Historic District remains the largest surviving contiguous Victorian-era neighborhood in the U.S.
Along with downtown, the geography of South Boston was particularly impacted by the Central Artery/Tunnel (CA/T) Project (or the "Big Dig"). The unstable reclaimed land in South Boston posed special problems for the project's tunnels. In the downtown area, the CA/T Project allowed for the removal of the unsightly elevated Central Artery and the incorporation of new green spaces and open areas.
Boston Common, located near the Financial District and Beacon Hill, is the oldest public park in the U.S. Along with the adjacent Boston Public Garden, it is part of the Emerald Necklace, a string of parks designed by Frederick Law Olmsted to encircle the city. Franklin Park, which is also part of the Emerald Necklace, is the city's largest park and houses a zoo. Another major park is the Esplanade, located along the banks of the Charles River. Other parks are scattered throughout the city, with the major parks and beaches located near Castle Island; in Charlestown; and along the Dorchester, South Boston, and East Boston shorelines.
The Charles River separates Boston proper from Cambridge, Watertown, and the neighborhood of Charlestown. To the east lies Boston Harbor and the Boston Harbor Islands National Recreation Area. The Neponset River forms the boundary between Boston's southern neighborhoods and the city of Quincy and the town of Milton. The Mystic River separates Charlestown from Chelsea and Everett, and Chelsea Creek and Boston Harbor separate East Boston from Boston property
Boston has what may basically be described as something between a humid continental climate and a humid subtropical climate, such as is very common in coastal southern New England. Summers are typically warm and humid, while winters are cold, windy, and snowy. Prevailing wind patterns that blow offshore affect Boston, minimizing the influence of the Atlantic Ocean.
Spring in Boston can be warm, with temperatures as high as the 90s when winds are offshore, although it is just as possible for a day in late May to remain in the lower 40s because of cool ocean waters. The hottest month is July, with an average high of 82 °F (28 °C) and an average low of 66 °F (18 °C), with conditions usually humid. The coldest month is January, with an average high of 36 °F (2 °C) and an average low of 22 °F (−6 °C).[36] Periods exceeding 90 °F (32 °C) in summer and below 10 °F (−12 °C) in winter are not uncommon but are rarely prolonged. The record high temperature is 104 °F (40 °C), recorded on July 4, 1911. The record low temperature is −18 °F (−28 °C), recorded on February 9, 1934. February in Boston has seen 70 °F (21 °C) only once in recorded history, on February 24, 1985. The highest temperature recorded in March was 89 °F (31 °C), on March 31, 1998.
The city averages about 43 in (108 cm) of precipitation a year, with 40.9 in (104 cm) of snowfall a year. Snowfall increases dramatically as one goes inland away from the city (Especially north and west of the city)—away from the warming influence of the ocean.[39] Most snowfall occurs from December through March. There is usually little or no snow in April and November, and snow is rare in May and October.
Boston's coastal location on the North Atlantic, although it moderates temperatures, also makes the city very prone to Nor'easter weather systems that can produce much snow and rain. Fog is prevalent, particularly in spring and early summer, and the occasional tropical storm or hurricane can threaten the region, especially in early autumn.
In 1630, Puritan colonists from England founded the city on the Shawmut Peninsula. During the late 18th century Boston was the location of several major events during the American Revolution, including the Boston Massacre and the Boston Tea Party. Several early battles of the American Revolution, such as the Battle of Bunker Hill and the Siege of Boston, occurred within the city and surrounding areas. Through land reclamation and municipal annexation, Boston has expanded beyond the peninsula. After American independence was attained Boston became a major shipping port and manufacturing center, and its rich history now attracts 16.3 million visitors annually. The city was the site of several firsts, including America's first public school, Boston Latin School (1635), and first college, Harvard College (1636), in neighboring Cambridge. Boston was also home to the first subway system in the United States.
With many colleges and universities within the city and surrounding area, Boston is a center of higher education[10] and a center for medicine. The city's economy is also based on research, finance, and technology – principally biotechnology. Boston ranks first in the country in jobs per square mile ahead of New York City and Washington, DC. The city has been experiencing gentrification and has one of the highest costs of living in the United States, though it remains high on world livability rankings.
Owing to its early founding, Boston is very compact. According to the United States Census Bureau, the city has a total area of 89.6 square miles (232.1 km²)—48.4 square miles (125.4 km²) (54.0%) of land and 41.2 square miles (106.7 km²) (46.0%) of water. Boston is the country's fourth most densely populated city that is not a part of a larger city's metropolitan area. Of United States cities with more than 600,000 people, only San Francisco is smaller in land area.
Boston is surrounded by the "Greater Boston" region and is bordered by the cities and towns of Winthrop, Revere, Chelsea, Everett, Somerville, Cambridge, Watertown, Newton, Brookline, Needham, Dedham, Canton, Milton, and Quincy.
Boston's official elevation, as measured at Logan International Airport, is 19 ft (5.8 m) above sea level. The highest point in Boston is Bellevue Hill at 330 ft (101 m) above sea level, and the lowest point is at sea level.
Much of the Back Bay and South End neighborhoods are built on reclaimed land—all of the earth from two of Boston's three original hills, the "trimount," was used as landfill material. Only Beacon Hill—the smallest of the three original hills—remains partially intact; only half of its height was cut down for landfill. The downtown area and immediate surroundings consist mostly of low-rise brick or stone buildings, with many older buildings in the Federal style. Several of these buildings mix in with modern high-rises, notably in the Financial District, Government Center, the South Boston waterfront, and Back Bay, which includes many prominent landmarks such as the Boston Public Library, Christian Science Center, Copley Square, Newbury Street, and New England's two tallest buildings—the John Hancock Tower and the Prudential Center. Near the John Hancock Tower is the old John Hancock Building with its prominent weather forecast beacon—the color of the illuminated light gives an indication of weather to come: "steady blue, clear view; flashing blue, clouds are due; steady red, rain ahead; flashing red, snow instead." (In the summer, flashing red indicates instead that a Red Sox game has been rained out.) Smaller commercial areas are interspersed among single-family homes and wooden/brick multi-family row houses. Currently, the South End Historic District remains the largest surviving contiguous Victorian-era neighborhood in the U.S.
Along with downtown, the geography of South Boston was particularly impacted by the Central Artery/Tunnel (CA/T) Project (or the "Big Dig"). The unstable reclaimed land in South Boston posed special problems for the project's tunnels. In the downtown area, the CA/T Project allowed for the removal of the unsightly elevated Central Artery and the incorporation of new green spaces and open areas.
Boston Common, located near the Financial District and Beacon Hill, is the oldest public park in the U.S. Along with the adjacent Boston Public Garden, it is part of the Emerald Necklace, a string of parks designed by Frederick Law Olmsted to encircle the city. Franklin Park, which is also part of the Emerald Necklace, is the city's largest park and houses a zoo. Another major park is the Esplanade, located along the banks of the Charles River. Other parks are scattered throughout the city, with the major parks and beaches located near Castle Island; in Charlestown; and along the Dorchester, South Boston, and East Boston shorelines.
