Saturday, August 29, 2009

Carte de l'Amerique et des Mers Voisines

Mississippi River

The Mississippi River is the second-longest river in the United States, with a length of 2,320 miles (3,730 km)[4] from its source in Lake Itasca in Minnesota to its mouth in the Gulf of Mexico.
The Mississippi River is part of the Missouri-Mississippi river system, which is the largest river system in North America and among the largest in the world: by length (3,900 miles (6,300 km)), it is the fourth longest, and by its average discharge of 572,000 cu ft/s (16,200 m³/s), it is the tenth largest.
The name Mississippi is derived from the Ojibwe word misi-ziibi ("Great River") or gichi-ziibi ("Big River").

The Missouri River flows from the confluence of the Jefferson, Madison and Gallatin Rivers and is the longest river in the United States.[3] Taken together, the Jefferson, the Missouri, and the Mississippi form the longest river system in North America. If measured from the source of the Jefferson at Brower's Spring, to the Gulf of Mexico, the length of the Mississippi-Missouri-Jefferson combination is approximately 3,900 miles (6,300 km), making the combination the 4th longest river in the world. The uppermost 207 miles (333 km) of this combined river are called the Jefferson, the lowest 1,352 miles (2,176 km) are part of the Mississippi, and the intervening 2,341 miles (3,767 km) are called the Missouri.
The Arkansas River is the second longest tributary of the Mississippi River. Measured by water volume, the largest of all Mississippi tributaries is the Ohio River.
The widest point of the Mississippi River is Lake Winnibigoshish, near Grand Rapids, Minnesota, at over 7 miles (11 km) across. Also of note is Lake Onalaska, near La Crosse, Wisconsin, where the river is over 4 miles (6.4 km) wide (created by Lock and Dam No. 7) and Lake Pepin at more than 2 miles (3.2 km) wide.[5] However, the first two areas are lakes or reservoirs rather than free flowing water. In other areas where the Mississippi is a flowing river (other than Lake Pepin), it exceeds 1 mile (1.6 km) in width in several places in its lower course.
Beginning with its source at Lake Itasca to Saint Louis Missouri, the Mississippi's flow is moderated by 43 dams. Fourteen of these dams are located above Minneapolis Minnesota in the Headwaters region and serve multiple purposes including power generation and recreation. The remaining 29 dams beginning in downtown Minneapolis all contain locks and were constructed to permit commercial navigation of the upper river. Taken as a whole these 43 dams significantly shape the geography and influence the ecology of the upper river. Beginning just below Saint Paul Minnesota and continuing throughout the upper and lower river, the Mississippi is further controlled by thousands of wing dikes that moderate the river's flow in order to maintain an open navigation channel and prevent the river from eroding its banks.
The Mississippi River runs through 10 states and was used to define portions of these states' borders. The middle of the riverbed at the time the borders were established was the line to define the borders between states. The river has since shifted, but the state borders of Wisconsin, Iowa, Illinois, Missouri, Kentucky, Arkansas, Tennessee, and Mississippi have not changed; they still follow the former bed of the Mississippi River as of their establishment.
The river is divided into the upper Mississippi, from its source south to the Ohio River, and the lower Mississippi, from the Ohio to its mouth near New Orleans.

The source of the Mississippi River is Lake Itasca, 1,475 feet (450 m) above sea level in Itasca State Park located in Clearwater County, Minnesota. The name "Itasca" is a combination of the last four letters of the Latin word for truth and the first two letters of the Latin word for head.
The uppermost lock and dam on the Mississippi River is the Upper St. Anthony Falls Lock and Dam in Minneapolis. Above the dam, the river's elevation is 799 feet (244 m). Below the dam, the river's elevation is 750 feet (230 m). This 49-foot (15 m) drop is the largest of all the Mississippi River locks and dams. The origin of the dramatic drop is a waterfall preserved adjacent to the lock under an apron of concrete. Saint Anthony Falls is the only true waterfall on the entire Mississippi River. The water elevation continues to drop steeply as it passes through the gorge carved by the waterfall. By the time the river reaches Saint Paul, Minnesota, below Lock and Dam #1, it has dropped more than half its original elevation and is 687 feet (209 m) above sea level. From St. Paul to St. Louis Missouri the river elevation falls much more slowly and is controlled and managed as a series of pools created by 26 locks and dams.[8] From St. Louis to the Ohio River confluence the Mississippi free falls a total of 220 feet (67 m) over a distance of 180 miles (290 km) for an average rate of 1.2 feet per mile (23 cm/km). At the Ohio River confluence the Mississippi is 315 feet (96 m) above sea level.