The Charles River separates Boston proper from Cambridge, Watertown, and the neighborhood of Charlestown. To the east lies Boston Harbor and the Boston Harbor Islands National Recreation Area. The Neponset River forms the boundary between Boston's southern neighborhoods and the city of Quincy and the town of Milton. The Mystic River separates Charlestown from Chelsea and Everett, and Chelsea Creek and Boston Harbor separate East Boston from Boston property
Boston has what may basically be described as something between a humid continental climate and a humid subtropical climate, such as is very common in coastal southern New England. Summers are typically warm and humid, while winters are cold, windy, and snowy. Prevailing wind patterns that blow offshore affect Boston, minimizing the influence of the Atlantic Ocean.
Spring in Boston can be warm, with temperatures as high as the 90s when winds are offshore, although it is just as possible for a day in late May to remain in the lower 40s because of cool ocean waters. The hottest month is July, with an average high of 82 °F (28 °C) and an average low of 66 °F (18 °C), with conditions usually humid. The coldest month is January, with an average high of 36 °F (2 °C) and an average low of 22 °F (−6 °C).[36] Periods exceeding 90 °F (32 °C) in summer and below 10 °F (−12 °C) in winter are not uncommon but are rarely prolonged. The record high temperature is 104 °F (40 °C), recorded on July 4, 1911. The record low temperature is −18 °F (−28 °C), recorded on February 9, 1934. February in Boston has seen 70 °F (21 °C) only once in recorded history, on February 24, 1985. The highest temperature recorded in March was 89 °F (31 °C), on March 31, 1998.
The city averages about 43 in (108 cm) of precipitation a year, with 40.9 in (104 cm) of snowfall a year. Snowfall increases dramatically as one goes inland away from the city (Especially north and west of the city)—away from the warming influence of the ocean.[39] Most snowfall occurs from December through March. There is usually little or no snow in April and November, and snow is rare in May and October.
Boston's coastal location on the North Atlantic, although it moderates temperatures, also makes the city very prone to Nor'easter weather systems that can produce much snow and rain. Fog is prevalent, particularly in spring and early summer, and the occasional tropical storm or hurricane can threaten the region, especially in early autumn.
New England
New England is a region of the United States located in the northeastern corner of the country, bounded by the Atlantic Ocean, Canada and New York State, and consisting of the modern states of Maine, New Hampshire, Vermont, Massachusetts, Rhode Island, and Connecticut.
In one of the earliest English settlements in the New World, English Pilgrims from Europe first settled in New England in 1620, in the colony of Plymouth. In the late 18th century, the New England colonies would be among the first North American British colonies to demonstrate ambitions of independence from the British Crown, although they would later oppose the War of 1812 between the United States and Britain.
New England produced the first pieces of American literature and philosophy and was home to the beginnings of free public education. In the 19th century, it played a prominent role in the movement to abolish slavery in the United States. It was the first region of the United States to be transformed by the Industrial Revolution from Great Britain.
It is one of the most liberal regions in the United States, with every state voting for the Democratic Party in the 1992, 1996, 2004, and 2008 Presidential elections, and every state but New Hampshire voting for Al Gore in 2000. Following the 2008 elections, all members of the House of Representatives from New England belong to the Democratic Party.
New England's long rolling hills, mountains, and jagged coastline are a consequence of retreating ice sheets from prehistoric times. The coast of the region, extending from southwestern Connecticut to northeastern Maine, is dotted with lakes, hills, swamps, and sandy beaches. Further inland are the Appalachian Mountains, extending through Connecticut, Massachusetts, Vermont, New Hampshire, and Maine. Among them, in the White Mountains of New Hampshire is Mount Washington, which at 1,917 m (6,288 ft), is the highest peak in the northeast United States. It is also the site of the highest recorded wind speed on Earth. Vermont's Green Mountains, which become the Berkshire Hills in western Massachusetts and Connecticut, are smaller than the White Mountains. Valleys in the region include the Connecticut River Valley and the Merrimack Valley.
The longest river is the Connecticut River, which flows from northeastern New Hampshire for 655 km (407 mi), emptying into the Long Island Sound, roughly bisecting the region. Lake Champlain, wedged between Vermont and New York, is the largest lake in the region, followed by Moosehead Lake in Maine and Lake Winnipesaukee in New Hampshire.
Weather patterns are highly variable and climate varies throughout the region. Maine, New Hampshire, and Vermont have a humid continental short summer climate, with cooler summers and long, cold winters. Connecticut, Massachusetts, and Rhode Island, have a humid continental long summer climate, with hot summers and cold winters. Owing to thick deciduous forests, fall in New England brings bright and colorful foliage, which comes earlier than in other regions, attracting tourism by 'leaf peepers'. Springs are generally wet and cloudy. Average rainfall generally ranges from 1,000 to 1,500 mm (40 to 60 in) a year, although the northern parts of Vermont and Maine see slightly less, from 500 to 1,000 mm (20 to 40 in). Snowfall can often exceed 2,500 mm (100 in) annually. As a result, the mountains and ski resorts of Vermont and New Hampshire are popular destinations in the winter.
The lowest recorded temperature in New England was -50 °F (-46 °C), at Bloomfield, Vermont, on December 30, 1933. This was tied by Big Black River, Maine in 2009
In one of the earliest English settlements in the New World, English Pilgrims from Europe first settled in New England in 1620, in the colony of Plymouth. In the late 18th century, the New England colonies would be among the first North American British colonies to demonstrate ambitions of independence from the British Crown, although they would later oppose the War of 1812 between the United States and Britain.
New England produced the first pieces of American literature and philosophy and was home to the beginnings of free public education. In the 19th century, it played a prominent role in the movement to abolish slavery in the United States. It was the first region of the United States to be transformed by the Industrial Revolution from Great Britain.
It is one of the most liberal regions in the United States, with every state voting for the Democratic Party in the 1992, 1996, 2004, and 2008 Presidential elections, and every state but New Hampshire voting for Al Gore in 2000. Following the 2008 elections, all members of the House of Representatives from New England belong to the Democratic Party.
New England's long rolling hills, mountains, and jagged coastline are a consequence of retreating ice sheets from prehistoric times. The coast of the region, extending from southwestern Connecticut to northeastern Maine, is dotted with lakes, hills, swamps, and sandy beaches. Further inland are the Appalachian Mountains, extending through Connecticut, Massachusetts, Vermont, New Hampshire, and Maine. Among them, in the White Mountains of New Hampshire is Mount Washington, which at 1,917 m (6,288 ft), is the highest peak in the northeast United States. It is also the site of the highest recorded wind speed on Earth. Vermont's Green Mountains, which become the Berkshire Hills in western Massachusetts and Connecticut, are smaller than the White Mountains. Valleys in the region include the Connecticut River Valley and the Merrimack Valley.
The longest river is the Connecticut River, which flows from northeastern New Hampshire for 655 km (407 mi), emptying into the Long Island Sound, roughly bisecting the region. Lake Champlain, wedged between Vermont and New York, is the largest lake in the region, followed by Moosehead Lake in Maine and Lake Winnipesaukee in New Hampshire.