A clear channel is needed for the barges and other vessels that make the main stem Mississippi one of the great commercial waterways of the world. The task of maintaining a navigation channel is the responsibility of the United States Army Corps of Engineers, which was established in 1802. Earlier projects began as early as 1829 to remove snags, close off secondary channels and excavate rocks and sandbars.
Steamboats entered trade in the 1820s, so the period 1830 – 1850 became the golden age of steamboats. As there were few roads or rails in the lands of the Louisiana Purchase, river traffic was an ideal solution. Cotton, timber and food came down the river, as did Appalachia coal. The port of New Orleans boomed as it was the trans-shipment point to deep sea ocean vessels. As a result, the image of the twin stacked, wedding cake Mississippi steamer entered into American mythology. Steamers worked the entire route from the trickles of Montana, to the Ohio river; down the Missouri and Tennessee. To the main channel of the Mississippi. Only the arrival of the railroads in the 1880s did steamboat traffic diminish. Steamboats remained a feature until the 1920s. Most have been superseded by pusher tugs. A few survive as icons—the Delta Queen and the River Queen for instance.
A series of 29 locks and dams on the upper Mississippi, most of which were built in the 1930s, is designed primarily to maintain a 9 feet (2.7 m) deep channel for commercial barge traffic. The lakes formed are also used for recreational boating and fishing. The dams make the river deeper and wider but do not stop it. No flood control is intended. During periods of high flow, the gates, some of which are submersible, are completely opened and the dams simply cease to function. Below St. Louis, the Mississippi is relatively free-flowing, although it is constrained by numerous levees and directed by numerous wing dams.

Embouchure du Fleuve St Louis ou Mississipi

Suite du Cours du Fleuve St Louis

Cours du Fleuve St Louis

New Orleans

New Orleans is a major U.S. port and the largest city in Louisiana. New Orleans is the center of the New Orleans Metropolitan Area, the largest metro area in the state.
New Orleans is located in southeastern Louisiana, straddling the Mississippi River. It is coextensive with Orleans Parish, meaning that the boundaries of the city and the parish are the same. It is bounded by the parishes of St. Tammany (north), St. Bernard (east), Plaquemines (south) and Jefferson (south and west). Lake Pontchartrain, part of which is included in the city limits, lies to the north and Lake Borgne lies to the east.
The city is named after Philippe II, Duc d'Orléans, Regent of France, and is well known for its multicultural and multilingual heritage cuisine, architecture, music (particularly as the birthplace of jazz), and its annual Mardi Gras and other celebrations and festivals. The city is often referred to as the "most unique" city in America.

La Nouvelle-Orléans (New Orleans) was founded May 7, 1718, by the French Mississippi Company, under the direction of Jean-Baptiste Le Moyne de Bienville, on land inhabited by the Chitimacha. It was named for Philippe II, Duke of Orléans, who was Regent of France at the time. His title came from the French city of Orléans. The French colony was ceded to the Spanish Empire in the Treaty of Paris (1763) and remained under Spanish control until 1801, when it reverted to French control. All of the surviving 18th century architecture of the Vieux Carré (French Quarter) dates from this Spanish period. Napoleon sold the territory to the United States in the Louisiana Purchase in 1803. Thereafter, the city grew rapidly with influxes of Americans, French, Creoles, Irish, Germans and Africans. Major commodity crops of sugar and cotton were cultivated with slave labor on large plantations outside the city.
The Haitian Revolution of 1804 established the second republic in the Western Hemisphere and the first led by blacks. Haitian refugees, both white and free people of color (affranchis or gens de couleur libres), arrived in New Orleans, often bringing slaves with them. While Governor Claiborne and other officials wanted to keep out more free black men, French Creoles wanted to increase the French-speaking population. As more refugees were allowed in Louisiana, Haitian émigrés who had gone to Cuba also arrived. Nearly 90 percent of the new immigrants settled in New Orleans. The 1809 migration brought 2,731 whites; 3,102 free persons of African descent; and 3,226 enslaved refugees to the city, doubling its French-speaking population.
During the last campaign of the War of 1812, the British sent their best forces to conquer New Orleans. Despite great challenges, the young Andrew Jackson successfully cobbled together a motley crew of local militia, free persons of color, United States regulars, Kentucky riflemen and area pirates to decisively defeat the British troops, led by Sir Edward Pakenham, in the Battle of New Orleans on January 8, 1815.
As a principal port, New Orleans played a major role during the antebellum era in the Atlantic slave trade. Its port handled huge quantities of commodities for export from the interior and imported goods from other countries, which were warehoused and then transferred in New Orleans to smaller vessels and distributed the length and breadth of the vast Mississippi River watershed. The river in front of the city was filled with steamboats, flatboats, and sailing ships. Despite its dealings with the slave trade, New Orleans at the same time had the largest and most prosperous community of free persons of color in the nation, who were often educated and middle-class property owners.
The population of the city doubled in the 1830s and by 1840, New Orleans had become the wealthiest and third-most populous city in the nation. Dwarfing in population the other cities in the antebellum South, New Orleans had, consequently, the largest slave market. Two-thirds of the more than one million slaves brought to the Deep South arrived via the forced migration of the internal slave trade. The money generated by sales of slaves in the Upper South has been estimated at fifteen percent of the value of the staple crop economy. The slaves represented half a billion dollars in property, and an ancillary economy grew up around the trade in slaves — for transportation, housing and clothing, fees, etc., estimated at 13.5 percent of the price per person. All of this amounted to tens of billions of dollars during the antebellum period, with New Orleans as a prime beneficiary.
The Union captured New Orleans early in the American Civil War, sparing the city the destruction suffered by many other cities of the American South.
During Reconstruction New Orleans was within the Fifth Military District of the United States. Louisiana was readmitted to the Union in 1868, and its Constitution of 1868 granted universal manhood suffrage. Due to the state's large African American population, many blacks held public office. In 1872, then-lieutenant governor P.B.S. Pinchback succeeded Henry Clay Warmouth as governor of Louisiana, becoming the first non-white governor of a U.S. state, and the last African American to lead a U.S. state until Douglas Wilder's election in Virginia, 117 years later. In New Orleans, Reconstruction was marked by the horrible Mechanics Institute race riot (1866), but also by the successful operation of a fully racially-integrated public school system. Meanwhile, the city's economy struggled to right itself after practically grinding to a halt upon the declaration of war in 1861, the nationwide Panic of 1873 conspiring to severely retard economic recovery.
Reconstruction ended in Louisiana in 1877, and white southern Democrats, the so-called Redeemers, succeeded in stripping power from the Republican Party and gradually circumscribing the only recently-acquired civil rights of African Americans. In New Orleans, the public schools were resegregated, and would remain so until 1960.
New Orleans' large community of well-educated, often French-speaking free persons of color (gens de couleur libres), who had not been enslaved prior to the Civil War, sought to fight back against the incipient forces of Jim Crow. As part of their ongoing campaign, they recruited one of their own, Homer Plessy to test whether Louisiana's newly-enacted Separate Car Act was constitutional. Plessy duly boarded a commuter train departing New Orleans for Covington, Louisiana, sat in the car reserved for whites only and was arrested. The case spawned by this incident, Plessy v. Ferguson, was heard by the U.S. Supreme Court in 1896. The court, in finding that "separate but equal" accommodations were constitutional, strengthened by effectively consecrating the already-underway Jim Crow movement. The ruling was a key development in the nadir of race relations reached during this period.