Weather patterns are highly variable and climate varies throughout the region. Maine, New Hampshire, and Vermont have a humid continental short summer climate, with cooler summers and long, cold winters. Connecticut, Massachusetts, and Rhode Island, have a humid continental long summer climate, with hot summers and cold winters. Owing to thick deciduous forests, fall in New England brings bright and colorful foliage, which comes earlier than in other regions, attracting tourism by 'leaf peepers'. Springs are generally wet and cloudy. Average rainfall generally ranges from 1,000 to 1,500 mm (40 to 60 in) a year, although the northern parts of Vermont and Maine see slightly less, from 500 to 1,000 mm (20 to 40 in). Snowfall can often exceed 2,500 mm (100 in) annually. As a result, the mountains and ski resorts of Vermont and New Hampshire are popular destinations in the winter.
The lowest recorded temperature in New England was -50 °F (-46 °C), at Bloomfield, Vermont, on December 30, 1933. This was tied by Big Black River, Maine in 2009
Monday, March 30, 2009
Canada
Canada is a country occupying most of northern North America, extending from the Atlantic Ocean in the east to the Pacific Ocean in the west and northward into the Arctic Ocean. It is the world's second largest country by total area and shares land borders with the United States to the south and northwest.
The land occupied by Canada was inhabited for millennia by various groups of aboriginal people. Beginning in the late 15th century, British and French expeditions explored, and later settled along, the Atlantic coast. France ceded nearly all of its colonies in North America in 1763 after the Seven Years' War. In 1867, with the union of three British North American colonies through Confederation, Canada was formed as a federal dominion of four provinces. This began an accretion of additional provinces and territories and a process of increasing autonomy from the United Kingdom, highlighted by the Statute of Westminster in 1931 and culminating in the Canada Act in 1982, which severed the vestiges of legal dependence on the British parliament.
A federation comprising ten provinces and three territories, Canada is a parliamentary democracy and a constitutional monarchy, with Queen Elizabeth II as its head of state. It is a bilingual and multicultural country, with both English and French as official languages both at the federal level and in the province of New Brunswick. Technologically advanced and industrialized, Canada maintains a diversified economy that is heavily reliant upon its abundant natural resources and upon trade—particularly with the United States, with which Canada has had a long and complex relationship. It is a member of the G8, NATO, the Commonwealth of Nations, the Francophonie, and the United Nations.
Canada occupies a major northern portion of North America, sharing land borders with the contiguous United States to the south and the U.S. state of Alaska to the northwest, stretching from the Atlantic Ocean in the east to the Pacific Ocean in the west; to the north lies the Arctic Ocean. By total area (including its waters), Canada is the second largest country in the world—after Russia—and largest on the continent. By land area, it ranks fourth. Since 1925, Canada has claimed the portion of the Arctic between 60°W and 141°W longitude, but this claim is not universally recognized. The northernmost settlement in Canada (and the world) is Canadian Forces Station (CFS) Alert on the northern tip of Ellesmere Island—latitude 82.5°N—just 817 kilometres (450 nautical miles, 508 miles) from the North Pole. Canada has the longest coastline in the world: 243,000 kilometres (151,000 miles).
The population density, 3.5 inhabitants per square kilometre (9.1/sq mi), is among the lowest in the world. The most densely populated part of the country is the Quebec City-Windsor Corridor, along the Great Lakes and Saint Lawrence River in the southeast.
To the north of this region is the broad Canadian Shield, an area of rock scoured clean by the last ice age—thinly soiled, rich in minerals, and dotted with lakes and rivers. Canada by far has more lakes than any other country and has much of the world's fresh water.
In eastern Canada, most people live in large urban centres on the flat Saint Lawrence Lowlands. The Saint Lawrence River widens into the world's largest estuary before flowing into the Gulf of Saint Lawrence. The gulf is bounded by Newfoundland to the north and the Maritimes to the south. The Maritimes protrude eastward along the Appalachian Mountain range, from northern New England and the Gaspé Peninsula of Quebec. New Brunswick and Nova Scotia are divided by the Bay of Fundy, which experiences the world's largest tidal variations. Ontario and Hudson Bay dominate central Canada. West of Ontario, the broad, flat Canadian Prairies spread toward the Rocky Mountains, which separate them from British Columbia.
In northwestern Canada, the Mackenzie River flows from the Great Slave Lake to the Arctic Ocean. A tributary of a tributary of the Mackenzie is the South Nahanni River, which is home to Virginia Falls, a waterfall about twice as high as Niagara Falls.
Northern Canadian vegetation tapers from coniferous forests to tundra to the Arctic barrens in the far north. The northern Canadian mainland is ringed with a vast archipelago containing some of the world's largest islands.
Average winter and summer high temperatures across Canada vary depending on the location. Winters can be harsh in many regions of the country, particularly in the interior and Prairie provinces, which experience a continental climate, where daily average temperatures are near −15 °C (5 °F) but can drop below −40 °C (−40 °F) with severe wind chills. In noncoastal regions, snow can cover the ground almost six months of the year (more in the north). Coastal British Columbia is an exception; it enjoys a temperate climate, with a mild and rainy winter.
On the east and west coast, average high temperatures are generally in the low 20s °C (70s °F), while between the coasts, the average summer high temperature ranges from 25 to 30 °C (75 to 85 °F), with occasional extreme heat in some interior locations exceeding 40 °C (104 °F).[73][74] For a more complete description of climate across Canada, see Environment Canada's Website.
Canada is also geologically active, having many earthquakes and potentially active volcanoes, notably Mount Meager, Mount Garibaldi, Mount Cayley, and the Mount Edziza volcanic complex. The volcanic eruption of Tseax Cone in 1775 caused a catastrophic disaster, killing 2,000 Nisga'a people and the destruction of their village in the Nass River valley of northern British Columbia; the eruption produced a 22.5-kilometre (14.0 mi) lava flow, and according to legend of the Nisga'a people, it blocked the flow of the Nass River.
The land occupied by Canada was inhabited for millennia by various groups of aboriginal people. Beginning in the late 15th century, British and French expeditions explored, and later settled along, the Atlantic coast. France ceded nearly all of its colonies in North America in 1763 after the Seven Years' War. In 1867, with the union of three British North American colonies through Confederation, Canada was formed as a federal dominion of four provinces. This began an accretion of additional provinces and territories and a process of increasing autonomy from the United Kingdom, highlighted by the Statute of Westminster in 1931 and culminating in the Canada Act in 1982, which severed the vestiges of legal dependence on the British parliament.
A federation comprising ten provinces and three territories, Canada is a parliamentary democracy and a constitutional monarchy, with Queen Elizabeth II as its head of state. It is a bilingual and multicultural country, with both English and French as official languages both at the federal level and in the province of New Brunswick. Technologically advanced and industrialized, Canada maintains a diversified economy that is heavily reliant upon its abundant natural resources and upon trade—particularly with the United States, with which Canada has had a long and complex relationship. It is a member of the G8, NATO, the Commonwealth of Nations, the Francophonie, and the United Nations.