Plan de la Nouvelle Orleans

La Louisiane et Pays Voisins

Plan de la Baye de Pensacola

Florida

Florida is a state located in the southeastern region of the United States, bordering Alabama to the northwest and Georgia to the north. It was the 27th state admitted to the United States. Much of the land mass of the state is a large peninsula with the Gulf of Mexico to the west, and the Atlantic Ocean to the east.
It is nicknamed the "Sunshine State" because of its generally warm climate—subtropical in many regions of the state, with true tropical climate in the far southern portions near Key West. The state has a few large urban areas, a number of smaller industrial cities, and many small towns. The United States Census Bureau estimates that the state population was 18,328,340 in 2008, ranking Florida as the fourth most populous state in the U.S. Tallahassee is the state capital and Miami is the largest metro area. Residents of Florida are properly known as "Floridians".

Much of the state of Florida is situated on a peninsula between the Gulf of Mexico, the Atlantic Ocean, and the Straits of Florida. Spanning two time zones, It extends to the northwest into a panhandle, extending along the northern Gulf of Mexico. It is bordered on the north by the states of Georgia and Alabama, and on the west, at the end of the panhandle, by Alabama. It is near several Caribbean countries, particularly The Bahamas and Cuba. Florida's extensive coastline made it a perceived target during World War II, so the government built airstrips throughout the state; today, approximately 400 airports are still in service. According to the National Drug Intelligence Center, Florida has 131 public airports, and more than 700 private airports, airstrips, heliports, and seaplane bases. Florida is one of the largest states east of the Mississippi River, and only Alaska and Michigan are larger in water area.

The Florida peninsula is a porous plateau of karst limestone sitting atop bedrock. Extended systems of underwater caves, sinkholes and springs are found throughout the state and supply most of the water used by residents. The limestone is topped with sandy soils deposited as ancient beaches over millions of years as global sea levels rose and fell. During the last glacial period, lower sea levels and a drier climate revealed a much wider peninsula, largely savanna. The Everglades, an enormously wide, very slow-flowing river encompasses the southern tip of the peninsula.
Because Florida is not located near any tectonic plate boundaries, earthquakes are very rare, but not totally unknown. In January, 1879, a shock occurred near St. Augustine. There were reports of heavy shaking that knocked plaster from walls and articles from shelves. Similar effects were noted at Daytona Beach 50 miles (80 km) south. The tremor was felt as far south as Tampa and as far north as Savannah, Georgia. In January 1880, Cuba was the center of two strong earthquakes that sent severe shock waves through the city of Key West, Florida. Another earthquake centered outside Florida was the 1886 Charleston earthquake. The shock was felt throughout northern Florida, ringing church bells at St. Augustine and severely jolting other towns along that section of Florida's east coast. Jacksonville residents felt many of the strong aftershocks that occurred in September, October, and November 1886.

At 345 feet (105 m) above mean sea level, Britton Hill is the highest point in Florida and the lowest highpoint of any U.S. state. Much of the state south of Orlando is low-lying and fairly level; however, some places, such as Clearwater, feature vistas that rise 50 to 100 feet (15 – 30 m) above the water. Much of Central and North Florida, typically 25 miles (40 km) or more away from the coastline, features rolling hills with elevations ranging from 100 to 250 feet (30 – 76 m). The highest point in peninsular Florida, Sugarloaf Mountain, is a 312-foot (95 m) peak in Lake County.

The climate of Florida is tempered somewhat by the fact that no part of the state is very distant from the ocean. North of lake Okeechobee, the prevalent climate is humid subtropical climate, while south of the lake has a true tropical climate.[24] High temperatures in the state seldom exceed 100 °F (38 °C), with much of Florida commonly seeing a high summer temperature of 90s °F (32+ °C).
During late autumn and winter months, Florida has experienced occasional cold fronts that can bring high winds and relatively cooler temperatures for the entire state, with high temperatures that could remain into the 40s and 50s (4–15 °C) and lows of 30s and 40s (0–10 °C) for few days.

The hottest temperature ever recorded in the Florida was 109 °F (43 °C), set on June 29, 1931 in Monticello. The coldest was–2 °F (−19 °C), on February 13, 1899, just 25 miles (40 km) away, in Tallahassee. Mean high temperatures for late July are primarily in the low 90s Fahrenheit (32–35 °C). Mean low temperatures for late January range from the low 40s Fahrenheit (4–7 °C) in northern Florida to the mid-50s (≈13 °C) in southern Florida.
The seasons in Florida are determined more by precipitation than by temperature, with the hot, wet springs and summers making up the wet season, and mild to cool, and the relatively dry winters and autumns, making the dry season.
The Florida Keys, because they are completely surrounded by water, have a tropical climate with lesser variability in temperatures. At Key West, temperatures rarely exceed 90 °F (32 °C) in the summer or fall below 60 °F (16 °C) in the winter, and frost has never been reported in the Keys.
Florida's nickname is the "Sunshine State", but severe weather is a common occurrence in the state. Central Florida is known as the lightning capital of the United States, as it experiences more lightning strikes than anywhere else in the country. Florida has the highest average precipitation of any state, in large part because afternoon thunderstorms are common in most of the state from late spring until early autumn. A fair day may be interrupted with a storm, only to return to sunshine an hour or so later. These thunderstorms, caused by overland collisions of moist masses of air from the Gulf of Mexico and Atlantic Ocean[citation needed], pop up in the early afternoon and can bring heavy downpours, high winds, and sometimes tornadoes. Florida leads the United States in tornadoes per square mile (when including waterspouts) but they do not typically reach the intensity of those in the Midwest and Great Plains. Hail often accompanies the most severe thunderstorms.
Snow in Florida is a rare occurrence. During the Great Blizzard of 1899, Florida experienced blizzard conditions; the Tampa Bay area had "gulf-effect" snow, similar to lake-effect snow in the Great Lakes region. During the 1899 blizzard was the only time the temperature in Florida is known to have fallen below 0 degrees Fahrenheit (−18 °C). The most widespread snowfall in Florida history occurred on January 19, 1977, when snow fell over much of the state, as far south as Homestead. Snow flurries fell on Miami Beach for the only time in recorded history. A hard freeze in 2003 brought "ocean-effect" snow flurries to the Atlantic coast as far south as Cape Canaveral. The 1993 Superstorm brought blizzard conditions to the panhandle, while heavy rain and tornadoes beset the peninsula. The storm is believed to have been similar in composition to a hurricane, some Gulf coast regions even seeing storm surges of six feet or more.

Hurricanes pose a severe threat during hurricane season, which lasts from June 1 to November 30, although some storms have been known to form out of season. Florida is the most hurricane-prone US state, with subtropical or tropical water on a lengthy coastline. From 1851 to 2006, Florida has been struck by 114 hurricanes, 37 of them major—category 3 and above. It is rare for a hurricane season to pass without any impact in the state by at least a tropical storm. For storms, category 4 or higher, 83% have either hit Florida or Texas. August to October is the most likely period for a hurricane in Florida.
In 2004, Florida was hit by a record four hurricanes. Hurricanes Charley (August 13), Frances (September 4–5), Ivan (September 16), and Jeanne (September 25–26) cumulatively cost the state's economy US$42 billion. In 2005, Hurricane Dennis (July 10) became the fifth storm to strike Florida within eleven months. Later, Hurricane Katrina (August 25) passed through South Florida and Hurricane Rita (September 20) swept through the Florida Keys. Hurricane Wilma (October 24) made landfall near Cape Romano, just south of Marco Island, finishing another very active hurricane season.
Florida was the site of the second costliest weather disaster in U.S. history, Hurricane Andrew, which caused more than US$25 billion in damage when it struck on August 24, 1992. In a long list of other infamous hurricane strikes are the 1926 Miami hurricane, the 1928 Okeechobee hurricane, the Labor Day Hurricane of 1935, Hurricane Donna in 1960, and Hurricane Opal in 1995. Recent research suggests the storms are part of a natural cycle and not a result of global warming.