Canada occupies a major northern portion of North America, sharing land borders with the contiguous United States to the south and the U.S. state of Alaska to the northwest, stretching from the Atlantic Ocean in the east to the Pacific Ocean in the west; to the north lies the Arctic Ocean. By total area (including its waters), Canada is the second largest country in the world—after Russia—and largest on the continent. By land area, it ranks fourth. Since 1925, Canada has claimed the portion of the Arctic between 60°W and 141°W longitude, but this claim is not universally recognized. The northernmost settlement in Canada (and the world) is Canadian Forces Station (CFS) Alert on the northern tip of Ellesmere Island—latitude 82.5°N—just 817 kilometres (450 nautical miles, 508 miles) from the North Pole. Canada has the longest coastline in the world: 243,000 kilometres (151,000 miles).
The population density, 3.5 inhabitants per square kilometre (9.1/sq mi), is among the lowest in the world. The most densely populated part of the country is the Quebec City-Windsor Corridor, along the Great Lakes and Saint Lawrence River in the southeast.
To the north of this region is the broad Canadian Shield, an area of rock scoured clean by the last ice age—thinly soiled, rich in minerals, and dotted with lakes and rivers. Canada by far has more lakes than any other country and has much of the world's fresh water.
In eastern Canada, most people live in large urban centres on the flat Saint Lawrence Lowlands. The Saint Lawrence River widens into the world's largest estuary before flowing into the Gulf of Saint Lawrence. The gulf is bounded by Newfoundland to the north and the Maritimes to the south. The Maritimes protrude eastward along the Appalachian Mountain range, from northern New England and the Gaspé Peninsula of Quebec. New Brunswick and Nova Scotia are divided by the Bay of Fundy, which experiences the world's largest tidal variations. Ontario and Hudson Bay dominate central Canada. West of Ontario, the broad, flat Canadian Prairies spread toward the Rocky Mountains, which separate them from British Columbia.
In northwestern Canada, the Mackenzie River flows from the Great Slave Lake to the Arctic Ocean. A tributary of a tributary of the Mackenzie is the South Nahanni River, which is home to Virginia Falls, a waterfall about twice as high as Niagara Falls.
Northern Canadian vegetation tapers from coniferous forests to tundra to the Arctic barrens in the far north. The northern Canadian mainland is ringed with a vast archipelago containing some of the world's largest islands.
Average winter and summer high temperatures across Canada vary depending on the location. Winters can be harsh in many regions of the country, particularly in the interior and Prairie provinces, which experience a continental climate, where daily average temperatures are near −15 °C (5 °F) but can drop below −40 °C (−40 °F) with severe wind chills. In noncoastal regions, snow can cover the ground almost six months of the year (more in the north). Coastal British Columbia is an exception; it enjoys a temperate climate, with a mild and rainy winter.
On the east and west coast, average high temperatures are generally in the low 20s °C (70s °F), while between the coasts, the average summer high temperature ranges from 25 to 30 °C (75 to 85 °F), with occasional extreme heat in some interior locations exceeding 40 °C (104 °F).[73][74] For a more complete description of climate across Canada, see Environment Canada's Website.
Canada is also geologically active, having many earthquakes and potentially active volcanoes, notably Mount Meager, Mount Garibaldi, Mount Cayley, and the Mount Edziza volcanic complex. The volcanic eruption of Tseax Cone in 1775 caused a catastrophic disaster, killing 2,000 Nisga'a people and the destruction of their village in the Nass River valley of northern British Columbia; the eruption produced a 22.5-kilometre (14.0 mi) lava flow, and according to legend of the Nisga'a people, it blocked the flow of the Nass River.
Quebec
Québec is the capital of the Canadian province of Quebec and is located within the Capitale-Nationale region. It is the second most populous city in the province after Montreal, which is about 233 kilometres (145 mi) to the southwest. As of the 2006 Canadian Census, the city has a population of 491,142,[1] and the metropolitan area has a population of 715,515.
The narrowing of the Saint Lawrence River approximate to Quebec City and Lévis, on the opposite bank, provided the name given to the city, Kébec, an Algonquin word meaning "where the river narrows". Founded in 1608 by Samuel de Champlain, Quebec City is one of the oldest cities in North America. The ramparts surrounding Old Quebec (Vieux-Québec) are the only remaining fortified city walls in the Americas north of Mexico, and were declared a World Heritage Site by UNESCO in 1985 as the 'Historic District of Old Québec'.
Quebec City is internationally known for its Summer Festival, Winter Carnival, and the Château Frontenac, a hotel which dominates the city skyline. The National Assembly of Quebec (provincial parliament), the Musée national des beaux-arts du Québec (National Museum of Fine Arts), and the Musée de la civilisation (Museum of Civilization) are found within or near Vieux-Québec. Among the other attractions near the city are Montmorency Falls and the Basilica of Sainte-Anne-de-Beaupré in the town of Sainte-Anne-de-Beaupré.
Quebec City is located in the Saint Lawrence River valley, on the north bank of the Saint Lawrence River near its meeting with the St. Charles River. The region is low-lying and flat. The river valley has rich, arable soil, which makes this region the most fertile in the province. The Laurentian Mountains lie to the north of the city.
Upper Town lies on the top of Cap-Diamant (Cape Diamond) promontory. A high stone wall surrounds this portion of the city. The Plains of Abraham are located near the edge of the promontory. Lower Town is located at shore level, below Cap-Diamant.
Quebec City has a humid continental climate characterized by cold and snowy winters, warm and rather humid summers, and ample precipitation throughout the year. Quebec City is one of the snowiest cities in Canada and is almost guaranteed a white Christmas. The prolonged winter season and ample snowfall led to the idea of establishing the Quebec Winter Carnival. The transitional seasons, spring and autumn, are rather short, although autumn produces spectacular foliage colours. The summer is the sunniest, and paradoxically, the wettest time of year.
The narrowing of the Saint Lawrence River approximate to Quebec City and Lévis, on the opposite bank, provided the name given to the city, Kébec, an Algonquin word meaning "where the river narrows". Founded in 1608 by Samuel de Champlain, Quebec City is one of the oldest cities in North America. The ramparts surrounding Old Quebec (Vieux-Québec) are the only remaining fortified city walls in the Americas north of Mexico, and were declared a World Heritage Site by UNESCO in 1985 as the 'Historic District of Old Québec'.
Quebec City is internationally known for its Summer Festival, Winter Carnival, and the Château Frontenac, a hotel which dominates the city skyline. The National Assembly of Quebec (provincial parliament), the Musée national des beaux-arts du Québec (National Museum of Fine Arts), and the Musée de la civilisation (Museum of Civilization) are found within or near Vieux-Québec. Among the other attractions near the city are Montmorency Falls and the Basilica of Sainte-Anne-de-Beaupré in the town of Sainte-Anne-de-Beaupré.
Quebec City is located in the Saint Lawrence River valley, on the north bank of the Saint Lawrence River near its meeting with the St. Charles River. The region is low-lying and flat. The river valley has rich, arable soil, which makes this region the most fertile in the province. The Laurentian Mountains lie to the north of the city.
Upper Town lies on the top of Cap-Diamant (Cape Diamond) promontory. A high stone wall surrounds this portion of the city. The Plains of Abraham are located near the edge of the promontory. Lower Town is located at shore level, below Cap-Diamant.
Quebec City has a humid continental climate characterized by cold and snowy winters, warm and rather humid summers, and ample precipitation throughout the year. Quebec City is one of the snowiest cities in Canada and is almost guaranteed a white Christmas. The prolonged winter season and ample snowfall led to the idea of establishing the Quebec Winter Carnival. The transitional seasons, spring and autumn, are rather short, although autumn produces spectacular foliage colours. The summer is the sunniest, and paradoxically, the wettest time of year.
The St. Lawrence estuary was visited by many navigators (such as John Cabot and Jacques Cartier) and Basque fishermen soon after the discovery of America (or perhaps even before). But the first known European explorer to sail the inland part of the St. Lawrence was Jacques Cartier, during his second trip to Canada in 1535, with the help of Iroquoian chief Donnacona's two sons. As he arrived in the estuary on St. Lawrence's feast day, Cartier accordingly named it the Gulf of St. Lawrence.[4] The land along the river was inhabited at the time by the St. Lawrence Iroquoians. The St. Lawrence River is partly with the U.S. and as such is that country's sixth oldest surviving European place-name.
Until the early 1600s, the French used the name Rivière du Canada to designate the Saint Lawrence upstream to Montreal and the Ottawa River after Montreal. The Saint Lawrence River served as the main route for European exploration of the North American interior, first pioneered by French explorer Samuel de Champlain.
Because of the virtually impassable Lachine Rapids, the St. Lawrence was once continuously navigable only as far as Montreal. Opened in 1825, the Lachine Canal was the first to allow ships to pass the rapids. An extensive system of canals and locks, known as the Saint Lawrence Seaway, was officially opened on 26 June 1959 by Queen Elizabeth II (representing Canada) and President Dwight D. Eisenhower (representing the United States of America). The Seaway now permits ocean-going vessels to pass all the way to Lake Superior.
During World War II, the Battle of the St. Lawrence involved a number of submarine and anti-submarine actions throughout the lower St. Lawrence River and the entire Gulf of Saint Lawrence, Strait of Belle Isle and Cabot Strait from May to October 1942, September 1943, and again in October and November 1944. During this time, German U-boats sank a number of merchant marine ships and three Canadian warships.
In the late 1970s, the river was the subject of a successful ecological campaign (called "Save the River"), originally responding to planned development by the United States Army Corps of Engineers. The campaign was organized, among others, by Abbie Hoffman, then on the run under the pseudonym of Barry Freed.
Until the early 1600s, the French used the name Rivière du Canada to designate the Saint Lawrence upstream to Montreal and the Ottawa River after Montreal. The Saint Lawrence River served as the main route for European exploration of the North American interior, first pioneered by French explorer Samuel de Champlain.
Because of the virtually impassable Lachine Rapids, the St. Lawrence was once continuously navigable only as far as Montreal. Opened in 1825, the Lachine Canal was the first to allow ships to pass the rapids. An extensive system of canals and locks, known as the Saint Lawrence Seaway, was officially opened on 26 June 1959 by Queen Elizabeth II (representing Canada) and President Dwight D. Eisenhower (representing the United States of America). The Seaway now permits ocean-going vessels to pass all the way to Lake Superior.
During World War II, the Battle of the St. Lawrence involved a number of submarine and anti-submarine actions throughout the lower St. Lawrence River and the entire Gulf of Saint Lawrence, Strait of Belle Isle and Cabot Strait from May to October 1942, September 1943, and again in October and November 1944. During this time, German U-boats sank a number of merchant marine ships and three Canadian warships.
In the late 1970s, the river was the subject of a successful ecological campaign (called "Save the River"), originally responding to planned development by the United States Army Corps of Engineers. The campaign was organized, among others, by Abbie Hoffman, then on the run under the pseudonym of Barry Freed.
Thursday, March 26, 2009
Louisbourg
The town's name was given by French military forces who founded the Fortress of Louisbourg and its fortified seaport on the southwest part of the harbour, in honour of Louis XV. The French fortress was demolished after its final capture in 1758 and the site was abandoned by British forces in 1768.
Subsequent English settlers built a small fishing village across the harbour from the abandoned site of the fortress. The village grew slowly with additional Loyalists settlers in the 1780s. The harbour grew more accessible with the construction of the second Louisbourg Lighthouse in 1842 on the site of the original French lighthouse destroyed in 1758. A railway first reached Louisbourg in 1877, but it was poorly built and abandoned after a forest fire. However the arrival of Sydney and Louisburg Railway in 1894 brought heavy volumes of winter coal exports to Louisbourg Harbour's ice-free waters as a winter coal port. The harbour was used by the Canadian government ship Montmagny in 1912 to land bodies from the sinking of the RMS Titanic.
Incorporated in 1901, the Town of Louisbourg was disincorporated when all municipal units in Cape Breton County were merged into a single tier regional municipality in 1995.
Subsequent English settlers built a small fishing village across the harbour from the abandoned site of the fortress. The village grew slowly with additional Loyalists settlers in the 1780s. The harbour grew more accessible with the construction of the second Louisbourg Lighthouse in 1842 on the site of the original French lighthouse destroyed in 1758. A railway first reached Louisbourg in 1877, but it was poorly built and abandoned after a forest fire. However the arrival of Sydney and Louisburg Railway in 1894 brought heavy volumes of winter coal exports to Louisbourg Harbour's ice-free waters as a winter coal port. The harbour was used by the Canadian government ship Montmagny in 1912 to land bodies from the sinking of the RMS Titanic.
Incorporated in 1901, the Town of Louisbourg was disincorporated when all municipal units in Cape Breton County were merged into a single tier regional municipality in 1995.
Acadia was the name given to lands in a portion of the French colonial empire in northeastern North America that included parts of eastern Quebec, the Maritime provinces, and modern-day New England, stretching as far south as Philadelphia.
The actual specification by the French government for the territory refers to lands bordering the Atlantic coast, roughly between the 40th and 46th parallels. Later, the territory was divided into the British colonies which became Canadian provinces and American states.
Today, Acadia has been used to refer to regions of Atlantic Canada with French roots, language, and culture, primarily in New Brunswick, Nova Scotia, Maine and Prince Edward Island. In the abstract, Acadia refers to the existence of a French culture on Canada’s east coast.
Early European colonists, who would later become known as Acadians, were French subjects primarily from the Pleumartin to Poitiers in the Vienne département of west-central France. The first French settlement was established by Pierre Dugua, Sieur de Monts, Governor of Acadia, under the authority of King Henry IV, on Saint Croix Island in 1604. The following year, the settlement was moved across the Bay of Fundy to Port Royal after a difficult winter on the island and deaths from scurvy. In 1607 the colony received bad news: King Henry had revoked Sieur de Monts' royal fur monopoly, citing that the income was insufficient to justify supplying the colony further. Thus recalled, the last of the Acadians left Port Royal in August of 1607. Their allies, the native Mi'kmaq nation, kept careful watch over their possessions, though. When the former Lieutenant Governor, Jean de Biencourt de Poutrincourt et de Saint-Just, returned in 1610, he found Port Royal just as it was left.