Carte de la Coste de la Floride

Plan du Port de St Augustin

Carte de la Nouvelle Georgie

Port et Ville de Charle-Town

South Carolina

The colony of Carolina was settled by English settlers, mostly from Barbados, sent by the Lords Proprietors in 1670, followed by French Huguenots. The original Carolina proprietors were aware of the threat posed by the French and Spanish presence to the south, whose Roman Catholic monarchies were enemies of England and English values. They needed to act swiftly to attract settlers. Therefore, they were one of the first colonies to grant liberty of religious practice in order to attract settlers who were Baptists, Quakers, Huguenots and Presbyterians. Jewish immigration was specifically encouraged in the Fundamental Constitutions, since Jews were seen as reliable citizens. The Jewish immigrants were fleeing the Spanish Inquisition, which was being perpetrated in the Spanish colonies in the New World. Most immigrants in the colonial period were African slaves, who constituted a majority of the colony's population throughout the period. The Carolina upcountry was settled largely by Scots-Irish migrants from Pennsylvania and Virginia, following the Great Wagon Road.
Between 1715–1717 the Yamasee War, between colonial South Carolina and several Indian tribes, was one of America’s bloodiest Indian Wars, which for over a year seriously threatened the continued existence of South Carolina. The impact of the wars included dissatisfaction with the Proprietors who had the right to govern the colony. As a result, The Carolinas was split, and South Carolina became a royal colony in 1719.
The colony declared its independence from Great Britain and set up its own government on March 15, 1776, becoming the first colony to do so. On February 5, 1778, South Carolina became the first state to ratify the document which created the "United States of America" as an entity — the Articles of Confederation. The current United States Constitution was proposed for adoption by the States on September 17, 1787, and South Carolina was the 8th state to ratify it, on May 23, 1788.
The American Revolution caused a shock to slavery in the South. Tens of thousands of slaves fought with the British and thousands left with them; others secured their freedom by escaping. Estimates are that 25,000 slaves (30% of those in South Carolina) fled, migrated or died during the disruption of the war.


This historic home is at "The Battery," a neighborhood/park area at the Downtown Historic District of Charleston - a well-known historical city in South Carolina. "The Battery" is also known as White Point Gardens.
South Carolina politics between 1783 and 1795 were marred by rivalry between a Federalist Elite supporting the central government in Philadelphia and a large proportion of common people, often members of 'Republican Societies', supporting the Republican-Democrats headed by Jefferson and Madison who wanted more democracy in the US especially in South Carolina. Most people also supported the onset of the French Revolution (1789-1795) as anti-British feelings were still running high after the devastation of the war during the American Revolution and Charleston was the most French-influenced city in the USA after New Orleans. Leading South Carolina figures such as Pinckney and Governor Moultrie backed with money and actions the plans of the French to further their political, strategic, and commercial goals in North America. This pro-French stance and attitude of South Carolina ended soon due to the XYZ Affair.
Antebellum, South Carolina did more to advance nullification and secession than any other Southern state. On December 20, 1860, after it was clear Lincoln would be the next president, South Carolina became the first state to declare its secession from the Union. On April 12, 1861, Confederate batteries began shelling Fort Sumter in Charleston Harbor, and the American Civil War began. Charleston was effectively blockaded and the Union Navy seized the Sea Islands, driving off the plantation owners and setting up an experiment in freedom for the ex-slaves. South Carolina troops participated in major Confederate campaigns, but no major battles were fought inland. General William Tecumseh Sherman marched through the state in early 1865, destroying numerous plantations, and captured the state capital of Columbia on February 17. Fires began that night and by next morning, most of the central city was destroyed.


Coastal towns and cities often have hurricane resistant Live oaks overarching the streets in historic neighborhoods, such as these on East Bay Street, Georgetown.
After the war, South Carolina was restored to the United States during Reconstruction. Under presidential Reconstruction (1865-66), freedmen (former slaves) were given limited rights. Under Radical reconstruction (1867-1877), a Republican coalition of freedmen, carpetbaggers and scalawags was in control, supported by Union army forces. The withdrawal of Union soldiers as part of the Compromise of 1877 ended Reconstruction. Whites used paramilitary groups such as the Red Shirts to intimidate and terrorize black voters, and regained political control under conservative white "Redeemers" and pro-business Bourbon Democrats.
The state became a hotbed of racial and economic tensions during the Populist and Agrarian movements of the 1890s. With the new conservative constitution of 1895, almost all blacks and many poor whites were effectively disfranchised by new requirements for poll taxes and literacy tests. By 1896, only 5,500 black voters remained on the registration rolls.[12] The 1900 census demonstrated the extent of disfranchisement: African Americans comprised more than 58% of the state's population, with a total of 782,509 citizens essentially without any political representation.[13] "Pitchfork Ben Tillman" controlled state politics from the 1890s to 1910 with a base among poor white farmers.