The French took control of the Abenaki First Nations territory. In 1654, King Louis XIV of France appointed aristocrat Nicolas Denys as governor of large portions of Acadia and granted him the confiscated lands and the right to all its minerals.
The Netherlands asserted sovereignty over Acadia in 1674 after privateer Jurriaen Aernoutsz captured the forts at Pentagoet and Jemseg. Control over the region reverted to France when Aernoutsz's appointed administrator, John Rhoades, was captured by New England within a few months. The Dutch West India Company continued to assert a paper claim over Acadia until 1678, appointing Cornelius Van Steenwyk as its governor, although they never successfully recaptured actual control of the territory.
British colonists captured Acadia in the course of King William's War (1690–1697), but Britain returned it to France at the peace settlement. It was recaptured in the course of Queen Anne's War (1702–1713), and its conquest was confirmed in the Treaty of Utrecht (1713).
On June 23, 1713, the French residents of Acadia were given one year to declare allegiance to Britain or leave Nova Scotia.[citation needed] In the meantime, the French signalled their preparedness for future hostilities by beginning the construction of Fortress Louisbourg on Isle Royale, now Cape Breton Island. The British grew increasingly alarmed by the prospect of disloyalty in wartime of the Acadians now under their rule.
The actual specification by the French government for the territory refers to lands bordering the Atlantic coast, roughly between the 40th and 46th parallels. Later, the territory was divided into the British colonies which became Canadian provinces and American states.
Today, Acadia has been used to refer to regions of Atlantic Canada with French roots, language, and culture, primarily in New Brunswick, Nova Scotia, Maine and Prince Edward Island. In the abstract, Acadia refers to the existence of a French culture on Canada’s east coast.
Early European colonists, who would later become known as Acadians, were French subjects primarily from the Pleumartin to Poitiers in the Vienne département of west-central France. The first French settlement was established by Pierre Dugua, Sieur de Monts, Governor of Acadia, under the authority of King Henry IV, on Saint Croix Island in 1604. The following year, the settlement was moved across the Bay of Fundy to Port Royal after a difficult winter on the island and deaths from scurvy. In 1607 the colony received bad news: King Henry had revoked Sieur de Monts' royal fur monopoly, citing that the income was insufficient to justify supplying the colony further. Thus recalled, the last of the Acadians left Port Royal in August of 1607. Their allies, the native Mi'kmaq nation, kept careful watch over their possessions, though. When the former Lieutenant Governor, Jean de Biencourt de Poutrincourt et de Saint-Just, returned in 1610, he found Port Royal just as it was left.
The French took control of the Abenaki First Nations territory. In 1654, King Louis XIV of France appointed aristocrat Nicolas Denys as governor of large portions of Acadia and granted him the confiscated lands and the right to all its minerals.
The Netherlands asserted sovereignty over Acadia in 1674 after privateer Jurriaen Aernoutsz captured the forts at Pentagoet and Jemseg. Control over the region reverted to France when Aernoutsz's appointed administrator, John Rhoades, was captured by New England within a few months. The Dutch West India Company continued to assert a paper claim over Acadia until 1678, appointing Cornelius Van Steenwyk as its governor, although they never successfully recaptured actual control of the territory.
British colonists captured Acadia in the course of King William's War (1690–1697), but Britain returned it to France at the peace settlement. It was recaptured in the course of Queen Anne's War (1702–1713), and its conquest was confirmed in the Treaty of Utrecht (1713).
On June 23, 1713, the French residents of Acadia were given one year to declare allegiance to Britain or leave Nova Scotia.[citation needed] In the meantime, the French signalled their preparedness for future hostilities by beginning the construction of Fortress Louisbourg on Isle Royale, now Cape Breton Island. The British grew increasingly alarmed by the prospect of disloyalty in wartime of the Acadians now under their rule.
Halifax
The Halifax Peninsula is a community and planning area located in the urban core of Halifax Regional Municipality (HRM) in the province of Nova Scotia. Halifax Peninsula is home to Downtown Halifax, the financial and economic heart of the region, which was also the site of the original settlement and town of Halifax. It is also home to the majority of the area of Nova Scotia's Capital District.
The town of Halifax was founded by the British government under the direction of the Board of Trade and Plantations under the command of Governor Edward Cornwallis in 1749
After a protracted struggle between residents and the Executive Council, the City of Halifax was incorporated in 1841. In 1969, the city, which then covered the entire peninsula, annexed the Mainland Halifax area as well. On 1 April 1996, the government of Nova Scotia formed Halifax Regional Municipality, a single-tier regional government governing all of Halifax County. The City of Halifax became a provincial metropolitan area, and the HRM divided the former city into two separate community planning areas, Halifax Peninsula and Mainland Halifax, with separate community councils inside of the regional government.
Geographically, the Halifax Peninsula is a Canadian peninsula in central Nova Scotia.
The town of Halifax was founded by the British government under the direction of the Board of Trade and Plantations under the command of Governor Edward Cornwallis in 1749
After a protracted struggle between residents and the Executive Council, the City of Halifax was incorporated in 1841. In 1969, the city, which then covered the entire peninsula, annexed the Mainland Halifax area as well. On 1 April 1996, the government of Nova Scotia formed Halifax Regional Municipality, a single-tier regional government governing all of Halifax County. The City of Halifax became a provincial metropolitan area, and the HRM divided the former city into two separate community planning areas, Halifax Peninsula and Mainland Halifax, with separate community councils inside of the regional government.
Geographically, the Halifax Peninsula is a Canadian peninsula in central Nova Scotia.
Thursday, March 12, 2009
St Pierre & Miquelon Islands
The Territorial Collectivity of Saint Pierre and Miquelon is a group of small French islands in the North Atlantic Ocean, the main ones being Saint Pierre and Miquelon, south of Newfoundland, Canada. The islands are as close as 25 kilometres (16 mi) from Newfoundland.
The archipelago is the only remnant of the former colonial empire of New France that remains under French control.
The archipelago is the only remnant of the former colonial empire of New France that remains under French control.
The early settlement of St. Pierre and Miquelon, which were prized by Europeans for their rich fishing grounds, was characterized by periods of conflict between the French and English.
There is evidence of prehistoric inhabitation on the islands (most likely Beothuk). The European settlements on the islands are some of the oldest in America (with the Spanish and Portuguese settlements), dating from at least the early 16th century. At first the Basque fishermen only visited the islands seasonally during the fishing season, and by the mid 17th century there were permanent French residents on the islands.
At the end of the 17th and into the early 18th century, British attacks on the islands caused the French settlers to abandon the islands, and the British took possession for 50 years (from 1713 to 1763). The French took the islands back in 1763 under the Treaty of Paris (which ceded all of New France to Britain except for Saint Pierre and Miquelon) and settlers returned to live peacefully for 15 years.