La Caroline

Virginia

The Commonwealth of Virginia is an American state on the Atlantic Coast of the Southern United States. Virginia is known as the "Old Dominion" and sometimes as "Mother of Presidents", because it is the birthplace of eight U.S. presidents. The geography and climate of the state are shaped by the Blue Ridge Mountains and the Chesapeake Bay, which are home to much of the state's flora and fauna. The capital of the Commonwealth is Richmond, Virginia Beach is the most populous city, and Fairfax County is the most populous political subdivision. The state population is nearly eight million.
State history begins with the founding of the Virginia Colony in 1607 by the Virginia Company of London as the first permanent New World English colony. Land from displaced Native American tribes, including the Powhatan, and slavery each played significant roles in Virginia's early politics and plantation economy. Virginia was one of the Thirteen Colonies in the American Revolution and joined the Confederacy in the American Civil War, during which the state of West Virginia separated. Although traditionally conservative and historically part of the South, both major national parties are competitive in modern Virginia.
The state government, home to the oldest legislature in the Americas, has been repeatedly ranked most effective among U.S. states. It is unique in how it treats cities and counties equally, maintains most of the state's roads, and prohibits its Governors from serving consecutive terms. Virginia's economy has many sectors: agriculture in places like the Shenandoah Valley; federal agencies in Northern Virginia, including the Pentagon and CIA; and military facilities in Hampton Roads, home to the region's main seaport. The growth of the media and technology sectors have made computer chips the state's leading export, with the industry based on the strength of Virginia's public schools and universities. Virginia does not have a major professional sports franchise, but is home to several prominent collegiate sports programs.

The Chesapeake Bay separates most of the contiguous portion of the Commonwealth from the two-county peninsula of Virginia's Eastern Shore. The bay was formed following a meteoroid impact crater during the Eocene. Many of Virginia's rivers flow into the Chesapeake Bay, including the Potomac, Rappahannock, James, and York. These form three peninsulas into the Chesapeake. Geographically and geologically, Virginia is divided into five regions from east to west: Tidewater, Piedmont, Blue Ridge Mountains, Ridge and Valley, and Cumberland Plateau, also called the Appalachian Plateau.
The Tidewater is a coastal plain between the Atlantic coast and the fall line. It includes the Eastern Shore and major estuaries which enter the Chesapeake Bay. The Piedmont are a series of sedimentary and igneous rock-based foothills east of the mountains which were formed in the Mesozoic. The region, known for its heavy clay soil, includes the Southwest Mountains. The Blue Ridge are a physiographic province of the chain of Appalachian Mountains with the highest points in the state, the tallest being Mount Rogers at 5,729 feet (1,746 m). The Ridge and Valley region is west of the mountains, and includes the Great Appalachian Valley. The region is carbonate rock based, and includes Massanutten Mountain. The Cumberland Plateau and the Cumberland Mountains are in the south-west corner of Virginia, below the Allegheny Plateau. In this region rivers flow northwest, with a dendritic drainage system, into the Ohio River basin.
More than four-thousand caves exist in Virginia, with ten open for tourism. The Virginia seismic zone has not had a history of regular activity. Earthquakes are rarely above 4.5 on the Richter magnitude scale because Virginia is located centrally on the North American Plate. The largest earthquake, at an estimated 5.9 magnitude, was in 1897 in Blacksburg. Coal mining takes place in the three mountainous regions at forty distinct coal beds near Mesozoic basins. Besides coal, resources such as slate, kyanite, and sand and gravel are mined, with an annual value over $2 billion.

Carte de la Virginie et du Mariland

Philadelphia

Philadelphia is the largest city in Pennsylvania and the sixth-most-populous city in the United States.
In 2008, the population of the city proper was estimated to be over 1.4 million, while the Greater Philadelphia metropolitan area's population of 5.8 million made it the country's fifth-largest. The city is the nation's fourth-largest urban area by population and its fourth-largest consumer media market as ranked by the Nielsen Media Research. It is the county seat of Philadelphia County (with which it is coterminous). Popular nicknames for Philadelphia include Philly and The City of Brotherly Love .
A commercial, educational, and cultural center, the city was once the second-largest in the British Empire, and the social and geographical center of the original 13 American colonies. Ben Franklin took a large role in Philadelphia's early rise to prominence. It was in this city that many of the ideas, and subsequent actions, gave birth to the American Revolution and American Independence, making Philadelphia a centerpiece of early American history. It was the most populous city of the young United States, and served as one of the nation's many capitals during the Revolutionary War and after. Following the ratification of the U.S. Constitution, it was the temporary national capital from 1790 to 1800 while Washington, DC was under construction.

Prior to the arrival of Europeans, the Philadelphia area was the location of the Lenape (Delaware) Indian village Shackamaxon.
Europeans arrived in the Delaware Valley in the early 1600s, with the first settlements founded by the Dutch, British and Swedish. After Sweden's first expedition to North America embarked in late 1637, the Swedes took control of land on the west side of the Delaware River from just below the Schuylkill River: today's Philadelphia, southeast Pennsylvania, Delaware, and Maryland. In 1644, New Sweden supported the Susquehannocks in their military defeat of the English province of Maryland. But 11 years later, the Dutch sent an army to the Delaware River, nominally taking control of the colony, though Swedish and Finnish settlers continued to have their own militia, religion, court, and lands. The English conquered the New Netherland colony in October 1663–1664, but the situation did not really change until 1682, when the area was included in William Penn's charter for Pennsylvania.
In 1681, in partial repayment of a debt, Charles II of England granted William Penn a charter for what would become the Pennsylvania colony. Despite the royal charter, Penn bought the land from the local Lenape to be on good terms with the Native Americans and ensure peace for his colony. According to legend Penn made a treaty of friendship with Lenape chief Tammany under an elm tree at Shackamaxon, in what is now the city's Fishtown section. As a Quaker, Penn had experienced religious persecution and wanted his colony to be a place where anyone could worship freely despite their religion. Penn named the city Philadelphia, which is Greek for brotherly love (philos, "love" or "friendship", and adelphos, "brother"). Penn planned a city on the Delaware River to serve as a port and place for government. Hoping that Philadelphia would become more like an English rural town instead of a city, Penn laid out roads on a grid plan to keep houses and businesses spread far apart, allowing them to be surrounded by gardens and orchards. The city's inhabitants didn't follow Penn's plans and crowded by the Delaware River and subdivided and resold their lots. Before Penn left Philadelphia for the last time, he issued the Charter of 1701 establishing Philadelphia as a city. The city soon established itself as an important trading center, poor at first, but with tolerable living conditions by the 1750s. Benjamin Franklin, a leading citizen of the time, helped improve city services and founded new ones, such as the American Colonies' first hospital.
Philadelphia's importance and central location in the colonies made it a natural center for America's revolutionaries. The city hosted the First Continental Congress before the war; the Second Continental Congress, which signed the United States Declaration of Independence, during the war; and the Constitutional Convention after the war. Several battles were fought in and near Philadelphia as well. After the war, Philadelphia served as the new United States' capital in the 1790s. In 1793, the largest yellow fever epidemic in U.S. history killed as many as 5,000 people in Philadelphia, roughly 10% of the population.

The state government left Philadelphia in 1799 and the federal government left soon after in 1800, but the city remained the young nation's largest and a financial and cultural center. New York City soon surpassed Philadelphia in population, but construction of roads, canals, and railroads helped turn Philadelphia into the United States' first major industrial city. Throughout the 19th century, Philadelphia had a variety of industries and businesses, the largest being textiles. Major corporations in the 19th and early 20th centuries included the Baldwin Locomotive Works, William Cramp and Sons Ship and Engine Building Company, and the Pennsylvania Railroad. Industry, along with the U.S. Centennial, was celebrated in 1876 with the Centennial Exposition, the first official World's Fair in the United States. Immigrants, mostly German and Irish, settled in Philadelphia and the surrounding districts. The rise in population of the surrounding districts helped lead to the Act of Consolidation of 1854 which extended the city of Philadelphia to include all of Philadelphia County. In the later half of the century immigrants from Russia, Eastern Europe and Italy and African Americans from the southern U.S. settled in the city.
By the 20th century, Philadelphia had become known as "corrupt and contented," with a complacent population and entrenched Republican political machine. The first major reform came in 1917 when outrage over the election-year murder of a police officer led to the shrinking of the Philadelphia City Council from two houses to just one. In the 1920s, the public flouting of Prohibition laws, mob violence, and police involvement in illegal activities led to the appointment of Brigadier General Smedley Butler of the U.S. Marine Corps as director of public safety, but political pressure prevented any long-term success in fighting crime and corruption.
The population peaked at more than two million residents in 1950, then began to decline while its suburban counties grew. Revitalization and gentrification of neighborhoods began in the 1960s and continues into the 21st century, with much of the development in the Center City and University City areas of the city. After many of the old manufacturers and businesses had left Philadelphia or shut down, the city started attracting service businesses and began to more aggressively market itself as a tourist destination. Glass-and-granite skyscrapers were built in Center City.

Plan de Philadelphie

Friday, August 14, 2009

Carte de la Nouvelle Angleterre New York Pensilvanie et Nouveau Jersay

New york

New York covers 54,556 square miles (141,300 km2) and ranks as the 27th largest state by size. The Great Appalachian Valley dominates eastern New York, while Lake Champlain is the chief northern feature of the valley, which also includes the Hudson River flowing southward to the Atlantic Ocean. The rugged Adirondack Mountains, with vast tracts of wilderness, lie west of the valley. Most of the southern part of the state is on the Allegheny plateau, which rises from the southeast to the Catskill Mountains. The western section of the state is drained by the Allegheny River and rivers of the Susquehanna and Delaware systems. The Delaware River Basin Compact, signed in 1961 by New York, New Jersey, Pennsylvania, Delaware, and the federal government, regulates the utilization of water of the Delaware system. The highest elevation in New York is Mount Marcy in the Adirondacks.
New York's borders touch (clockwise from the west) two Great Lakes (Erie and Ontario, which are connected by the Niagara River); the provinces of Ontario and Quebec in Canada; Lake Champlain; three New England states (Vermont, Massachusetts, and Connecticut); the Atlantic Ocean, and two Mid-Atlantic States, New Jersey and Pennsylvania. In addition, Rhode Island shares a water border with New York.
Contrasting with New York City's urban atmosphere, the vast majority of the state is dominated by farms, forests, rivers, mountains, and lakes. New York's Adirondack Park is the largest state park in the United States. It is larger than the Yellowstone, Yosemite, Grand Canyon, Glacier and Olympic National Parks combined. New York established the first state park in the United States at Niagara Falls in 1885. Niagara Falls, on the Niagara River as it flows from Lake Erie to Lake Ontario, is a popular attraction. The Hudson River begins with Lake Tear of the Clouds and flows south through the eastern part of the state without draining Lakes George or Champlain. Lake George empties at its north end into Lake Champlain, whose northern end extends into Canada, where it drains into the Richelieu and then the St. Lawrence Rivers. Four of New York City's five boroughs are on the three islands at the mouth of the Hudson River: Manhattan Island, Staten Island, and Brooklyn and Queens on Long Island.
Upstate and downstate are often used informally to distinguish New York City or its greater metropolitan area from the rest of New York state. The placement of a boundary between the two is a matter of great contention. Unofficial and loosely defined regions of Upstate New York include the Southern Tier, which often includes the counties along the border with Pennsylvania. and the North Country, which can mean anything from the strip along the Canadian border to everything north of the Mohawk River.