French support of the American Revolution led to a British attack on the islands, and the deportation of the French settlers. Possession of Miquelon and St. Pierre passed back and forth between France and Great Britain for the next 38 years, as the islands suffered attacks by both countries, voluntary or forced removal of the island's residents, and upheaval associated with the French Revolution.
France finally took the islands back after Napoleon's second abdication in 1815, and there followed 70 years of prosperity for the French fishing industry and residents on Miquelon and St. Pierre. However, political and economic changes led to a slow decline of the fishing industry after the late 19th century.
In 1920, a 13-year economic boom took place on the islands beginning with the period of Prohibition in the United States, when Miquelon and St. Pierre were prominent bases for alcohol smuggling. This boom ended with the repeal of Prohibition in 1933, and the economy sank into depression.
During the Second World War, the governor, Gilbert de Bournat, was loyal to the Vichy regime; he had to negotiate financial arrangements with U.S. authorities to obtain loans guaranteed by the French treasury. At the same time, Canada was considering an invasion of Saint-Pierre and Miquelon. Several pretexts were put forward, notably radio broadcasts of Vichy propaganda. It was alleged that the radio was helping German U-Boats on the Grand Banks, though this was never proven. On the advice of his Prime Minister, William Lyon Mackenzie King, Governor General Alexander Cambridge, 1st Earl of Athlone, never authorised the implementation of the plans.
Under orders from de Gaulle, Admiral Émile Muselier organised the liberation of Saint-Pierre and Miquelon, without the consent and knowledge of the Canadian and U.S. authorities. On 24 December 1941, a Free French flotilla led by the submarine cruiser Surcouf took control of the islands without resistance. De Gaulle had a referendum organised, which was favourable to him, and Saint-Pierre and Miquelon thus became one of the first French territories to join Free France. The affair led to a lasting distrust between De Gaulle and Roosevelt
There is evidence of prehistoric inhabitation on the islands (most likely Beothuk). The European settlements on the islands are some of the oldest in America (with the Spanish and Portuguese settlements), dating from at least the early 16th century. At first the Basque fishermen only visited the islands seasonally during the fishing season, and by the mid 17th century there were permanent French residents on the islands.
At the end of the 17th and into the early 18th century, British attacks on the islands caused the French settlers to abandon the islands, and the British took possession for 50 years (from 1713 to 1763). The French took the islands back in 1763 under the Treaty of Paris (which ceded all of New France to Britain except for Saint Pierre and Miquelon) and settlers returned to live peacefully for 15 years.
French support of the American Revolution led to a British attack on the islands, and the deportation of the French settlers. Possession of Miquelon and St. Pierre passed back and forth between France and Great Britain for the next 38 years, as the islands suffered attacks by both countries, voluntary or forced removal of the island's residents, and upheaval associated with the French Revolution.
France finally took the islands back after Napoleon's second abdication in 1815, and there followed 70 years of prosperity for the French fishing industry and residents on Miquelon and St. Pierre. However, political and economic changes led to a slow decline of the fishing industry after the late 19th century.
In 1920, a 13-year economic boom took place on the islands beginning with the period of Prohibition in the United States, when Miquelon and St. Pierre were prominent bases for alcohol smuggling. This boom ended with the repeal of Prohibition in 1933, and the economy sank into depression.
During the Second World War, the governor, Gilbert de Bournat, was loyal to the Vichy regime; he had to negotiate financial arrangements with U.S. authorities to obtain loans guaranteed by the French treasury. At the same time, Canada was considering an invasion of Saint-Pierre and Miquelon. Several pretexts were put forward, notably radio broadcasts of Vichy propaganda. It was alleged that the radio was helping German U-Boats on the Grand Banks, though this was never proven. On the advice of his Prime Minister, William Lyon Mackenzie King, Governor General Alexander Cambridge, 1st Earl of Athlone, never authorised the implementation of the plans.
Under orders from de Gaulle, Admiral Émile Muselier organised the liberation of Saint-Pierre and Miquelon, without the consent and knowledge of the Canadian and U.S. authorities. On 24 December 1941, a Free French flotilla led by the submarine cruiser Surcouf took control of the islands without resistance. De Gaulle had a referendum organised, which was favourable to him, and Saint-Pierre and Miquelon thus became one of the first French territories to join Free France. The affair led to a lasting distrust between De Gaulle and Roosevelt
Saint Pierre and Miquelon are situated south of Newfoundland in the North Atlantic Ocean. Their distance north-south from Newfoundland is 60 kilometres (32 nmi). The islands are even closer to the long Burin Peninsula, which is situated just 25 kilometres (13 nmi) to the east. In addition, Green Island, which belongs to Newfoundland, is located about halfway between the southern part of Miquelon-Langlade and Newfoundland at 46°52′44″N 56°05′21″W, only 10 kilometres (6 mi) from both Langlade and St. Pierre.
Saint Pierre and Miquelon is an archipelago of eight islands, Saint-Pierre (26 km2 or 10 sq mi) and Miquelon-Langlade (total 216 km2 or 83 sq mi) being the major ones. Collectively the area of the islands is 242 km² (93.4 sq mi). The total coastline is 120 kilometres (75 mi) long.
The island of Saint-Pierre is surrounded to the south-east by smaller dependencies, Petit Colombier, Île aux Marins, Île aux Pigeons and Île aux Vainqueurs, and Grand Colombier to the north. Some of these have been previously inhabited at one time or another, but none are permanently inhabited anymore.
St. Pierre is separated from Miquelon by a 6 kilometres (3.2 nmi) strait with very fierce currents. Fishermen call this section of ocean "The Mouth of Hell". The waters around these islands are very treacherous, and there have been over 600 shipwrecks along the coasts of the islands.
The island(s) of Miquelon-Langlade consists of three formerly separate islands, Miquelon (110 km2 or 42 sq mi), Langlade (91 km2 or 35 sq mi) and Le Cap. In the 18th century an isthmus of sand formed naturally between Miquelon and Langlade. The isthmus was reinforced by hand with sand and quaternary deposits to what is now an 13 kilometres (8.1 mi) sand dune. Local legend says that the entire isthmus was built around the over 500 wrecks that took place in the area. While the ships using that channel between the islands began to get stranded there and certainly contributed to the formation of the isthmus, the legend may be exaggerated. What was originally the island Miquelon is now also called Grande Miquelon while Petite Miquelon refers to Langlade
The climate is very damp and windy, and winters are harsh and long. The spring and early summer are foggy and cool. Late summer and early fall are sunny.
Seals and other wildlife can be found in the Grand Barachois lagoon of Miquelon. Every spring, whales migrating to Greenland are visible off the coasts of Miquelon and St Pierre.
Trilobite fossils have been found on Langlade. There were a number of stone pillars off the island coasts called "L'anse aux Soldats" that have been eroded away and disappeared in the 1970s.
The island of Saint-Pierre is surrounded to the south-east by smaller dependencies, Petit Colombier, Île aux Marins, Île aux Pigeons and Île aux Vainqueurs, and Grand Colombier to the north. Some of these have been previously inhabited at one time or another, but none are permanently inhabited anymore.
St. Pierre is separated from Miquelon by a 6 kilometres (3.2 nmi) strait with very fierce currents. Fishermen call this section of ocean "The Mouth of Hell". The waters around these islands are very treacherous, and there have been over 600 shipwrecks along the coasts of the islands.
The island(s) of Miquelon-Langlade consists of three formerly separate islands, Miquelon (110 km2 or 42 sq mi), Langlade (91 km2 or 35 sq mi) and Le Cap. In the 18th century an isthmus of sand formed naturally between Miquelon and Langlade. The isthmus was reinforced by hand with sand and quaternary deposits to what is now an 13 kilometres (8.1 mi) sand dune. Local legend says that the entire isthmus was built around the over 500 wrecks that took place in the area. While the ships using that channel between the islands began to get stranded there and certainly contributed to the formation of the isthmus, the legend may be exaggerated. What was originally the island Miquelon is now also called Grande Miquelon while Petite Miquelon refers to Langlade
The climate is very damp and windy, and winters are harsh and long. The spring and early summer are foggy and cool. Late summer and early fall are sunny.
Seals and other wildlife can be found in the Grand Barachois lagoon of Miquelon. Every spring, whales migrating to Greenland are visible off the coasts of Miquelon and St Pierre.
Trilobite fossils have been found on Langlade. There were a number of stone pillars off the island coasts called "L'anse aux Soldats" that have been eroded away and disappeared in the 1970s.
Wednesday, March 11, 2009
Hudson Bay
Hudson Bay is a large (1.23 million km²), relatively shallow body of water in northeastern Canada. It is approximately 850 miles long and 650 miles wide. It drains a very large area that includes parts of Ontario, Quebec, Saskatchewan, Alberta, most of Manitoba, parts of North Dakota, South Dakota, Minnesota, and Montana, and the southeastern area of Nunavut. A smaller offshoot of the bay, James Bay, lies to the south. The International Hydrographic Organization lists Hudson Bay as part of the Arctic Ocean. On the east it is connected with the Atlantic Ocean by Hudson Strait, and on the north with the rest of the Arctic Ocean by Foxe Basin (which is not considered part of the bay) and Fury and Hecla Strait. Geographic coordinates: 78° to 95° W, 51° to 70° N.
The Eastern Cree name for Hudson and James Bay is Wînipekw or Wînipâkw , meaning muddy or brackish water. Lake Winnipeg is similarly named by the local Cree, as is the location for the City of Winnipeg.
Hudson Bay was the growth centre for the main ice sheet that covered northern North America during the last Ice Age. The whole region has very low year round average temperatures. (The average annual temperature for Churchill at 59°N is -5°C; by comparison Arkhangelsk at 64°N in a similar cold continental position in northern Russia has an average of 2°C.) Water temperature peaks at 8°-9°C on the western side of the bay in late summer. It is largely frozen over from mid-December to mid-June when it usually clears from its eastern end westwards and southwards. A steady increase in regional temperatures over the last 100 years has been reflected in a lengthening of the ice-free period which was as short as four months in the late 17th century.
Hudson Bay has a salinity that is lower than the world ocean on average. This is caused mainly by the low rate of evaporation (the bay is ice-covered for much of the year), the large volume of terrestrial runoff entering the bay (about 700 km³ annually; the Hudson Bay watershed covers much of Canada, with many rivers and streams discharging into the bay), and the limited connection with the larger Atlantic Ocean (and its higher salinity). The annual freeze-up and thaw of sea ice significantly alters the salinity of the surface layer, representing roughly three years' worth of river inflow.
The western shores of the bay are a lowland known as the "Hudson Bay Lowlands" which covers 324,000 km². The area is drained by a large number of rivers and has formed a characteristic vegetation known as muskeg. Much of the landform has been shaped by the actions of glaciers and the shrinkage of the bay over long periods of time. Signs of numerous former beachfronts can be seen far inland from the current shore. A large portion of the lowlands in the province of Ontario is part of the Polar Bear Provincial Park, and a similar portion of the lowlands in Manitoba is contained in Wapusk National Park, the latter location being a significant Polar Bear maternity denning area.
In contrast, most of the eastern shores (the Quebec portion) form the western edge of the Canadian Shield in Quebec. The area is rocky and hilly. Its vegetation is typically boreal forest, and to the north, tundra.
Measured by shoreline, Hudson Bay is the largest bay in the world (the largest in area being the Bay of Bengal).
There are many islands in Hudson Bay, mostly near the eastern coast. All are part of the territory Nunavut. One group of islands, with a reputable name, is the Belcher Islands. Another group includes the Ottawa Islands.
The Eastern Cree name for Hudson and James Bay is Wînipekw or Wînipâkw , meaning muddy or brackish water. Lake Winnipeg is similarly named by the local Cree, as is the location for the City of Winnipeg.
Hudson Bay was the growth centre for the main ice sheet that covered northern North America during the last Ice Age. The whole region has very low year round average temperatures. (The average annual temperature for Churchill at 59°N is -5°C; by comparison Arkhangelsk at 64°N in a similar cold continental position in northern Russia has an average of 2°C.) Water temperature peaks at 8°-9°C on the western side of the bay in late summer. It is largely frozen over from mid-December to mid-June when it usually clears from its eastern end westwards and southwards. A steady increase in regional temperatures over the last 100 years has been reflected in a lengthening of the ice-free period which was as short as four months in the late 17th century.
Hudson Bay has a salinity that is lower than the world ocean on average. This is caused mainly by the low rate of evaporation (the bay is ice-covered for much of the year), the large volume of terrestrial runoff entering the bay (about 700 km³ annually; the Hudson Bay watershed covers much of Canada, with many rivers and streams discharging into the bay), and the limited connection with the larger Atlantic Ocean (and its higher salinity). The annual freeze-up and thaw of sea ice significantly alters the salinity of the surface layer, representing roughly three years' worth of river inflow.
The western shores of the bay are a lowland known as the "Hudson Bay Lowlands" which covers 324,000 km². The area is drained by a large number of rivers and has formed a characteristic vegetation known as muskeg. Much of the landform has been shaped by the actions of glaciers and the shrinkage of the bay over long periods of time. Signs of numerous former beachfronts can be seen far inland from the current shore. A large portion of the lowlands in the province of Ontario is part of the Polar Bear Provincial Park, and a similar portion of the lowlands in Manitoba is contained in Wapusk National Park, the latter location being a significant Polar Bear maternity denning area.
In contrast, most of the eastern shores (the Quebec portion) form the western edge of the Canadian Shield in Quebec. The area is rocky and hilly. Its vegetation is typically boreal forest, and to the north, tundra.
Measured by shoreline, Hudson Bay is the largest bay in the world (the largest in area being the Bay of Bengal).
There are many islands in Hudson Bay, mostly near the eastern coast. All are part of the territory Nunavut. One group of islands, with a reputable name, is the Belcher Islands. Another group includes the Ottawa Islands.
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