In general, New York has a humid continental climate, though a plausible argument can be made that under the Köppen climate classification, New York City has a humid subtropical climate as it falls very near the boundary. Weather in New York is heavily influenced by two continental air masses: a warm, humid one from the southwest and a cold, dry one from the northwest.
The winters are long and cold in the Plateau Divisions of the state. In the majority of winter seasons, a temperature of −13 °F (−25 °C) or lower can be expected in the northern highlands (Northern Plateau) and 5 °F (−15 °C) or colder in the southwestern and east-central highlands (Southern Plateau).
The summer climate is cool in the Adirondacks, Catskills and higher elevations of the Southern Plateau. The New York City area and lower portions of the Hudson Valley have rather warm summers by comparison, with some periods of high, uncomfortable humidity. The remainder of New York State enjoys pleasantly warm summers, marred by only occasional, brief intervals of sultry conditions. Summer daytime temperatures usually range from the upper 70s to mid 80s °F (25 to 30 °C), over much of the state.
New York ranks 46th among the 50 states in the amount of greenhouse gases generated per person. This efficiency is primarily due to the state's relatively higher rate of mass transit use.


New York's gross state product in 2007 was $1.1 trillion, ranking third in size behind the larger states of California and Texas. If New York were an independent nation, it would rank as the 16th largest economy in the world behind Turkey. Its 2007 per capita personal income was $46,364, placing it sixth in the nation behind Maryland, and eighth in the world behind Ireland. New York's agricultural outputs are dairy products, cattle and other livestock, vegetables, nursery stock, and apples. Its industrial outputs are printing and publishing, scientific instruments, electric equipment, machinery, chemical products, and tourism.
A recent review by the Center on Budget and Policy Priorities found 13 states, including several of the nation's largest, face budget shortfalls for FY2009. New York faces a deficit that could be as large as $4.3 billion.
New York exports a wide variety of goods such as foodstuffs, commodities, minerals, computers and electronics, cut diamonds, and automobile parts. In 2007, the state exported a total of $71.1 billion worth of goods, with the five largest foreign export markets being Canada ($15 billion), United Kingdom ($6 billion), Switzerland ($5.9 billion), Israel ($4.9 billion), and Hong Kong ($3.4 billion). New York's largest imports are oil, gold, aluminum, natural gas, electricity, rough diamonds, and lumber.
Canada is a very important economic partner for the state. 21% of the state's total worldwide exports went to Canada in 2007. Tourism from the north is also a large part of the economy. Canadians spent US$487 million in 2004 while visiting the state.
New York City is the leading center of banking, finance and communication in the United States and is the location of the New York Stock Exchange, the largest stock exchange in the world by dollar volume. Many of the world's largest corporations are based in the city.
The state also has a large manufacturing sector that includes printing and the production of garments, furs, railroad equipment and bus line vehicles. Many of these industries are concentrated in upstate regions. Albany and the Hudson Valley are major centers of nanotechnology and microchip manufacturing, while the Rochester area is important in photographic equipment and imaging.
New York is a major agricultural producer, ranking among the top five states for agricultural products such as dairy, apples, cherries, cabbage, potatoes, onions, maple syrup and many others. The state is the largest producer of cabbage in the U.S. The state has about a quarter of its land in farms and produced US$3.4 billion in agricultural products in 2001. The south shore of Lake Ontario provides the right mix of soils and microclimate for many apple, cherry, plum, pear and peach orchards. Apples are also grown in the Hudson Valley and near Lake Champlain.
New York is the nation's third-largest grape-producing state, behind California, and second-largest wine producer by volume. The south shore of Lake Erie and the southern Finger Lakes hillsides have many vineyards. In addition, the North Fork of Long Island developed vineyards, production and visitors' facilities in the last three decades of the 20th century. In 2004, New York's wine and grape industry brought US$6 billion into the state economy.
The state has 30,000 acres (120 km2) of vineyards, 212 wineries, and produced 200 million bottles of wine in 2004. A moderately sized saltwater commercial fishery is located along the Atlantic side of Long Island. The principal catches by value are clams, lobsters, squid, and flounder. These areas of the economy have been increasing as environmental protection has led to an increase in ocean wildlife.

Ville de Manathe ou Nouvelle Yorc

Baye et Port de Yorc Capitale de la Nouvelle York